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Contents

   



(Top)
 


1 Prelaunch (20042011)  



1.1  Landing site selection  







2 Launch (2011)  





3 Landing (2012)  





4 Prime mission (2012 - September 2014)  



4.1  Evidence for ancient water  





4.2  Evidence for ancient habitability  





4.3  Evidence for atmospheric loss  





4.4  Other 2013 events  





4.5  Search for ancient life  





4.6  Arrival at Mount Sharp  





4.7  Detection of organics  





4.8  Other 2014 events  







5 First extended mission (October 2014 - September 2016)  





6 Second extended mission (October 2016 - September 2019)  





7 Third extended mission (October 2019 - September 2022)  





8 Fourth extended mission (October 2022 - Present)  





9 Current status  



9.1  Weather  





9.2  Location and travel statistics  





9.3  Equipment status  







10 Images  



10.1  Self-portraits  





10.2  Videos  





10.3  Gallery  





10.4  Wide images  







11 See also  





12 References  





13 External links  














Timeline of Mars Science Laboratory: Difference between revisions






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{{Short description |Event timeline of the NASA Mars Science Laboratory mission}}

{{cleanup-link rot|date=August 2012}}

{{About|events|the spaceflight mission to Mars|Mars Science Laboratory|the surface rover|Curiosity (rover)}}

{{wikify|date=August 2012}}

{{Use American English |date=January 2022}}

{{Use dmy dates |date=January 2022}}

[[File:PIA19808-MarsCuriosityRover-AeolisMons-BuckskinRock-20150805.jpg|thumb|right|300px|''Curiosity'' rover on Mars (5 August 2015)]]



The [[Mars Science Laboratory]] and its rover, [[Curiosity rover|''Curiosity'']], were launched from [[Earth]] on 26 November 2011. As of {{CURRENTMONTHNAME}} {{CURRENTDAY}}, {{CURRENTYEAR}}, ''Curiosity'' has been on the [[Mars|planet Mars]] for {{Curiosity Mission Timer}} [[Sol (day on Mars)|sols]] ({{age in days|2012|08|06}} [[days|total days]]; <SMALL>''{{Age in years and days|06 AUG 2012}}''</SMALL>) since landing on 6 August 2012. ''(See [[Timeline of Mars Science Laboratory#Current status|Current status]].)''

This is a chronological list of discovery, information, pictures, and videos about the [[Mars]] [[NASA]] [[Mars Science Laboratory|MSL]] [[Curiosity rover|Curiosity]] mission.



==Prelaunch (2004–2011)==

{| style="float: right;background: orange; color: black"

[[File:MSL-Cruise Stage Test.jpg|thumb|Cruise stage is tested in 2010.<ref>[http://marsprogram.jpl.nasa.gov/msl/multimedia/images/?ImageID=3351 Mars Science Laboratory's Cruise Stage in Test Chamber - NASA]</ref>]]

|-


! MSL Curiosity rover has spent

In April 2004, the United States [[National Aeronautics and Space Administration]] (NASA) called for scientific experiments and instruments proposals for the [[Mars Science Laboratory]] and rover mission.<ref name="Stathopoulos">{{cite web|url= http://www.aerospaceguide.net/mars/science_laboratory.html |title=Mars Science Laboratory |access-date=4 February 2012 |last=Stathopoulos |first=Vic |date=October 2011 |work=Aerospace Guide}}</ref> Launch was proposed for September 2009.<ref name= 'Idaho National Laboratory'>{{cite web|url= https://inlportal.inl.gov/portal/server.pt/community/newsroom/257/feature_story_details/1269?featurestory=DA_584674 |title=Mars Science Laboratory team accomplishes mission goal by working together |access-date=2012-08-12 |first=Teri Ehresman |last=INL |publisher=Idaho National Laboratory |archive-url= https://web.archive.org/web/20120925165336/https://inlportal.inl.gov/portal/server.pt/community/newsroom/257/feature_story_details/1269?featurestory=DA_584674 |archive-date=2012-09-25 |url-status=dead }}</ref><ref name='NASAfacts'>{{cite web|url= http://www.nasa.gov/pdf/482645main_MSL%20Fact%20Sheet.pdf |title=NASA Facts - MSL |access-date=2012-08-13 |work=NASA}}</ref> By 14 December 2004, eight proposals were selected, including instruments from Russia and Spain.<ref name="Stathopoulos"/><ref name='NASAfacts'/>

|-

! ''' <big> {{age in days|2012|08|06}} </big> '''

|-

! days on Mars

|}



Testing of components also began in late 2004, including [[Aerojet]]'s [[monopropellant]] engine with the ability to throttle from 15 to 100 percent thrust with a fixed propellant inlet pressure.<ref name=Stathopoulos/> By November 2008 most hardware and software development was complete, and testing continued.<ref name="usra">[http://www.lpi.usra.edu/meetings/lpsc2009/pdf/2364.pdf 40th Lunar and Planetary Science Conference] (2009); [http://www.lpi.usra.edu/meetings/lpsc2010/pdf/2539.pdf 41st Lunar and Planetary Science Conference] (2010)</ref> At this point, cost overruns were approximately $400 million.<ref name="universetoday">[http://www.universetoday.com/2008/10/10/mars-science-laboratory-still-alive-for-now/ Mars Science Laboratory: Still Alive, For Now]. 10 October 2008. ''Universe Today''.</ref> In December 2008, lift-off was delayed to November 2011 due to insufficient time for testing and integration.<ref name="Next NASA Mars Mission Rescheduled For 2011">{{cite web|url= https://www.nasa.gov/mission_pages/mars/news/msl-20081204.html|title=Next NASA Mars Mission Rescheduled For 2011|publisher=NASA/JPL|date=4 December 2008|access-date=3 March 2021}}</ref><ref name="thespacereview">{{Cite web |last=Brown |first=Adrian |title=Mars Science Laboratory: the budgetary reasons behind its delay: MSL: the budget story |url= http://www.thespacereview.com/article/1318/1 |work=The Space Review |date=2 March 2009 |access-date=26 January 2010 |quote=NASA first put a reliable figure of the cost of the MSL mission at the "Phase A/Phase B transition", after a preliminary design review (PDR) that approved instruments, design and engineering of the whole mission. That was in August 2006—and the Congress-approved figure was $1.63 billion. … With this request, the MSL budget had reached $1.9 billion. … NASA HQ requested JPL prepare an assessment of costs to complete the construction of MSL by the next launch opportunity (in October 2011). This figure came in around $300 million, and NASA HQ has estimated this will translate to at least $400 million (assuming reserves will be required), to launch MSL and operate it on the surface of Mars from 2012 through 2014.}}</ref><ref name='audit2011'>{{cite web |url=http://oig.nasa.gov/audits/reports/FY11/IG-11-019.pdf |title=Audit Report: NASA'S MANAGEMENT OF THE MARS SCIENCE LABORATORY PROJECT |access-date=2012-08-13 |date=8 June 2011 |work=OFFICE OF INSPECTOR GENERAL |publisher=NASA |quote=REPORT NO. IG-11-019 |archive-date=3 December 2011 |archive-url=https://web.archive.org/web/20111203022237/http://oig.nasa.gov/audits/reports/FY11/IG-11-019.pdf |url-status=dead }}</ref>

==Before landing on Mars==



Between 23–29 March 2009, the general public ranked nine finalist rover names (''Adventure, Amelia, Journey, Perception, Pursuit, Sunrise, Vision, Wonder'', and ''Curiosity'')<ref>[https://web.archive.org/web/20090326013016/http://marsrovername.jpl.nasa.gov/SubmitVoteForm/index.cfm Mars rover name]</ref> through a public poll on the NASA website.<ref name=MSLNameWebsite>{{cite web|title=Name NASA's Next Mars Rover|url=https://mars.nasa.gov/namerover/|publisher=NASA/JPL|date=27 May 2009|access-date=3 March 2021}}</ref> On 27 May 2009, the winning name was announced to be ''Curiosity''. The name had been submitted in an essay contest by Clara Ma, a then sixth-grader from Kansas.{{r|MSLNameWebsite}}

{| class="wikitable"


===Landing site selection===

At the first MSL Landing Site workshop, 33 potential landing sites were identified.<ref name="nasa9">{{cite web|url= http://marsoweb.nas.nasa.gov/landingsites/msl/memoranda/MSL_Eng_User_Guide_v3.pdf |title=MSL Landing Site Selection User's Guide to Engineering Constraints |access-date=29 May 2007 |date=12 June 2006 }}</ref> By the second workshop in late 2007, the list had grown to include almost 50 sites,<ref name="Second MSL Landing Site Workshop">{{cite web|url= http://marsoweb.nas.nasa.gov/landingsites/msl2009/workshops/2nd_workshop/2nd_announcement.html |title=Second MSL Landing Site Workshop}}</ref> and by the end of the workshop, the list was reduced to six;<ref name="MSL3WorkshopVotes">{{cite web|url= http://marsoweb.nas.nasa.gov/landingsites/msl2009/workshops/3rd_workshop/talks/MSL_Wkshp3_vote_chart.pdf |title=MSL Workshop Voting Chart |date=18 September 2008}}</ref><ref name="Reconnaissance of MSL Sites">{{cite web|url= http://hirise.lpl.arizona.edu/HiBlog/?p=131 |title=Reconnaissance of MSL Sites |access-date=21 October 2008 |date=4 January 2008 |work=HiBlog |author=GuyMac}}</ref><ref name="Mars Exploration Science Monthly Newsletter">{{cite web|url= http://mepag.jpl.nasa.gov/calendar/MEPAG_Newsletter(08_19C3B3.pdf |title=Mars Exploration Science Monthly Newsletter |date=1 August 2008 |url-status=dead |archive-url= https://web.archive.org/web/20110721050857/http://mepag.jpl.nasa.gov/calendar/MEPAG_Newsletter(08_19C3B3.pdf |archive-date=21 July 2011 }}</ref> in November 2008, project leaders at a third workshop reduced the list to these four landing sites:<ref name="Site List Narrows For NASA's Next Mars Landing">{{cite web|url=https://mars.nasa.gov/news/59/site-list-narrows-for-nasas-next-mars-landing/|title=Site List Narrows For NASA's Next Mars Landing|date=19 November 2008|access-date=3 March 2021|work=NASA}}</ref><ref name="Looking at Landing Sites for the Mars Science Laboratory">{{cite web|url= https://www.youtube.com/watch?v=sfYK8r6tlrg| title=Looking at Landing Sites for the Mars Science Laboratory| date=27 May 2009 |access-date=28 May 2009 |work=YouTube| publisher=NASA/JPL}}</ref><ref name="ISStD">{{cite web |url=http://marsoweb.nas.nasa.gov/landingsites/index.html |title=Final 7 Prospective Landing Sites |access-date=9 February 2009 |publisher=NASA |date=19 February 2009 |archive-date=13 April 2011 |archive-url=https://web.archive.org/web/20110413014816/http://marsoweb.nas.nasa.gov/landingsites/index.html |url-status=dead }}</ref>


{| class="wikitable" style="margin: 1em auto;"

|-

|-

! Name

! style="text-align: center; background: #aabccc;"|Date

! Location

! style="text-align: center; background: #aabccc;"|Event

! Elevation

! style="text-align: center; background: #aabccc;"|Notes

! Notes

|-

|-

| [[Eberswalde (crater)|Eberswalde Crater]] || {{Coord|23.86|S|326.73|E|globe:mars}} || {{convert|-1450|m|ft|abbr=on}} || Ancient river delta.<ref name="nasa10">{{Cite web|url=https://mars.nasa.gov/msl/timeline/prelaunch/landing-site-selection/seven-possible-msl-landing-sites/#eberswalde-crater|title=Mars Science Laboratory: Possible MSL Landing Site: Eberswalde Crater|access-date=3 March 2021}}</ref>

|April 2004 || Mission proposals. || NASA called for proposals for the rover's scientific experiments and instruments. <ref name="Stathopoulos"> {{cite web |url=http://www.aerospaceguide.net/mars/science_laboratory.html |title=Mars Science Laboratory |accessdate=February 4, 2012 |last=Stathopoulos |first=Vic |date=October 2011 |work=Aerospace Guide}}</ref> Launch was proposed for September 2009.<ref name= 'Idaho National Laboratory'> {{cite web | url= https://inlportal.inl.gov/portal/server.pt/community/newsroom/257/feature_story_details/1269?featurestory=DA_584674 | title = Mars Science Laboratory team accomplishes mission goal by working together | accessdate = 2012-08-12 | first = Teri Ehresman | author = INL | publisher = Idaho National Laboratory}}</ref><ref name='NASAfacts'> {{cite web | url = http://www.nasa.gov/pdf/482645main_MSL%20Fact%20Sheet.pdf | title = NASA Facts - MSL | accessdate = 2012-08-13 | format = PDF | work = NASA}}</ref>

|-

|-

| [[Holden (Martian crater)|Holden Crater]] || {{Coord|26.37|S|325.10|E|globe:mars}} || {{convert|−1940|m|ft|abbr=on}} || Dry lake bed.<ref name="nasa11">{{Cite web|url=https://mars.nasa.gov/msl/timeline/prelaunch/landing-site-selection/seven-possible-msl-landing-sites/#holden-crater|title=Mars Science Laboratory: Possible MSL Landing Site: Holden Crater|access-date=3 March 2021}}</ref>

|December 14, 2004 || Instruments selected. || Eight proposals were selected, including instruments from Russia and Spain.<ref name='NASAfacts'/>

|- style="background:#cfc;"

|-

| [[Gale (crater)|Gale Crater]] || {{Coord|4.49|S|137.42|E|globe:mars}} || {{convert|-4451|m|ft|abbr=on}} || Features {{convert|5|km|mi|abbr=on}} tall mountain <br />of layered material near center.<ref name="nasa11"/><ref name="nasa12">{{Cite web|url=https://mars.nasa.gov/msl/timeline/prelaunch/landing-site-selection/seven-possible-msl-landing-sites/#gale-crater|title=Mars Science Laboratory: Possible MSL Landing Site: Gale Crater|access-date=3 March 2021}}</ref> selected.<ref name="Gale Crater3"/>

| December 2004 || Design and testing of components began. ||

|-

| November 2008 || Most hardware and software development were completed.<ref name="usra">[http://www.lpi.usra.edu/pss/jan92009/presentations/mslTechnicalCook.pdf MSL Technical and Replan Status]. Richard Cook. (January 9, 2009)</ref> || Testing continues.

|-

| December 2008 || Launch rescheduled for November 2011. || Delay due to insufficient time for testing and integration.<ref name='audit2011'> {{cite web | url = http://oig.nasa.gov/audits/reports/FY11/IG-11-019.pdf | title = Audit Report: NASA’S MANAGEMENT OF THE MARS SCIENCE LABORATORY PROJECT | accessdate = 2012-08-13 | date = 8 June 2011 | work = OFFICE OF INSPECTOR GENERAL | publisher = NASA | quote = REPORT NO. IG-11-019}}</ref>

|-

| July 22, 2011 || Landing site selection || [[Gale (crater)|Gale Crater]] selected, as its deep [[alluvial fan]] is where ancient water shed debris from the crater’s rim and nearby [[Aeolis Mons]] peak.<ref> {{cite news | title = Curiosity Mission Could Reveal Mars’ Deepest Secrets | date = 2 August 2011 | url = http://tamutimes.tamu.edu/tag/mars/ | work = Texas A & M University | accessdate = 2012-08-13}}</ref>

|-

|-

| [[Mawrth Vallis]] || {{Coord|24.01|N|341.03|E|globe:mars}} || {{convert|-2246|m|ft|abbr=on}} || Channel carved by catastrophic floods.<ref name="nasa13">{{Cite web |url=https://mars.nasa.gov/msl/timeline/prelaunch/landing-site-selection/seven-possible-msl-landing-sites/#mawrth-vallis|title=Mars Science Laboratory: Possible MSL Landing Site: Mawrth Vallis|access-date=3 March 2021}}</ref>

|}

|}



A fourth landing site workshop was held in late September 2010,<ref name="nasa14">[http://marsoweb.nas.nasa.gov/landingsites/msl/workshops/4th_workshop/program.html Presentations for the Fourth MSL Landing Site Workshop] September 2010</ref> and the fifth and final workshop 16–18 May 2011.<ref name="marstoday">[http://www.marstoday.com/news/viewsr.rss.html?pid=36353 Second Announcement for the Final MSL Landing Site Workshop and Call for Papers] {{Webarchive|url= https://archive.today/20120908020952/http://www.marstoday.com/news/viewsr.rss.html?pid=36353 |date=2012-09-08 }} March 2011</ref> On 22 July 2011, it was announced that [[Gale (crater)|Gale Crater]] had been selected as the landing site of the Mars Science Laboratory mission.

<br />



{{wide image|Curiosity Cradled by Gale Crater.jpg|500px|align-cap=center|[[Aeolis Mons]] rises from the middle of [[Gale Crater]] - Green dot marks the [[Curiosity (rover)|''Curiosity'' rover]] landing site in [[Aeolis Palus]]<ref name="Gale Crater3">{{cite news |last1=Amos |first1=Jonathan |title=Mars rover aims for deep crater |date=22 July 2011 |url= https://www.bbc.co.uk/news/science-environment-14249524 |work=BBC News |access-date =22 July 2011 }}</ref><ref name="ellipse">{{cite news |author=Amos, Jonathan |title=Nasa's Curiosity rover targets smaller landing zone |date=12 June 2012 |url= https://www.bbc.co.uk/news/science-environment-18401248 |work=BBC News |access-date=12 June 2012 }}</ref> - North is down.}}

===November 2011===

<!---

{{Gallery |align=center |title={{center|1=[[Gale Crater]]}} |lines=10 |width=250 |height=250 |File:Curiosity Cradled by Gale Crater.jpg|{{center|1=[[Aeolis Mons]] rises from the middle of [[Gale Crater]] - Green dot marks the [[Curiosity (rover)|''Curiosity'' rover]] landing site in [[Aeolis Palus]]<ref name="Gale Crater3">{{cite news |last1=Amos |first1=Jonathan |title=Mars rover aims for deep crater |date=July 22, 2011 |url= https://www.bbc.co.uk/news/science-environment-14249524 |work=BBC News |access-date =July 22, 2011 }}</ref><ref name="ellipse">{{cite news |author=Amos, Jonathan |title=Nasa's Curiosity rover targets smaller landing zone |date=June 12, 2012 |url= https://www.bbc.co.uk/news/science-environment-18401248 |publisher=BBC News |access-date=June 12, 2012 }}</ref> - North is down.}} }}

[[File:Curiosity Cradled by Gale Crater.jpg|thumb|[[Aeolis Mons]] rises from the middle of [[Gale Crater]] - Green dot marks the [[Curiosity (rover)|''Curiosity'' rover]] landing site in [[Aeolis Palus]]<ref name="Gale Crater3">{{cite news |last1=Amos |first1=Jonathan |title=Mars rover aims for deep crater |date=July 22, 2011 |url= https://www.bbc.co.uk/news/science-environment-14249524 |work=BBC News |access-date =July 22, 2011 }}</ref><ref name="ellipse">{{cite news |author=Amos, Jonathan |title=Nasa's Curiosity rover targets smaller landing zone |date=June 12, 2012 |url= https://www.bbc.co.uk/news/science-environment-18401248 |publisher=BBC News |access-date=June 12, 2012 }}</ref> - North is down.]]--->



====November 26 - Launch from Earth====

==Launch (2011)==

{{main|Mars Science Laboratory#Launch|Mars Science Laboratory#Cruise}}

[[File:MSL Launches to the Red Planet.ogg|left|thumb|350px| November 26, 2011 15:02:00.211 UTC<ref>{{cite web |title=NASA - Multimedia - Video Gallery |url=http://www.nasa.gov/mission_pages/msl/news/msl20120810.html|publisher=Nasa.gov|date=2010-04-28|accessdate=2012-08-10}}</ref>]]

[[File:MSL Launches to the Red Planet.ogg|thumb|200px|left|MSL Launch - 26 November 2011 15:02:00.211 UTC<ref>{{cite web |title=NASA - Multimedia - Video Gallery |url= http://www.nasa.gov/mission_pages/msl/news/msl20120810.html|publisher=Nasa.gov|date=2010-04-28|access-date=2012-08-10}}</ref>]]

<!---

[[File:Atlas V 541 into the flight.png|thumb|150px|left|MSL launched (November 26, 2011).]]--->

MSL was launched from [[Cape Canaveral Air Force Station Space Launch Complex 41]] on 26 November 2011, at 10:02 EST (15:02 [[Coordinated Universal Time|UTC]]) aboard an [[Atlas V]] 541 provided by [[United Launch Alliance]].<ref name=ula20120819>

{{cite web |title=United Launch Alliance Atlas V Rocket Successfully Launches NASA's Mars Science Lab on Journey to Red Planet |url= http://www.ulalaunch.com/site/pages/News.shtml#/89/ |work=ULA Launch Information |date=2011-11-26 |publisher=United Launch Alliance |access-date=2012-08-19 |url-status=dead |archive-url= https://web.archive.org/web/20131207160150/http://www.ulalaunch.com/site/pages/News.shtml#/89/ |archive-date=2013-12-07 }}</ref><ref name="nasa3">[http://marsprogram.jpl.nasa.gov/msl/mission/spacecraft/cruiseconfig/ MSL cruise configuration]</ref> The first and second rocket stages, along with the rocket motors, were stacked on 9 October 2011, near the launch pad.<ref name="universetoday7">[http://www.universetoday.com/89346/assembling-curiosity%E2%80%99s-rocket-to-mars/ Assembling Curiosity's Rocket to Mars.]</ref> The fairing containing the spacecraft was transported to the launch pad on 3 November 2011.<ref name="NASA's new Mars rover reaches Florida launch pad">{{cite news| url= https://www.reuters.com/article/us-space-mars-idUSTRE7A26VA20111103 |work=Reuters |first=Jane |last=Sutton |title=NASA's new Mars rover reaches Florida launch pad |date=3 November 2011}}</ref>



On 13 December 2011, the rover began monitoring [[Health threat from cosmic rays|space radiation]] to aid in planning for future crewed missions to Mars.<ref name='radiation'>{{cite news |last=Brown |first=Dwayne |title=NASA Mars-Bound Rover Begins Research in Space |date=13 December 2011 |url=http://www.jpl.nasa.gov/news/news.cfm?release=2011-386 |work=[[NASA]] |access-date=21 August 2012 |archive-date=5 February 2022 |archive-url=https://web.archive.org/web/20220205150143/https://www.jpl.nasa.gov/news/news.cfm?release=2011-386 |url-status=dead }}</ref>

[[File:606779main msl20111126b-br2.jpg|thumb|right|350px|[[NASA|NASA's]] [[Mars Science Laboratory]] spacecraft, sealed inside its payload fairing atop the [[United Launch Alliance]] [[Atlas V]] rocket, clears the tower at [[Cape Canaveral Air Force Station Space Launch Complex 41|Space Launch Complex 41]] on [[Cape Canaveral Air Force Station]] in [[Florida]].<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=3776 Mars Science Laboratory: Images]</ref>]]<br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br />



The interplanetary journey to Mars took more than eight months,<ref name="NASA-2">{{cite web|url= http://mars.jpl.nasa.gov/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1185 |title=NASA's Mars Science Laboratory Launch Rescheduled for Nov. 26 |first=Allard |last=Beutel |date=19 November 2011 |publisher=[[NASA]] |access-date=21 November 2011}}</ref> time during which, the spacecraft performed four trajectory corrections: on 11 January, 26 March, 26 June and on 28 July. Mission design had allowed for a maximum of 6 trajectory correction opportunities.<ref name='TrajecoryCorrectons'>{{cite web|url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1292 |title=Status Report - Curiosity's Daily Update |access-date=13 August 2012 |date=6 August 2012 |publisher=NASA |quote=This morning, flight controllers decided to forgo the sixth and final opportunity on the mission calendar for a course-correction maneuver. |archive-url= https://web.archive.org/web/20160916041332/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1292 |archive-date=16 September 2016 |url-status=dead }}</ref><ref name="space">{{cite web|url= http://www.space.com/16972-mars-rover-curiosity-landing-mohawk-guy.html |title=Mars Rover 'Mohawk Guy' a Space Age Internet Sensation &#124; Curiosity Rover |date=7 August 2012 |publisher=Space.com |access-date=2012-08-08}}</ref>

<br />



==Landing (2012)==

====November 28 - Separation====

{{main|Mars Science Laboratory#Entry, descent and landing (EDL)}}

''Curiosity'' landed in the [[Gale Crater]] at 05:17 [[Coordinated Universal Time|UTC]] on 6 August 2012.<ref name ="Space-20120806">{{cite web |last=Wall |first=Mike |title=Touchdown! Huge NASA Rover Lands on Mars |url= http://www.space.com/16932-mars-rover-curiosity-landing-success.html |date=6 August 2012 |publisher=[[Space.com]] |access-date=14 December 2012 }}</ref><ref name="NASA-1">{{cite web|url= http://www.nasa.gov/mission_pages/msl/index.html |title=Curiosity: NASA's Next Mars Rover |date=6 August 2012 |publisher=NASA |access-date=6 August 2012}}</ref><ref name=Sol3>{{cite web |title=MSL Sol 3 Update| url= https://www.youtube.com/watch?v=6f8HHQ2U2jg| publisher=NASA Television| access-date=9 August 2012| date=8 August 2012}}</ref><ref name="SF1012012-07-06">{{cite news |url= http://www.spaceflight101.com/msl-mission-updates-3.html |title=MSL Mission Updates |newspaper=Spaceflight101.com |date=6 August 2012 |url-status=dead |archive-url= https://web.archive.org/web/20120825095610/http://www.spaceflight101.com/msl-mission-updates-3.html |archive-date=25 August 2012 }}</ref> Upon reaching Mars, an automated precision landing sequence took over the entire landing events.<ref name="cruise">{{cite web|url= http://mars.jpl.nasa.gov/msl/mission/spacecraft/cruiseconfig/ |title=MSL - Cruise Configuration |access-date=2012-08-08 |author=NASA |work=JPL}}</ref> A cable cutter separated the cruise stage from the aeroshell and then the cruise stage was diverted into a trajectory for burn-up in the atmosphere.<ref>{{cite book |author=Dahya, N. |title=2008 IEEE Aerospace Conference |pages=1–6 |date=1–8 March 2008 |publisher=IEEE Explore| doi=10.1109/AERO.2008.4526539 |isbn=978-1-4244-1487-1 |chapter=Design and Fabrication of the Cruise Stage Spacecraft for MSL |s2cid=21599522 }}</ref><ref>{{cite web|url= http://mars.jpl.nasa.gov/msl/multimedia/interactives/edlcuriosity/ |title=Follow Curiosity's descent to Mars |access-date=2012-08-23 |date=2012 |work=NASA |quote=Animation |url-status=dead |archive-url= https://web.archive.org/web/20120821024425/http://mars.jpl.nasa.gov/msl/multimedia/interactives/edlcuriosity/ |archive-date=2012-08-21 }}</ref> Landing was confirmed simultaneously by 3 monitoring Mars orbiters. ''Curiosity'' landed on target and only {{convert|2.4|km|mi|abbr=on}} from its center.<ref>{{cite news |first=Jonathan |last=Amos |title=Curiosity rover made near-perfect landing |date=11 August 2012 |url= https://www.bbc.co.uk/news/science-environment-19219782 |work=BBC News |access-date=2012-08-14}}</ref> The coordinates of the landing site (named "[[Bradbury Landing]]") are: {{coord|4.5895|S|137.4417|E|globe:Mars}}.<ref name="MSNBC-20120806">{{cite web |author=MSNBC Staff |title=Video from rover looks down on Mars during landing |url= http://www.nbcnews.com/id/48540619 |date=6 August 2012 |work=[[NBC News]] |access-date=7 October 2012 }}</ref><ref name="S&T-20120807">{{cite web |last=Young |first=Monica |title=Watch Curiosity Descend onto Mars |url= http://www.skyandtelescope.com/news/home/165273796.html |date=7 August 2012 |publisher=[[SkyandTelescope.com]] |access-date=7 October 2012 |url-status=dead |archive-url= https://archive.today/20121209035852/http://www.skyandtelescope.com/news/home/165273796.html |archive-date=9 December 2012 }}</ref>



Some low resolution [[Hazcam]] images were beamed to Earth by relay orbiters confirming the rover's wheels were deployed correctly and on the ground.<ref name="SF1012012-07-06"/><ref name='First Hours'>{{cite news |title=Mars Rover Beams Back Images Showing Its Descent |date=6 August 2012 |url= http://www.nasa.gov/mission_pages/msl/news/msl20120806c.html |work=NASA |access-date=2012-08-15}}</ref> Three hours later, the rover begins to beam detailed data on its systems' status as well as on its entry, descent and landing experience.<ref name='First Hours'/> Aerial 3-D images of the landing site are available and include: [https://web.archive.org/web/20130512005245/http://mars.jpl.nasa.gov/msl/images/Rover3D-pia16208-br2.jpg the ''Curiosity'' rover] and [https://web.archive.org/web/20160305012939/http://mars.jpl.nasa.gov/msl/images/Parachute3D-pia16209-br2.jpg related Parachute] ([[HiRISE]], 10 October 2012).

[[File:Msl20111128 640.ogv|left|frame|30x300px|The Mars Science Laboratory spacecraft separates from the upper stage of its Atlas V launch vehicle and heads on its way to Mars.<ref>[http://www.jpl.nasa.gov/video/index.cfm?id=1040 Video: Curiosity Heads to Mars - NASA Jet Propulsion Laboratory]</ref>]]



On 8 August 2012, Mission Control began upgrading the rover's dual computers by deleting the entry-descent-landing software, then uploading and installing the surface operation software;<ref>[http://science.time.com/2012/08/09/the-curiosity-rover-preps-for-big-plans-after-its-daring-decent/?iid=sci-main-lede?xid=gonewsedit The ''Curiosity'' Rover Preps for Big Plans After its Daring Descent] ''Time''. 9 August 2012</ref> the switchover was completed by 15 August.<ref>[http://www.nbcnews.com/id/48668419 M. Wall - Mars rover survives 'brain transplant' with flying colors - NBC]</ref>

<br />


{| class="wikitable"

|-

! style="text-align: center; background: #aabccc;"|Date

! style="text-align: center; background: #aabccc;"|Event

! style="text-align: center; background: #aabccc;"|Notes

|-

| December 13, 2011 || ''Curiosity'' rover begins monitoring space radiation environment en route to Mars.<ref name="space"> [http://www.space.com/16385-curiosity-rover-mars-science-laboratory.html MSL - Highlights] Space.com</ref> ||

|-

| January 11, 2012 || First trajectory correction. <ref name="space"/> ||

|-

| March 26, 2012 || Second trajectory correction.<ref name="space"/> ||

|-

| June 26, 2012 || Third trajectory correction.<ref name="space"/> ||

|-

| July 28, 2012 || Fourth and last trajectory correction maneuver.<ref name='TrajecoryCorrectons'> {{cite web | url = http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1292 | title = Status Report - Curiosity's Daily Update | accessdate = 2012-08-13 | date = 6 August 2012 | publisher = NASA | quote = This morning, flight controllers decided to forgo the sixth and final opportunity on the mission calendar for a course-correction maneuver.}}</ref> || Mission design allowed for a maximum of 6 trajectory correction opportunities.<ref name='TrajecoryCorrectons'/>

|-

|}


<br />


==Landing on Mars==

{| class="wikitable"

|-

! style="text-align: center; background: #aabccc;"|Date

! style="text-align: center; background: #aabccc;"|Event

! style="text-align: center; background: #aabccc;"|Notes

|-

| August 6, 2012 || Automated precision landing at 05:17:57 [[Coordinated Universal Time|UTC]] || Successful landing confirmed simultaneously by monitoring Mars orbiters. ''Curiosity'' landed on target and only {{convert|2.4|km|mi}} from its center.<ref> {{cite news | first = Jonathan | last = Amos | title = Curiosity rover made near-perfect landing | date = 11 August 2012 | url = http://www.bbc.co.uk/news/science-environment-19219782 | work = BBC News | accessdate = 2012-08-14}}</ref> Some low resolution images were beamed to Earth by relay orbiters.<ref name='First Hours'> {{cite news | title = Mars Rover Beams Back Images Showing Its Descent | date = 6 AUgust 2012 | url = http://www.nasa.gov/mission_pages/msl/news/msl20120806c.html | work = NASA | accessdate = 2012-08-15}}</ref>

|-

| August 6, 2012 || Status report. || Hours after landing, the rover begins to beam detailed data on its systems' status as well as on its entry, descent and landing experience. <ref name='First Hours'/>

|-

|}



<gallery>

<gallery>

File:Curiosity's Descent.ogv|The Curiosity Mars Descent Imager (MARDI) captured the rover's descent to the surface of Mars. The instrument shot 4 fps video from heatshield separation to the ground.<ref>http://www.jpl.nasa.gov/video/index.cfm?id=1106</ref>

Image:Curiosity's Descent.ogv|The ''Curiosity'' rover lands on the surface of Mars (video-03:26; August 6, 2012).<ref>{{Cite web |url= http://www.jpl.nasa.gov/video/index.cfm?id=1106 |title= Curiosity's Descent |website= [[Jet Propulsion Laboratory]] |access-date= 9 August 2012 |archive-date= 9 September 2012 |archive-url= https://web.archive.org/web/20120909072235/http://www.jpl.nasa.gov/video/index.cfm?id=1106 |url-status= dead }}</ref>

Image:MRO sees Curiosity landing.jpg|''Curiosity'' descending under its parachute (August 6, 2012; [[Mars Reconnaissance Orbiter|MRO]]/[[HiRISE]]).<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia15978b.html Mars Science Laboratory: Multimedia-Images]</ref>

Image:PIA15696-HiRISE-MSL-Sol11 2 -br2.jpg|[[Mars Science Laboratory|MSL]] [[Space debris|debris field]] - parachute landed 615 m from ''Curiosity'' (3-D: [https://web.archive.org/web/20130512005245/http://mars.jpl.nasa.gov/msl/images/Rover3D-pia16208-br2.jpg rover] & [https://web.archive.org/web/20160305012939/http://mars.jpl.nasa.gov/msl/images/Parachute3D-pia16209-br2.jpg parachute]) (August 17, 2012; [[Mars Reconnaissance Orbiter|MRO]]).

Image:Cheering hq msl20120805-br2.jpg|Engineers at NASA's [[Jet Propulsion Laboratory]] celebrate the landing.<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4208 Mars Science Laboratory: Multimedia-Images]</ref>

Image:NASA-MarsCuriosityRover-TeamOfWomen-20140626.jpg|''Curiosity'' rover - women team members (June 26, 2014).

Image:673885main PIA15986-full full.jpg|''Curiosity'' landed on August 6, 2012,<ref name ="Space-20120806" /> about 10&nbsp;km from the base of [[Aeolis Mons|Mount Sharp]]).<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/PIA15986.html Mars Science Laboratory: Multimedia-Images]</ref>

Image:First colored image from Curiosity.jpg|First colored image from ''Curiosity'' (August 6, 2012).

Image:PIA16149-Mars Curiosity Rover Takes Self Portrait.jpg|''Curiosity''{{'s}} self-portrait - with closed dust cover (September 7, 2012).

File:PIA16149 MSL Curiosity Rover Self Portrait colour correction.jpg|''Curiosity''{{'s}} self-portrait (September 7, 2012; color-corrected).

Image:Martian gravel beneath one of the wheels of the Curiosity rover.jpg|Gravel below one of the 6 wheels on the rover.

</gallery>



{{Wide image|First 360 panorama from the Curosity rover.jpg|800px|First 360-degree panoramic view of Mars taken by the ''Curiosity'' rover (7 August 2012).<ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=NLA_397682534EDR_F0020000AUT_04096M_&s=2 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=NLA_397673010EDR_F0010008AUT_04096M_&s=2 Mars Science Laboratory: Raw Images]</ref>}}

File:0000MD9999000036E1 DXXX.jpg|This image was taken by Mars Descent Imager (MARDI) onboard NASA's Mars rover Curiosity on Sol 0 (2012-08-06 05:15:30 UTC).<ref>http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0000MD9999000036E1_DXXX&s=0</ref>



==Prime mission (2012 - September 2014)==

File:MRO sees Curiosity landing.jpg|NASA's Curiosity rover and its parachute were spotted by NASA's [[Mars Reconnaissance Orbiter]] as Curiosity descended to the surface on 5 Aug 2012 PDT (6 Aug EDT).<ref>http://www.nasa.gov/mission_pages/msl/multimedia/pia15978b.html</ref>

{{see also|Glenelg, Mars}}

{{wide image|PIA16154 fig1-Mars Curiosity Rover - Road To Glenelg.jpg|800px|align-cap=center|''[[Curiosity rover|Curiosity]]''{{'s}} view, from about {{convert|200|m|ft|abbr=on}} away, of the ''[[Glenelg, Mars|Glenelg Area]]'' - an important science destination (19 September 2012).}}



On 15 August 2012, the rover began several days of instrument checks and mobility tests.<ref name='driving tests'>{{cite news |author=Harwood, William |title=Rover software updated, first driving tests on tap |date=14 August 2012 |url= http://news.cnet.com/8301-11386_3-57493178-76/rover-software-updated-first-driving-tests-on-tap/ |work=C-Net News |access-date=2012-08-15}}</ref><ref name='first drive'>[http://mars.jpl.nasa.gov/msl/mission/timeline/firstdrive/ First drive]</ref> The first laser testing of the [[Chemistry and Camera complex|ChemCam]] by ''Curiosity'' on Mars was performed on a rock, [[N165|N165 ("Coronation" rock)]], near [[Bradbury Landing]] on 19 August 2012.<ref name="NASA-20120819a">{{cite web |last1=Webster |first1=Guy |last2=Agle |first2=D.C. |title=Mars Science Laboratory/Curiosity Mission Status Report |url= http://www.jpl.nasa.gov/news/news.php?release=2012-248 |date=19 August 2012 |publisher=[[NASA]] |access-date=3 September 2012 }}</ref><ref name="NASA-20120819">{{cite web |author=Staff |title='Coronation' Rock on Mars |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4492 |publisher=[[NASA]] |access-date=3 September 2012 }}</ref><ref name="BBC-20120817">{{cite news |last=Amos |first=Jonathan |title=Nasa's Curiosity rover prepares to zap Martian rocks |url= https://www.bbc.co.uk/news/science-environment-19302886 |date=17 August 2012 |work=[[BBC News]] |access-date=3 September 2012 }}</ref>

File:Milkovich-1ANNOTATED-pia16001-br2.jpg|The four main pieces of hardware that arrived on Mars with NASA's Curiosity rover were spotted by NASA's Mars Reconnaissance Orbiter (MRO).<ref>http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4299</ref>

</gallery>



The science and operations teams have identified at least six possible routes to the base of [[Aeolis Mons|Mount Sharp]], and estimate about a year studying the rocks and soil of the crater floor while ''Curiosity'' slowly makes its way to the base of the mountain.<ref name='driving tests'/><ref>{{cite news |title=Mars rover could start moving in a week |date=15 August 2012 |url= http://edition.cnn.com/2012/08/14/us/mars-curiosity/index.html?hpt=hp_c2 |work=CNN News |access-date=2012-08-15}}</ref> The ChemCam team expects to take approximately one dozen compositional measurements of rocks per day.<ref>{{cite web|url= http://www.msl-chemcam.com/index.php?menu=inc&page_consult=textes&rubrique=64&sousrubrique=224&soussousrubrique=0 |title=How Does ChemCam Work? |access-date=2012-08-20 |date=2011 |work=ChemCam Team}}</ref>

<br />

{{multiple image|align=center|total_width=800

|header=[[Curiosity (rover)|''Curiosity'' rover]] - [[Temperature]], [[Pressure]], [[Humidity]] at [[Gale Crater]] on [[Mars]] {{small|(August 2012 - February 2013)}}|width1=700 |height1=534|image1=PIA16913-MarsCuriosityRover-SteadyTemperature-GaleCrater.jpg |caption1=[[Temperature]]|width2=664|height2=531 |image2=PIA16912-MarsCuriosityRover-SeasonalPressure-GaleCrater.jpg|caption2=[[Pressure]]|width3=831 |height3=637 |image3=PIA16915-MarsCuriosityRover-Humidity-GaleCrater.jpg|caption3=[[Humidity]] }}

Having completed its mobility tests, the rover's first drive began on 29 August 2012, to a place called [[Glenelg, Mars|Glenelg]] about {{convert|400|m |ft|abbr=on}} to the east.<ref>{{cite news |last=Brown |first=Dwayne |title=NASA Curiosity Rover Begins Eastbound Trek on Martian Surface |date=29 August 2012 |url= http://www.jpl.nasa.gov/news/news.php?release=2012-269 |work=[[JPL]] |access-date=2012-08-30}}</ref> Glenelg is a location where three types of terrain intersect, and is the mission's first major driving destination. The drive across may take up to two months, after which ''Curiosity'' will stay at Glenelg for a month.<ref>{{cite news |last=Zakutnyaya |first=Olga |title=Curiosity expected to boost Martian science worldwide |date=21 August 2012 |url= http://english.ruvr.ru/2012_08_21/Curiosity-expected-to-boost-Martian-science-worldwide/ |work=[[The Voice of Russia]] |access-date=21 August 2012 |archive-url= https://web.archive.org/web/20120823231851/http://english.ruvr.ru/2012_08_21/Curiosity-expected-to-boost-Martian-science-worldwide/ |archive-date=23 August 2012 |url-status=dead }}</ref>



On the way, ''Curiosity'' studied a pyramidal rock dubbed "[[Jake Matijevic (rock)|Jake Matijevic]]" after a mathematician-turned-rover-engineer who played a critical role in the design of the six-wheeled rover, but died just days after ''Curiosity'' landed in August.

{{Wide image|Pia16056-br2.jpg|3000px|<center>This color-enhanced view — taken by the High Resolution Imaging Science Experiment (HiRISE) on NASA's [[Mars Reconnaissance Orbiter]] as the satellite flew overhead — shows the terrain around the rover's landing site within Gale Crater on Mars. Colors were enhanced to bring out subtle differences.<ref>[http://marsprogram.jpl.nasa.gov/msl/multimedia/images/?ImageID=4454 Mars Science Laboratory: Images]</ref>}}

<ref>{{cite web |last=Doyle |first=Kathryn |url= http://www.popularmechanics.com/how-to/blog/curiosity-ready-to-blast-rocks-and-study-moons-12868558 |title=''Curiosity'' Ready to Blast Rocks and Study Moons |access-date=2012-09-19 |date=2012 |work=Popular Mechanics}}</ref> The ''Jake rock'' measures about {{convert|25|cm|in|abbr=on}} tall and {{convert|40|cm|in|abbr=on}} wide.<ref>{{cite news |last=Boyle |first=Alan |title=Mars rover targets a rock called Jake |date=19 September 2012 |url= http://cosmiclog.nbcnews.com/_news/2012/09/19/13967230-mars-rover-targets-a-rock-called-jake |work=Cosmic Log on NBC News |access-date=2012-09-19}}</ref> It is an [[igneous rock]] and may be a [[mugearite]], a sodium rich [[oligoclase]]-bearing basaltic [[trachyandesite]].<ref name="BBC-20121017">{{Cite web|last=Amos |first=Jonathan |title=Cosmic coincidence on the road to Glenelg |url= https://www.bbc.co.uk/news/19979798 |date=17 October 2012 |work=[[BBC News]] |access-date=17 October 2012 }}</ref> Afterwards, on 30 September 2012, a finely-grained rock, named "[[Bathurst Inlet (rock)|Bathurst Inlet]]", was examined by ''Curiosity''{{'s}} [[Mars Hand Lens Imager|Mars Hand Lens Imager (MAHLI)]] and [[Alpha particle X-ray spectrometer|Alpha particle X-ray spectrometer (APXS)]]. The rock was named after [[Bathurst Inlet]], a deep inlet located along the [[Northern Canada|northern coast]] of the Canadian mainland. Also, a [[Sand|sand patch]], named "[[Rocknest (Mars)|Rocknest]]", is a test target for the first use of the scoop on the arm of the ''Curiosity rover''.<ref name="Space-20121004">{{cite web |last=Wall |first=Mike |title=''Curiosity'' Rover to Scoop Up 1st Mars Samples This Weekend |url= http://www.space.com/17896-mars-rover-curiosity-first-scoop-samples.html |date=4 October 2012 |publisher=[[Space.com]] |access-date=5 October 2012 }}</ref>



===Evidence for ancient water===

<br />

On 27 September 2012, [[NASA|NASA scientists]] announced that the ''Curiosity'' rover found evidence for an ancient [[streambed]] suggesting a "vigorous flow" of [[water on Mars]].<ref name="NASA-20120927">{{cite web |last1=Brown |first1=Dwayne |last2=Cole |first2=Steve |last3=Webster |first3=Guy |last4=Agle |first4=D.C. |title=NASA Rover Finds Old Streambed On Martian Surface |url= http://www.nasa.gov/home/hqnews/2012/sep/HQ_12-338_Mars_Water_Stream.html |date=27 September 2012 |publisher=[[NASA]] |access-date=28 September 2012 }}</ref><ref name="NASA-20120927a">{{cite web |author=NASA |author-link=NASA |title=NASA's Curiosity Rover Finds Old Streambed on Mars - video (51:40) |url= https://www.youtube.com/watch?v=fYo31XjoXOk |date=27 September 2012 |publisher=[[NASA]]television |access-date=28 September 2012 }}</ref><ref name="AP-20120927">{{cite web |last=Chang|first=Alicia |title=Mars rover Curiosity finds signs of ancient stream| url= http://apnews.excite.com/article/20120927/DA1IDOO00.html |date=27 September 2012 |publisher=[[AP News]]|access-date=27 September 2012 }}</ref>

{{multiple image|align=center|total_width=600

|header=Evidence of [[water on Mars]]<ref name="NASA-20120927" /><ref name="NASA-20120927a" /><ref name="AP-20120927" /><br /> [[Curiosity (rover)|''Curiosity'' rover]] on the way to [[Glenelg, Mars|Glenelg]] (26 September 2012)|width1=776 |height1=600 |image1=PIA16158-Mars Curiosity Rover-Water-AlluvialFan.jpg|caption1=[[Peace Vallis]] and related [[alluvial fan]] near the ''Curiosity'' rover landing ellipse and [[Bradbury Landing|landing site]] (noted by +). |width2=771|height2=600|image2=PIA16156-Mars Curiosity Rover-Water-AncientStreambed.jpg |caption2="[[Hottah (Mars)|Hottah]]" [[rock outcrop]] on Mars - an ancient [[streambed]] viewed by the ''Curiosity'' rover (14 September 2012) ([http://photojournal.jpl.nasa.gov/figures/PIA16156_fig1.jpg close-up]) ([https://web.archive.org/web/20130521042719/http://mars.jpl.nasa.gov/msl/images/pia16223-stereoHattah-Mastcam-br2.jpg 3-D version]). |width3=800|height3=598|image3=PIA16189 fig1-Curiosity Rover-Rock Outcrops-Mars and Earth.jpg |caption3="[[Link (Mars)|Link]]" [[outcrop|rock outcrop]] on Mars - compared with a terrestrial [[Conglomerate (geology)#Fluvial|fluvial conglomerate]] - suggesting water "vigorously" flowed in a [[stream]].}}



On 7 October 2012, a mysterious "bright object" ([[:File:PIA16225-MarsCuriosityRover-ScooperTest&MysteryObject-20121008a.jpg|image]]), discovered in the sand at ''[[Rocknest (Mars)|Rocknest]]'', drew scientific interest. Several close-up pictures ([http://mars.jpl.nasa.gov/msl-raw-images/proj/msl/redops/ods/surface/sol/00062/opgs/edr/ccam/CR0_403005421EDR_F0050104CCAM01062M_.JPG close-up 1]) ([http://photojournal.jpl.nasa.gov/jpeg/PIA16230.jpg close-up 2]) were taken of the object and preliminary interpretations by scientists suggest the object to be "debris from the spacecraft".<ref name="Space-20121018">{{cite web |last=Wall |first=Mike |title=Yum! Curiosity Rover Swallows 1st Mars Sample, Finds Odd Bright Stuff |url= http://www.space.com/18122-mars-rover-curiosity-swallows-soil-sample.html|date=18 October 2012 |publisher=[[Space.com]] |access-date=19 October 2012 }}</ref><ref name="NASA-20121015a">{{cite web |author=Staff |title=Small Debris on the Ground Beside Curiosity |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4806 |date=15 October 2012 |publisher=[[NASA]] |access-date=15 October 2012 }}</ref><ref name="UT-20121009">{{cite web |last=Major |first=Jason|title=Curiosity Finds…SOMETHING…on Martian Surface|url= http://www.universetoday.com/97774/curiosity-finds-something-on-martian-surface/|date=9 October 2012|publisher=[[UniverseToday]] |access-date=9 October 2012 }}</ref> Nonetheless, further images in the nearby sand have detected other "bright particles" ([http://photojournal.jpl.nasa.gov/jpeg/PIA16229.jpg image]) ([http://photojournal.jpl.nasa.gov/jpeg/PIA16233.jpg close-up 1]). These newly discovered objects are presently thought to be "native Martian material".<ref name="Space-20121018" /><ref name="NASA-20121018">{{cite web |author=Staff |title=Bright Particle in Hole Dug by Scooping of Martian Soil |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4817|date=18 October 2012 |publisher=[[NASA]] |access-date=18 October 2012 }}</ref><ref name="NASA-20121015b">{{cite web |author=Staff |title=Bright Particle of Martian Origin in Scoop Hole |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4807 |date=15 October 2012 |publisher=[[NASA]] |access-date=15 October 2012 }}</ref>

[[File:Cheering hq msl20120805-br2.jpg|left|thumb|360px|Engineers at NASA's Jet Propulsion Laboratory in Pasadena, California, celebrate the landing of NASA's Curiosity rover on Mars.<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4208 Mars Science Laboratory: Images]</ref>]]

{{multiple image|align=center|total_width=700

|header="Bright particles" found by the [[Curiosity (rover)|''Curiosity'' rover]] at ''[[Rocknest (Mars)|Rocknest]]'' (October, 2012)<ref name="Space-20121018" /><ref name="NASA-20121015a" /> |width1=672 |height1=600|image1=PIA16225-MarsCuriosityRover-ScooperTest%26MysteryObject-20121008a.jpg|caption1="Bright object" (BO)|width2=600 |height2=600 |image2=MarsCuriosityRover-Raw-ChemCamRI-Sol62-20121008.jpg |caption2=BO Close-up 1|width3=800 |height3=598 |image3=PIA16230.jpg |caption3=BO Close-up 2|width4=800 |height4=597 |image4=PIA16229-MarsCuriosityRover-Sand-20121012.jpg |caption4="Bright particles"|width5=800 |height5=501|image5=PIA16233-MarsCuriosityRover-Sand-Closeup-20121015.jpg |caption5=BP Close-up 1

}}

On 17 October 2012, at ''Rocknest'', the first [[X-ray crystallography#Mineralogy and metallurgy|X-ray diffraction analysis]] of [[Martian soil]] was performed. The results revealed the presence of several minerals, including [[feldspar]], [[pyroxene]]s and [[olivine]], and suggested that the Martian soil in the sample was similar to the weathered basaltic soils of [[Hawaii Volcanoes|Hawaiian volcanoes]]. The sample used is composed of [[dust]] distributed from [[Martian soil#Atmospheric dust|global dust storms]] and local fine sand. So far, the materials ''Curiosity'' has analyzed are consistent with the initial ideas of deposits in Gale Crater recording a transition through time from a wet to dry environment.<ref name="NASA-20121030">{{cite web |last=Brown |first=Dwayne |title=NASA Rover's First Soil Studies Help Fingerprint Martian Minerals|url= http://www.nasa.gov/home/hqnews/2012/oct/HQ_12-383_Curiosity_CheMin.html |date=30 October 2012 |publisher=[[NASA]] |access-date=31 October 2012}}</ref>

On 22 November 2012, the ''Curiosity'' rover analyzed a rock named "[[Rocknest 3 (rock)|Rocknest 3]]" with the [[Curiosity rover#Alpha Particle X-ray Spectrometer (APXS)|APXS]] and then resumed traveling toward "Point Lake" overlook on its way to [[Glenelg, Mars|Glenelg Intrigue]].<ref name="Space-20121122">{{cite web |author=Staff |title=Thanksgiving on Mars: Working Holiday for Curiosity Rover |url= http://www.space.com/18594-mars-thanksgiving-curiosity-rover.html |date=22 November 2012 |publisher=[[Space.com]] |access-date=22 November 2012 }}</ref>



On 3 December 2012, NASA reported that ''[[Curiosity (rover)|Curiosity]]'' performed its first extensive [[soil analysis]], revealing the presence of [[Water on Mars|water molecules]], [[sulfur]] and [[chlorine]] in the [[Martian soil]].<ref name="NASA-20121203">{{cite web |last1=Brown |first1=Dwayne |last2=Webster |first2=Guy |last3=Neal-Jones |first3=Nancy |title=NASA Mars Rover Fully Analyzes First Martian Soil Samples |url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1399 |date=3 December 2012 |publisher=[[NASA]] |access-date=3 December 2012 |archive-url= https://web.archive.org/web/20160823211438/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1399 |archive-date=23 August 2016 |url-status=dead }}</ref><ref name="NYT-20121203">{{cite web |last=Chang |first=Ken |title=Mars Rover Discovery Revealed |url= http://thelede.blogs.nytimes.com/2012/12/03/mars-rover-discovery-revealed |date=3 December 2012 |work=[[New York Times]] |access-date=3 December 2012 }}</ref> The presence of [[perchlorates]] in the sample seems highly likely. The presence of [[sulfate]] and [[sulfide]] is also likely because [[sulfur dioxide]] and [[hydrogen sulfide]] were detected. Small amounts of [[chloromethane]], [[dichloromethane]] and [[trichloromethane]] were detected. The source of the carbon in these molecules is unclear. Possible sources include contamination of the instrument, organics in the sample and inorganic [[carbonates]].<ref name="NASA-20121203" /><ref name="NYT-20121203" />

[[File:Cheering-full-br2.jpg|right|thumb|360px|The Mars Science Laboratory (MSL) team in the MSL Mission Support Area react after learning the the Curiosity rove has landed safely on Mars and images start coming in at the Jet Propulsion Laboratory on Mars.<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4210 Mars Science Laboratory: Images]</ref>]] <br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br />



===Evidence for ancient habitability===

The following data were compiled by Curiosity's Entry, Descent and Landing team at [[Jet Propulsion Laboratory|NASA's Jet Propulsion Laboratory]] in [[Pasadena]], [[California]]. It provides a timeline of critical mission events that occurred on the evening of August 5 PDT (early on August 6 EDT).<ref>[http://www.nasa.gov/mission_pages/msl/news/edl20120809.html NASA - Timeline Mission Milestones During Curiosity's Landing]</ref>

In February 2013, the rover used its drill for the first time.<ref>[https://web.archive.org/web/20130213041314/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1423 NASA Curiosity Rover Collects First Martian Bedrock Sample]</ref>

{{multiple image|align=center|total_width=800

|header= [[Curiosity (rover)|''Curiosity'' rover]] - First drilling tests (''[[List of rocks on Mars#Curiosity|"John Klein" rock]]'', ''Yellowknife Bay'', 2–6 February 2013).<ref name="TMJ-20130203">{{cite web |last=Anderson |first=Paul Scott |title=Curiosity 'hammers' a rock and completes first drilling tests |url= http://themeridianijournal.com/2013/02/curiosity-hammers-a-rock-and-completes-first-drilling-tests/ |date=3 February 2013 |publisher=themeridianijournal.com |access-date=3 February 2013 |url-status=dead |archive-url= https://web.archive.org/web/20130206162148/http://themeridianijournal.com/2013/02/curiosity-hammers-a-rock-and-completes-first-drilling-tests/ |archive-date=6 February 2013 }}</ref> |width1=8510 |height1=12204 |image1=PIA16937-MarsCuriosityRover-SelfPortraitAtJohnKlein-20130510.jpg|caption1=[[Curiosity rover#Robotic arm|Drilling site]] |width2=3921 |height2=4325|image2=MarsCuriosityRover-Drilling-Sol170++-2.jpg |caption2=[[Curiosity rover#Robotic arm|Drill]] in [[List of rocks on Mars#Curiosity|place]]. |width3=750 |height3=750|image3=PIA16718-MarsCuriosityRover-DrillBit-20130129.jpg |caption3=[[Curiosity rover#Robotic arm|Drill bit]]|width4=1605 |height4=1196 |image4=PIA16717-MarsCuriosityRover-DrillTest-20130202.jpg |caption4="[[Curiosity rover#Robotic arm|Drill]] on [[List of rocks on Mars#Curiosity|Rock checkout]]." |width5=1584 |height5=1184 |image5=PIA16761-MarsCuriosityRover-DrilledHole-20130206.jpg|caption5=[[Curiosity rover#Robotic arm|Drill hole]]. |width6=1200 |height6=1200|image6=PIA16762-MarsCuriosityRover-DrilledHole-20130206.gif |caption6=[[Curiosity rover#Robotic arm|Drill hole]] - [[List of rocks on Mars#Curiosity|before/after]].}}



{{wide image |PIA16685-MarsCuriosityRover-YellowknifeBay-DrillArea-20121228.jpg |800px|align-cap=center|Drilling Area at Yellowknife Bay (28 December 2012).}}

{| class="wikitable"

|-

! Event !! Time of Event Occurrence at [[Mars]] ([[PDT]]) !! Time Event Occurrence Received on [[Earth]] (PDT)

|-

| Atmospheric entry || 10:10:45.7 PM || 10:24:33.8 PM

|-

| Parachute deployment || 10:15:04.9 PM || 10:28:53.0 PM

|-

| Heat shield separation || 10:15:24.6 PM || 10:29:12.7 PM

|-

| Rover lowered by the sky crane || 10:17:38.6 PM ||10:31:26.7 PM

|-

| Touchdown || 10:17:57.3 PM || 10:31:45.4 PM

|}



In March 2013, NASA reported ''[[Curiosity (rover)|Curiosity]]'' found evidence that [[Geochemistry|geochemical]] conditions in [[Gale Crater]] were once suitable for [[microbial life]] after analyzing the first drilled sample of [[list of rocks on Mars|Martian rock]], [[List of rocks on Mars#Curiosity|"John Klein" rock]] at ''Yellowknife Bay'' in [[Gale Crater]]. The rover detected [[water]], [[carbon dioxide]], [[oxygen]], [[sulfur dioxide]] and [[hydrogen sulfide]].<ref name="NASA-20130312">{{cite web |last1=Agle |first1=DC |last2=Brown |first2=Dwayne |title=NASA Rover Finds Conditions Once Suited for Ancient Life on Mars |url= http://www.jpl.nasa.gov/news/news.php?release=2013-092 |publisher=[[NASA]] |date=12 March 2013 |access-date=12 March 2013}}</ref><ref name="Space-20130312">{{cite web |last=Wall |first=Mike |title=Mars Could Once Have Supported Life: What You Need to Know |url= http://www.space.com/20187-ancient-mars-life-curiosity-faq.html |date=12 March 2013 |work=[[Space.com]] |access-date=12 March 2013 }}</ref><ref name="NYT-20130312">{{cite news |last=Chang |first=Kenneth |title=Mars Could Once Have Supported Life, NASA Says |url= https://www.nytimes.com/2013/03/13/science/space/mars-could-have-supported-life-nasa-says.html |date=12 March 2013 |work=[[New York Times]] |access-date=12 March 2013 }}</ref> [[Chloromethane]] and [[dichloromethane]] were also detected. Related tests found results consistent with the presence of [[Clay minerals|smectite clay minerals]].<ref name="NASA-20130312" /><ref name="Space-20130312" /><ref name="NYT-20130312" /><ref name="SFN-20130312">{{cite news |last=Harwood |first=William |title=Mars rover finds habitable environment in distant past |url= http://www.spaceflightnow.com/mars/msl/130312life/ |date=12 March 2013 |work=Spaceflightnow |access-date=12 March 2013 }}</ref><ref name="HP-20130312">{{cite news |last=Grenoble |first=Ryan |title=Life On Mars Evidence? NASA's Curiosity Rover Finds Essential Ingredients In Ancient Rock Sample |url= https://www.huffingtonpost.com/2013/03/12/life-on-mars-evidence-nasa-curiosity_n_2861505.html |date=12 March 2013 |work=[[Huffington Post]] |access-date=12 March 2013 }}</ref> In addition, sandstone beds associated with the [[Yellowknife Bay, Mars#Yellowknife Bay Geology|Gillespie Lake Member]] of ''[[Yellowknife Bay, Mars|Yellowknife Bay]]'' seem similar to [[microbially induced sedimentary structure]]s (MISS) found on Earth, according to one study.<ref name="ASB-20150214">{{cite journal |last=Nora |first=Noffke |author-link=Nora Noffke |title=Ancient Sedimentary Structures in the <3.7 Ga Gillespie Lake Member, Mars, That Resemble Macroscopic Morphology, Spatial Associations, and Temporal Succession in Terrestrial Microbialites |date=14 February 2015 |journal=[[Astrobiology (journal)|Astrobiology]] |volume=15 |issue=2 |doi=10.1089/ast.2014.1218 |pmid=25495393 |bibcode=2015AsBio..15..169N |pages=169–192}}</ref>

[[File:675608main edl20120809-full.jpg|770px]]

{{multiple image|align=center|total_width=800

|header=[[Curiosity (rover)|''Curiosity'' rover]] - Chemical analysis<br />(drilled sample of [[List of rocks on Mars#Curiosity|"John Klein" rock]], ''Yellowknife Bay'', 27 February 2013).<ref name="NASA-20130312" /><ref name="Space-20130312" /><ref name="NYT-20130312" />|width1=1242 |height1=782 |image1=PIA16817-MarsCuriosityRover-Analysis-JohnKleinRock-4thPortion.jpg |caption1=[[Sample Analysis at Mars|Sample Analysis at Mars (SAM) (4th rock portion) (April, 2013)]] |width2=929 |height2=720 |image2=PIA16835-MarsCuriosityRover-JohnKleinRock-ChemAnal1.jpg |caption2=[[Sample Analysis at Mars|Sample Analysis at Mars (SAM)]] |width3=844 |height3=720 |image3=PIA16836-MarsCuriosityRover-JohnKleinRock-ChemAnal2.jpg |caption3=[[Sample Analysis at Mars|Gas chromatograph mass spectrometer (GCMS)]] |width4=2856 |height4=1470 |image4=PIA16830-fig1-MarsCuriosityRover-JohnKleinRock-ChemAnal0.jpg |caption4=[[CheMin|Chemistry and Mineralogy instrument (CheMin)]] }}



===Evidence for atmospheric loss===

Curiosity's EDL team releases a timeline for mission milestones (depicted in this artist's concept) surrounding the landing of the Mars rover.

On 8 April 2013, NASA reported that much of the [[Atmosphere of Mars#Argon|atmosphere of Mars]] has been [[Atmospheric escape#Comparison of non-thermal loss processes based on planet and particle mass|lost]] based on [[Argon#Isotopes|argon isotope ratios]] studies.<ref name="NASA-20130408">{{cite web |last=Webster |first=Guy |title=Remaining Martian Atmosphere Still Dynamic |url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1461 |date=8 April 2013 |work=[[NASA]] |access-date=9 April 2013 |archive-url= https://web.archive.org/web/20170213164204/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1461 |archive-date=13 February 2017 |url-status=dead }}</ref><ref name="Space-20130408">{{cite web |last=Wall |first=Mike|title=Most of Mars' Atmosphere Is Lost in Space|url= http://www.space.com/20560-mars-atmosphere-lost-curiosity-rover.html |date=8 April 2013|work=[[Space.com]] |access-date=9 April 2013 }}</ref>



On 19 July 2013, NASA scientists published the results of a new analysis of the [[atmosphere of Mars]], reporting a lack of [[Atmosphere of Mars#Methane|methane]] around the [[Gale Crater|landing site]] of the ''Curiosity'' rover. In addition, the scientists found evidence that Mars "has lost a good deal of its atmosphere over time", based on the abundance of isotopic compositions of gases, particularly those related to [[argon]] and [[carbon]].<ref name="Wired-20130718">{{cite magazine |last=Mann |first=Adam |title=Mars Rover Finds Good News for Past Life, Bad News for Current Life on Mars|url= https://www.wired.com/wiredscience/2013/07/curiosity-mars-atmosphere |date=18 July 2013|magazine=[[Wired (magazine)|Wired]] |access-date=19 July 2013 }}</ref><ref name="SCI-20130719a">{{cite journal|author=Webster Chris R. |title=Isotope Ratios of H, C, and O in CO2 and H2O of the Martian Atmosphere|date=19 July 2013|journal=[[Science (journal)|Science]]|volume=341 |number=6143 |pages=260–263|doi=10.1126/science.1237961 |display-authors=etal |pmid=23869013|bibcode=2013Sci...341..260W|s2cid=206548962|url=https://authors.library.caltech.edu/102999/1/260.full.pdf}}</ref><ref name="SCI-20130719b">{{cite journal |author=Mahaffy, Paul R. |title=Abundance and Isotopic Composition of Gases in the Martian Atmosphere from the Curiosity Rover| date=19 July 2013 |journal=[[Science (journal)|Science]] |volume=341 |number=6143 |pages=263–266|doi=10.1126/science.1237966|display-authors=etal |bibcode=2013Sci...341..263M |pmid=23869014|s2cid=206548973}}</ref>

<br />



{{wide image|ESP-032436-1755-MarsCuriosityRover-MRO-HiRISE-20130627.jpg|500px|align-cap=center|[[Curiosity (rover)|''Curiosity'' rover]] (very bright spot near the lower right) and "Tracks" from ''[[Bradbury Landing]]'' to ''[[List of rocks on Mars#Curiosity|John Klein]]'' in ''Yellowknife Bay'' - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; 27 June 2013).}}

==After landing on Mars==

===Surface mission start===

----

====Sol 0====



===Other 2013 events===

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

[[File:PIA16818-MarsCuriosityRover-Argon-AtmosphericLoss.png|thumb|200px|right|[[Argon#Isotopes|Argon isotope ratios]] are used to estimate [[Atmosphere of Mars#Argon|atmospheric loss]] on [[Mars]]. ([[Curiosity (rover)|''Curiosity'' rover]], April, 2013)]]

! style="margin; background: lavender;" colspan="3" | '''06 August 2012'''

On 28 February 2013, NASA was forced to switch to the backup computer due to an issue with the then active computer's flash memory which resulted in the computer continuously rebooting in a loop. The backup computer was turned on in safe mode and was converted to operational status on 19 March 2013.<ref name="NASA-20130318">{{cite web |last=Webster|first=Guy |title=New 'Safe Mode' Status of Curiosity Expected to be Brief - Mission Status Report - 03.18.13|url= http://www.nasa.gov/mission_pages/msl/news/msl20130318b.html |date=18 March 2013 |work=[[NASA]]|access-date=19 March 2013 }}</ref><ref name="NYT-20130319">{{cite news |last=Fountain |first=Henry |title=Mars Rover Is Repaired, NASA Says|url= https://www.nytimes.com/2013/03/20/science/space/on-mars-curiosity-rover-repaired-nasa-says.html |date=19 March 2013 |work=[[New York Times]] |access-date=19 March 2013 }}</ref>

|-

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=7yB9-oMj2ew NASA Video 1] [http://www.youtube.com/watch?v=Ps01BLaO7D8 Video 2] [http://www.youtube.com/watch?v=imOr0y74FxI Video 3] [http://www.youtube.com/watch?v=wnG-rFFpP8A Video 4] [http://www.youtube.com/watch?v=FVzfDZlEwaU Video 5] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1286 NASA News 1] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1292 News 2]

|}



On 18 March 2013, NASA reported evidence of [[mineral hydration]], likely hydrated [[calcium sulfate]], in several [[Rock (geology)|rock samples]] including the broken fragments of [[Tintina (rock)|"Tintina" rock]] and [[List of rocks on Mars#Curiosity|"Sutton Inlier" rock]] as well as in [[Vein (geology)|veins]] and [[Nodule (geology)|nodules]] in other rocks like [[List of rocks on Mars#Curiosity|"Knorr" rock]] and [[List of rocks on Mars#Curiosity|"Wernicke" rock]].<ref name="NASA-20130318a">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |title=Curiosity Mars Rover Sees Trend In Water Presence |url=http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1446 |date=18 March 2013 |work=[[NASA]] |access-date=20 March 2013 |archive-url=https://web.archive.org/web/20130424111259/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1446 |archive-date=24 April 2013 |url-status=dead }}</ref><ref name="BBC-20130319">{{cite web |last=Rincon |first=Paul |title=Curiosity breaks rock to reveal dazzling white interior |url= https://www.bbc.co.uk/news/science-environment-21340279 |date=19 March 2013 |publisher=[[BBC]] |access-date=19 March 2013 }}</ref><ref name="MSN-20130120">{{cite web |author=Staff |title=Red planet coughs up a white rock, and scientists freak out |url= http://now.msn.com/white-mars-rock-called-tintina-found-by-curiosity-rover |date=20 March 2013 |work=[[MSN]] |access-date=20 March 2013 |url-status=dead |archive-url= https://web.archive.org/web/20130323164757/http://now.msn.com/white-mars-rock-called-tintina-found-by-curiosity-rover |archive-date=23 March 2013 }}</ref> Analysis using the rover's [[Dynamic Albedo of Neutrons|DAN instrument]] provided evidence of subsurface water, amounting to as much as 4% water content, down to a depth of {{convert|60|cm|ft|abbr=on}}, in the rover's traverse from the ''[[Bradbury Landing]]'' site to the ''Yellowknife Bay'' area in the [[Glenelg, Mars|''Glenelg'']] terrain.<ref name="NASA-20130318a" />

<gallery>

[[File:PIA16791-MarsCuriosityRover-Composition-YellowknifeBayRocks.png|thumb|200px|left|Composition of [[List of rocks on Mars#Curiosity|"Yellowknife Bay" rocks]] - [[Vein (geology)|rock veins]] are higher in [[calcium]] and [[sulfur]] than "Portage" soil - [[Curiosity (rover)#Alpha Particle X-ray Spectrometer (APXS)|APXS]] results - ''Curiosity'' rover (March, 2013).]]

File:Sample thumbnail by Curiosity at NASA-JPL.jpg|First picture by MSL [[Curiosity rover|Curiosity]] from [[Mars]]<ref>http://www.nasa.gov/mission_pages/msl/multimedia/mccuistion.html</ref>

Between 4 April – 1 May 2013, ''Curiosity'' operated autonomously due to a Martian [[solar conjunction]] with Earth. While ''Curiosity'' transmitted a beep to Earth each day and the ''[[2001 Mars Odyssey|Odyssey]] ''spacecraft continued to relay information from the rover, no commands were sent from mission control since there was a possibility of data corruption due to interference from the Sun. ''Curiosity'' continued to perform stationary science at Yellowknife Bay for the duration of the conjunction.<ref name="NASA-20130408" /><ref name="Space-20130404">{{cite news|url= http://www.space.com/20501-mars-rover-curiosity-solar-conjunction.html |title=Curiosity Rover Goes Solo on Mars for 1st Time Today |work=Space.com |first=Mike |last=Wall |date=4 April 2013 |access-date=9 April 2013}}</ref>



On 5 June 2013, NASA announced that ''Curiosity'' will soon begin a {{convert|8|km|mi|abbr=on}} journey from the [[Glenelg, Mars|Glenelg area]] to the base of [[Mount Sharp]]. The trip is expected to take nine months to a year with stops along the way to study the local terrain.<ref name="NASA-20130605">{{cite web |author=Staff|title=From 'Glenelg' to Mount Sharp |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=5326 |date=5 June 2013 |work=[[NASA]] |access-date=6 June 2013 }}</ref><ref name="AP-20130605">{{cite news |last=Chang |first=Alicia |title=Curiosity rover to head toward Mars mountain soon |url= http://apnews.excite.com/article/20130605/DA6NQG0G2.html |date=5 June 2013 |work=[[AP News]] |access-date=7 June 2013 }}</ref><ref name="NYT-20130607">{{cite news |last=Chang |first=Kenneth |title=Martian Rock Another Clue to a Once Water-Rich Planet|url= https://www.nytimes.com/2013/06/08/science/space/martian-rock-another-clue-to-a-once-water-rich-planet.html|date=7 June 2013 |work=[[New York Times]] |access-date=7 June 2013 }}</ref>

File:Landscape-MarsCuriosity.png|This is the full-resolution version of one of the first images taken by a rear Hazard-Avoidance camera on NASA's Curiosity rover.<ref>http://www.nasa.gov/mission_pages/msl/multimedia/pia15987.html</ref>



On 16 July 2013, the ''Curiosity'' rover reached a milestone in its journey across [[Mars]], having traveled {{convert|1|km|mi|abbr=on}}, since its landing in 2012;<ref name="NASA-20130716">{{cite web |author=Staff |title=One Down, Many Kilometers to Go |url= http://www.jpl.nasa.gov/spaceimages/details.php?id=PIA17279 |publisher=[[NASA]] |date=16 July 2013 |access-date=19 July 2013}}</ref> on 1 August 2013, the rover traveled over one mile: {{convert|1.686|km|mi|abbr=on}}.<ref name="NASA-20130801">{{cite web |author=Staff |title=PIA17085: Full Curiosity Traverse Passes One-Mile Mark |url= http://photojournal.jpl.nasa.gov/catalog/PIA17085 |date=2 August 2013 |work=[[NASA]] |access-date=2 August 2013 }}</ref>

File:673885main PIA15986-full full.jpg|The Curiosity rover landed on August 6, 2012 about 10 kilometres (6.2 mi) from the base of [[Aeolis Mons]] (or Mount Sharp)<ref>http://www.nasa.gov/mission_pages/msl/multimedia/PIA15986.html</ref>



On 6 August 2013, NASA celebrated ''Curiosity''{{'s}} first year on [[Mars]] (6 August 2012 to 5 August 2013) by programming the rover to perform the "[[Happy Birthday to You|Happy Birthday]]" song to itself.<ref name="WP-20130806">{{cite news |last=Dewey |first=Caitlin |title=Lonely Curiosity rover sings 'Happy Birthday' to itself on Mars |url= https://www.washingtonpost.com/blogs/the-switch/wp/2013/08/06/lonely-curiosity-rover-sings-happy-birthday-to-itself-on-mars/ |date=6 August 2013 |newspaper=[[Washington Post]] |access-date=7 August 2013 }}</ref><ref name="ATL-20170810">{{cite web |last=Koren |first=Marina |title=Why the Curiosity Rover Stopped Singing 'Happy Birthday' to Itself |url= https://www.theatlantic.com/science/archive/2017/08/why-the-curiosity-rover-stopped-singing-happy-birthday-to-itself/536487/ |date=10 August 2017 |work=[[The Atlantic]] |access-date=11 August 2017 }}</ref> NASA also released [[Timeline of Mars Science Laboratory#Videos|several videos]] ([http://mars.jpl.nasa.gov/multimedia/videos/movies/msl20130801/msl20130801-480.mov video-1], [http://mars.jpl.nasa.gov/multimedia/videos/movies/msl20130802/msl20130802-480.mov video-2]) summarizing the rover's accomplishments over the year.<ref name="NYT-20130805a">{{cite news |last=Chang |first=Kenneth |title=An Earth Year on Mars |url= https://www.nytimes.com/2013/08/06/science/space/an-earth-year-on-mars.html |date=5 August 2013 |work=[[New York Times]] |access-date=5 August 2013 }}</ref><ref name="NYT-20130805b">{{cite news |last1=Corum |first1=Jonathan |last2=White |first2=Jeremy |title=Mars Curiosity Rover Tracker - Front-Page Interactive Feature |url= https://www.nytimes.com/interactive/science/space/mars-curiosity-rover-tracker.html |date=5 August 2013 |work=[[New York Times]] |access-date=5 August 2013 }}</ref> Primarily, the mission found evidence of "[[Timeline of Mars Science Laboratory#Evidence for ancient habitability|ancient environments suitable for life]]" on Mars. The rover drove over one-mile across the Martian terrain, transmitted more than 190 gigabits of data to Earth, including 70,000 images (36,700 full images and 35,000 thumbnails), and the rover's [[Chemistry and Camera complex|laser]] fired more than 75,000 times at 2,000 targets.<ref name="NASA-20130806" />

</gallery>

----



On 27 August 2013, ''Curiosity'' used [[Autonomous Navigation System|autonomous navigation]] (or ''"autonav"''- the ability of the rover to decide for itself how to drive safely) over unknown Martian ground for the first time.<ref name="NASA-20130827">{{cite web |last=Webster |first=Guy |title=NASA's Mars Curiosity Debuts Autonomous Navigation |url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1514 |date=27 August 2013 |work=[[NASA]] |access-date=27 August 2013 |archive-url= https://web.archive.org/web/20161028020036/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1514 |archive-date=28 October 2016 |url-status=dead }}</ref>

====Sol 1====

[[File:PIA17603 Erosion by Scarp Retreat in Gale Crater, Annotated Version.jpg|thumb|right|300px|''Curiosity'' rover - view of "[[List of rocks on Mars#Curiosity|Sheepbed]]" [[mudstone]] (lower left) and surroundings (February 14, 2013).]]

On 19 September 2013, NASA scientists, on the basis of further measurements by ''Curiosity'', reported no detection of [[atmospheric methane]] with a measured value of {{val|0.18|0.67}} ppbv corresponding to an upper limit of only 1.3 ppbv (95% confidence limit) and, as a result, conclude that the probability of current methanogenic microbial activity on Mars is reduced.<ref name="SJ-20130919">{{cite journal |last1=Webster|first1=Christopher R. |last2=Mahaffy |first2=Paul R. |last3=Atreya |first3=Sushil K. |last4=Flesch|first4=Gregory J. |last5=Farley |first5=Kenneth A. |last6=Kemppinen |first6=O. |last7=Bridges |first7=N. |last8=Johnson |first8=J. R. |last9=Minitti |first9=M. |last10=Cremers |first10=D. |last11=Bell |first11=J. F. |last12=Edgar |first12=L. |last13=Farmer |first13=J. |last14=Godber |first14=A. |last15=Wadhwa |first15=M. |author15-link=Meenakshi Wadhwa |last16=Wellington |first16=D. |last17=McEwan |first17=I. |last18=Newman |first18=C. |last19=Richardson |first19=M. |last20=Charpentier |first20=A. |last21=Peret |first21=L. |last22=King |first22=P. |last23=Blank |first23=J. |last24=Weigle |first24=G. |last25=Schmidt |first25=M. |last26=Li |first26=S. |last27=Milliken |first27=R. |last28=Robertson |first28=K. |last29=Sun |first29=V. |last30=Baker |first30=M. |title=Low Upper Limit to Methane Abundance on Mars|url= https://www.science.org/doi/abs/10.1126/science.1242902 |date=19 September 2013|journal=[[Science (journal)|Science]] |volume=342 |issue=6156 |pages=355–357 |doi=10.1126/science.1242902 |access-date=19 September 2013 |display-authors=29 |bibcode=2013Sci...342..355W |pmid=24051245|s2cid=43194305 |doi-access=free }}</ref><ref name="SCI-20130919">{{cite journal |last=Cho |first=Adrian |title=Mars Rover Finds No Evidence of Burps and Farts |url= http://news.sciencemag.org/space/2013/09/mars-rover-finds-no-evidence-burps-and-farts

|date=19 September 2013 |journal=[[Science (journal)|Science]] |access-date=19 September 2013 }}</ref><ref name="NYT-20130919">{{cite news |last=Chang |first=Kenneth |title=Mars Rover Comes Up Empty in Search for Methane|url= https://www.nytimes.com/2013/09/20/science/space/mars-rover-comes-up-empty-in-search-for-methane.html|date=19 September 2013 |work=[[New York Times]] |access-date=19 September 2013 }}</ref>



On 26 September 2013, NASA scientists reported the [[Mars]] [[Curiosity (rover)|''Curiosity'' rover]] detected "abundant, easily accessible" [[Water on Mars|water]] (1.5 to 3 weight percent) in [[Martian soil|soil samples]] at the [[Rocknest (Mars)|Rocknest region]] of [[Aeolis Palus]] in [[Gale Crater]].<ref name="ST-20130926">{{cite web |last=Lieberman |first=Josh |title=Mars Water Found: Curiosity Rover Uncovers 'Abundant, Easily Accessible' Water In Martian Soil |url= http://www.isciencetimes.com/articles/6131/20130926/mars-water-soil-nasa-curiosity-rover-martian.htm |date=26 September 2013 |work=iSciencetimes |access-date=26 September 2013 |archive-url= https://web.archive.org/web/20170623005252/http://www.isciencetimes.com/articles/6131/20130926/mars-water-soil-nasa-curiosity-rover-martian.htm |archive-date=23 June 2017 |url-status=dead }}</ref><ref name="Science-20130926a">{{cite journal |author=Leshin, L. A |title=Volatile, Isotope, and Organic Analysis of Martian Fines with the Mars Curiosity Rover |date=27 September 2013 |journal=[[Science (journal)|Science]] |volume=341 |issue=6153 <!---|pages=1238937 |number=6153--->

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

|doi=10.1126/science.1238937|last2=Mahaffy |first2=P. R. |display-authors=1 |last3=Webster |last4=Cabane |last5=Coll |last6=Conrad |last7=Archer |last8=Atreya |last9=Brunner |last10=Buch |last11=Eigenbrode |last12=Flesch |last13=Franz |last14=Freissinet |last15=Glavin |last16=McAdam |last17=Miller |last18=Ming |last19=Morris |last20=Navarro-Gonzalez |last21=Niles |last22=Owen |last23=Pepin |last24=Squyres |last25=Steele |last26=Stern |last27=Summons |last28=Sumner |last29=Sutter |last30=Szopa |last31=Teinturier |last32=Trainer |last33=Wray |last34=Grotzinger |author35=MSL Science Team |pages=1238937 |pmid=24072926|bibcode=2013Sci...341E...3L |citeseerx=10.1.1.397.4959 |s2cid=206549244 }}</ref><ref name="Science-20130926">{{cite journal |last=Grotzinger |first=John|title=Introduction To Special Issue: Analysis of Surface Materials by the Curiosity Mars Rover|date=26 September 2013 |journal=[[Science (journal)|Science]] |volume=341 |issue=6153 <!---|number=6153---> |page=1475 |doi=10.1126/science.1244258 |pmid=24072916|bibcode=2013Sci...341.1475G|doi-access=free }}</ref><ref name="NASA-20130926a">{{cite web |last1=Neal-Jones |first1=Nancy |last2=Zubritsky |first2=Elizabeth|last3=Webster |first3=Guy |last4=Martialay |first4=Mary |title=Curiosity's SAM Instrument Finds Water and More in Surface Sample |url= http://www.nasa.gov/content/goddard/curiositys-sam-instrument-finds-water-and-more-in-surface-sample/ |date=26 September 2013 |work=[[NASA]] |access-date=27 September 2013 }}</ref><ref name="NASA-20130926b">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |title=Science Gains From Diverse Landing Area of Curiosity |url= http://www.nasa.gov/mission_pages/msl/news/msl20130926.html |date=26 September 2013 |work=[[NASA]] |access-date=27 September 2013 }}</ref><ref name="NYT-20131001">{{cite news |last=Chang|first=Kenneth |title=Hitting Pay Dirt on Mars |url= https://www.nytimes.com/2013/10/01/science/space/hitting-pay-dirt-on-mars.html |date=1 October 2013 |work=[[New York Times]] |access-date=2 October 2013 }}</ref> In addition, NASA reported that the ''Curiosity'' rover found two principal soil types: a fine-grained [[Mafic|mafic type]] and a locally derived, coarse-grained [[Felsic|felsic type]].<ref name="Science-20130926" /><ref name="NASA-20130926b" /><ref name="Science-20130913b">{{cite journal |title=Soil Diversity and Hydration as Observed by ChemCam at Gale Crater, Mars |url= https://www.science.org/doi/10.1126/science.1238670 |date=26 September 2013 |journal=[[Science (journal)|Science]] |volume=341 |issue=6153 |pages=1238670 |doi=10.1126/science.1238670|access-date=27 September 2013 |last1=Meslin |first1=P.-Y. |display-authors=1 |last2=Gasnault |first2=O. |last3=Forni |first3=O. |last4=Schroder |first4=S. |last5=Cousin |first5=A. |last6=Berger |first6=G. |last7=Clegg |first7=S. M. |last8=Lasue |first8=J. |last9=Maurice |first9=S. |last10=Sautter |first10=V. |author10-link=Violaine Sautter|last11=Le Mouelic |first11=S. |last12=Wiens |first12=R. C. |last13=Fabre |first13=C. |last14=Goetz |first14=W. |last15=Bish |first15=D. |last16=Mangold |first16=N. |last17=Ehlmann |first17=B. |last18=Lanza |first18=N. |last19=Harri |first19=A.- M. |last20=Anderson |first20=R. |last21=Rampe |first21=E. |last22=McConnochie |first22=T. H. |last23=Pinet |first23=P. |last24=Blaney |first24=D. |last25=Leveille |first25=R. |last26=Archer |first26=D. |last27=Barraclough |first27=B. |last28=Bender |first28=S. |last29=Blake |first29=D. |last30=Blank |first30=J. G. |pmid=24072924|bibcode=2013Sci...341E...1M |citeseerx=10.1.1.397.5426 |s2cid= 7418294 }}</ref> The mafic type, similar to other [[Martian soil]]s and [[Martian dust]], was associated with hydration of the amorphous phases of the soil.<ref name="Science-20130913b" /> Also, [[perchlorates]], the presence of which may make detection of life-related [[Organic matter|organic molecules]] difficult, were found at the ''Curiosity'' rover landing site (and earlier at the more polar site of the [[Phoenix (spacecraft)|Phoenix lander]]) suggesting a "global distribution of these salts".<ref name="NYT-20131001" /> NASA also reported that [[Jake M (rock)|Jake M rock]], a rock encountered by ''Curiosity'' on the way to [[Glenelg, Mars|Glenelg]], was a [[mugearite]] and very similar to terrestrial mugearite rocks.<ref name="Science-20130926c">{{Cite journal|last1=Stolper|first1=E.M.|last2=Baker|first2=M.B.|last3=Newcombe|first3=M.E.|last4=Schmidt|first4=M.E.|last5=Treiman|first5=A.H.|last6=Cousin|first6=A.|last7=Dyar|first7=M.D.|last8=Fisk|first8=M.R.|last9=Gellert|first9=R.|last10=King|first10=P.L.|last11=Leshin|first11=L.|last12=Maurice|first12=S.|last13=McLennan|first13=S.M.|last14=Minitti|first14=M.E.|last15=Perrett|first15=G.|last16=Rowland|first16=S.|last17=Sautter|first17=V.|author17-link=Violaine Sautter|last18=Wiens|first18=R.C.|last19=MSL ScienceTeam|first19=O.|last20=Bridges|first20=N.|last21=Johnson|first21=J. R.|last22=Cremers|first22=D.|last23=Bell|first23=J. F.|last24=Edgar|first24=L.|last25=Farmer|first25=J.|last26=Godber|first26=A.|last27=Wadhwa|first27=M.|last28=Wellington|first28=D.|last29=McEwan|first29=I.|last30=Newman|first30=C.|title=The Petrochemistry of Jake_M: A Martian Mugearite|journal=[[Science (journal)|Science]]|volume=341|issue=6153|pages=1239463|doi=10.1126/science.1239463|date=2013|display-authors=29|pmid=24072927|bibcode=2013Sci...341E...4S|s2cid=16515295|url=https://authors.library.caltech.edu/41547/13/Jake_M%20Stolper%20et%20al.%20%282013%29%20Science.pdf|access-date=6 December 2019|archive-date=11 August 2021|archive-url=https://web.archive.org/web/20210811150621/https://authors.library.caltech.edu/41547/13/Jake_M%20Stolper%20et%20al.%20(2013)%20Science.pdf|url-status=dead}}</ref>

! style="margin; background: lavender;" colspan="3" | '''07 August 2012'''

|-

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=drGX9SVQQRI NASA Video 1] [http://www.youtube.com/watch?v=AAA3ANe8FMs Video 2] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1295 NASA News]

|}



On 17 October 2013, NASA reported, based on analysis of [[argon]] in the [[Atmosphere of Mars|Martian atmosphere]], that certain [[List of Martian meteorites|meteorites]] found on Earth thought to be from Mars are confirmed to be from Mars.<ref name="NASA-20131017">{{cite web |last=Webster |first=Guy |title=NASA Rover Confirms Mars Origin of Some Meteorites |url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1525 |date=17 October 2013 |work=[[NASA]] |access-date=29 October 2013 |archive-url= https://web.archive.org/web/20131115114647/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1525 |archive-date=15 November 2013 |url-status=dead }}</ref>

<br />

[[File:PIA17604-MarsCuriosityRover-ScarpRetreatModel-20131209.png|thumb|left|300px|[[Scarp retreat]] by [[History of Mars observation|windblown sand]] over time on [[Mars]] (Yellowknife Bay, December 9, 2013).]]

On 13 November 2013, NASA announced the names of two features on Mars important to two active [[Mars exploration rovers]] in honor of [[planetary scientist]] [[Bruce C. Murray]] (1931-2013): "Murray Buttes", an entryway the [[Curiosity (rover)|''Curiosity'' rover]] will traverse on its way to [[Aeolis Mons|Mount Sharp]] and "Murray Ridge", an uplifted crater that the [[Opportunity (rover)|Opportunity rover]] is exploring.<ref name="NASA-20131113">{{cite web|last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |title=Mars Rover Teams Dub Sites In Memory of Bruce Murray |url= http://mars.jpl.nasa.gov/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1542 |date=13 November 2013 |work=[[NASA]] |access-date=14 November 2013 }}</ref>



On 25 November 2013, NASA reported that ''Curiosity'' has resumed full science operations, with no apparent loss of capability, after completing the diagnosis of an electrical problem first observed on 17 November. Apparently, an internal short in the rover's power source, the [[Multi-Mission Radioisotope Thermoelectric Generator]], caused an unusual and intermittent decrease in a voltage indicator on the rover.<ref name="NASA-20131120">{{cite web|last=Webster|first=Guy |title=Rover Team Working to Diagnose Electrical Issue|url= http://www.nasa.gov/mission_pages/msl/news/jpl/msl20131120.html |date=20 November 2013|work=[[NASA]] |access-date=21 November 2013 }}</ref><ref name="NASA-20131125">{{cite web|author=Staff |title=Curiosity Resumes Science After Analysis of Voltage Issue|url= http://www.nasa.gov/jpl/msl/mars-rover-curiosity-20131125.html |date=25 November 2013|work=[[NASA]] |access-date=25 November 2013 }}</ref>

[[File:First colored image from Curiosity.jpg|350px]]

<br />



On 27 November 2013, an overview (titled, "[https://www.nytimes.com/2013/11/28/opinion/the-world-of-mars.html The World of Mars]") of current and proposed Mars exploration by [[John Grotzinger]], [[Chief science officer|chief scientist]] of the ''Curiosity'' rover mission, was published in the [[New York Times]].<ref name="NYT-20131127">{{cite news |last=Grotzinger|first=John |author-link=John Grotzinger |title=The World of Mars|url= https://www.nytimes.com/2013/11/28/opinion/the-world-of-mars.html |work=[[New York Times]]|date=26 November 2013 |access-date=27 November 2013 }}</ref>

First Color Image of the Martian Landscape Returned from Curiosity

<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4282 Mars Science Laboratory: Images]</ref>

----



On 9 December 2013, NASA reported that the planet [[Mars]] had a large [[freshwater lake]] (which could have been a hospitable environment for [[microbial life]]) based on evidence from the [[Curiosity (rover)|''Curiosity'' rover]] studying [[Aeolis Palus]] near [[Aeolis Mons|Mount Sharp]] in [[Gale (crater)|Gale Crater]].<ref name="NYT-20131209">{{cite news |last=Chang |first=Kenneth |title=On Mars, an Ancient Lake and Perhaps Life |url= https://www.nytimes.com/2013/12/10/science/space/on-mars-an-ancient-lake-and-perhaps-life.html |date=9 December 2013 |work=[[New York Times]] |access-date=9 December 2013 }}</ref><ref name="SCI-20131209">{{cite journal |author=Various |title=Science - Special Collection - Curiosity Rover on Mars |url= https://www.science.org/action/doSearch?AllField=Curiosity+Mars |date=9 December 2013 |journal=[[Science (journal)|Science]] |access-date=9 December 2013 }}</ref>

====Sol 2====

{{Multiple image|direction=vertical|align=right|width=200|image1=PIA17594-MarsCuriosityRover-JohKleinMudstoneDrillHole-20130510.jpg|image2=PIA17599-MarsCuriosityRover-CumberlandRock-Spectra-20121209.jpg|image3=PIA17598-MarsCuriosityRover-Mudstone-ClayMineralStructure-20131209.jpg|caption1=[[Curiosity rover#Robotic arm|Hole ({{convert|1.6|cm|in|abbr=on}}) drilled]] into "[[List of rocks on Mars#Curiosity|John Klein]]" [[mudstone]].|caption2=[[Sample Analysis at Mars|Spectral Analysis (SAM)]] of "[[List of rocks on Mars#Curiosity|Cumberland]]" [[mudstone]].|caption3=[[Clay minerals|Clay mineral]] structure of [[mudstone]].|footer=The [[Curiosity (rover)|''Curiosity'' rover]] examines [[mudstone]] near Yellowknife Bay on [[Mars]] (May 2013).}}

On 9 December 2013, NASA researchers described, in a series of six articles in the journal [[Science (journal)|Science]], many new discoveries from the ''Curiosity'' rover. Possible organics were found that could not be explained by contamination.<ref name="SCI-2013-Blake">

{{cite journal |date=2013 |title=Curiosity at Gale crater, Mars: characterization and analysis of the Rocknest sand shadow |journal=[[Science (journal)|Science]] |volume=341 |issue=6153 |pages=1239505 |doi=10.1126/science.1239505 |display-authors=1 |last1=Blake |first1=D. F. |last2=Morris |first2=R. V. |last3=Kocurek |first3=G. |last4=Morrison |first4=S. M. |last5=Downs |first5=R. T. |last6=Bish |first6=D. |last7=Ming |first7=D. W. |last8=Edgett |first8=K. S. |last9=Rubin |first9=D. |last10=Goetz |first10=W. |last11=Madsen |first11=M. B. |last12=Sullivan |first12=R. |last13=Gellert |first13=R. |last14=Campbell |first14=I. |last15=Treiman |first15=A. H. |last16=McLennan |first16=S. M. |last17=Yen |first17=A. S. |last18=Grotzinger |first18=J. |last19=Vaniman |first19=D. T. |last20=Chipera |first20=S. J. |last21=Achilles |first21=C. N. |last22=Rampe |first22=E. B. |last23=Sumner |first23=D. |last24=Meslin |first24=P.- Y. |last25=Maurice |first25=S. |last26=Forni |first26=O. |last27=Gasnault |first27=O. |last28=Fisk |first28=M. |last29=Schmidt |first29=M. |last30=Mahaffy |first30=P. |pmid=24072928|bibcode=2013Sci...341E...5B |s2cid=14060123 |url= https://authors.library.caltech.edu/41551/7/Blake.SM.pdf }}</ref><ref name="SCI-2013-Leshin">

{{cite journal |date=2013 |title=Volatile, isotope, and organic analysis of Martian fines with the Mars Curiosity rover |journal=[[Science (journal)|Science]]|volume=341 |issue=6153 |pages=1238937 |doi=10.1126/science.1238937 |display-authors=1 |last1=Leshin |first1=L. A. |last2=Mahaffy |first2=P. R. |last3=Webster |first3=C. R. |last4=Cabane |first4=M. |last5=Coll |first5=P. |last6=Conrad |first6=P. G. |last7=Archer |first7=P. D. |last8=Atreya |first8=S. K. |last9=Brunner |first9=A. E. |last10=Buch |first10=A. |last11=Eigenbrode |first11=J. L. |last12=Flesch |first12=G. J. |last13=Franz |first13=H. B. |last14=Freissinet |first14=C. |last15=Glavin |first15=D. P. |last16=McAdam |first16=A. C. |last17=Miller |first17=K. E. |last18=Ming |first18=D. W. |last19=Morris |first19=R. V. |last20=Navarro-Gonzalez |first20=R. |last21=Niles |first21=P. B. |last22=Owen |first22=T. |last23=Pepin |first23=R. O. |last24=Squyres |first24=S. |last25=Steele |first25=A. |last26=Stern |first26=J. C. |last27=Summons |first27=R. E. |last28=Sumner |first28=D. Y. |last29=Sutter |first29=B. |last30=Szopa |first30=C. |pmid=24072926|bibcode=2013Sci...341E...3L |citeseerx=10.1.1.397.4959 |s2cid=206549244 }}</ref> Although the organic carbon was probably from Mars, it can all be explained by dust and meteorites that have landed on the planet.<ref name="SCI-2013-McLennan">

{{cite journal |date=2013 |title=Elemental geochemistry of sedimentary rocks at Yellowknife Bay, Gale Crater, Mars |journal=[[Science (journal)|Science]] |volume=343 |issue=6169 |pages=1244734 |doi=10.1126/science.1244734 |display-authors=1 |last1=McLennan |first1=S. M. |last2=Anderson |first2=R. B. |last3=Bell |first3=J. F. |last4=Bridges |first4=J. C. |last5=Calef |first5=F. |last6=Campbell |first6=J. L. |last7=Clark |first7=B. C. |last8=Clegg |first8=S. |last9=Conrad |first9=P. |last10=Cousin |first10=A. |last11=Des Marais |first11=D. J. |last12=Dromart |first12=G. |last13=Dyar |first13=M. D. |last14=Edgar |first14=L. A. |last15=Ehlmann |first15=B. L. |last16=Fabre |first16=C. |last17=Forni |first17=O. |last18=Gasnault |first18=O. |last19=Gellert |first19=R. |last20=Gordon |first20=S. |last21=Grant |first21=J. A. |last22=Grotzinger |first22=J. P. |last23=Gupta |first23=S. |last24=Herkenhoff |first24=K. E. |last25=Hurowitz |first25=J. A. |last26=King |first26=P. L. |last27=Le Mouelic |first27=S. |last28=Leshin |first28=L. A. |last29=Leveille |first29=R. |last30=Lewis |first30=K. W. |pmid=24324274|bibcode=2014Sci...343C.386M |hdl=2381/42019 |s2cid=36866122 |url= https://authors.library.caltech.edu/42646/1/McLennan_etal_Science_ms124473_Accepted.pdf |hdl-access=free }}</ref><ref name="SCI-1996-Flynn">

{{cite journal |date=1996 |title=The delivery of organic matter from asteroids and comets to the early surface of Mars |journal=Earth Moon Planets |volume=72|issue=1–3 |pages=469–474 |doi=10.1007/BF00117551 |pmid=11539472 |bibcode=1996EM&P...72..469F|last1=Flynn |first1=George J. |s2cid=189901503 }}</ref><ref name="PNAS-2000-Benner">{{cite journal |date=2000 |title=The missing organic molecules on Mars |journal=Proc. Natl. Acad. Sci. U.S.A. |volume=97 |issue=6 |pages=2425–2430 |doi=10.1073/pnas.040539497 |pmid=10706606 |pmc=15945|last1=Benner |first1=S. A. |last2=Devine |first2=K. G. |last3=Matveeva |first3=L. N. |last4=Powell |first4=D. H. |bibcode=2000PNAS...97.2425B|doi-access=free }}</ref> Because much of the carbon was released at a relatively low temperature in ''Curiosity''{{'s}} [[Sample Analysis at Mars]] (SAM) instrument package, it probably did not come from carbonates in the sample. The carbon could be from organisms, but this has not been proven. This organic-bearing material was obtained by drilling 5 centimeters deep in a site called ''Yellowknife Bay'' into a rock called "''[[List of rocks on Mars#Curiosity|Sheepbed mudstone]]''". The samples were named ''[[List of rocks on Mars#Curiosity|John Klein]]'' and ''[[List of rocks on Mars#Curiosity|Cumberland]]''. Microbes could be living on Mars by obtaining energy from chemical imbalances between minerals in a process called [[chemolithotrophy]] which means "eating rock."<ref name="SCI-2013-Grotzinger">

{{cite journal |date=2013 |title=A Habitable Fluvio-Lacustrine Environment at Yellowknife Bay, Gale Crater, Mars |journal=[[Science (journal)|Science]] |volume=343 |issue=6169 |pages=1242777 |doi=10.1126/science.1242777 |display-authors=1 |last1=Grotzinger |first1=J. P. |last2=Sumner |first2=D. Y. |last3=Kah |first3=L. C. |last4=Stack |first4=K. |last5=Gupta |first5=S. |last6=Edgar |first6=L. |last7=Rubin |first7=D. |last8=Lewis |first8=K. |last9=Schieber |first9=J. |last10=Mangold |first10=N. |last11=Milliken |first11=R. |last12=Conrad |first12=P. G. |last13=Desmarais |first13=D. |last14=Farmer |first14=J. |last15=Siebach |first15=K. |last16=Calef |first16=F. |last17=Hurowitz |first17=J. |last18=McLennan |first18=S. M. |last19=Ming |first19=D. |last20=Vaniman |first20=D. |last21=Crisp |first21=J. |last22=Vasavada |first22=A. |last23=Edgett |first23=K. S. |last24=Malin |first24=M. |last25=Blake |first25=D. |last26=Gellert |first26=R. |last27=Mahaffy |first27=P. |last28=Wiens |first28=R. C. |last29=Maurice |first29=S. |last30=Grant |first30=J. A. |bibcode=2014Sci...343A.386G |pmid=24324272|citeseerx=10.1.1.455.3973 |s2cid=52836398 }}</ref> However, in this process only a very tiny amount of carbon is involved — much less than was found at ''Yellowknife Bay''.<ref name="SCI-2013-Kerr">

{{cite journal|author=Kerr, R. |date=2013 |title=New Results Send Mars Rover on a Quest for Ancient Life |journal=[[Science (journal)|Science]] |volume=342 |number=6164 |pages=1300–1301 |doi=10.1126/science.342.6164.1300 |pmid=24337267|bibcode=2013Sci...342.1300K }}</ref><ref name="SCI-2013-Ming">

{{cite journal |date=2013 |title=Volatile and Organic Compositions of Sedimentary Rocks in Yellowknife Bay, Gale Crater, Mars |journal=[[Science (journal)|Science]]

|volume=343 |issue=6169 |pages=1245267 |doi=10.1126/science.1245267 |last2=Archer |first2=P. D. Jr. |display-authors=1 |last1=Ming |first1=D. W. |last3=Glavin |first3=D. P. |last4=Eigenbrode |first4=J. L. |last5=Franz |first5=H. B. |last6=Sutter |first6=B. |last7=Brunner |first7=A. E. |last8=Stern |first8=J. C. |last9=Freissinet |first9=C. |last10=McAdam |first10=A. C. |last11=Mahaffy |first11=P. R. |last12=Cabane |first12=M. |last13=Coll |first13=P. |last14=Campbell |first14=J. L. |last15=Atreya |first15=S. K. |last16=Niles |first16=P. B. |last17=Bell |first17=J. F. |last18=Bish |first18=D. L. |last19=Brinckerhoff |first19=W. B. |last20=Buch |first20=A. |last21=Conrad |first21=P. G. |last22=Des Marais |first22=D. J. |last23=Ehlmann |first23=B. L. |last24=Fairen |first24=A. G. |last25=Farley |first25=K. |last26=Flesch |first26=G. J. |last27=Francois |first27=P. |last28=Gellert |first28=R. |last29=Grant |first29=J. A. |last30=Grotzinger |first30=J. P. |pmid=24324276|bibcode=2014Sci...343E.386M |s2cid=10753737 |url= https://authors.library.caltech.edu/42647/1/Ming_et%20al_2013_Science_Sheepbed%20Volatiles_Accepted.pdf }}</ref>



Using SAM's [[mass spectrometer]], scientists measured [[isotopes]] of [[helium]], [[neon]], and [[argon]] that [[cosmic rays]] produce as they go through rock. The fewer of these isotopes they find, the more recently the rock has been exposed near the surface. The 4-billion-year-old lakebed rock drilled by ''Curiosity'' was uncovered between 30 million and 110 million years ago by winds which sandblasted away 2 meters of overlying rock. Next, they hope to find a site tens of millions of years younger by drilling close to an overhanging outcrop.<ref name="SCI-2013-Farley">{{cite journal |date=2013 |title=In Situ Radiometric and Exposure Age Dating of the Martian Surface |journal=[[Science (journal)|Science]]|volume=343 |issue=6169 |pages=1247166 |doi=10.1126/science.1247166 |display-authors=1 |last1=Farley |first1=K. A. |last2=Malespin |first2=C. |last3=Mahaffy |first3=P. |last4=Grotzinger |first4=J. P. |last5=Vasconcelos |first5=P. M. |last6=Milliken |first6=R. E. |last7=Malin |first7=M. |last8=Edgett |first8=K. S. |last9=Pavlov |first9=A. A. |last10=Hurowitz |first10=J. A. |last11=Grant |first11=J. A. |last12=Miller |first12=H. B. |last13=Arvidson |first13=R. |last14=Beegle |first14=L. |last15=Calef |first15=F. |last16=Conrad |first16=P. G. |last17=Dietrich |first17=W. E. |last18=Eigenbrode |first18=J. |last19=Gellert |first19=R. |last20=Gupta |first20=S. |last21=Hamilton |first21=V. |last22=Hassler |first22=D. M. |last23=Lewis |first23=K. W. |last24=McLennan |first24=S. M. |last25=Ming |first25=D. |last26=Navarro-Gonzalez |first26=R. |last27=Schwenzer |first27=S. P. |last28=Steele |first28=A. |last29=Stolper |first29=E. M. |last30=Sumner |first30=D. Y. |pmid=24324273|bibcode=2014Sci...343F.386H |s2cid=3207080 |doi-access=free }}</ref>

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''08 August 2012'''

|-

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=m5YtXtp5WAc NASA Video] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1298 NASA News]

|}



The absorbed dose and dose equivalent from galactic cosmic rays and [[solar energetic particle]]s on the Martian surface for ~300 days of observations during the current solar maximum was measured. These measurements are necessary for human missions to the surface of Mars, to provide microbial survival times of any possible extant or past life, and to determine how long potential organic [[biosignature]]s can be preserved. This study estimates that a 1-meter depth drill is necessary to access possible viable [[radioresistant]] microbe cells. The actual absorbed dose measured by the [[Radiation assessment detector|Radiation Assessment Detector]] (RAD) is 76 mGy/yr at the surface. Based on these measurements, for a round trip Mars surface mission with 180 days (each way) cruise, and 500 days on the Martian surface for this current solar cycle, an astronaut would be exposed to a total mission dose equivalent of ~1.01 [[sievert]]. Exposure to 1 sievert is associated with a 5 percent increase in risk for developing fatal cancer. NASA's current lifetime limit for increased risk for its astronauts operating in low-Earth orbit is 3 percent.<ref name="SREF-20131209">{{cite web |author=Staff |title=Understanding Mars' Past and Current Environments |url=http://spaceref.com/mars/understanding-mars-past-and-current-environments.html |date=9 December 2013 |work=[[NASA]] |access-date=20 December 2013 }}{{Dead link|date=July 2023 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> Maximum shielding from galactic cosmic rays can be obtained with about 3 meters of [[Martian soil]].<ref name="SCI-2013-Hassler">{{cite journal|date=2013 |title=Mars' Surface Radiation Environment Measured with the Mars Science Laboratory's Curiosity Rover|journal=[[Science (journal)|Science]]|volume=343 |issue=6169 |pages=1244797 |doi=10.1126/science.1244797 |display-authors=1 |last1=Hassler |first1=D. M. |last2=Zeitlin |first2=Cary |last3=Wimmer-Schweingruber |first3=R. F. |last4=Ehresmann |first4=B. |last5=Rafkin |first5=S. |last6=Eigenbrode |first6=J. L. |last7=Brinza |first7=D. E. |last8=Weigle |first8=G. |last9=Bottcher |first9=S. |last10=Bohm |first10=E. |last11=Burmeister |first11=S. |last12=Guo |first12=J. |last13=Kohler |first13=J. |last14=Martin |first14=C. |last15=Reitz |first15=G. |last16=Cucinotta |first16=F. A. |last17=Kim |first17=M.-H. |last18=Grinspoon |first18=D. |last19=Bullock |first19=M. A. |last20=Posner |first20=A. |last21=Gomez-Elvira |first21=J. |last22=Vasavada |first22=A. |last23=Grotzinger |first23=J. P. |last24=MSL Science Team |pmid=24324275|bibcode=2014Sci...343D.386H |url= https://authors.library.caltech.edu/42648/1/RAD_Surface_Results_paper_SCIENCE_12nov13_FINAL.pdf|hdl=1874/309142|s2cid=33661472}}</ref>

<br />



The samples examined were probably once mud that for millions to tens of millions of years could have hosted living organisms. This wet environment had neutral [[pH]], low [[salinity]], and variable [[redox]] states of both [[iron]] and [[sulfur]] species.<ref name="SCI-2013-McLennan" /><ref name="SCI-2013-Vaniman">

{| class="wikitable"

{{cite journal |date=2013 |title=Mineralogy of a mudstone at Yellowknife Bay, Gale crater, Mars |journal=[[Science (journal)|Science]] |volume=343 |issue=6169 |pages=1243480 |doi=10.1126/science.1243480 |display-authors=1 |last1=Vaniman |first1=D. T. |last2=Bish |first2=D. L. |last3=Ming |first3=D. W. |last4=Bristow |first4=T. F. |last5=Morris |first5=R. V. |last6=Blake |first6=D. F. |last7=Chipera |first7=S. J. |last8=Morrison |first8=S. M. |last9=Treiman |first9=A. H. |last10=Rampe |first10=E. B. |last11=Rice |first11=M. |last12=Achilles |first12=C. N. |last13=Grotzinger |first13=J. P. |last14=McLennan |first14=S. M. |last15=Williams |first15=J. |last16=Bell |first16=J. F. |last17=Newsom |first17=H. E. |last18=Downs |first18=R. T. |last19=Maurice |first19=S. |last20=Sarrazin |first20=P. |last21=Yen |first21=A. S. |last22=Morookian |first22=J. M. |last23=Farmer |first23=J. D. |last24=Stack |first24=K. |last25=Milliken |first25=R. E. |last26=Ehlmann |first26=B. L. |last27=Sumner |first27=D. Y. |last28=Berger |first28=G. |last29=Crisp |first29=J. A. |last30=Hurowitz |first30=J. A. |pmid=24324271|bibcode=2014Sci...343B.386V |s2cid=9699964 |url= https://authors.library.caltech.edu/42649/7/Vaniman1243480s%20Supplemental%20material%20revised%20Nov%20final.pdf }}</ref><ref name="SCI-2006-Bibring">

|-

{{cite journal |date=2006 |title=Global mineralogical and aqueous mars history derived from OMEGA/Mars Express data. |journal=[[Science (journal)|Science]] |volume=312|issue=5772 |pages=400–404 |doi=10.1126/science.1122659 |pmid=16627738 |display-authors=1 |last1=Bibring |first1=J. P. |last2=Langevin |first2=Yves |last3=Mustard |first3=J. F. |last4=Poulet |first4=F |last5=Arvidson |first5=R |last6=Gendrin |first6=A |last7=Gondet |first7=B |last8=Mangold |first8=N |last9=Pinet |first9=P |last10=Forget |first10=F |last11=Berthé |first11=M |last12=Bibring |first12=J. P. |last13=Gendrin |first13=A |last14=Gomez |first14=C |last15=Gondet |first15=B |last16=Jouglet |first16=D |last17=Poulet |first17=F |last18=Soufflot |first18=A |last19=Vincendon |first19=M |last20=Combes |first20=M |last21=Drossart |first21=P |last22=Encrenaz |first22=T |last23=Fouchet |first23=T |last24=Merchiorri |first24=R |last25=Belluci |first25=G |last26=Altieri |first26=F |last27=Formisano |first27=V |last28=Capaccioni |first28=F |last29=Cerroni |first29=P |last30=Coradini |first30=A |bibcode=2006Sci...312..400B |doi-access=free }}</ref><ref name="SCI-LET-2005-Squyres">

! style="text-align: center; background: #aabccc;"|Date

{{cite journal |date=2005 |title=Sedimentary rocks and Meridiani Planum: Origin, diagenesis, and implications for life of Mars. Earth Planet |journal=Sci. Lett. |volume=240 |pages=1–10|doi=10.1016/j.epsl.2005.09.038 |bibcode=2005E&PSL.240....1S|last1=Squyres |first1=Steven W. |last2=Knoll |first2=Andrew H. |issue=1 }}</ref> These types of iron and sulfur could have been used by living organisms.<ref name="PHIL-1999-Nealson">{{cite journal |author=Nealson, K. |author2=P. Conrad. |date=1999 |title=Life: past, present and future. |journal=Phil. Trans. R. Soc. Lond. B |volume=354 |issue=1392 |pages=1923–1939 |doi=10.1098/rstb.1999.0532 |pmid=10670014 |pmc=1692713 }}</ref> [[Carbon|C]], [[Hydrogen|H]], [[Oxygen|O]], [[Sulfur|S]], [[Nitrogen|N]], and [[Phosphorus|P]] were measured directly as key biogenic elements, and by inference, P is assumed to have been there as well.<ref name="SCI-2013-Grotzinger" /><ref name="SCI-2013-Ming" /> The two samples, ''[[List of rocks on Mars#Curiosity|John Klein]]'' and ''[[List of rocks on Mars#Curiosity|Cumberland]]'', contain basaltic minerals, Ca-sulfates, Fe oxide/hydroxides, Fe-sulfides, amorphous material, and trioctahedral [[smectite]]s (a type of clay). Basaltic minerals in the [[mudstone]] are similar to those in nearby [[aeolian processes|aeolian]] deposits. However, the mudstone has far less Fe-[[forsterite]] plus [[magnetite]], so Fe-forsterite (type of [[olivine]]) was probably altered to form smectite (a type of clay) and [[magnetite]].<ref name="GEO-1994-Keller">

! style="text-align: center; background: #aabccc;"|Event

{{cite journal |date=1994 |title=Aqueous alteration of the Bali CV3 chondrite: Evidence from mineralogy, mineral chemistry, and oxygen isotopic compositions. |journal=Geochim. Cosmochim. Acta|volume=58 |issue=24 |pages=5589–5598 |doi=10.1016/0016-7037(94)90252-6 |bibcode=1994GeCoA..58.5589K |pmid=11539152 |display-authors=1 |last1=Keller |first1=Lindsay P. |last2=Thomas |first2=Kathie L. |last3=Clayton |first3=Robert N. |last4=Mayeda |first4=Toshiko K. |last5=Dehart |first5=John M. |last6=McKay |first6=David S. }}</ref> A Late [[Noachian]]/Early [[Hesperian]] or younger age indicates that clay mineral formation on Mars extended beyond Noachian time; therefore, in this location neutral pH lasted longer than previously thought.<ref name="SCI-2013-Vaniman" />

! style="text-align: center; background: #aabccc;"|Notes

|-

| August 8, 2012 || Scheduled software upgrade. || Mission Control spent parts of the next days upgrading the rover's dual computers by switching the entry-descent-landing software to the surface operation software;<ref>[http://science.time.com/2012/08/09/the-curiosity-rover-preps-for-big-plans-after-its-daring-decent/?iid=sci-main-lede?xid=gonewsedit The Curiosity Rover Preps for Big Plans After its Daring Descent] ''Time''. August 9, 2012</ref> the switchover was completed by August 15.<ref>[http://www.msnbc.msn.com/id/48668419/ns/technology_and_science-space/ M. Wall - Mars rover survives 'brain transplant' with flying colors - NBC]</ref>

|-

|}



On 20 December 2013, NASA reported that ''Curiosity'' has successfully upgraded, for the third time since [[Bradbury Landing|landing]], its software programs and is now operating with version 11. The new software is expected to provide the rover with better [[Curiosity (rover)#Robotic arm|robotic arm]] and [[Autonomous Navigation System|autonomous driving]] abilities. Due to wheel wear, a concern to drive more carefully over the rough terrain the rover is currently traveling on to [[Aeolis Mons|Mount Sharp]], was also reported.<ref name="NASA-20131220a">{{cite web |last=Webster |first=Guy |title=Curiosity Team Upgrades Software, Checks Wheel Wear - Mars Science Laboratory Mission Status Report|url= http://www.jpl.nasa.gov/news/news.php?release=2013-374 |date=20 December 2013 |work=[[NASA]]|access-date=23 December 2013 }}</ref>

<br />



===Search for ancient life===

[[File:PIA16011.jpg|770px]]

On 24 January 2014, NASA reported that current studies by the ''Curiosity'' and [[Opportunity (rover)|''Opportunity'']] [[Mars rover|rovers]] will now be searching for evidence of ancient life, including a [[biosphere]] based on [[autotroph]]ic, [[chemotroph]]ic and/or [[Lithotroph#Chemolithotrophs|chemolithoautotrophic]] [[microorganism]]s, as well as ancient water, including [[Lacustrine plain|fluvio-lacustrine environments]] ([[plain]]s related to ancient [[river]]s or [[lake]]s) that may have been [[Planetary habitability|habitable]].<ref name="SCI-20140124a">

<br />

{{cite journal |last=Grotzinger |first=John P.|title=Introduction to Special Issue - Habitability, Taphonomy, and the Search for Organic Carbon on Mars|journal=[[Science (journal)|Science]] |date=24 January 2014 |volume=343 |issue=6169<!---|number=6169---> |pages=386–387 |doi=10.1126/science.1249944 |bibcode=2014Sci...343..386G |pmid=24458635|doi-access=free }}</ref><ref name="SCI-20140124special">

{{cite journal |author=Various |title=Special Issue - Table of Contents - Exploring Martian Habitability |url= https://www.science.org/toc/science/343/6169|date=24 January 2014|journal=[[Science (journal)|Science]] |volume=343 |number=6169 |pages=345–452|access-date=24 January 2014 }}</ref><ref name="SCI-20140124">{{cite journal |author=Various |title=Special Collection - Curiosity - Exploring Martian Habitability|url= https://www.science.org/action/doSearch?AllField=Curiosity+Mars|date=24 January 2014 |journal=[[Science (journal)|Science]] |access-date=24 January 2014 }}</ref><ref name="SCI-2013-Grotzinger" /> The search for evidence of [[Planetary habitability|habitability]], [[taphonomy]] (related to [[fossils]]), and [[organic carbon]] on the planet [[Mars]] is now a primary [[NASA]] objective.<ref name="SCI-20140124a" />



===Arrival at Mount Sharp===

This is the first 360-degree panoramic view from NASA's Curiosity rover, taken with the Navigation cameras.<ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=NLA_397682534EDR_F0020000AUT_04096M_&s=2 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=NLA_397673010EDR_F0010008AUT_04096M_&s=2 Mars Science Laboratory: Raw Images]</ref>

{{see also|Mount Sharp#Curiosity mission}}

On 11 September 2014 (Sol 746), ''Curiosity'' reached the slopes of [[Aeolis Mons]] (or [[Mount Sharp (Mars)|Mount Sharp]]), the rover mission's long-term prime destination<ref name="NASA-20140911">{{cite web |last1=Webster |first1=Guy |last2=Agle |first2=DC |last3=Brown |first3=Dwayne |title=NASA's Mars Curiosity Rover Arrives at Martian Mountain |url= http://www.jpl.nasa.gov/news/news.php?release=2014-307 |date=11 September 2014 |work=[[NASA]] |access-date=10 September 2014 }}</ref><ref name="NYT-20140911">{{cite news |last=Chang |first=Kenneth |title=After a Two-Year Trek, NASA's Mars Rover Reaches Its Mountain Lab |url= https://www.nytimes.com/2014/09/12/science/space/after-a-two-year-trek-nasa-mars-rover-reaches-its-mountain-lab.html |date=11 September 2014 |work=[[New York Times]] |access-date=12 September 2014 }}</ref> and where the rover is expected to learn more about the [[Geological history of Mars|history of Mars]].<ref name="NASA-20130806">{{cite web |last=Webster |first=Guy |title=Mars Curiosity Landing: Relive the Excitement |url= http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1503 |date=6 August 2013 |work=[[NASA]] |access-date=7 August 2013 |archive-url= https://web.archive.org/web/20130911053938/http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1503 |archive-date=11 September 2013 |url-status=dead }}</ref> ''Curiosity'' had traveled an estimated linear distance of {{convert|6.9|km|mi|abbr=on}}<ref name="NASA-20130827a" /> to the mountain slopes since leaving its "''start''" point in Yellowknife Bay on 4 July 2013.<ref name="NASA-20130827a" />

<gallery>

Image:PIA16064-Mars Curiosity Rover Treasure Map.jpg|Overview map - blue oval marks "Base of [[Aeolis Mons|Mount Sharp]]" (August 17, 2012).

Image:MarsCuriosityRover-TraverseMap-Sol-0746-20140911.jpg|Traverse map - route from [[Bradbury Landing|Landing]] to slopes on [[Mount Sharp (Mars)|Mount Sharp]] (September 11, 2014).

Image:PIA18475-MarsCuriosityRover--HIRISE-TraverseMap-PahrumpHills-20140911.jpg|Close-up map - new route (yellow) - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:PIA18780-MarsCuriosityRover-HIRISE-PlannedRouteMap-PahrumpHills-MountSharp-20140911.jpg|Close-up map - new route (yellow) - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:PIA18474-MarsCuriosityRover-GaleCrater-TopographicMap-PahrumpHills-20140911.jpg|Close-up map - [[Mount Sharp (Mars)|Mount Sharp]] slopes - with few craters (bottom) (September 11, 2014).

Image:PIA18785-MarsCuriosityRover-HIRISE-MurrayRidge-Transition-20140911.jpg|Geology map - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:PIA18781-MarsCuriosityRover-GeologyMap-LowerMountSharp-20140911.jpg|Geology map - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:PIA17587-MarsCuriosityRover-MurrayButtes-20131113.jpg|"Murray Buttes" knobs - [[Aeolis Mons|Mount Sharp]] slopes (November 13, 2013).<ref name="NASA-20131113" />

Image:PIA18783-MarsCuriosityRover-HIRISE-MurrayButtesMesa-20140911.jpg|"Murray Buttes" mesa - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:PIA18784-MarsCuriosityRover-HIRISE-MurrayRidgeFormation-20140911.jpg|"Murray Formation" bands - [[Mount Sharp (Mars)|Mount Sharp]] slopes (September 11, 2014).

Image:Pia19039 some key places in a survey of the "Pahrump Hills" .jpg|"Pahrump Hills" - Notable places at base of [[Mount Sharp]] (Autumn, 2014).

Image:PIA18883-MarsCuriosityRover-PahrumpHills-Sand-20141113.jpg|"Pahrump Hills" [[Martian soil|sand]] - viewed by ''Curiosity'' (November 13, 2014).

Image:PIA18882-MarsCuriosityRover-PahrumpHillsSand-WheelTrack-20141107.tif|"Pahrump Hills" [[Martian soil|sand]] - ''Curiosity''{{'s}} tracks (November 7, 2014).

Image:PIA18610-MarsCuriosityRover-PahrumpHillsOutcrop-Mahli-Sol758-20140923.jpg|"[[List of rocks on Mars#Curiosity|Pahrump Hills]]" [[rock outcrop]] on Mars – viewed by [[Curiosity (rover)|''Curiosity'']] (September 23, 2014).

Image:PIA18609 - First Sampling Hole in Mount Sharp .jpg|"[[List of rocks on Mars#Curiosity|Confidence Hills]]" rock on Mars - [[Curiosity (rover)|''Curiosity''{{'s}}]] 1st target at [[Mount Sharp]] (September 24, 2014).

Image:PIA18881-MarsCuriosityRover-PahrumpHillsBedrock-20141109.tif|"Pahrump Hills" [[bedrock]] on Mars - viewed by ''Curiosity'' (November 9, 2014).

Image:PIA18880-MarsCuriosityRover-PinkCliffs-20141007.jpg|"Pink Cliffs" [[rock outcrop]] on Mars - viewed by ''Curiosity'' (October 7, 2014).

Image:PIA19066-MarsCuriosityRover-AlexanderHillsRock-20141123-Fig1.jpg|"Alexander Hills" [[bedrock]] on Mars - viewed by ''Curiosity'' (November 23, 2014).

Image:PIA19080-MarsRoverCuriosity-AncientGaleLake-Simulated-20141208.jpg|Ancient Lake fills Gale Crater on Mars (simulated view).

</gallery>



{{wide image|PIA18782-MarsCuriosityRover-GeologyMap-LowerMountSharp-20140911.png|800px|align-cap=center|Geology map - from the crater floor in [[Aeolis Palus]] up the Slopes of [[Mount Sharp (Mars)|Mount Sharp]]<br />(11 September 2014).}}

<br />

{{wide image|PIA19840-MarsCuriosityRover-HiddenValley-Sol703-Rel20151008.jpg|800px|align-cap=center|Rocks in "Hidden Valley" near the "Pahrump Hills" on the slopes of [[Aeolis Mons|Mount Sharp]] as viewed from the [[Curiosity (rover)|''Curiosity'' Rover]]<br />(11 September 2014; [[Color balance|white balanced]]).}}



===Detection of organics===

[[File:NLA 397682534EDR F0020000AUT 04096M.JPG|385px]] [[File:NLA 397673010EDR F0010008AUT 04096M.JPG|385px]]

{{See also|Atmosphere of Mars#Methane}}

<br />

On 16 December 2014, NASA reported the ''Curiosity'' rover detected a "tenfold spike", likely localized, in the amount of [[methane]] in the [[Atmosphere of Mars|Martian atmosphere]]. Sample measurements taken "a dozen times over 20 months" showed increases in late 2013 and early 2014, averaging "7 parts of methane per billion in the atmosphere." Before and after that, readings averaged around one-tenth that level.<ref name="NASA-20141216-GW">{{cite web |last1=Webster |first1=Guy |last2=Neal-Jones |first2=Nancy |last3=Brown |first3=Dwayne |title=NASA Rover Finds Active and Ancient Organic Chemistry on Mars |url= http://www.jpl.nasa.gov/news/news.php?release=2014-432 |date=16 December 2014 |work=[[NASA]] |access-date=16 December 2014 }}</ref><ref name="NYT-20141216-KC">{{cite news |last=Chang |first=Kenneth |title='A Great Moment': Rover Finds Clue That Mars May Harbor Life |url= https://www.nytimes.com/2014/12/17/science/a-new-clue-in-the-search-for-life-on-mars.html |date=16 December 2014 |work=[[New York Times]] |access-date=16 December 2014 }}</ref>

<!---{{wide image|PIA19087-MarsCuriosityRover-GaleCrater-MethaneChart-20141216.png|600px|align-cap=center|[[Methane]] measurements in the [[Atmosphere of Mars|atmosphere]] of [[Mars]]<br />([[Curiosity (rover)|''Curiosity'' rover]]; August 2012 to September 2014).}}--->

{{multiple image

| align = center

| direction = horizontal

| image1 = PIA19091-MarsCuriosityRover-OrganicsDetected-CumberlandRockPowder-20141216.png

| width1 = 250

| alt1 =

| caption1 = Detecting organics on Mars is a challenge.

| image2 = PIA19087-MarsCuriosityRover-GaleCrater-MethaneChart-20141216.png

| width2 = 250

| alt2 =

| caption2 = [[Methane]] measurements in the [[Atmosphere of Mars|atmosphere]] of [[Mars]] by the [[Curiosity (rover)|''Curiosity'' rover]] (August 2012 to September 2014).

| image3 = PIA19088-MarsCuriosityRover-MethaneSource-20141216.png

| width3 = 250

| alt3 =

| caption3 = [[Atmosphere of Mars#Methane|Methane]] (CH<sub>4</sub>) on Mars - potential sources and sinks.

}}



In addition, high levels of [[Organic compound|organic chemicals]], particularly [[chlorobenzene]], were detected in powder drilled from one of the rocks, named "[[List of rocks on Mars|Cumberland]]", analyzed by the Curiosity rover.<ref name="NASA-20141216-GW" /><ref name="NYT-20141216-KC" />

This is the first image taken by the Navigation cameras on NASA's Curiosity rover. It shows the shadow of the rover's now-upright mast in the center, and the arm's shadow at left. The arm itself can be seen in the foreground.

{{multiple image

<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4348 Mars Science Laboratory: Images]</ref>

| align = center

| direction = horizontal

| image1 = PIA19090-MarsCuriosityRover-CumberlandRockAnalysis-20141216.png

| width1 = 250

| alt1 =

| caption1 = Comparison of [[Organic compound|Organics]] in [[List of rocks on Mars|Martian rocks]] - [[Chlorobenzene]] levels were much higher in the "[[List of rocks on Mars|Cumberland]]" rock sample.

| image2 = PIA19089-MarsCuriosityRover-CumberlandRockAnalysis-Organics-20141216.png

| width2 = 250

| alt2 =

| caption2 = Detection of [[Organic compound|Organics]] in the "[[List of rocks on Mars|Cumberland]]" rock sample.

| image3 = PIA17599-MarsCuriosityRover-CumberlandRock-Spectra-20121209.jpg

| width3 = 250

| alt3 =

| caption3 = Spectral Analysis (SAM) of [[List of rocks on Mars#Curiosity|"Cumberland" rock]].

}}



===Other 2014 events===

<br />

On 6 February 2014, the ''Curiosity'' rover, in order to reduce wear on its [[:Commons:Category:Curiosity rover wheels|wheels]] by avoiding rougher terrain,<ref name="NASA-20140129">{{cite web |last=Webster |first=Guy |title=Mars Science Laboratory Mission Status Report |url= http://www.jpl.nasa.gov/news/news.php?release=2014-028 |date=29 January 2014 |work=[[NASA]] |access-date=8 February 2014 }}</ref> successfully crossed ([[:File:MarsCuriosityRover-TracksAfterCrossing-DingoGapSandDune-20140206.jpg|image]]) the "[[:File:PIA17931 Martian Valley May Be Curiosity's Route, Figure 1.jpg|Dingo Gap]]" [[sand dune]] and is now expected to travel a smoother route to [[Aeolis Mons|Mount Sharp]].<ref name="NASA-20140206">{{cite web |last=Webster |first=Guy |title=Through the Gap: Curiosity Mars Rover Crosses Dune |url= http://www.jpl.nasa.gov/news/news.php?release=2014-035 |date=6 February 2014 |work=[[NASA]] |access-date=8 February 2014 }}</ref>

{{multiple image

| align = center

| direction = horizontal

| image1 = PIA17751-MarsCuriosityRover-DentedWheelAfter3Miles-20131130.jpg

| width1 = 300

| alt1 =

| caption1 = NOV-2013 - [[Curiosity (rover)|''Curiosity'']]{{'s}} wheel - dents & holes - 3 miles on Mars (30 November 2013).

| image2 = MarsCuriosityRover-WornWheel-20140218.jpg

| width2 = 300

| alt2 =

| caption2 = FEB-2014 - [[Curiosity (rover)|''Curiosity'']]{{'s}} wheel - dents & holes - 3 miles on Mars (18 February 2014).

}}

On 19 May 2014, scientists announced that numerous [[microbes]], like ''[[Tersicoccus phoenicis]]'', may be resistant to methods usually used in [[Cleanroom|spacecraft assembly clean rooms]]. It's not currently known if such [[Extremophile|resistant microbes]] could have withstood [[Interplanetary spaceflight|space travel]] and are present on the ''Curiosity'' rover now on Mars.<ref name="NAT-20140519">{{cite journal |last=Madhusoodanan |first=Jyoti |title=Microbial stowaways to Mars identified |url= http://www.nature.com/news/microbial-stowaways-to-mars-identified-1.15249 |date=19 May 2014 |journal=[[Nature (journal)|Nature]] |doi=10.1038/nature.2014.15249 |s2cid=87409424 |access-date=23 May 2014 }}</ref>



On 25 May 2014, ''Curiosity'' discovered an [[iron meteorite]], and named it "[[List of rocks on Mars#Curiosity|Lebanon]]" ([[:File:PIA18387-MarsCuriosityRover-Lebanon-IronMeteorite-20140525.jpg|image]]).

[[File:675732main pia16040-full full.jpg|300px]]

<br />



On 3 June 2014, ''Curiosity'' observed the planet [[Mercury (planet)|Mercury]] transiting the [[Sun]], marking the first time a [[planetary transit]] has been observed from a celestial body besides [[Earth]].<ref name="NASA-20140610">{{cite web |last=Webster |first=Guy |title=Mercury Passes in Front of the Sun, as Seen From Mars |url= http://www.jpl.nasa.gov/news/news.php?release=2014-183 |date=10 June 2014 |work=[[NASA]] |access-date=10 June 2014 }}</ref>

This mosaic image shows part of the left side of NASA's Curiosity rover and two blast marks from the descent stage's rocket engines. The images that were used to make the mosaic were obtained by the rover's Navigation cameras.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16040.html NASA - Traces of Landing]</ref>



On 24 June 2014, ''Curiosity'' completed a [[Martian year]]—687 Earth days—after finding that Mars once had [[Timeline of Mars Science Laboratory#Evidence for ancient habitability|environmental conditions favorable for microbial life]].<ref name="NASA-20140623">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |title=NASA's Mars Curiosity Rover Marks First Martian Year |url= http://www.jpl.nasa.gov/news/news.php?release=2014-199 |date=23 June 2014 |work=[[NASA]] |access-date=23 June 2014 }}</ref>

<br />



On 27 June 2014, ''Curiosity'' crossed the [[:File:Mars Science Laboratory landing ellipse reduced.jpg|boundary line]] of its "[[:File:Curiosity Rover Landing Site - Quadmapping Yellowknife.jpg|3-sigma safe-to-land ellipse]]" and is now in territory that may get even more interesting, especially in terms of [[Martian geology]] and landscape ([[:File:PIA18399-MarsCuriosityRover-NowOutside3SigmaLandingEllipse-20140627.jpg|view from space]]).<ref name="NASA-20140708">{{cite web |author=Staff |title=Curiosity Mars Rover Reaching Edge of Its Landing Ellipse |url= http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=6421 |date=8 July 2014 |work=[[NASA]] |access-date=11 July 2014 }}</ref>

[[File:Self-portrait of Curiosity.jpg|300px]]

<br />



On 12 July 2014, ''Curiosity'' imaged the first [[ChemCam|laser spark]] on Mars ([[:File:PIA18401-MarsCuriosityRover-NovaRock-LaserSpark-20140712.jpg|related image]]; [https://web.archive.org/web/20140808083944/http://www.jpl.nasa.gov/video/?id=1317 video (01:07)].)

This self portrait of NASA's Curiosity rover was taken by its navigation cameras, located on the now-upright mast.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16012.html NASA - Rover's Self Portrait]</ref>



On 6 August 2014, ''Curiosity'' celebrated its second anniversary since [[Bradbury Landing|landing]] on Mars in 2012.<ref name="NASA-20140805">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |title=NASA Mars Curiosity Rover: Two Years and Counting on Red Planet |url= http://www.jpl.nasa.gov/news/news.php?release=2014-262 |date=5 August 2014 |work=[[NASA]] |access-date=6 August 2014 }}</ref>

<br />



On 11 September 2014, a panel of NASA scientists announced ([https://www.youtube.com/watch?v=7szg3JrNT-4 video (01:25)]) the arrival of ''Curiosity'' at [[Mount Sharp]] and discussed future rover plans.<ref name="NYT-20140911" />

[[File:Clear Views on Mars.jpg|500px]]

<br />



== First extended mission (October 2014 - September 2016) ==

This image comparison shows a view through a Hazard-Avoidance camera on NASA's Curiosity rover before and after the clear dust cover was removed.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16005.html NASA - Clear Views on Mars]</ref>

On 19 October 2014, the ''Curiosity'' rover viewed the flyby of [[C/2013 A1|Comet C/2013 A1]].

----



On 8 December 2014, a panel of NASA scientists discussed ([http://www.ustream.tv/recorded/56255521 archive 62:03)] the latest observations of ''Curiosity'', including findings about how water may have helped shape the landscape of Mars and had a climate long ago that could have produced long-lasting lakes at many Martian locations.<ref name="NASA-20141208">{{cite web |last1=Brown |first1=Dwayne |last2=Webster |first2=Guy |title=Release 14-326 - NASA's Curiosity Rover Finds Clues to How Water Helped Shape Martian Landscape |url= http://www.nasa.gov/press/2014/december/nasa-s-curiosity-rover-finds-clues-to-how-water-helped-shape-martian-landscape/ |date=8 December 2014 |work=[[NASA]] |access-date=8 December 2014 }}</ref><ref name="NYT-20141208">{{cite news |last=Kaufmann |first=Marc |title=(Stronger) Signs of Life on Mars |url= https://www.nytimes.com/2014/12/09/science/-stronger-signs-of-life-on-mars.html |date=8 December 2014 |work=[[New York Times]] |access-date=8 December 2014 }}</ref><ref name="NYT-20141208-KC">{{cite news |last=Chang |first=Kenneth |title=Curiosity Rover's Quest for Clues on Mars |url= https://www.nytimes.com/2014/12/09/science/curiosity-rovers-quest-for-clues-on-mars.html |date=8 December 2014 |work=[[New York Times]] |access-date=9 December 2014 }}</ref>

====Sol 3====



On 16 December 2014, NASA reported detecting an unusual increase, then decrease, in the amounts of [[methane]] in the [[Atmosphere of Mars|atmosphere]] of the planet [[Mars]]; in addition, [[organic chemical]]s were detected in powder drilled from a [[List of rocks on Mars|rock]] by the [[Curiosity (rover)|''Curiosity'' rover]]. Also, based on [[deuterium]] to [[hydrogen]] ratio studies, much of the [[Water on Mars|water]] at [[Gale Crater]] on Mars was found to have been lost during ancient times, before the lakebed in the crater was formed; afterwards, large amounts of water continued to be lost.<ref name="NASA-20141216-GW" /><ref name="NYT-20141216-KC" /><ref name="SCI-20141216-PRM">{{cite journal |author=Mahaffy, P.R. |display-authors=etal |title=Mars Atmosphere - The imprint of atmospheric evolution in the D/H of Hesperian clay minerals on Mars |date=16 December 2014 |journal=[[Science (journal)|Science]] |doi=10.1126/science.1260291 |volume=347 |issue=6220 |pages=412–414 |bibcode=2015Sci...347..412M |pmid=25515119|s2cid=37075396 |url= https://authors.library.caltech.edu/52528/7/Mahaffy-SM.pdf }}</ref>

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

{| class="wikitable" style="margin:0.5em auto; width:600px;"

! style="margin; background: lavender;" colspan="3" | '''09 August 2012'''

! ''[[Curiosity (rover)|Curiosity]]'' at ''The Kimberley''

|-

|-

| style="font-size:88%" |[[File:PIA18081-MarsCuriosityRover-TheKimberley-20140411.jpg|600px]]

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=6f8HHQ2U2jg NASA Video] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1301 NASA News]

{{center|1=[[Curiosity (rover)|''Curiosity'' rover]] (lower left quadrant of image) and "Tracks" near ''The Kimberley'' - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; 11 April 2014).}}

|}

|}

{| class="wikitable" style="margin:0.5em auto; width:600px;"

! ''[[Curiosity (rover)|Curiosity]]'' at Mount Sharp

|-

| style="font-size:88%" |[[File:PIA19114-MarsCuriosityRover-PahrumpHills-20141213.jpg|600px]]

{{center|1=[[Curiosity (rover)|''Curiosity'' rover]] (within rectangle) in the ''Pahrump Hills'' of [[Aeolis Mons|Mount Sharp]] - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; 13 December 2014).}}

|}

[[File:PIA21709-Mars-CuriosityRover-PahrumpHills.jpg|thumb|center|500px|{{center|1=Pahrump Hills as viewed by the ''Curiosity'' rover (2014).}}]]

<!---

{{wide image|PIA18081-MarsCuriosityRover-TheKimberley-20140411.jpg|500px|align-cap=center|[[Curiosity (rover)|''Curiosity'' rover]] (lower left quadrant of image) and "Tracks" near ''The Kimberley'' - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; April 11, 2014).}}

{{wide image|PIA19114-MarsCuriosityRover-PahrumpHills-20141213.jpg|800px|align-cap=center|[[Curiosity (rover)|''Curiosity'' rover]] (within rectangle) in the ''Pahrump Hills'' of [[Aeolis Mons|Mount Sharp]] - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; December 13, 2014).}}

--->On 21 January 2015, NASA announced a collaborative effort with [[Microsoft]] that developed a software project called [[:File:MarsCuriosityRover-OnSight-3dSimulation-20150121.jpg|OnSight]] which allows scientists to perform virtual work on Mars based on data from the ''Curiosity ''rover.<ref name="NASA-20150121">{{cite web |last1=Webster |first1=Guy |last2=McGregor |first2=Veroica |last3=Brown |first3=Dwayne |title=NASA, Microsoft Collaboration Will Allow Scientists to 'Work on Mars' |url= http://www.jpl.nasa.gov/news/news.php?release=2015-025 |date=21 January 2015 |work=[[NASA]] |access-date=21 January 2015 }}</ref>

<!---{{multiple image

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| direction = horizontal

| image1 = MarsCuriosityRover-OnSight-3dSimulation-20150121.jpg

| width1 = 250

| alt1 =

| caption1 = Mars rover - OnSight 3D simulation project.

}}--->

<!---{{Wide image|PIA19142-MarsCuriosityRover-Self-Mojave-20150131.jpg|600px|''Curiosity'' at Mojave site on [[Aeolis Mons|Mount Sharp]] (January 31, 2015).}}--->

{| class="wikitable" style="margin:0.5em auto; width:600px;"

! ''Curiosity'' at [[Aeolis Mons|Mount Sharp]]

|-

| style="font-size:88%" |[[File:PIA19142-MarsCuriosityRover-Self-Mojave-20150131.jpg|800px]]

{{center|1=Self-portrait of the ''[[Curiosity (rover)|Curiosity]]'' rover at the Mojave site (31 January 2015).}}

|}

On 6 March 2015, NASA reported performing tests on the rover to help uncover the reason for intermittent problems with the robotic arm used for rock drilling and analysis.<ref name="NYT-20150306">{{cite news |last=Chang |first=Kenneth |title=Mars Rover Curiosity Is Suffering Short Circuits in Arm, NASA Says |url= https://www.nytimes.com/2015/03/07/science/space/mars-rover-curiosity-is-suffering-short-circuits-in-arm-nasa-says.html |date=6 March 2015 |work=[[New York Times]] |access-date=6 March 2015 }}</ref> Results of preliminary tests suggest the intermittent short-circuit problem may be related to the percussion mechanism of the drill. Further tests are planned to verify and adjust to the problem.<ref name="SP-20150306">{{cite web |last=Wall |first=Mike |title=NASA Finds Likely Source of Mars Rover Curiosity's Short Circuit |url= http://www.space.com/28758-mars-rover-curiosity-short-circuit-drill.html |date=6 March 2015 |work=[[Space.com]] |access-date=8 March 2015 }}</ref>



On 24 March 2015, NASA reported the first detection of [[nitrogen]] released after heating surface sediments on the planet [[Mars]]. The nitrogen, in the form of [[nitric oxide]], was detected by the [[Sample Analysis at Mars|SAM]] instrument on the ''Curiosity'' rover and can be used by [[living organisms]]. The discovery supports the notion that ancient Mars may have been habitable for [[life]].<ref name="NASA-20150324">{{cite web |last1=Neal-Jones |first1=Nancy |last2=Steigerwald |first2=William |last3=Webster |first3=Guy |last4=Brown |first4=Dwayne |title=Curiosity Rover Finds Biologically Useful Nitrogen on Mars |url= http://www.jpl.nasa.gov/news/news.php?feature=4516 |date=24 March 2015 |work=[[NASA]] |access-date=25 March 2015 }}</ref>

<br />



On 27 March 2015, NASA reported that the [[Bradbury Landing|landing site]] was fading from view in the two-and-a-half years since landing in 2012, as shown in the following animation:

{{Wide image|First 360 color panorama from the Curosity rover.jpg|1500px|<center>This is the first 360-degree panorama in color of the [[Gale (crater)|Gale Crater]] landing site taken by NASA's Curiosity rover. The panorama was made from thumbnail versions of images taken by the Mast Camera.<ref>[http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=4372 Mars Science Laboratory: Images]</ref>}}

{{Multiple image|direction=horizontal|align=center|width=300|image1=PIA19159-MarsCuriosityRover-FadingLandingSite-20150327.gif|caption1=Landing site fading from view after first several years.}}



On 4 April 2015, NASA reported studies, based on measurements by the [[Sample Analysis at Mars]] (SAM) instrument on the [[Curiosity (rover)|''Curiosity'' rover]], of the [[Atmosphere of Mars|Martian atmosphere]] using [[xenon]] and [[argon]] [[isotope]]s. Results provided support for a "vigorous" loss of atmosphere early in the history of Mars and were consistent with an [[Climatology|atmospheric signature]] found in bits of atmosphere captured in some [[Martian meteorite]]s found on Earth.<ref name="NASA-20150331">{{cite web |last1=Brown |first1=Dwayne |last2=Neal-Jones |first2=Nancy |title=RELEASE 15-055 Curiosity Sniffs Out History of Martian Atmosphere |url= http://www.nasa.gov/press/2015/march/curiosity-sniffs-out-history-of-martian-atmosphere/ |date=31 March 2015 |work=[[NASA]] |access-date=4 April 2015 }}</ref>

<br />

{{Wide image|Pia16051 figure 1 raw smaller-br2.jpg|1500px|<center>First High-Resolution Color Mosaic of Curiosity's Mastcam Images<ref>[http://mars.jpl.nasa.gov/multimedia/images/?ImageID=4421 Mars Exploration Program: Images]</ref>''</center>}}

<br />



On 19 August 2015, NASA scientists reported that the [[Dynamic Albedo of Neutrons]] (DAN) instrument on the ''Curiosity'' rover detected an unusual hydrogen-rich area, at "Marias Pass," on Mars. The hydrogen found seemed related to water or hydroxyl ions in rocks within three feet beneath the rover, according to the scientists.<ref name="NASA-20150819">{{cite web |author=Staff |title=PIA19809: Curiosity Finds Hydrogen-Rich Area of Mars Subsurface |url= http://photojournal.jpl.nasa.gov/catalog/PIA19809 |date=19 August 2015 |work=[[NASA]] |access-date=19 August 2015 }}</ref>

[[File:0003ML0000139000E1 DXXX.jpg|385px]] [[File:0003ML0000125000E1 DXXX.jpg|385px]]<br />

[[File:PIA19809-MarsCuriosityRover-HydrogenRichAreaFound-20150721.jpg|thumb|300px|center|{{center|1=Hydrogen-rich area detected at 'Marias Pass" on Mars by ''Curiosity''.<ref name="NASA-20150819" />}}]]



On 5 October 2015, possible [[recurrent slope lineae]], wet [[brine]] flows, were reported on [[Mount Sharp]] near [[Curiosity (rover)|''Curiosity'']].<ref name="NYT-20151005-kc">{{cite news |last=Chang |first=Kenneth |title=Mars Is Pretty Clean. Her Job at NASA Is to Keep It That Way. |url= https://www.nytimes.com/2015/10/06/science/mars-catharine-conley-nasa-planetary-protection-officer.html |date=5 October 2015 |work=[[New York Times]] |access-date=6 October 2015 }}</ref> In addition, on 5 October 2015, NASA reported an estimated 20,000 to 40,000 heat-resistant [[bacterial spores]] were on ''Curiosity'' at launch, as much as 1,000 times more than that may not have been counted.<ref name="NYT-20151005-kc" />

These images were taken by Mastcam: Left (MAST_LEFT) onboard NASA's Mars rover Curiosity on Sol 3<ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000125000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000139000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref>



On 8 October 2015, NASA confirmed that lakes and streams existed in [[Gale (crater)|Gale crater]] 3.3 - 3.8 billion years ago delivering sediments to build up the lower layers of [[Mount Sharp]].<ref name="NASA-20151008">{{cite web |last=Clavin |first=Whitney |title=NASA's Curiosity Rover Team Confirms Ancient Lakes on Mars |url= http://www.jpl.nasa.gov/news/news.php?feature=4734 |date=8 October 2015 |work=[[NASA]] |access-date=9 October 2015 }}</ref><ref name="SCI-20151009">{{cite journal |author=Grotzinger, J.P.| display-authors=etal

<br />

|title=Deposition, exhumation, and paleoclimate of an ancient lake deposit, Gale crater, Mars |date=9 October 2015 |journal=[[Science (journal)|Science]] |volume=350 |number=6257 |doi=10.1126/science.aac7575 |pages=aac7575 |pmid=26450214|bibcode=2015Sci...350.7575G | s2cid=586848

| url=https://resolver.caltech.edu/CaltechAUTHORS:20151009-084255932

}}</ref>

[[File:PIA20281-MarsCuriosityRover-NamibSandDune-DownwindSide-20151217.jpg|thumb|center|400px|{{center|1=[[List of extraterrestrial dune fields#Mars|Namib sand dune]] (downwind side) on Mars<br />(''Curiosity'' rover; December 17, 2015).}}]]

On 17 December 2015, NASA reported that as ''Curiosity'' climbed higher up Mount Sharp, the composition of rocks were changing substantially. For example, rocks found higher up the mountain contained much higher levels of [[silica]] than the [[Basalt|basaltic rocks]] found earlier. After further analysis, the silica-rich rocks on Mars were found to be [[Tridymite#Mars|tridymite]], a mineral that is not commonly found on Earth. [[Opal#Noncrystalline opal|Opal-A]], another form of silica, was also found on Mars.<ref name="NYT-20151217">{{cite news |last=Chang |first=Kenneth |title=Mars Rover Finds Changing Rocks, Surprising Scientists |url= https://www.nytimes.com/2015/12/18/science/mars-rover-finds-changing-rocks-surprising-scientists.html |date=17 December 2015 |work=[[New York Times]] |access-date=22 December 2015 }}</ref>



==Second extended mission (October 2016 - September 2019)==

[[File:676029main pia16052-color-full full.jpg|775px]]<br />

The second extended mission began on 1 October 2016.<ref>{{Cite web |title=In Depth {{!}} Curiosity (MSL) |url=https://solarsystem.nasa.gov/missions/curiosity-msl/in-depth |access-date=2023-06-04 |website=NASA Solar System Exploration}}</ref> The rover explored a ridge known as the [[Murray Formation]] for most of the mission.



As of 3 October 2016, NASA summarized the findings of the mission, thus far, as follows: "The Curiosity mission has already achieved its main goal of determining whether the landing region ever offered environmental conditions that would have been favorable for microbial life, if Mars has ever hosted life. The mission found evidence of ancient rivers and lakes, with a chemical energy source and all of the chemical ingredients necessary for life as we know it."<ref name="NASA-20161003">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |last3=Cantillo |first3=Laurie |title=NASA's Curiosity Rover Begins Next Mars Chapter |url= http://www.jpl.nasa.gov/news/news.php?feature=6632 |date=3 October 2016 |work=[[NASA]] |access-date=4 October 2016 }}</ref> Plans for the next two years, up to September 2018, include further explorations of the uphill slopes of [[Aeolis Mons|Mount Sharp]], including a ridge rich in the mineral [[hematite]] and a region of clay-rich bedrock.<ref name="NASA-20161003" />

This color image from NASA's Curiosity rover shows part of the wall of Gale Crater, the location on Mars where the rover landed on August 5, 2012 PDT (August 6, 2012 EDT). This is part of a larger, high-resolution color mosaic made from images obtained by Curiosity's Mast Camera.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16052-color.html NASA - Wall of Gale Crater]</ref>

{{multiple image|align=center|total_width=600|header=[[List of rocks on Mars#2012 .E2.80.93 Curiosity rover .28Mars Science Laboratory.29|"Egg Rock" Meteorite]] (27 October 2016)<ref name="NASA-20161102">{{cite web |last1=Webster |first1=Guy |last2=Brown |first2=Dwayne |last3=Cantillo |first3=Laurie |title=Curiosity Mars Rover Checks Odd-looking Iron Meteorite |url= http://www.jpl.nasa.gov/news/news.php?feature=6667 |date=2 November 2016 |work=[[NASA]] |access-date=2 November 2016 }}</ref>

|image1=PIA21134-MarsCuriosityRoverFindsMeteorite-EggRockContext-20161027.jpg

|width1=1120

|height1=1000

|caption1=Context view

|image2=PIA21133 Iron-Nickel Meteorite Zapped by Mars Rover's Laser, Figure 1.jpg

|width2=1169

|height2=1154

|caption2=Close-up view

}}

On 13 December 2016, NASA reported further evidence supporting habitability on Mars as the ''Curiosity'' rover climbed higher, studying younger layers, on Mount Sharp.<ref name="NASA-20161213">{{cite web |last1=Cantillo |first1=Laurie |last2=Brown |first2=Dwayne |last3=Webster |first3=Guy |last4=Agle |first4=DC |last5=Tabor |first5=Abigail |last6=Mullane |first6=Laura |title=Mars Rock-Ingredient Stew Seen as Plus for Habitability |url= http://www.jpl.nasa.gov/news/news.php?feature=6700 |date=13 December 2016 |work=[[NASA]] |access-date=14 December 2016}}</ref> Also reported, the very soluble element [[boron]] was detected for the first time on Mars.<ref name="NASA-20161213" /> Since landing on Mars in August 2012, ''Curiosity'' has driven {{convert|15.0|km|mi|abbr=on}} and climbed {{convert|165|m|ft|abbr=on}} in elevation.<ref name="NASA-20161213a" />

[[File:PIA21256 - Color Variations on Mount Sharp, Mars (White Balanced), Figure 1.jpg|thumb|center|600px|{{center|1=''Curiosity'' rover view of [[Mount Sharp]] (November 10, 2016).}}]]

[[File:PIA21145-MarsCuriosityRoverMission-20161213.png|thumb|center|600px|{{center|1=Summary of the ''Curiosity'' rover mission (14-fold exaggerated elevation; 13 December 2016)<ref name="NASA-20161213a">{{cite web |author=Staff |title=PIA21145: Curiosity Rover's Martian Mission, Exaggerated Cross Section |url= http://photojournal.jpl.nasa.gov/catalog/PIA21145 |date=13 December 2016 |work=[[NASA]] |access-date=December 15, 2016 }}</ref>}} ]]

[[File:PIA21146-MarsCuriosityRover-MudstoneMineralogy-20161213.png|thumb|center|600px|{{center|1=''Curiosity'' rover - [[Mudstone]] [[Mineralogy]] - 2013 to 2016 on Mars ([[CheMin]]; December 13, 2016)<ref name="NASA-20161213b">{{cite web |author=Staff |title=PIA21146: Mudstone Mineralogy from Curiosity's CheMin, 2013 to 2016 |url= http://photojournal.jpl.nasa.gov/catalog/PIA21146 |date=December 13, 2016 |work=[[NASA]] |access-date=December 16, 2016 }}</ref>}}]]On 17 January 2017, NASA released an image of a rock slab, named "Old Soaker", which may contain mud cracks. Also, somewhat later, it released an animation of [[Martian soil|sand]] moving in a nearby area.

<gallery mode="packed" heights="180">

Image:PIA21262-MarsCuriosityRover-PossibleMudCracks-OldSoaker-20161220.jpg|Rock slab, named "Old Soaker", which may contain mud cracks – as viewed by ''Curiosity'' (December 20, 2016).

Image:PIA21143 - Sand Moving Under Curiosity, One Day to Next, Animation.gif|[[Martian soil|Sand]] moving on Mars – as viewed by ''Curiosity'' (January 23, 2017).

</gallery>

On 6 February 2017, NASA reported that rock samples analyzed by the rover have not revealed any significant [[carbonate]]. This poses a puzzle to researchers: the same rocks that indicate a lake existed also indicate there was very little [[carbon dioxide]] in the air to help keep the lake unfrozen.<ref name="NASA-20170206">{{cite web |last1=Webster |first1=Guy |last2=Cantillo |first2=Laurie |last3=Brown |first3=Dwayne |last4=Tabor |first4=Abigail |title=NASA's Curiosity Rover Sharpens Paradox of Ancient Mars |url= http://www.jpl.nasa.gov/news/news.php?feature=6734 |date=6 February 2017 |work=[[NASA]] |access-date=27 February 2017 }}</ref>



On 27 February 2017, NASA presented the following mission overview: "During the first year after Curiosity's 2012 landing in Gale Crater, the mission fulfilled its main goal by finding that the region once offered environmental conditions favorable for microbial life. The conditions in long-lived ancient freshwater Martian lake environments included all of the key chemical elements needed for life as we know it, plus a chemical source of energy that is used by many microbes on Earth. The extended mission is investigating how and when the habitable ancient conditions evolved into conditions drier and less favorable for life."<ref name="NASA-20170227">{{cite web |last1=Webster |first1=Guy |last2=Cantillo |first2=Laurie |last3=Brown |first3=Dwayne |title=Martian Winds Carve Mountains, Move Dust, Raise Dust |url= http://www.jpl.nasa.gov/news/news.php?feature=6758 |date=27 February 2017 |work=[[NASA]] |access-date=27 February 2017 }}</ref>

<br />



From 3 to 7 May 2017, ''Curiosity'' used ChemCam to study what turned out to be [[manganese oxide]] deposits on the Sutton Island and Blunts Point layers of the Murray Formation. According to a 2024 paper, the deposits suggest Earth-level amounts of oxygen were present in the very early Martian atmosphere, hinting at microbial life.<ref name="Gasda Lanza Meslin Lamm 2024">{{cite journal | last=Gasda | first=P. J. | last2=Lanza | first2=N. L. | last3=Meslin | first3=P.‐Y. | last4=Lamm | first4=S. N. | last5=Cousin | first5=A. | last6=Anderson | first6=R. | last7=Forni | first7=O. | last8=Swanner | first8=E. | last9=L’Haridon | first9=J. | last10=Frydenvang | first10=J. | last11=Thomas | first11=N. | last12=Gwizd | first12=S. | last13=Stein | first13=N. | last14=Fischer | first14=W. W. | last15=Hurowitz | first15=J. | last16=Sumner | first16=D. | last17=Rivera‐Hernández | first17=F. | last18=Crossey | first18=L. | last19=Ollila | first19=A. | last20=Essunfeld | first20=A. | last21=Newsom | first21=H. E. | last22=Clark | first22=B. | last23=Wiens | first23=R. C. | last24=Gasnault | first24=O. | last25=Clegg | first25=S. M. | last26=Maurice | first26=S. | last27=Delapp | first27=D. | last28=Reyes‐Newell | first28=A. | title=Manganese‐Rich Sandstones as an Indicator of Ancient Oxic Lake Water Conditions in Gale Crater, Mars | journal=Journal of Geophysical Research: Planets | volume=129 | issue=5 | date=2024 | issn=2169-9097 | doi=10.1029/2023JE007923| doi-access=free }}</ref>

[[File:0003ML0000128000E1 DXXX.jpg|250px]] [[File:0003ML0000095000E1 DXXX.jpg|250px]] [[File:0003ML0000062000E1 DXXX.jpg|250px]]



On 1 June 2017, NASA reported that the ''Curiosity'' rover provided evidence of an ancient lake in [[Gale (crater)|Gale crater]] on Mars that could have been favorable for [[microorganism|microbial life]]; the ancient lake was [[Lake stratification|stratified]], with shallows rich in [[Oxidizing agent|oxidants]] and depths poor in oxidants, particularly [[silica]]; the ancient lake provided many different types of microbe-friendly environments at the same time. NASA further reported that the ''Curiosity'' rover will continue to explore higher and younger layers of [[Mount Sharp]] in order to determine how the lake environment in ancient times on Mars became the drier environment in more modern times.<ref name="NASA-20170531">{{cite web |last1=Webster |first1=Guy |last2=Mullane |first2=Laura |last3=Cantillo |first3=Laurie |last4=Brown |first4=Dwayne |title=High-Silica 'Halos' Shed Light on Wet Ancient Mars |url= https://www.jpl.nasa.gov/news/news.php?feature=6859 |date=31 May 2017 |work=[[NASA]] |access-date=1 June 2017 }}</ref><ref name="NASA-20170601">{{cite web |last1=Webster |first1=Guy |last2=Filiano |first2=Gregory |last3=Perkins |first3=Robert|last4=Cantillo |first4=Laurie |last5=Brown |first5=Dwayne |title=Curiosity Peels Back Layers on Ancient Martian Lake |url= https://www.jpl.nasa.gov/news/news.php?feature=6863 |date=1 June 2017 |work=[[NASA]] |access-date=1 June 2017 }}</ref><ref name="SCI-20170602">{{cite journal |author=Hurowitz, J.A. |display-authors=etal |title=Redox stratification of an ancient lake in Gale crater, Mars |date=2 June 2017 |journal=[[Science (journal)|Science]] |volume=356 |issue=6341 |doi=10.1126/science.aah6849 |pmid=28572336 |bibcode=2017Sci...356.6849H |page=eaah6849|doi-access=free |hdl=10044/1/53715 |hdl-access=free }}</ref>

[[File:0003ML0000082000E1 DXXX.jpg|250px]] [[File:0003ML0000043000E1 DXXX.jpg|250px]] [[File:0003ML0000113000E1 DXXX.jpg|250px]] <br />

[[File:PIA21500-Mars-GaleCrater-LakeStratification.png|thumb|center|600px|{{center|1=Stratification of an ancient lake in [[Gale (crater)|Gale crater]].}}]]

[[File:PIA21710-MarsCuriosityRoverOnMountSharp-MRO-20170605.jpg|thumb|center|600px|{{center|1=''Curiosity'' rover (center bright blue) on Mount Sharp viewed from space by [[Mars Reconnaissance Orbiter|MRO]] (June 5, 2017).<ref name="NASA-20170622">{{cite news |last=Chang |first=Kenneth |title=High Above Mars, a NASA Orbiter Spies the Curiosity Rover |url= https://www.nytimes.com/2017/06/22/science/mars-curiosity-reconnaissance-orbiter.html |date=22 June 2017 |work=[[NASA]] |access-date=23 June 2017 }}</ref>}}]]



Between 22 July – 1 August 2017, few commands were sent from the Earth to Mars since Mars was in [[Conjunction (astronomy)|conjunction]] with the sun.<ref name="ES-20170715">{{cite web |last=Byrd |first=Deborah |title=No commands to Mars craft in late July |url= http://earthsky.org/space/nasa-moratorium-commands-mars-july-22-aug-1-2017 |date=15 July 2017 |work=[[Earth & Sky]] |access-date=15 July 2017 }}</ref>

Pictures acquired by the Mastcam of the surface of Mars.

<ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000128000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000095000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000062000E1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000082000E1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000043000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref><ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=0003ML0000113000I1_DXXX&s=3 Mars Science Laboratory: Raw Images]</ref>



On 5 August 2017, NASA celebrated the fifth anniversary of the [[Curiosity (rover)|''Curiosity'' rover mission]] landing, and related exploratory accomplishments, on the planet [[Mars]].<ref name="NASA-20170802">{{cite web |last1=Webster |first1=Guy |last2=Cantillo |first2=Laurie |last3=Brown |first3=Dwayne |title=Five Years Ago and 154 Million Miles Away: Touchdown! |url= https://mars.jpl.nasa.gov/news/2017/five-years-ago-and-154-million-miles-away-touchdown |date=2 August 2017 |work=[[NASA]] |access-date=6 August 2017 }}</ref><ref name="SP-20170805">{{cite web |last=Wall |first=Mike |title=After 5 Years on Mars, NASA's Curiosity Rover Is Still Making Big Discoveries |url= https://www.space.com/37722-mars-rover-curiosity-five-years-anniversary.html |date=5 August 2017 |work=[[Space.com]] |access-date=6 August 2017 }}</ref> (Videos: [https://www.youtube.com/watch?v=IxvODcuFb1s ''Curiosity''{{'s}} First Five Years (02:07)]; [https://www.youtube.com/watch?v=O0nPFaBU98k ''Curiosity''{{'s}} POV: Five Years Driving (05:49)]; [https://www.youtube.com/watch?v=Q-uAz82sH-E ''Curiosity''{{'s}} Discoveries About Gale Crater (02:54)])

<br />



On 5 September 2017, scientists reported that the ''Curiosity'' rover detected [[boron]], an essential ingredient for [[life]] on [[Earth]], on the planet Mars. Such a finding, along with previous discoveries that water may have been present on ancient Mars, further supports the possible early habitability of [[Gale (crater)|Gale Crater]] on Mars.<ref name="GPL-20170905">{{cite journal |author=Gasda, Patrick J. |display-authors=etal |title=In situ detection of boron by ChemCam on Mars |date=5 September 2017 |journal=[[Geophysical Research Letters]] |doi=10.1002/2017GL074480 |bibcode=2017GeoRL..44.8739G |volume=44 |issue=17 |pages=8739–8748|doi-access=free |hdl=2381/41995 |hdl-access=free }}</ref><ref name="GZ-20170906">{{cite news |last=Paoletta |first=Rae |title=Curiosity Has Discovered Something That Raises More Questions About Life on Mars |url= https://gizmodo.com/curiosity-has-discovered-something-that-raises-more-que-1800879035 |date=6 September 2017 |work=[[Gizmodo]] |access-date=6 September 2017 }}</ref>

[[File:PIA16068 - Mars Curiosity Rover - Aeolis Mons - 20120817.jpg|center|framed|350x350px|The Promised Land This image (cut out from a mosaic) shows the view from the landing site of NASA's Curiosity rover toward the lower reaches of Mount Sharp, where Curiosity is likely to begin its ascent through hundreds of feet (meters) of layered deposits. The lower several hundred feet (meters) show evidence of bearing hydrated minerals, based on orbiter observations. The terrain Curiosity will explore is marked by hills, buttes, mesas and canyons on the scale of one-to-three story buildings, very much like the Four Corners region of the western United States.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16068.html NASA - The Promised Land]</ref>]]



[[File:PIA21851-CuriosityRover-VeraRubinRidge-20170819.jpg|thumb|center|600px|{{center|1=''Curiosity'' climbed ''Vera Rubin Ridge'' on [[Mount Sharp]] (September 13, 2017).<ref name="NASA-20170913" />}}]]

<br />



On 13 September 2017, NASA reported that the ''Curiosity'' rover climbed an iron-oxide-bearing ridge called ''Vera Rubin Ridge'' (or ''Hematite Ridge'') and will now start studying the numerous bright veins embedded in the various layers of the ridge, in order to provide more details about the history and habitability of ancient Mars.<ref name="NASA-20170913">{{cite web |last1=Webster |first1=Guy |last2=Cantiollo |first2=Laurie |last3=Brown |first3=Dwayne |title=NASA's Curiosity Mars Rover Climbing Toward Ridge Top |url= https://www.jpl.nasa.gov/news/news.php?feature=6946 |date=13 September 2017 |work=[[NASA]] |access-date=13 September 2017 }}</ref>

----



On 30 September 2017, NASA reported [[Radiation|radiation levels]] on the surface of the planet [[Mars]] were temporarily [[Orders of magnitude (radiation)|doubled]], and were associated with an [[aurora]] 25-times brighter than any observed earlier, due to a massive, and unexpected, [[Coronal mass ejection|solar storm]] in the middle of the month.<ref name="PHYS-20170930">{{cite web |last=Scott |first=Jim |title=Large solar storm sparks global aurora and doubles radiation levels on the martian surface |url= https://phys.org/news/2017-09-large-solar-storm-global-aurora.html |date=30 September 2017 |work=[[Phys.org]] |access-date=30 September 2017 }}</ref>

====Sol 4====

[[File:PIA22063-MarsCuriosityRover-DrillingTests-20171017.jpg|thumb|center|600px|{{center|1=''Curiosity'' testing its systems in order to better resume the drilling process.<ref name="NASA-20171023" />}}]]

On 17 October 2017, NASA announced the testing of its systems on ''Curiosity'' in an attempt to better resume drilling. The drilling system had stopped working reliably in December 2016.<ref name="NASA-20171023">{{cite web |author=Staff |title=PIA22063: Mars Rover Step Toward Possible Resumption of Drilling |url= https://photojournal.jpl.nasa.gov/catalog/PIA22063 |date=23 October 2017 |work=[[NASA]] |access-date=25 October 2017 }}</ref>



[[File:PIA22210-Mars-CuriosityRover-GaleCrater-20171025-annotated.jpg|thumb|center|1000px|{{center|1=''Curiosity''{{'s}} view of [[Gale (crater)|Gale Crater]] from the slopes (at {{convert|327|m|ft|abbr=on}} elevation) of [[Mount Sharp]] ([https://www.youtube.com/watch?v=U5nrrnAukwI video (1:53)]) (October 25, 2017)}}]]On 2 January 2018, ''Curiosity'' captured images of rock shapes that may require further study in order to help better determine whether the shapes are biological or geological.<ref name="SPC-20180105">{{cite web |last=David |first=Leonard |title=Structures on Mars |url= https://www.space.com/39294-mars-rover-curiosity-weird-tube-structures.html |date=5 January 2018 |work=[[Space.com]] |access-date=5 January 2018 }}</ref><ref name="NASA-20180103">{{cite web |last=Edwards |first=Christopher |title=Sols 1913-1924: Curiosity's Working Holiday |url= https://mars.nasa.gov/msl/mission/mars-rover-curiosity-mission-updates/?mu=sols-1913-1924-curiositys-working-holiday |date=3 January 2018 |work=[[NASA]] |access-date=6 January 2018 }}</ref>

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

[[File:Mars-Curiosity-RockStructures-20180102.jpg|thumb|center|400px|{{center|1=[[List of rocks on Mars#2012 – Curiosity rover (Mars Science Laboratory)|Curious rock structures (biological or geological?)]]<br />(''Curiosity'', January 2, 2018)<ref name="SPC-20180105" /><ref name="NASA-20180103" />}}]]

! style="margin; background: lavender;" colspan="3" | '''10 August 2012'''

On 22 March 2018, ''Curiosity'' had spent 2000 [[Timekeeping on Mars#Sols|sols]] (2054 days) on Mars,<ref name="BBC-20180322">{{cite web |author=Bridges, John |display-authors=etal |title=Curiosity rover: 2,000 days on Mars |url= https://www.bbc.com/news/science-environment-43494227 |date=22 March 2018 |work=[[BBC News]] |access-date=22 March 2018 }}</ref> and prepares to study a region of clay-bearing rocks.

|-

[[File:PIA22312-Mars-CuriosityRover-ClayBearingRocks-Sol1931-20180111.jpg|thumb|center|400px|{{center|1=''Curiosity'' views a region of clay-bearing rocks (highlighted) on the slopes of Mount Sharp.}}]]

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=drGX9SVQQRI NASA Video 1] [http://www.youtube.com/watch?v=yKDBojlncss Video 2] [http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1305 NASA News]

|}



In June 2018, a [[Opportunity mission timeline#Dust storm|local dust storm]] occurred near the [[Opportunity (rover)|''Opportunity'']] rover which may affect ''Curiosity''.<ref name="SPC-20180612" /><ref name="NYT-20180613">{{cite news |last=Chokshi |first=Niraj |title=Huge Dust Storm on Mars Threatens NASA's Opportunity Rover |url= https://www.nytimes.com/2018/06/13/science/mars-dust-storm-martian.html |date=13 June 2018 |work=[[The New York Times]] |access-date=13 June 2018 }}</ref> The first signs of the storm, {{convert|1000|km|mi|abbr=on}} from ''Opportunity'', were discovered on 1 June 2018, in [[:File:PIA22329-Mars-DustStorm-20180606.jpg|photographs]] by the [[Mars Reconnaissance Orbiter#MARCI (camera)|Mars Color Imager]] (MARCI) camera on the [[Mars Reconnaissance Orbiter]] (MRO). More weather reports from the MRO and the MARCI team indicated a prolonged storm. Although this was, at that time, still far away from the rover, it influenced the atmospheric permeability (opacity) at the location. Within days, the storm had spread. As of 12 June 2018, the storm spanned an area of {{convert|41|e6km2|e6sqmi|abbr=unit}} - about the area of North America and Russia combined.<ref name="SPC-20180612">{{cite web |last=Wall |first=Mike |title=NASA's Curiosity Rover Is Tracking a Huge Dust Storm on Mars (Photo) |url= https://www.space.com/40867-nasa-curiosity-rover-mars-dust-storm.html |date=12 June 2018 |work=[[Space.com]] |access-date=13 June 2018 }}</ref><ref name="NASA-20180612">{{cite web |last1=Good |first1=Andrew |last2=Brown |first2=Dwayne |last3=Wendell |first3=JoAnna |title=NASA to Hold Media Teleconference on Martian Dust Storm, Mars Opportunity Rover |url= https://www.jpl.nasa.gov/news/news.php?feature=7158 |date=12 June 2018 |work=[[NASA]] |access-date=12 June 2018 }}</ref> Although such dust storms are not surprising, they rarely occur. They can arise within a short time and then persist for weeks to months. During the southern season of summer, the sunlight heats dust particles and brings them higher into the atmosphere. This creates wind, which in turn stirs up more dust. This results in a feedback loop that scientists are still trying to understand. NASA reported on 20 June 2018, that the dust storm had grown to completely cover the entire planet.<ref name="NASA-20180620">{{cite web |last1=Shekhtman |first1=Lonnie |last2=Good |first2=Andrew |title=Martian Dust Storm Grows Global; Curiosity Captures Photos of Thickening Haze |url= https://www.jpl.nasa.gov/news/news.php?feature=7164 |date=20 June 2018 |work=[[NASA]] |access-date=21 June 2018 }}</ref><ref name="SPC-20180621">{{cite web |last=Malik |first=Tariq |title=Epic Dust Storm on Mars Now Completely Covers the Red Planet |url= https://www.space.com/40952-mars-dust-storm-2018-covers-entire-planet.html |date=21 June 2018 |work=[[Space.com]] |access-date=21 June 2018 }}</ref>

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''15 August 2012'''

|}



[[File:PIA22737-Mars-2018DustStorm-MCS-MRO-Animation-20181030.webm|thumb|center|550px|{{center|1=[[Atmosphere of Mars|Mars dust storm]] – [[Optical depth|optical depth tau]] – May to September 2018<br />([[Mars Climate Sounder]]; [[Mars Reconnaissance Orbiter]])<br />(1:38; animation; 30 October 2018; [[:File:PIA22737-Mars-2018DustStorm-MCS-MRO-Animation-20181030.webm|file description]])}}]]

{| class="wikitable"

<gallery mode="packed" heights="180">

! style="text-align: center; background: #F4C430;"|Date

Image:PIA22487-Mars-BeforeAfterDust-20180719.gif|{{center|1=Mars (before/after) dust storm (July 2018)}}

! style="text-align: center; background: #F4C430;"|Event

Image:PIA22486-MarsCuriosityRover-DustStormSelfie-Sol2082-20180615.jpg|{{center|1=[[Curiosity (rover)|''Curiosity'']]<!---{{'s}} self-portrait---> during dust storm<!---<br />(June 2018) (Sol2082/June 15, 2018)---><ref name="NASA-20180620" /><ref name="SPC-20180621" />}}

! style="text-align: center; background: #F4C430;"|Notes

</gallery>

|-

On 4 June 2018, NASA announced that ''Curiosity''{{'s}} ability to drill has been sufficiently restored by engineers. The rover had experienced drill mechanical problems since December 2016.<ref name="NASA-20180604">{{cite web |last=Good |first=Andrew |title=Mars Curiosity's Labs Are Back in Action |url= https://www.jpl.nasa.gov/news/news.php?feature=7149 |date=4 June 2018 |work=[[NASA]] |access-date=4 June 2018 }}</ref>

| August 10, 2012 || Curiosity Preps for a Planned 'Brain Transplant'|| A healthy Curiosity spent Sol 4, its fifth day on Mars, preparing for this weekend's planned "brain transplant"--transitioning to a new version of flight software on both of Curiosity's redundant main computers. The new software is better suited for Mars surface operations, such as driving and using Curiosity's robotic arm. The "brain transplant" will take place during a series of steps beginning this evening and continuing through Aug. 13. The new software was uploaded to the rover's memory during the Mars Science Laboratory spacecraft's flight from Earth. Key capabilities in the new software enable full use of Curiosity's powerful robotic arm and drill, and advanced image processing to check for obstacles while driving. This will ultimately allow Curiosity to make longer drives by giving the rover more autonomy to identify and avoid potential hazards and to drive along a safe path that the rover identifies for itself.<ref name=autogenerated2>[http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1305 Mars Science Laboratory: Curiosity's Daily Update: Curiosity Preps for a Planned 'Brain Transplant']</ref><ref>[http://marsprogram.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1305 Mars Science Laboratory: Curiosity's Daily Update: Curiosity Preps for a Planned 'Brain Transplant']</ref>

[[File:PIA22327-MarsCuriosityRover-DrillBitOverSampleInlet-Sol2068-20180531.jpg|thumb|center|400px|{{center|1=Drill bit over a sample inlet on the deck of ''Curiosity''<br />(31 May 2018/Sol 2068)<ref name="NASA-20180604" />}}]]



On 7 June 2018, NASA announced a cyclical seasonal variation in atmospheric [[methane]], as well as the presence of [[kerogen]] and other complex [[organic compound]]s. The organic compounds were from [[mudstone]] rocks aged approximately 3.5 billion years old, sampled from two distinct sites in a dry lake in the [[Pahrump Hills]] of the [[Gale (crater)|Gale crater]]. The rock samples, when [[Pyrolysis|pyrolyzed]] via the ''Curiosity''{{'}}s [[Sample Analysis at Mars]] instrument, released an array of organic molecules; these include sulfur-containing [[thiophene]]s, [[aromatic]] compounds such as [[benzene]] and [[toluene]], and [[aliphatic]] compounds such as [[propane]] and [[butene]]. The concentration of organic compounds are 100-fold higher than earlier measurements. The authors speculate that the presence of sulfur may have helped preserve them. The products resemble those obtained from the breakdown of [[kerogen]], a precursor to oil and natural gas on Earth. NASA stated that these findings are not evidence that life existed on the planet, but that the organic compounds needed to sustain microscopic life were present, and that there may be deeper sources of organic compounds on the planet.<ref name="NASA-20180607">{{cite web |last1=Brown |first1=Dwayne |last2=Wendel |first2=JoAnna |last3=Steigerwald |first3=Bill |last4=Jones |first4=Nancy |last5=Good |first5=Andrew |title=Release 18-050 - NASA Finds Ancient Organic Material, Mysterious Methane on Mars |url= https://www.nasa.gov/press-release/nasa-finds-ancient-organic-material-mysterious-methane-on-mars |date=7 June 2018 |work=[[NASA]] |access-date=7 June 2018 }}</ref><ref name="NASA-20180607vid">{{cite web |author=NASA |title=Ancient Organics Discovered on Mars - video (03:17) |url= https://www.youtube.com/watch?v=a0gsz8EHiNc |date=7 June 2018 |work=[[NASA]] |access-date=7 June 2018 }}</ref><ref name="SPC-20180607">{{cite web |last=Wall |first=Mike |title=Curiosity Rover Finds Ancient 'Building Blocks for Life' on Mars |url= https://www.space.com/40819-mars-methane-organics-curiosity-rover.html |date=7 June 2018 |work=[[Space.com]] |access-date=7 June 2018 }}</ref><ref name="NYT-20180607">{{cite news |last=Chang |first=Kenneth |title=Life on Mars? Rover's Latest Discovery Puts It 'On the Table' - The identification of organic molecules in rocks on the red planet does not necessarily point to life there, past or present, but does indicate that some of the building blocks were present. |url= https://www.nytimes.com/2018/06/07/science/mars-nasa-life.html |date=7 June 2018 |work=[[The New York Times]] |access-date=8 June 2018 }}</ref><ref name="SCI-20180607">{{cite journal |last=Voosen |first=Paul |title=NASA rover hits organic pay dirt on Mars |url= https://www.science.org/content/article/nasa-rover-hits-organic-pay-dirt-mars |date=7 June 2018 |journal=[[Science (journal)|Science]] |access-date=7 June 2018 | doi = 10.1126/science.aau3992 |s2cid=115442477 }}</ref><ref name="SCI-20180608a">{{cite journal |last=ten Kate |first=Inge Loes |title=Organic molecules on Mars |date=8 June 2018 |journal=[[Science (journal)|Science]] |volume=360 |issue=6393 |pages=1068–1069 |doi=10.1126/science.aat2662 |pmid=29880670|bibcode=2018Sci...360.1068T |s2cid=46952468 }}</ref><ref name="SCI-20180608b">{{cite journal |author=Webster, Christopher R. |display-authors=etal |title=Background levels of methane in Mars' atmosphere show strong seasonal variations |date=8 June 2018 |journal=[[Science (journal)|Science]] |volume=360 |issue=6393 |pages=1093–1096 |doi=10.1126/science.aaq0131|pmid=29880682 |bibcode=2018Sci...360.1093W |doi-access=free }}</ref><ref name="SCI-20180608c">{{cite journal |author=Eigenbrode, Jennifer L. |author-link1=Jennifer Eigenbrode|display-authors=etal |title=Organic matter preserved in 3-billion-year-old mudstones at Gale crater, Mars |date=8 June 2018 |journal=[[Science (journal)|Science]] |volume=360 |issue=6393 |pages=1096–1101 |doi=10.1126/science.aas9185|pmid=29880683 |bibcode=2018Sci...360.1096E |doi-access=free |hdl=10044/1/60810 |hdl-access=free }}</ref>

The flight team elected to defer further science activities until after the flight software transition is completed. Several Mastcam color images were downlinked. The mission's science team is busy analyzing images Curiosity has taken of its surroundings, and is discussing features of interest that they will investigate in a few weeks once initial checkouts of the rover and the landing site are completed.<ref name=autogenerated2 />

[[File:PIA22328-MarsCuriosityRover-Methane-SeasonalCycle-20180607.jpg|thumb|center|600px|{{center|1=''Curiosity'' detected a cyclical seasonal variation in atmospheric methane.}}]]

|}

[[File:PIA22545-MarsCuriosityRover-VeraRubinRidge-20180809.jpg|thumb|center|600px|{{center|1=''Curiosity'' – 360° panoroma at Vera Rubin Ridge (9 August 2018/Sol 2137; [[Color balance|white balanced]])<ref name="NASA-20180906">{{cite web |last=Good |first=Andrew |title=Curiosity Surveys a Mystery Under Dusty Skies |url= https://www.jpl.nasa.gov/news/news.php?feature=7230 |date=September 6, 2018 |work=[[NASA]] |access-date=September 9, 2018 }}</ref>}}]]



Since 15 September 2018, a glitch in ''Curiosity''<nowiki/>'s active computer (Side-B) has prevented ''Curiosity'' from storing science and key engineering data.<ref name=":0"/> On 3 October 2018, the [[Jet Propulsion Laboratory|JPL]] began operating ''Curiosity'' on its backup computer (Side-A).<ref name=":0" /> ''Curiosity'' will store science and engineering data normally using its Side-A computer until the cause of the glitch in Side-B is determined and remedied.<ref name=":0" />

====Sol 5====



{{multiple image |header=Rocks viewed by ''Curiosity'' - [[Climate of Mars#Effect of dust storms|Effect of 2018 dust storm winds]]<ref name="NASA-20191029">{{cite news |last=Rice |first=Melissa |title=Sol 2216: A Windswept Workspace |url= https://mars.nasa.gov/msl/mission/mars-rover-curiosity-mission-updates/?mu=sol-2216-a-windswept-workspace |date=29 October 2018 |work=[[NASA]] |access-date=2 November 2018 }}</ref> |align=center |direction=horizontal |width=400 |image1=NASA-MarsCuriosity-RocksBeforeDustStorm-20180914.jpg |caption1='''Before''' dust storm winds (14 September 2018) |image2=NASA-MarsCuriosity-RocksAfterDustStorm-20181025.jpg |caption2='''After''' dust storm winds (25 October 2018)}}

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''11 August 2012'''

|-

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=BArApRIjdTI NASA Video]

|}



On 4 November 2018, geologists presented evidence, based on studies in [[Gale (crater)|Gale Crater]] by the [[Curiosity (rover)|''Curiosity'' rover]], that there was plenty of [[Water on Mars|water]] on early [[Mars]].<ref name="EA-20181103-gsa">{{cite news |author=Geological Society of America |title=Evidence of outburst flooding indicates plentiful water on early Mars |url= https://www.eurekalert.org/pub_releases/2018-11/gsoa-eoo110318.php |date= 3 November 2018 |work=[[EurekAlert!]] |access-date=5 November 2018 |author-link=Geological Society of America }}</ref><ref name="GSA-20181104">{{cite journal |author=Heydari, Ezat |display-authors=etal |title=Significance of Flood Depositis in Gale Crater, Mars |url= https://gsa.confex.com/gsa/2018AM/webprogram/Paper319960.html |date=4 November 2018 |journal=[[Geological Society of America]] |access-date=5 November 2018 }}</ref>

<br />



[[File:NASA-MarsCurioistyRover-ViewsShinyObject-20181126.png|thumb|center|300px|{{center|1=''Curiosity'' viewed a shiny object (named "Little Colonsay") on Mars (26 November 2018)<ref name="NASA-20181128" />}}]]

No science or instrument activities planned on Sol 5 <ref>[http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1306 Mars Science Laboratory: Curiosity Sends High-Resolution Color Images from Gale Crater]</ref>

----



On 26 November 2018, ''Curiosity'' viewed a shiny object (named, "Little Colonsay") on Mars.<ref name="NASA-20181128">{{cite news |last=Schwenzer |first=Susanne |title=Sol 2245-2246: Hunting shiny things! |url= https://mars.nasa.gov/msl/mission/mars-rover-curiosity-mission-updates/?mu=sol-2245-2246-hunting-shiny-things |date=28 November 2018 |work=[[NASA]] |access-date=1 December 2018 }}</ref> Although possibly a meteorite, further studies are planned to better understand its nature.

====Sol 6====



On 1 February 2019, NASA scientists reported that the [[Curiosity (rover)|Mars ''Curiosity'' rover]] determined, for the first time, the [[density]] of Mount Sharp in [[Gale (crater)|Gale crater]], thereby establishing a clearer understanding of how the mountain was formed.<ref name="NYT-20100131">{{cite news |last=Chang |first=Kenneth |title=How NASA's Curiosity Rover Weighed a Mountain on Mars - With a bit of technical improvisation, scientists worked out that the bedrock of Mount Sharp appeared to be less dense than had been expected. |url= https://www.nytimes.com/2019/01/31/science/mars-curiosity-rover-mount-sharp.html |date=31 January 2019 |work=[[The New York Times]] |access-date=1 February 2019 }}</ref><ref name="SCI-20190201">{{cite journal |author=Lewis, Kevin W. |title=A surface gravity traverse on Mars indicates low bedrock density at Gale crater |date=1 February 2019 |journal=[[Science (journal)|Science]] |volume=363 |issue=6426 |pages=535–537 |doi=10.1126/science.aat0738 |pmid=30705193 |bibcode=2019Sci...363..535L |s2cid=59567599 |doi-access=free }}</ref>

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''12 August 2012'''

|}



On 4 April 2019, [[NASA]] released images of [[solar eclipse]]s by the [[Moons of Mars|two moons of the planet Mars]], [[Phobos (moon)|Phobos]] ([[:File:PIA23133-MarsCuriosityRover-PhobosEclipse-20190326.gif|animation1]]) and [[Deimos (moon)|Deimos]] ([[:File:PIA23134-MarsCuriosityRover-DeimosEclipse-20190317.gif|animation2]]), as viewed by the [[Curiosity (rover)|''Curiosity'' rover]] on the planet Mars in March 2019.<ref name="NASA-20190404">{{cite news |last1=Good |first1=Andrew |last2=Greiciua |first2=Tony |title=Curiosity Captured Two Solar Eclipses on Mars |url= https://www.nasa.gov/feature/jpl/curiosity-captured-two-solar-eclipses-on-mars |date=4 April 2019 |work=[[NASA]] |access-date=5 April 2019 }}</ref><ref name="GIZ-20190405">{{cite news |last=Dvorsky |first=George |title=Curiosity Rover Spots a Pair of Solar Eclipses on Mars |url= https://gizmodo.com/curiosity-rover-spots-a-pair-of-solar-eclipses-on-mars-1833834577 |date=5 April 2019 |work=[[Gizmodo]] |access-date=5 April 2019 }}</ref>

{{expand section|date=August 2012}}

{{multiple images | caption_align=center |header=Solar eclipses by two moons of Mars viewed by ''Curiosity'' (March, 2019)<ref name="NASA-20190404" /><ref name="GIZ-20190405" /> |align=center |direction=horizontal |width=300 |image1=PIA23134-MarsCuriosityRover-DeimosEclipse-20190317.gif |caption1=[[Deimos (moon)|Deimos]] (17 March 2019) |width1= |image2=PIA23133-MarsCuriosityRover-PhobosEclipse-20190326.gif |caption2=[[Phobos (moon)|Phobos]] (27 March 2019) |width2= |footer= }}



On 11 April 2019, NASA announced that the [[Curiosity (rover)|''Curiosity'' rover]] on the planet [[Mars]] drilled into, and closely studied, a "[[Clay|clay-bearing unit]]" which, according to the rover Project Manager, is a "major milestone" in ''Curiosity''{{'s}} journey up [[Mount Sharp]].<ref name="NASA-20190411">{{cite news |last=Good |first=Andrew |title=Curiosity Tastes First Sample in 'Clay-Bearing Unit' |url= https://www.jpl.nasa.gov/news/news.php?feature=7376 |date=11 April 2019 |work=[[NASA]] |access-date=12 April 2019 }}</ref>

<br />

[[File:PIA23138-MarsCuriosityRover-Drills-ClayBearingUnit-20190406.gif|thumb|center|300px|<div align="center">''Curiosity'' drilled into a "[[Clay|clay-bearing unit]]".<ref name="NASA-20190411" /></div>]]

[[File:PIA23241-MarsCuriosityRover-MovingClouds-20190512.gif|thumb|center|300px|<div align="center">''Curiosity'' views moving clouds (12 May 2019)</div>]]

[[File:PIA23179-MarsCuriosityRoverExploersMountSharp-20190515.jpg|thumb|center|600px|<div align="center">Mars ''Curiosity'' rover explores Mount Sharp (15 May 2019)</div>]]



During June 2019, while still studying the clay-bearing unit, ''Curiosity'' detected the highest levels of [[Methane on Mars|methane]] gas, 21 parts per billion, compared to the typical 1 part per billion the rover detects as normal background readings. The levels of methane dropped quickly over a few days, leading NASA to call this event one of several methane plumes that they have observed before but without any observable pattern. The rover lacked the necessary instrumentation to determine if the methane was biological or inorganic in nature.<ref>{{cite web|url= https://www.nasa.gov/feature/jpl/curiosity-detects-unusually-high-methane-levels |title=Curiosity's Mars Methane Mystery Continues |date=23 June 2019 |access-date=25 June 2019 |work=[[NASA]] }}</ref><ref>{{cite web|url= https://www.engadget.com/2019/06/25/nasa-methane-plume-curiosity/ |title=NASA just witnessed its biggest methane gas emission on Mars |first=MAriella |last=Moon |date=24 June 2019 |access-date=24 June 2019 |work=[[Engadget]] }}</ref><ref name="NYT-20190626">{{cite news |last=Overbye |first=Dennis |author-link=Dennis Overbye |title=With a Poof, Mars Methane Is Gone - Last week, NASA's Curiosity rover detected a belch of natural gas on the red planet. The gas has since dissipated, leaving only a mystery. |url= https://www.nytimes.com/2019/06/25/science/mars-methane-nasa.html |date=26 June 2019 |work=[[The New York Times]] |access-date=26 June 2019 }}</ref>

----

[[File:PIA23341-MarsCuriosityRover-WoodlandBay-20190531.jpg|thumb|center|600px|<div align="center">''Curiosity'' viewed at Woodland Bay from space (31 May 2019)</div>]]

{{multipleimage|caption_align=center|header=[[List of rocks on Mars#2012 – Curiosity rover (Mars Science Laboratory)|Strathdon rock]] (July 2019) |align=center |direction=horizontal|image1=PIA23348-MarsCuriosityRover-StrathdonRock-20190709.jpg|caption1=Overall |width1=339|image2=PIA23347-MarsCuriosityRover-StrathdonRock-CloseUp-20190710.jpg|caption2=CloseUp|width2=257|footer= }}

[[File:PIA23377-MarsCuriosityRover-MovesAcrossClayUnit-20190720.gif|thumb|center|600px|<div align="center">''Curiosity'' moves across clay unit (May–July 2019)</div>]]



== Third extended mission (October 2019 - September 2022) ==

====Sol 7====

The third extended mission began on 1 October 2019 - the rover's 2544th sol on Mars.<ref>{{Cite journal |last=Vasavada |first=Ashwin |date=5 April 2022 |title=Mission Overview and Scientific Contributions from the Mars Science Laboratory Curiosity Rover After Eight Years of Surface Operations |journal=Space Science Reviews |volume=218 |issue=3 |page=14 |doi=10.1007/s11214-022-00882-7 |pmid=35399614 |pmc=8981195 |bibcode=2022SSRv..218...14V }}</ref>



In October 2019, evidence in the form of [[magnesium sulfate]] deposits left behind in ways that suggested evaporation, uncovered by the ''Curiosity'' rover on Mount Sharp, was reported of a {{convert|150|km|mi|abbr=on}} wide ancient basin in Gale crater that once may have contained a salty lake.<ref name="NASA-20191007">{{cite web |last1=Good |first1=Andrew |last2=Johnson |first2=Alana |title=NASA's Curiosity Rover Finds an Ancient Oasis on Mars |url= https://www.jpl.nasa.gov/news/news.php?feature=7514 |date=7 October 2019 |work=[[NASA]] |access-date=7 October 2019 }}</ref><ref name="NG-20191007">{{cite journal |author=Rapin, W. |display-authors=et al. |title=An interval of high salinity in ancient Gale crater lake on Mars |date=7 October 2019 |journal=[[Nature Geoscience]] |volume=317 |issue=11 |pages=889–895 |doi=10.1038/s41561-019-0458-8 |bibcode=2019NatGe..12..889R |s2cid=203848784 |url=https://hal.archives-ouvertes.fr/hal-02344302/file/wrapin_manuscript_sulfate_enrichments_final.pdf }}</ref>[[File:PIA23977-MarsCuriosityRover-DrillHoles-20200701.jpg|thumb|center|600px|<div align="center">[[List of rocks on Mars#2012 – Curiosity rover (Mars Science Laboratory)|Mars rocks]] - 26 drill holes (1 July 2020)</div>]]

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''13 August 2012'''

|}



In January 2020, a report was presented that compared ''Curiosity'' at the time of its landing on Mars in 2012, with the rover over seven years later in 2020.<ref name="INV-20200127">{{cite news |last=Rabie |first=Passant |title=Mars: Viral Photo Shows What 7 Years On The Red Planet Did To Curiosity Rover - The Red Planet Took A Toll On This Little Robot |url=https://www.inverse.com/science/mars-curiosity-rover-after-7-years-photo |date=27 January 2020 |work=[[Inverse (website)|Inverse]] |access-date=27 January 2020}}</ref>

[[File:President Obama Phones Mars Rover Team.jpg|left|frame|300x300px|President [[Barack Obama]] talks on the phone with NASA's Curiosity Mars rover team aboard [[Air Force One]] during a flight to Ouffutt [[Air Force Base]] in [[Nebraska]].<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/obama20120813.html NASA - President Obama Phones Mars Rover Team]</ref>]]

<br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br /><br />

----



In February 2020, scientists reported the detection of [[thiophene]] [[Organic compound|organic molecules]] by the [[Curiosity (rover)|''Curiosity'' rover]] on the planet [[Mars]]. It is not currently known if the detected thiophenes — usually associated on Earth with [[kerogen]], [[coal]] and [[Petroleum|crude oil]] — are the result of biological or non-biological processes.<ref name="AB-20200224">{{cite journal |last1=Heinz |first1=Jacob |last2=Schulze-Makuch |first2=Dirk |title=Thiophenes on Mars: Biotic or Abiotic Origin? |date=24 February 2020 |journal=[[Astrobiology (journal)|Astrobiology]] |volume=20 |issue=4 |pages=552–561 |doi=10.1089/ast.2019.2139 |pmid=32091933 |bibcode=2020AsBio..20..552H |doi-access=free }}</ref><ref name="PHYS-20200305">{{cite news |author=Washington State University |title=Organic molecules discovered by Curiosity Rover consistent with early life on Mars: study |url=https://phys.org/news/2020-03-molecules-curiosity-rover-early-life.html |date=5 March 2020 |work=[[Phys.org]] |access-date=5 March 2020 |author-link=Washington State University }}</ref>

====Sol 8====

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''14 August 2012'''

|}



In April 2020, scientists began operating the rover remotely from their homes due to the [[COVID-19 pandemic]].<ref name="NASA-20200414">{{cite news |last1=Good |first1=Andrew |last2=Johnson |first2=Alana |title=NASA's Curiosity Keeps Rolling As Team Operates Rover From Home |url=https://www.jpl.nasa.gov/news/news.php?feature=7638 |date=14 April 2020 |work=[[NASA]] |access-date=14 April 2020 }}</ref>

{{expand section|date=August 2012}}



{{multipleimage |caption_align=center|header=Curiosity's views (released July 2020) |direction=horizontal |align=center |width= |image1=PIA23974-MarsCuriosityRover-ViewFromTopOfGreenheughPediment-20200706.jpg |caption1=Pediment top view |width1=134|image2=PIA23975-MarsCurosityRover-NodulesNearPedimentSlope-20200706.jpg |caption2=Nodules found |width2=325 |image3=PIA23973-MarsCuriosityRover-SulfateBearingArea-20200706.jpg |caption3=Sulfate area |width3=98 |footer= }}

<br />



[[File:PIA24039-MarsCuriosityRover-DustDevil-20200809.gif|thumb|center|565px|<div align="center">Dust devil on Mars - viewed by the ''Curiosity'' rover (9 August 2020)</div>]]

----



On 29 August 2020, NASA released several videos taken by the ''Curiosity'' rover, including those involving [[dust devils]], as well as very high resolution images of the related local martian terrain.<ref name="SPC-20200829">{{cite news |last=Wall |first=Mike |title=Mars dust devil! Curiosity rover spots Red Planet twister (photos) - Curiosity doesn't always have its eyes on the ground. |url=https://www.space.com/mars-dust-devil-curiosity-rover.html |date=29 August 2020 |work=[[Space.com]] |access-date=29 August 2020 }}</ref>

====Sol 9====



[[File:PIA24262-MarsCuriosityRover-HousedonHill-20201221.jpg|thumb|center|800px|<div align="center">Housedon Hill distant outcrop mosaic viewed by ''Curiosity'' rover between 9 September – 23 October 2020 (posted 21 December 2020)</div>]][[File:PIA24266-MarsCuriosityRover-MountMercou-20210304.jpg|thumb|600px|center|<div align="center">Mount Mercou − viewed by ''Curiosity'' (4 March 2021)</div>]]

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

[[File:PIA24622-MarsCuriosityRover-MontMercou-20210319.jpg|thumb|600px|center|<div align="center">Mont Mercou beneath Martian clouds (19 March 2021)</div>]]

! style="margin; background: lavender;" colspan="3" | '''15 August 2012'''

In June 2021, scientists determined that the methane concentration around ''Curiosity'' varied according to the time of sol, with methane present only at night. This explains the difference in methane levels detected by ''Curiosity'' and the [[Trace Gas Orbiter]] (an open question since 2016), although it does not explain what is creating the methane or why the methane seems to be more short-lived than current models predict.<ref>{{Cite web|last=mars.nasa.gov|title=First You See It, Then You Don't: Scientists Closer to Explaining Mars Methane Mystery|url=https://mars.nasa.gov/news/8976/first-you-see-it-then-you-dont-scientists-closer-to-explaining-mars-methane-mystery?site=msl|access-date=2021-06-30|website=NASA’s Mars Exploration Program|language=en}}</ref>

|}

On 3 July 2021, the ''Curiosity'' rover viewed the "[[:File:PIA24643-MarsCuriosityRover-RafaelNavarroMountain-20210703.jpg|Rafael Navarro Mountain]]" area.

[[File:PIA24764-MarsCuriosityRover-32DrillHoles-20210817.jpg|thumb|600px|center|<div align="center">''Curiosity'' − [[List of rocks on Mars#2012 – Curiosity rover (Mars Science Laboratory)|32 drill holes]] (17 August 2021)</div>]]

On 1 November 2021, astronomers reported detecting, in a "first-of-its-kind" process based on [[Sample Analysis at Mars|SAM instruments]], [[organic molecules]], including [[benzoic acid]], [[ammonia]] and other related unknown compounds, on the [[Mars|planet Mars]] by the [[Curiosity (rover)|''Curiosity'']] rover.<ref name="INV-20211101">{{cite news |last=Rabie |first=Passant |title=Organic Molecules Found On Mars For The First Time - The Curiosity rover demonstrated a useful technique to search for Martian biosignatures. |url=https://www.inverse.com/science/organic-molecules-found-on-mars-for-the-first-time |date=1 November 2021 |work=[[Inverse (website)|Inverse]] |accessdate=2 November 2021 }}</ref><ref name="NAT-20211101">{{cite journal |author=Millan, M. |display-authors=et al. |title=Organic molecules revealed in Mars's Bagnold Dunes by Curiosity's derivatization experiment |url=https://www.nature.com/articles/s41550-021-01507-9 |date=1 November 2021 |journal=[[Nature Astronomy]] |volume=6 |pages=129–140 |doi=10.1038/s41550-021-01507-9 |s2cid=240490556 |accessdate=2 November 2021 }}</ref>

[[File:PIA24937-MarsCuriosityRover-20211116.jpg|thumb|center|600px|<div align="center">Panorama - viewed by ''Curiosity'' (16 November 2021)</div>]]On 17 January 2022, scientists reported finding an unusual signal of carbon isotopes on Mars by the ''Curiosity'' rover which may (or may not) be associated with ancient Martian life and suggesting, according to the scientists, that microbes residing underground may have emitted the "enriched carbon as methane gas". However, abiotic sources of the unusual carbon signal have not been completely ruled out.<ref name="SCI-20220117">{{cite journal |last=Voosen |first=Paul |title=Mars rover detects carbon signature that hints at past life source - Dramatically "light" carbon could also be explained by atmospheric reactions or cosmic dust |url=https://www.science.org/content/article/mars-rover-detects-carbon-signature-hints-past-life-source |date=17 January 2022 |journal=[[Science (journal)|Science]] |volume=375 |issue=6578 |page=254 |doi=10.1126/science.ada0234 |pmid=35050666 |s2cid=246151537 |accessdate=18 January 2022 }}</ref><ref name="PNAS-20220125">{{cite journal| author=House, Christopher H. |display-authors=et al. |title=Depleted carbon isotope compositions observed at Gale crater, Mars |date=25 January 2022 |journal=[[Proceedings of the National Academy of Sciences of the United States of America|PNAS]] |volume=119 |issue=4 |doi=10.1073/pnas.2115651119 |pmid=35042808 |pmc=8795525 |bibcode=2022PNAS..11915651H }}</ref><ref name="UT-20220121">{{cite news |last=Gough |first=Evan |title=Curiosity Sees a Strong Carbon Signature in a Bed of Rocks |url=https://www.universetoday.com/154139/curiosity-sees-a-strong-carbon-signature-in-a-bed-of-rocks/ |date=21 January 2022 |work=[[Universe Today]] |accessdate=22 January 2022 }}</ref>



In April 2022, Mars Science Laboratory was renewed for a fourth extended mission, which will include the exploration of the sulfate-bearing unit.<ref>{{Cite web |last=Talbert |first=Tricia |date=2022-04-25 |title=NASA Extends Exploration for 8 Planetary Science Missions |url=http://www.nasa.gov/feature/nasa-extends-exploration-for-8-planetary-science-missions |access-date=2022-04-28 |website=NASA}}</ref>

{| class="wikitable"

[[File:PIA25288-MarsCuriosityRover-DoorFracture-EastCliffs-20220507.jpg|thumb|center|800px|<div align=center>Mars Curiosity Rover - East Cliffs (noted door-shaped fracture) (7 May 2022)</div>]]

! style="text-align: center; background: #F4C430;"|Date

[[File:MarsCuriosityRover-36DrillHoles.jpg|thumb|600px|center|<div align="center">''Curiosity'' − [[List of rocks on Mars#2012 – Curiosity rover (Mars Science Laboratory)|36 drill holes]]</div>]]

! style="text-align: center; background: #F4C430;"|Event

[[File:PIA25733-MarsCuriosityRover-GedizVallis-20221107.jpg|thumb|center|800px|<div align="center">Panorama of rocks viewed by [[Curiosity (rover)|''Curiosity'']] on the slopes of [[Aeolis Mons|Mount Sharp]] at Gediz Valles (November 7, 2022).</div>]]

! style="text-align: center; background: #F4C430;"|Notes

[[File:PIA25732-MarsCuriosityRover-MarkerBandValley-20221216.jpg|thumb|center|800px|<div align="center">Panorama of rocks viewed by [[Curiosity (rover)|''Curiosity'']] on the slopes of [[Aeolis Mons|Mount Sharp]] at Marker Band Valley (December 16, 2022).</div>]]

|-

| {{As of|2012|08|15}} || Self-diagnosis and route planning || The rover will spend several days performing instrument checks and mobility tests.<ref name='driving tests'> {{cite news | first = William Harwood | title = Rover software updated, first driving tests on tap | date = August 14, 2012 | url = http://news.cnet.com/8301-11386_3-57493178-76/rover-software-updated-first-driving-tests-on-tap/ | work = C-Net News | accessdate = 2012-08-15}}</ref><ref name='first drive'/> The science and operations teams have identified at least six possible routes to the base of the mountain, and estimate about a year studying the rocks and soil of the crater floor while ''Curiosity'' slowly makes its way to the base of Mount Sharp.<ref name='driving tests'/><ref> {{cite news | title = Mars rover could start moving in a week | date = 15 August 2012 | url = http://edition.cnn.com/2012/08/14/us/mars-curiosity/index.html?hpt=hp_c2 | work = CNN News | accessdate = 2012-08-15}}</ref> Its first drive is planned to start in September to a rock formation called ''Glenelg'' about {{convert|460|m |ft}} to the East.<ref> {{cite web | url = http://www.nasa.gov/mission_pages/msl/multimedia/pia16064b.html | title = MSL Media Teleconference on August 17, 2012 | accessdate = 2012-08-17 | publisher = NASA}}</ref>

|}



== Fourth extended mission (October 2022 - Present) ==

----

The rover began its fourth extended mission on 1 October 2022, which will last until October 2025.<ref>{{Cite web |title=NASA Planetary Mission Senior Reviews - PMSR {{!}} Science Mission Directorate |url=https://science.nasa.gov/solar-system/documents/senior-review |access-date=2023-06-04 |website=science.nasa.gov}}</ref>



In January 2023, the Curiosity Rover viewed and studied the "Cacao" meteorite.

<br />

[[File:PIA25737-MarsCuriosityRover-CacaoMeteorite-20230128.jpg|thumb|center|500px|<div align="center">''Curiosity'' views the "Cacao" meteorite (28 January 2023)</div>]]



In August 2023, ''Curiosity'' explored the upper [[Gediz Vallis Ridge]].<ref>{{Cite web |last=Laboratory |first=Deborah Padgett, OPGS Task Lead at NASA's Jet Propulsion |title=Sols 3923-3925: Approaching the Ridgetop – "Bermuda Triangle" Ahead! |url=https://mars.nasa.gov/msl/mission-updates/9465/sols-3923-3925-approaching-the-ridgetop-bermuda-triangle-ahead |access-date=2023-09-16 |website=NASA Mars Exploration |language=en}}</ref><ref>{{Cite web |last=London |first=Emma Harris, Graduate Student at Natural History Museum |title=Sols 3930-3931: Wrapping up at the Ridge |url=https://mars.nasa.gov/msl/mission-updates/9470/sols-3930-3931-wrapping-up-at-the-ridge |access-date=2023-09-16 |website=NASA Mars Exploration |language=en}}</ref> A panoramic view of the ridge is [[:File:PIA26019-MarsCuriosityRover-GedizVallisRidge-20230814.jpg|here]], and a 3D rendered view is [[:File:PIA26020-MarsCuriosityRover-GedizVallisRidge-3dRendered-Aug2023.jpg|here]].

====Sol 10====



[[File:PIA26042-MarsCuriosityRover-PathToGedizVallisRidge-Animation-Aug2023.gif|thumb|center|500px|<div align="center">The path of ''Curiosity'' to [[Gediz Vallis Ridge]] and beyond (August 2023)</div>]]

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''16 August 2012'''

|}



{{multiple images |header=A Day on Mars (''Curiosity'' rover; 8 November 2023) |direction=horizontal |align=center | width= |image1=PIA26209-MarsDay-HazcamNW-20231108.webm |caption1=<div align="center">[[:File:PIA26209-MarsDay-HazcamNW-20231108.webm|NorthWest Hazcam]]</div> |width1=250 |image2=PIA26209-MarsDay-HazcamSE-20231108.webm |caption2=<div align="center">[[:File:PIA26209-MarsDay-HazcamSE-20231108.webm|SouthEast Hazcam]]</div> |width2=250 |footer= }}In February 2024, Curiosity completed its 40th successful drilling,<ref>{{Cite web |last=Thompson |first=Lucy |title=Sols 4114-4115: Bingo! It's Official – Curiosity's 40th Successful Drill Hole on Mars! |url=https://mars.nasa.gov/msl/mission-updates/9557/sols-4114-4115-bingo-its-official-curiositys-40th-successful-drill-hole-on-mars |access-date=2024-03-02 |website=NASA Mars Exploration |language=en}}</ref><ref>{{Cite web |last=Purdy |first=Sharon |title=Sols 4107-4109: Drilling Mineral King |url=https://mars.nasa.gov/msl/mission-updates/9554/sols-4107-4109-drilling-mineral-king |access-date=2024-03-02 |website=NASA Mars Exploration |language=en}}</ref> of a rock named "Mineral King" in Gediz Vallis.

[[Image:NLA 398381736EDR F0030000NCAM15000M.JPG|300px]]



==Current status==

This image was taken by Navcam: Left A (NAV_LEFT_A) onboard NASA's Mars rover Curiosity <ref>[http://mars.jpl.nasa.gov/msl/multimedia/raw/?rawid=NLA_398381736EDR_F0030000NCAM15000M_&s=10 Mars Science Laboratory: Raw Images]</ref>

----



===Weather===

<br />

* [https://cab.inta-csic.es/rems/marsweather.html Current Weather Report] {{Webarchive|url=https://web.archive.org/web/20130621012418/https://cab.inta-csic.es/rems/marsweather.html |date=21 June 2013 }} on Mars by the [[Curiosity (rover)|''Curiosity'' rover]]


* [https://mars.nasa.gov/insight/weather/ Current Weather Report] on Mars by the ''[[InSight]]'' lander<ref name="GZM-20190220">{{cite news |last=Dvorsky |first=George |title=You Can Now Check the Weather on Mars Every Day |url= https://gizmodo.com/you-can-now-check-the-weather-on-mars-every-day-1832752785 |date=20 February 2019 |work=[[Gizmodo]] |access-date=20 February 2019 }}</ref><ref name="AT-20190220">{{cite web |last=Berger |first=Eric |title=With the best air pressure sensor ever on Mars, scientists find a mystery |url= https://arstechnica.com/science/2019/02/some-weird-things-are-happening-with-air-pressure-on-mars/ |date=20 February 2019 |work=[[Ars Technica]] |access-date=20 February 2019 }}</ref>

====Sol 11====

*[https://mars.nasa.gov/mars2020/weather/ Current Weather Report] on Mars by the [[Perseverance (rover)|''Perseverance'' rover]]


{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''17 August 2012'''

|-

| style="text-align: center;margin; background: white;" | Status of MSL Mission [http://www.youtube.com/watch?v=mz2eVthmNn4 NASA Video]

|}


{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: #FF6700;" colspan="4" | '''MSL Curiosity rover Experiment No. 1<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16072.html NASA - Curiosity's First Rock Star]</ref>'''

|-

! style="text-align: center; background: #F4C430;"|Image

! style="text-align: center; background: #F4C430;"|Instrument

! style="text-align: center; background: #F4C430;"|Notes

! style="text-align: center; background: #F4C430;"|Status

|-

| [[File:677559main pia16073-unanno.jpg|center|framed|100x100px]] || style="text-align: center;" | Chemistry and Camera (ChemCam) instrument || This close-up image shows the first target NASA's Curiosity rover aims to zap with its Chemistry and Camera (ChemCam) instrument. ChemCam will be firing a laser at this rock, provisionally named N165, and analyzing the glowing, ionized gas, called plasma, that the laser excites. The instrument will analyze that spark with a telescope and identify the chemical elements in the target.<ref name=autogenerated1>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16073.html NASA - Curiosity's First Rock Star, Up-Close]</ref> || style="background: yellow; text-align: center;" | {{Black| '''Planned''' <ref name=autogenerated1 />}}

|}



===Location and travel statistics===

* [https://mars.nasa.gov/msl/mission/where-is-the-rover/ This up-to-date NASA link shows ''Curiosity''{{'}} travels and present location]

[[File:Curiosity Distance Graph.svg|center|thumb|440x440px|Distance traveled over time by ''Curiosity'']]

As of {{CURRENTMONTHNAME}} {{CURRENTDAY}}, {{CURRENTYEAR}}, ''Curiosity'' has been on the [[Mars|planet Mars]] for {{Curiosity Mission Timer}} [[Martian day|sols]] ({{time interval|6 August 2012 05:17:57|show=d|disp=raw}} [[day|total days]]) since landing on 6 August 2012. Since 11 September 2014, ''Curiosity'' has been [http://mars.jpl.nasa.gov/msl/mission/whereistherovernow/ exploring] the slopes of [[Aeolis Mons|Mount Sharp]],<ref name="NASA-20140911" /><ref name="NYT-20140911" /> where more information about the [[Geological history of Mars|history of Mars]] is expected to be found.<ref name="NASA-20130806" /> As of 26 January 2021, the rover has traveled over {{convert|24.15|km|mi|abbr=on}} and climbed over {{convert|327|m|ft|abbr=on}} in elevation<ref name="NASA-20130827a">{{cite web |author=Staff |title=PIA17355: Curiosity's Progress on Route from 'Glenelg' to Mount Sharp |url= http://mars.nasa.gov/msl/mission/whereistherovernow/|date=19 January 2017 |work=[[NASA]] |access-date=22 January 2017 }}</ref><ref name="NASA-20161213a" /><ref name="NASA-20180130">{{cite web |author=Staff |title=Wide-Angle Panorama from Ridge in Mars' Gale Crater |url= https://www.jpl.nasa.gov/spaceimages/details.php?id=PIA22210 |date=30 January 2018 |work=[[NASA]] |access-date=31 January 2018 }}</ref> to, and around, the mountain base since arriving at [[Bradbury Landing]] in August 2012.<ref name="NASA-20130827a" /><ref name="NASA-20161213a" />

{{multiple image

| header = The [[Curiosity (rover)|''Curiosity'' rover]] is exploring the slopes of [[Aeolis Mons|Mount Sharp]].<ref name="NASA-20140911" /><ref name="NYT-20140911" />

| align = center

| total_width = 1000

| direction = horizontal

| image1 = PIA17946-MarsCuriosityRover-PlannedRoute-20140218.jpg

| width1 =

| alt1 =

| caption1 = [http://mars.jpl.nasa.gov/msl/mission/whereistherovernow/ Close-up map] - planned route from "Dingo Gap" to "Kimberley" (KMS-9) ([http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=6015 HiRISE image])<br />(18 February 2014/Sol 547).

| image2 = TraverseMap-MarsCuriosityRover-Sol2692-20200303.jpg

| width2 =

| alt2 =

| caption2 = [http://mars.jpl.nasa.gov/msl/mission/whereistherovernow/ Traverse map] - ''Curiosity'' has traveled over {{convert|21.92|km|mi|abbr=on}} since leaving its "''start''" point in Yellowknife Bay on 4 July 2013 (now beyond the "[[:File:Curiosity Rover Landing Site - Quadmapping Yellowknife.jpg|3-sigma safe-to-land ellipse]]" [[:File:Mars Science Laboratory landing ellipse reduced.jpg|border]]) ([https://mars.jpl.nasa.gov/msl/mission/whereistherovernow/?ImageID=9836 HiRISE image])<br />(3 March 2020/Sol 2692).

| image3 = PIA23412-MarsCuriosityRover-Mid2019Map-20190822.jpg

| width3 =

| alt3 =

| caption3 = [http://mars.jpl.nasa.gov/msl/mission/whereistherovernow/ Context map] - ''Curiosity''{{'s}} trip to [[Aeolis Mons|Mount Sharp]] (''star'' = landing)<br />(22 August 2019/Sol 2504).

| image4 = Curiosity Traverse Path showing its current location.png

| width4 =

| alt4 =

| caption4 = ''Curiosity'' traverse path showing location as of June 2021. [https://mars.nasa.gov/msl/mission/where-is-the-rover/ An up-to-date live link]

| footer = Credit: NASA/JPL-Caltech/University of Arizona

| footer_align = right

}}

<br />

<br />

{{wide image|LocationMap-MarsCuriosityRover-Sol2692-20200303.jpg|800px|align-cap=center|Location map - [[Curiosity (rover)|''Curiosity'' rover]] at the base of [[Aeolis Mons|Mount Sharp]] - as viewed from Space ([[Mars Reconnaissance Orbiter|MRO]]; [[HiRISE]]; 3 March 2020/Sol 2692).}}

{{wide image|PIA25914-MarsCuriosityRover-QuadrantThemes-20230608.jpg|800px|align-cap=center|Mars Curiosity Rover - Quadrant Themes (8 June 2023)}}



===Equipment status===

----

Since early 2015, the percussive mechanism in the drill that helps chisels into rock has had an intermittent electrical [[short circuit]].<ref name=drill-fault>{{cite web | url=https://spaceflightnow.com/2016/12/29/internal-debris-may-be-causing-problem-with-mars-rovers-drill/ | title=Internal debris may be causing problem with Mars rover's drill | publisher=Spaceflight Now | first=Stephen | last=Clark | date=29 December 2016 | accessdate=20 March 2024}}</ref>



In December 2016, the motor inside the drill caused a malfunction that prevented the rover from moving its robotic arm and driving to another location.<ref name="popmech20161213">{{cite news |url= http://www.popularmechanics.com/space/moon-mars/a24288/nasa-curiosity-arm-drill-stuck/ |title=NASA Is Trying to Get Mars Rover Curiosity's Arm Unstuck |work=Popular Mechanics |agency=Associated Press |date=13 December 2016 |access-date=18 January 2017}}</ref> The fault is in the drill feed motor - internal debris is suspected.<ref name=drill-fault/> The fault was determined to be limited to the drill mechanism and the rover started moving again on 9 December. The robotic arm is functional, and the ''Curiosity'' team performed diagnostics on the drill mechanism throughout 2017.<ref>{{Cite web|url= https://mars.nasa.gov/msl/mission/mars-rover-curiosity-mission-updates/?View=All |title=Curiosity Mission Updates - Mars Science Laboratory}}</ref> On 4 June 2018, NASA announced that ''Curiosity''{{'s}} ability to drill has been sufficiently restored by changing the drilling methods.<ref name="NASA-20180604" />

====Sol 12====



Since 15 September 2018, a glitch in ''Curiosity''<nowiki/>'s active computer (Side-B) has prevented ''Curiosity'' from storing science and key engineering data.<ref name=":0">{{Cite news|url= https://www.nasa.gov/feature/jpl/curiosity-rover-to-temporarily-switch-brains|title=Curiosity Rover to Temporarily Switch 'Brains'|last=Greicius|first=Tony|date=2018-10-02|work=NASA|access-date=2018-10-09|language=en}}</ref> On 3 October 2018, the [[Jet Propulsion Laboratory|JPL]] began operating ''Curiosity'' on its backup computer (Side-A).<ref name=":0" /> ''Curiosity'' will store science and engineering data normally using its Side-A computer until the cause of the glitch in Side-B is determined and remedied.<ref name=":0" />

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

! style="margin; background: lavender;" colspan="3" | '''18 August 2012'''

|}



==Images==

{{expand section|date=August 2012}}



===Self-portraits===

<br />

{{multiple image |align=center |total_width=600 |header=[[Curiosity (rover)|''Curiosity'' rover]] on [[Mount Sharp]] on [[Mars]] — self-portraits

|width1=5247 |height1=7295 |image1=PIA16239 High-Resolution Self-Portrait by Curiosity Rover Arm Camera.jpg |caption1="[[Rocknest (Mars)|Rocknest]]"<br />(Oc2012)

|width2=5831 |height2=8109 |image2=PIA16937-MarsCuriosityRover-SelfPortraitAtJohnKlein-20130510.jpg |caption2="[[List of rocks on Mars#Curiosity|JohnKlein]]"<br />(Ma2013)

|width3=4576 |height3=6669 |image3=PIA18390-MarsCuriosityRover-SelfPortraitAtWindjana-20140512.jpg |caption3="[[List of rocks on Mars#Curiosity|Windjana]]"<br />

(Ma2014)

|width4=1988 |height4=2765 |image4=PIA19142-MarsCuriosityRover-SelfPortrait-Mojave-20150131.jpg |caption4="[[List of rocks on Mars#Curiosity|Mojave]]"<br />(Ja2015)

|width5=818 |height5=810 |image5=PIA19808-MarsCuriosityRover-AeolisMons-BuckskinRock-20150805.jpg |caption5="[[List of rocks on Mars#Curiosity|Buckskin]]"<br />

(Aug2015)

|width6=5082 |height6=8260 |image6=PIA19920-MarsCuriosityRover-SelfPortrait-Sol1126-20151006-crop.jpg |caption6="[[List of rocks on Mars#Curiosity|BigSky]]"<br />

(Oc2015)

|width7=3032 |height7=4216 |image7=PIA20316-MarsCuriosityRover-SelfPortrait-SandDune-20160119.jpg |caption7="[[List of rocks on Mars#Curiosity|Namib]]"<br />(Ja2016)

|width8=1673 |height8=2121 |image8=PIA20844-MarsCuriosityRover-SelfPortrait-Sol1466-20160920.jpg |caption8="[[List of rocks on Mars#Curiosity|Murray]]"<br />(Se2016)

}}

{{multiple image |align=center |total_width=600 |header=<!---[[Curiosity (rover)|''Curiosity'' rover]] on [[Mount Sharp]] on [[Mars]] — self-portraits--->

|width9=3864 |height9=5040|image9=PIA22207-Mars-CuriosityRover-SelfPortrait-20180123.jpg |caption9="[[List of rocks on Mars#Curiosity|VeraRub]]"<br />(Ja2018)

|width10=4392 |height10=6066|image10=NASA-CuriosityRover-Selfie-June2018.jpg |caption10="[[Timeline of Mars Science Laboratory#2018 events|DustStrm]]"<br />

(Ju2018)

|width11=4050 |height11=5760 |image11=PIA22960-MarsCuriosityRover-SelfPortrait-RockHall-VeraRubinRidge-20190115.jpg |caption11="[[List of rocks on Mars#Curiosity|VeraRub]]"<br />(Ja2019)

|width12=4811 |height12=7174 |image12=PIA23240-MarsCuriosityRover-SelfPortrait-Aberlady-Kilmarie-20190512.jpg |caption12="[[List of rocks on Mars#Curiosity|Aberlady]]"<br />(Ma2019)

|width13=1792 |height13=3276 |image13=PIA23378-MarsCuriosityRover-SelfPortrait-GlenEtive-20191011.jpg|caption13="[[List of rocks on Mars#Curiosity|GlenE]]"<br />(Oc2019)

|width14=3774 |height14=5474

|image14=PIA24173-MarsCuriosityRover-SelfPortrait-20201112.jpg|caption14="[[List of rocks on Mars#Curiosity|MaryAnn]]"<br />(No2020)

|image15=MSL Sol 3070 - MAHLI (Version 2) (51084526931).jpg

|caption15="MtMercou"<br />(March 2021) |image16=PIA24938-MarsCuriosityRover-GreenheughPediment-20211120.jpg|caption16="[[List of rocks on Mars#Curiosity|Greenh]]"<br />(No2021)

|width16=3774 |height16=5474

}}

[[File:PIA23624-MarsCuriosityRover-HuttonDrillSite-20200226.jpg|thumb|600px|center|<div align="center">''Curiosity'' rover self-portrait ("Hutton" Drill Site; 26 February 2020)</div>]]



===Videos===

----

{{multiple image

| align = center

| image1 = MarsCuriosityRover- FirstYearOverview-20130802.ogv

| width1 = 200

| alt1 =

| caption1 = [[Curiosity (rover)|''Curiosity'' rover]] mission - One Year on [[Mars]] (6 August 2012 – 5 August 2013) ([[:File:MarsCuriosityRover- FirstYearOverview-20130802.ogv|03:58/file]])<br />(2 August 2013).<ref name="NYT-20130805a" /><ref name="NYT-20130805b" />

| image2 = MarsCuriosityRover-FirstYear-20130801.ogv

| width2 = 200

| alt2 =

| caption2 = [[Curiosity (rover)|''Curiosity'' rover]] views - First Year on [[Mars]] (6 August 2012 – 5 August 2013) ([[:File:MarsCuriosityRover-FirstYear-20130801.ogv|02:13/file]])<br />(1 August 2013).<ref name="NYT-20130805a" /><ref name="NYT-20130805b" />

| image3 = MarsCuriosityRover-PhobosEclipsesSun-20130820.ogv

| width3 = 200

|alt3 =

|caption3 = [[Curiosity (rover)|''Curiosity'']] views a [[Solar eclipses on Mars|''Solar Eclipse'']] by [[Phobos (moon)|Phobos]], largest of the two [[Moons of Mars]] (01:30/''[[Real time (media)|real-time]]'')<br />(20 August 2013).

}}



===Gallery===

<!--

<gallery>

====Sol 13====

Image:PIA17085-MarsCuriosityRover-TraverseMap-Sol351-20130801.jpg|First-Year and First-Mile [http://mars.jpl.nasa.gov/msl/mission/whereistherovernow/ Traverse Map] of the ''Curiosity'' rover on Mars (August 1, 2013; [http://photojournal.jpl.nasa.gov/jpeg/PIA16210.jpg 3-D]).

====Sol 14====

Image:PIA19674-Mars-GaleCrater-SurfaceMaterials-20150619.jpg|Gale crater - surface materials ([[False color|false colors]]; [[Thermal Emission Imaging System|THEMIS]]; [[2001 Mars Odyssey]]).

====Sol 15====

Image:Mars Science Laboratory landing ellipse reduced.jpg|''Curiosity'' rover - diagram noting "[[:File:Curiosity Rover Landing Site - Quadmapping Yellowknife.jpg|3-sigma safe-to-land ellipse]]".

====Sol 16====

Image:PIA17596-MarsCuriosityRover-AncientLake-20131209.jpg|Estimate of ancient lake on [[Aeolis Palus]] in [[Gale (crater)|Gale Crater]].<ref name="NYT-20131209" /><ref name="SCI-20131209" />

====Sol 17====

Image:Curiosity Rover Landing Site - Quadmapping Yellowknife.jpg|''Curiosity'' rover - image noting "[[:File:Mars Science Laboratory landing ellipse reduced.jpg|3-sigma safe-to-land ellipse]]".

====Sol 18====

Image:PIA18399-MarsCuriosityRover-NowOutside3SigmaLandingEllipse-20140627.jpg|''Curiosity'' viewed from space crosses edge of its "[[:File:Curiosity Rover Landing Site - Quadmapping Yellowknife.jpg|3-sigma safe-to-land ellipse]]" (June 27, 2014).

====Sol 19====

Image:PIA16064-Mars Curiosity Rover Treasure Map.jpg|''Curiosity''{{'s}} [[Bradbury Landing|landing site]] - Blue oval marks the base of [[Aeolis Mons|Mount Sharp]] (August 17, 2012).

====Sol 20====

Image:PIA16068 - Mars Curiosity Rover - Aeolis Mons - 20120817.jpg|Base of [[Aeolis Mons]], an area of varied terran that ''Curiosity'' is expected to study.<ref>[http://www.nasa.gov/mission_pages/msl/multimedia/pia16068.html NASA - The Promised Land]</ref>

====Sol 21====

Image:PIA16105 malin04ano-br2.jpg|Layers at the base of [[Aeolis Mons]] - dark rock in inset is same size as the ''Curiosity'' rover.

====Sol 22====

Image:PIA16225-MarsCuriosityRover-ScooperTest&MysteryObject-20121008a.jpg|''Curiosity'' finds a "bright object" in the [[Martian soil|sand]] at [[Rocknest (Mars)|Rocknest]] (October 7, 2012)<ref name="UT-20121009" /> ([http://photojournal.jpl.nasa.gov/jpeg/PIA16230.jpg close-up]).

====Sol 23====

Image:PIA16226-MarsCuriosityRover-FirstScoopOfSoil-20121007.jpg|First use of ''Curiosity''{{'s}} [[Curiosity rover#Robotic arm|scooper]] as it sifts a load of [[Martian soil|sand]] at [[Rocknest (Mars)|Rocknest]] (October 7, 2012).

====Sol 24====

Image:PIA16089.jpg|First [[Laser-induced breakdown spectroscopy|laser spectrum]] of [[chemical elements]] on the [[N165|Coronation rock]] (August 19, 2012).

====Sol 25====

Image:PIA18389-MarsCuriosityRover-MercuryTransitsSun-20140603.gif|Planet [[Mercury (planet)|Mercury]] transiting the [[Sun]] as viewed by the ''Curiosity'' rover (June 3, 2014).<ref name="NASA-20140610" />

====Sol 26====

Image:PIA17356-MarsCuriosityRover-EclipseOfSunByPhobos.jpg|[[Annular eclipse]] of the [[Sun]] by [[Phobos (moon)|Phobos]] as viewed by the ''Curiosity'' rover (August 20, 2013).

====Sol 27====

Image:PIA17352-MarsMoons-PhobosPassesDeimos-RealTime.gif|''Curiosity''{{'s}} view of the [[Moons of Mars|Mars moons]]: [[Phobos (moon)|Phobos]] passes [[Deimos (moon)|Deimos]] - in [[Real time (media)|real-time]] (August 1, 2013; video-gif).

====Sol 28====

Image:PIA17937-MarsCuriosityRover-FirstAsteroidImage-20140420.jpg|First [[asteroid]] image ([[Ceres (dwarf planet)|Ceres]] and [[4 Vesta|Vesta]]) from [[Mars]] - viewed by [[Curiosity (rover)|''Curiosity'']] (April 20, 2014).

====Sol 29====

Image:PIA17360-MarsCuriosityRover-Waypoint1-DarwinOutcrop-20130907.jpg|''Curiosity''{{'s}} SW view near [[List of rocks on Mars#Curiosity|Darwin Outcrop]] (lower-center) (Waypoint 1; September 7, 2013).

====Sol 30====

Image:PIA17938-MarsCuriosityRover-CrossingDingoGapDune-20140206.gif|''Curiosity''{{'s}} view of tracks while crossing the Dingo Gap [[sand dune]] (February 6, 2014; video-gif).

====Sol 31====

Image:PIA17944-MarsCuriosityRover-AfterCrossingDingoGapSanddune-20140209.jpg|''Curiosity''{{'s}} view after crossing the Dingo Gap [[sand dune]] (February 9, 2014; [http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=6012 raw color]).

Image:PIA17939-MarsCuriosityRover-AfterCrossingDingoGapSanddune-20140210.jpg|''Curiosity''{{'s}} view after crossing the Dingo Gap [[sand dune]] (February 10, 2014).

Image:PIA17959-MarsCuriosityRover-SandstoneErosion-20140225.jpg|''Curiosity''{{'s}} view of sandstone at different levels of erosion (February 25, 2014; [http://mars.jpl.nasa.gov/msl/multimedia/images/?ImageID=6097 raw color]).

Image:PIA18075-MarsCuriosityRover-TheKimberley-20140402.jpg|Map of ''Curiosity''{{'s}} drive to The Kimberley Waypoint (KMS-9; April 2, 2014).

Image:PIA18073-MarsCuriosityRover-TheKimberley-20140403.jpg|''Curiosity''{{'s}} view of The Kimberley Waypoint (KMS-9; April 2, 2014; [https://web.archive.org/web/20140407094635/http://mars.jpl.nasa.gov/msl/images/pia18074_SOL589-ncam-anaglyph-CYP-full.jpg 3-D]).

Image:PIA18077-MarsCuriosityRover-TheKimberley-BrightSpot-20140403.jpg|''Curiosity''{{'s}} view of a bright spot near "The Kimberley" (KMS-9; April 3, 2014).<ref name="HP-20140706">{{cite news |last=Speigel |first=Lee |title=Did Mars Curiosity Rover Snap Images Of A UFO? |url= https://www.huffingtonpost.com/2014/07/06/mars-curiosity-rover-ufo-pictures_n_5538801.html |date=July 6, 2014 |newspaper=[[Huffington Post]] |access-date=July 6, 2014 }}</ref>

Image:PIA18387-MarsCuriosityRover-Lebanon-IronMeteorite-20140525.jpg|''Curiosity''{{'s}} view of an [[iron meteorite]] (called "[[List of rocks on Mars#Curiosity|Lebanon]]") (May 25, 2014).

Image:PIA18401-MarsCuriosityRover-NovaRock-LaserSpark-20140712.jpg|First [[ChemCam|laser spark]] imaged on Mars by [[Curiosity (rover)|''Curiosity'']] ([[List of rocks on Mars#Curiosity|"Nova" rock]]; July 12, 2014; [https://web.archive.org/web/20140808083944/http://www.jpl.nasa.gov/video/?id=1317 video (01:07)]).

Image:PIA18408-MarsCuriosityRover-TraverseMap-Sol705-20140731.jpg|Map of ''Curiosity''{{'s}} drive to "[[:File:PIA18409-MarsCuriosityRover-HiddenValley-ncam-CYL-Sol705-20140731.jpg|Hidden Valley]]" (July 31, 2014).

Image:PIA18590-MarsCuriosityRover-HiddenValleyTracks-20140804.jpg|''Curiosity''{{'s}} tracks in the [[Martian soil|sands]] of "[[:File:PIA18409-MarsCuriosityRover-HiddenValley-ncam-CYL-Sol705-20140731.jpg|Hidden Valley]]" (August 4, 2014).

Image:PIA23047-MarsCuriosityRover-OnTheClayUnit-20190210.jpg|''Curiosity'' near a lot of clay material in "Glen Torridon" (February 10, 2019).

Image:PIA21718-Mars-CuriosityRover-IresonHill-MountSharp-20170202.jpg|''Curiosity'' views "Ireson Hill" on Mount Sharp (February 2, 2017).

Image:PIA19043-MarsCuriosityRover-CometSidingSpring-20141019.gif|Comet [[C/2013 A1]] during flyby of Mars (October 19, 2014).

Image:PIA19400-MarsCuriosityRover-GaleCrater-Sunset-20150415.jpg|Sunset - [[Gale crater]] (April 15, 2015).

Image:PIA19401-MarsCuriosityRover-GaleCrater-Sunset-Animation-20150415.gif|Sunset (animated) - [[Gale crater]] (April 15, 2015).

</gallery>

<!---Related "Gallery" Images - Extras

Image:PIA16239 High-Resolution Self-Portrait by Curiosity Rover Arm Camera.jpg|''Curiosity'' self-portrait on [[Mars]] at [[Rocknest (Mars)|"Rocknest"]] (October 31, 2012).

Image:PIA16937-MarsCuriosityRover-SelfPortraitAtJohnKlein-20130310.jpg|''Curiosity'' self-portrait on [[Mars]] at [[List of rocks on Mars#Curiosity|"John Klein"]] - ''after'' drilling (May 10, 2013).

Image:PIA18390-MarsCuriosityRover-SelfPortraitAtWindjana-20140512.jpg|''Curiosity'' self-portrait on [[Mars]] at [[List of rocks on Mars#Curiosity|"Windjana"]] - ''after'' drilling (May 12, 2014).

Image:PIA17751-MarsCuriosityRover-DentedWheelAfter3Miles-20131130.jpg|NOV-2013 - ''Curiosity''{{'s}} wheel - dents & holes - 3 miles on Mars (November 30, 2013).

Image:MarsCuriosityRover-WornWheel-20140218.jpg|FEB-2014 - ''Curiosity''{{'s}} wheel - dents & holes - 3 miles on Mars (February 18, 2014).

Image:MarsCuriosityRover-TracksAfterCrossing-DingoGapSandDune-20140206.jpg|''Curiosity''{{'s}} view of tracks

after crossing the Dingo Gap [[sand dune]] (February 6, 2014).

--->



===Wide images===

-->

{{wide image |PIA16768-MarsCuriosityRover-AeolisMons-20120920.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of [[Aeolis Mons|Mount Sharp]] (20 September 2012; [[Color balance|white balanced]]; [http://photojournal.jpl.nasa.gov/jpeg/PIA16769.jpg raw color]).}}


{{wide image|PIA16918-MarsCuriosityRover-RockNest-HiRezWB-20121116.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of the [[Rocknest (Mars)|Rocknest]] area - South is center/North at both ends; [[Aeolis Mons|Mount Sharp]] at SE horizon (somewhat left-of-center); [[Glenelg, Mars|Glenelg]] at East (left-of-center); rover tracks at West (right-of-center) (16 November 2012; [[Color balance|white balanced]]; [http://photojournal.jpl.nasa.gov/catalog/PIA16919 raw color]; [http://mars.nasa.gov/multimedia/interactives/billionpixel/ interactives]).}}

<br />

{{wide image |PIA16453-MarsCuriosityRover-RocknestPanorama-20121126.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view from [[Rocknest (Mars)|Rocknest]] looking eastward toward Point Lake (center) on the way to [[Glenelg, Mars|Glenelg Intrigue]] (26 November 2012; [[Color balance|white balanced]]; [[:File:PIA16453-MarsCuriosityRover-RocknestPanorama-Raw-20121126.jpg|raw color]]).}}


{{wide image |PIA17595-MarsCuriosityRover-YellowknifeBay-DrillSites-20131224.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of Drilling Sites of [[List of rocks on Mars#Curiosity|Rocks]] at Yellowknife Bay (24 December 2012).}}

== Planned events ==

<!---

{| class="wikitable" style="margin: 1em auto 1em auto;width: 100%"

{{wide image |PIA17931 Martian Valley May Be Curiosity's Route, Figure 1.jpg|800px|align-cap=center| ''[[Curiosity (rover)|Curiosity]]''{{'s}} view of Dingo Gap on the way to [[Aeolis Mons|Mount Sharp]] (January 30, 2014; [[Color balance|white balanced]]; [https://web.archive.org/web/20140222100259/http://mars.jpl.nasa.gov/msl/images/PIA17931-FigB_M34-sol528-raw-full.jpg raw color]).}}

! style="margin; background: #FF6700;" colspan="4" | '''August 2012'''

{{wide image|PIA18473-MarsCuriosityRover-AeolisMons-AmargosaValley-20140911.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of "Amargosa Valley" on the lower slopes of "[[Aeolis Mons|Mount Sharp]]" (September 11, 2014).}}

|-

{{wide image |PIA19818-MarsCuriosityRover-MountSharpSandDunes-20150827.jpg|800px|align-cap=center|''Curiosity''{{'s}} view of [[sand dunes]] on the lower slopes of "[[Aeolis Mons|Mount Sharp]]" (August 27, 2015).}}

! style="text-align: center; background: #F4C430;"|Date

--->

! style="text-align: center; background: #F4C430;"|Event

[[File:PIA23623-CuriosityRoverPanorama-Nov24-Dec01-2019.jpg|thumb|center|800px|<div align="center">''[[Curiosity (rover)|Curiosity]]''{{'s}} view from the slopes of Mount Sharp (December 1, 2019; [https://www.youtube.com/watch?v=X2UaFuJsqxk video (3:09)]).</div>]]

! style="text-align: center; background: #F4C430;"|Notes

{{wide image|PIA19912-MarsCuriosityRover-MountSharp-20151002.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of Mount Sharp (9 September 2015).}}

! style="text-align: center; background: #F4C430;"|Status

[[File:Rafael_Navarro_Mountain.png|thumb|center|800px|<div align="center">''[[Curiosity (rover)|Curiosity]]''{{'s}} view of Rafael Navarro Mountain (April 5, 2021).</div>]]

|-

{{wide image|PIA25912-MarsCuriosityRover-MarkerBandValley-20230408.png|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]'' views Marker Band Valley (8 April 2023).}}

| style="text-align: center;" scope="col" width="60" | 10-13 August || style="text-align: center;" scope="col" width="120" | Software update || NASA's Mars rover Curiosity will spend its first weekend on Mars transitioning to software better suited for tasks ahead, such as driving and using its robotic arm. The rover's change of operating software will occur during a series of steps August 10 through August 13. This software for Mars surface operations was uploaded to the rover's memory during the Mars Science Laboratory spacecraft's flight from Earth.<ref>[http://www.nasa.gov/mission_pages/msl/news/msl20120810.html NASA - NASA Curiosity Mars Rover Installing Smarts for Driving]</ref> || style="background: green; text-align: center;" | {{White| '''Success Complete''' <ref>[http://mars.jpl.nasa.gov/msl/news/whatsnew/index.cfm?FuseAction=ShowNews&NewsID=1309 Mars Science Laboratory: NASA Hosts Teleconference About Curiosity Rover Progess]</ref>}}

{{wide image|Martian-Sunset-O-de-Goursac-Curiosity-2013.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view of [[Extraterrestrial skies#Mars|Mars sky]] at [[Sunset#Planets|sunset]] (February 2013; Sun simulated by artist).}}

|}

{{wide image|PIA17936-f2-MarsCuriosityRover-EarthMoon-20140131.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} first view of the [[Earth]] and the [[Moon]] from the [[Extraterrestrial skies#Mars|surface]] of [[Mars]] (31 January 2014).<ref name="NYT-20140206">{{cite web |last=Revkin |first=Andrew C. |title=Martian View of Our Pale Dot |url= http://dotearth.blogs.nytimes.com/2014/02/06/a-martian-view-of-our-pale-dot |date=6 February 2014 |work=[[New York Times]] |access-date=9 February 2014 }}</ref>}}


<!---Related "Wide" Images - Extras

==Sol==

{{wide image |PIA16227-MarsCuriosityRover-Rocknest-20121012.jpg|800px|align-cap=center|''Curiosity''{{'s}} view of the [[Sand|sand patch]] at ''"[[Rocknest (Mars)|Rocknest]]"'' - South is center/North at both ends; "[[Aeolis Mons|Mount Sharp]]" at SE horizon (somewhat left-of-center); "[[Glenelg, Mars|Glenelg]]" at East (left-of-center); rover tracks at West (right-of-center) (October 5, 2012).}}

{{Main|Timekeeping on Mars}}

{{wide image |PIA17766-MarsCuriosityRover-DingoGap-20140128.jpg|800px|align-cap=center| ''[[Curiosity (rover)|Curiosity]]''{{'s}} view of ''"Dingo Gap"'' on the way to [[Aeolis Mons|Mount Sharp]] (January 28, 2014; [[Color balance|white balanced]]; [https://web.archive.org/web/20150121025648/http://mars.jpl.nasa.gov/msl/images/pia17766-FigB_Mastcam-sol526-raw-full.jpg raw color]).}}

The term sol is used by planetary astronomers to refer to the duration of a solar day on Mars.<ref>[http://www.nasa.gov/mission_pages/mer/images/pia01892.html NASA - Opportunity's View, Sol 959 (Vertical)]</ref> A mean Martian solar day, or "sol", is 24 hours, 39 minutes, and 35.244 seconds.<ref>[http://www.giss.nasa.gov/tools/mars24/help/notes.html NASA GISS: Technical Notes on Mars Solar Time]

{{wide image |PIA17083-MarsCuriosityRover-ToAeolisMons-20130724.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view on the way to [[Aeolis Mons]] near "Twin Cairns Island" (center is southwest) (July 24, 2013).}}

</ref>

{{wide image |PIA17354-MarsCuriosityRover-DiscoveryRidge-20130827.jpg|800px|align-cap=center|''[[Curiosity (rover)|Curiosity]]''{{'s}} view on the way to [[Aeolis Mons]] near "Discovery Ridge" (left-of-center) (left is east; center is southwest; right is north) (August 27, 2013).}}

--->

{{Clear}}



==See also==

==See also==

{{div col|colwidth=20em}}

* [[Mars]]

* [[Aeolis quadrangle]]

* [[Astrobiology]]

* [[Composition of Mars]]

* [[ExoMars|ExoMars programme]]

* [[Exploration of Mars]]

* [[Exploration of Mars]]

* [[NASA Missions]]

* [[Geography of Mars]]

* [[Geology of Mars]]

* [[InSight|''InSight'' lander]]

* [[List of missions to Mars]]

* [[List of rocks on Mars]]

* [[Mars Exploration Rover]]

* ''[[Mars Express]]'' orbiter

* [[2001 Mars Odyssey|''Mars Odyssey Orbiter'']]

* [[Mars Orbiter Mission]]

* [[Mars Pathfinder|''Mars Pathfinder'' (''Sojourner'' rover)]]

* [[Mars Reconnaissance Orbiter]]

* [[Mars 2020 rover mission]]

* [[MAVEN|''MAVEN'' orbiter]]

* [[Moons of Mars]]

* [[Phoenix (spacecraft)|''Phoenix'' lander]]

* [[Robotic spacecraft]]

* [[Scientific information from the Mars Exploration Rover mission]]

* [[Space exploration]]

* [[Timeline of Mars 2020]]

* [[U.S. Space Exploration History on U.S. Stamps]]

* [[Viking program]]

* [[Water on Mars]]

{{div col end}}

{{Clear}}



==References==

==References==

<!--Please consider using this "Reference generator" page for correct reference format:

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http://toolserver.org/~magnus/makeref.php

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{{Reflist|30em}}


{{Reflist |3}}



==External links==

==External links==

*[http://mars.jpl.nasa.gov/msl/ MSL Official Page]

* [https://mars.nasa.gov/msl/home/ ''Curiosity'' Rover Official Page.]

*[http://www.nasa.gov/mission_pages/msl/index.html NASA Official MSL Page]

* [https://www.nasa.gov/mission_pages/msl/index.html MSL/NASA Official Page.]

* [[Atmosphere of Mars|Mars Weather]]: [https://web.archive.org/web/20210410062007/https://mars.nasa.gov/mars2020/weather/ ''Perseverance'']*[https://mars.nasa.gov/msl/weather/ ''Curiosity'']*[https://mars.nasa.gov/insight/weather/ ''InSight'']<!---({{small|[http://www.csgnetwork.com/temp2conv.html TempConv]}})--->

*[http://www.jpl.nasa.gov/msl/ JPL Official MSL Page]

* [https://www.nytimes.com/interactive/science/space/mars-curiosity-rover-tracker.html ''Curiosity'' Rover Tracker (6 August 2012 to 5 August 2013 and beyond).]


* [https://www.wired.com/wiredscience/2013/03/4-billion-pixel-mars-panorama/ Panoramic View of Gale Crater on Mars (4 billion pixels)] (March 2013).

{{Portal bar|Mars|Robotics|Spaceflight}}

* [https://www.youtube.com/watch?v=Jr1Xu2i-Uc0 Video (04:32) - ''Evidence for 'Vigorously' Flowing Water on Ancient Mars''] (September 2012).

* [https://www.youtube.com/watch?v=8DZl56tS9ko Video (02:52) - ''Curiosity''{{'s}} view from Mount Sharp] ([[NASA]]; August 2021)

* https://archive.today/20140627092658/https://webcast.stsci.edu/webcast/detail.xhtml?talkid=4006 - ([[Robert Hazen]]; [[NASA]]; April 2014).

* [https://www.youtube.com/watch?v=GNjuz6MO0eU Video (86:49) - ''Search for Life in the Universe''] - ([[NASA]]; July 2014).



{{Curiosity Rover Timeline}}

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{{spacecraft-stub}}


Latest revision as of 09:25, 1 July 2024

Curiosity rover on Mars (5 August 2015)

The Mars Science Laboratory and its rover, Curiosity, were launched from Earth on 26 November 2011. As of July 10, 2024, Curiosity has been on the planet Mars for 4240 sols (4356 total days; 11 years, 339 days) since landing on 6 August 2012. (See Current status.)

Prelaunch (2004–2011)[edit]

Cruise stage is tested in 2010.[1]

In April 2004, the United States National Aeronautics and Space Administration (NASA) called for scientific experiments and instruments proposals for the Mars Science Laboratory and rover mission.[2] Launch was proposed for September 2009.[3][4] By 14 December 2004, eight proposals were selected, including instruments from Russia and Spain.[2][4]

Testing of components also began in late 2004, including Aerojet's monopropellant engine with the ability to throttle from 15 to 100 percent thrust with a fixed propellant inlet pressure.[2] By November 2008 most hardware and software development was complete, and testing continued.[5] At this point, cost overruns were approximately $400 million.[6] In December 2008, lift-off was delayed to November 2011 due to insufficient time for testing and integration.[7][8][9]

Between 23–29 March 2009, the general public ranked nine finalist rover names (Adventure, Amelia, Journey, Perception, Pursuit, Sunrise, Vision, Wonder, and Curiosity)[10] through a public poll on the NASA website.[11] On 27 May 2009, the winning name was announced to be Curiosity. The name had been submitted in an essay contest by Clara Ma, a then sixth-grader from Kansas.[11]

Landing site selection[edit]

At the first MSL Landing Site workshop, 33 potential landing sites were identified.[12] By the second workshop in late 2007, the list had grown to include almost 50 sites,[13] and by the end of the workshop, the list was reduced to six;[14][15][16] in November 2008, project leaders at a third workshop reduced the list to these four landing sites:[17][18][19]

Name Location Elevation Notes
Eberswalde Crater 23°52′S 326°44′E / 23.86°S 326.73°E / -23.86; 326.73 −1,450 m (−4,760 ft) Ancient river delta.[20]
Holden Crater 26°22′S 325°06′E / 26.37°S 325.10°E / -26.37; 325.10 −1,940 m (−6,360 ft) Dry lake bed.[21]
Gale Crater 4°29′S 137°25′E / 4.49°S 137.42°E / -4.49; 137.42 −4,451 m (−14,603 ft) Features 5 km (3.1 mi) tall mountain
of layered material near center.[21][22] selected.[23]
Mawrth Vallis 24°01′N 341°02′E / 24.01°N 341.03°E / 24.01; 341.03 −2,246 m (−7,369 ft) Channel carved by catastrophic floods.[24]

A fourth landing site workshop was held in late September 2010,[25] and the fifth and final workshop 16–18 May 2011.[26] On 22 July 2011, it was announced that Gale Crater had been selected as the landing site of the Mars Science Laboratory mission.

Aeolis Mons rises from the middle of Gale Crater - Green dot marks the Curiosity rover landing site in Aeolis Palus[23][27] - North is down.

Launch (2011)[edit]

MSL Launch - 26 November 2011 15:02:00.211 UTC[28]

MSL was launched from Cape Canaveral Air Force Station Space Launch Complex 41 on 26 November 2011, at 10:02 EST (15:02 UTC) aboard an Atlas V 541 provided by United Launch Alliance.[29][30] The first and second rocket stages, along with the rocket motors, were stacked on 9 October 2011, near the launch pad.[31] The fairing containing the spacecraft was transported to the launch pad on 3 November 2011.[32]

On 13 December 2011, the rover began monitoring space radiation to aid in planning for future crewed missions to Mars.[33]

The interplanetary journey to Mars took more than eight months,[34] time during which, the spacecraft performed four trajectory corrections: on 11 January, 26 March, 26 June and on 28 July. Mission design had allowed for a maximum of 6 trajectory correction opportunities.[35][36]

Landing (2012)[edit]

Curiosity landed in the Gale Crater at 05:17 UTC on 6 August 2012.[37][38][39][40] Upon reaching Mars, an automated precision landing sequence took over the entire landing events.[41] A cable cutter separated the cruise stage from the aeroshell and then the cruise stage was diverted into a trajectory for burn-up in the atmosphere.[42][43] Landing was confirmed simultaneously by 3 monitoring Mars orbiters. Curiosity landed on target and only 2.4 km (1.5 mi) from its center.[44] The coordinates of the landing site (named "Bradbury Landing") are: 4°35′22S 137°26′30E / 4.5895°S 137.4417°E / -4.5895; 137.4417.[45][46]

Some low resolution Hazcam images were beamed to Earth by relay orbiters confirming the rover's wheels were deployed correctly and on the ground.[40][47] Three hours later, the rover begins to beam detailed data on its systems' status as well as on its entry, descent and landing experience.[47] Aerial 3-D images of the landing site are available and include: the Curiosity rover and related Parachute (HiRISE, 10 October 2012).

On 8 August 2012, Mission Control began upgrading the rover's dual computers by deleting the entry-descent-landing software, then uploading and installing the surface operation software;[48] the switchover was completed by 15 August.[49]

First 360-degree panoramic view of Mars taken by the Curiosity rover (7 August 2012).[54][55]

Prime mission (2012 - September 2014)[edit]

Curiosity's view, from about 200 m (660 ft) away, of the Glenelg Area - an important science destination (19 September 2012).

On 15 August 2012, the rover began several days of instrument checks and mobility tests.[56][57] The first laser testing of the ChemCambyCuriosity on Mars was performed on a rock, N165 ("Coronation" rock), near Bradbury Landing on 19 August 2012.[58][59][60]

The science and operations teams have identified at least six possible routes to the base of Mount Sharp, and estimate about a year studying the rocks and soil of the crater floor while Curiosity slowly makes its way to the base of the mountain.[56][61] The ChemCam team expects to take approximately one dozen compositional measurements of rocks per day.[62]

Curiosity rover - Temperature, Pressure, HumidityatGale CrateronMars (August 2012 - February 2013)

Having completed its mobility tests, the rover's first drive began on 29 August 2012, to a place called Glenelg about 400 m (1,300 ft) to the east.[63] Glenelg is a location where three types of terrain intersect, and is the mission's first major driving destination. The drive across may take up to two months, after which Curiosity will stay at Glenelg for a month.[64]

On the way, Curiosity studied a pyramidal rock dubbed "Jake Matijevic" after a mathematician-turned-rover-engineer who played a critical role in the design of the six-wheeled rover, but died just days after Curiosity landed in August. [65] The Jake rock measures about 25 cm (9.8 in) tall and 40 cm (16 in) wide.[66] It is an igneous rock and may be a mugearite, a sodium rich oligoclase-bearing basaltic trachyandesite.[67] Afterwards, on 30 September 2012, a finely-grained rock, named "Bathurst Inlet", was examined by Curiosity's Mars Hand Lens Imager (MAHLI) and Alpha particle X-ray spectrometer (APXS). The rock was named after Bathurst Inlet, a deep inlet located along the northern coast of the Canadian mainland. Also, a sand patch, named "Rocknest", is a test target for the first use of the scoop on the arm of the Curiosity rover.[68]

Evidence for ancient water[edit]

On 27 September 2012, NASA scientists announced that the Curiosity rover found evidence for an ancient streambed suggesting a "vigorous flow" of water on Mars.[69][70][71]

Evidence of water on Mars[69][70][71]
Curiosity rover on the way to Glenelg (26 September 2012)
Peace Vallis and related alluvial fan near the Curiosity rover landing ellipse and landing site (noted by +).
"Hottah" rock outcrop on Mars - an ancient streambed viewed by the Curiosity rover (14 September 2012) (close-up) (3-D version).
"Link" rock outcrop on Mars - compared with a terrestrial fluvial conglomerate - suggesting water "vigorously" flowed in a stream.

On 7 October 2012, a mysterious "bright object" (image), discovered in the sand at Rocknest, drew scientific interest. Several close-up pictures (close-up 1) (close-up 2) were taken of the object and preliminary interpretations by scientists suggest the object to be "debris from the spacecraft".[72][73][74] Nonetheless, further images in the nearby sand have detected other "bright particles" (image) (close-up 1). These newly discovered objects are presently thought to be "native Martian material".[72][75][76]

"Bright particles" found by the Curiosity roveratRocknest (October, 2012)[72][73]
"Bright object" (BO)
BO Close-up 1
BO Close-up 2
"Bright particles"
BP Close-up 1

On 17 October 2012, at Rocknest, the first X-ray diffraction analysisofMartian soil was performed. The results revealed the presence of several minerals, including feldspar, pyroxenes and olivine, and suggested that the Martian soil in the sample was similar to the weathered basaltic soils of Hawaiian volcanoes. The sample used is composed of dust distributed from global dust storms and local fine sand. So far, the materials Curiosity has analyzed are consistent with the initial ideas of deposits in Gale Crater recording a transition through time from a wet to dry environment.[77] On 22 November 2012, the Curiosity rover analyzed a rock named "Rocknest 3" with the APXS and then resumed traveling toward "Point Lake" overlook on its way to Glenelg Intrigue.[78]

On 3 December 2012, NASA reported that Curiosity performed its first extensive soil analysis, revealing the presence of water molecules, sulfur and chlorine in the Martian soil.[79][80] The presence of perchlorates in the sample seems highly likely. The presence of sulfate and sulfide is also likely because sulfur dioxide and hydrogen sulfide were detected. Small amounts of chloromethane, dichloromethane and trichloromethane were detected. The source of the carbon in these molecules is unclear. Possible sources include contamination of the instrument, organics in the sample and inorganic carbonates.[79][80]

Evidence for ancient habitability[edit]

In February 2013, the rover used its drill for the first time.[81]

Curiosity rover - First drilling tests ("John Klein" rock, Yellowknife Bay, 2–6 February 2013).[82]
Drilling Area at Yellowknife Bay (28 December 2012).

In March 2013, NASA reported Curiosity found evidence that geochemical conditions in Gale Crater were once suitable for microbial life after analyzing the first drilled sample of Martian rock, "John Klein" rockatYellowknife BayinGale Crater. The rover detected water, carbon dioxide, oxygen, sulfur dioxide and hydrogen sulfide.[83][84][85] Chloromethane and dichloromethane were also detected. Related tests found results consistent with the presence of smectite clay minerals.[83][84][85][86][87] In addition, sandstone beds associated with the Gillespie Lake MemberofYellowknife Bay seem similar to microbially induced sedimentary structures (MISS) found on Earth, according to one study.[88]

Curiosity rover - Chemical analysis
(drilled sample of "John Klein" rock, Yellowknife Bay, 27 February 2013).[83][84][85]

Evidence for atmospheric loss[edit]

On 8 April 2013, NASA reported that much of the atmosphere of Mars has been lost based on argon isotope ratios studies.[89][90]

On 19 July 2013, NASA scientists published the results of a new analysis of the atmosphere of Mars, reporting a lack of methane around the landing site of the Curiosity rover. In addition, the scientists found evidence that Mars "has lost a good deal of its atmosphere over time", based on the abundance of isotopic compositions of gases, particularly those related to argon and carbon.[91][92][93]

Curiosity rover (very bright spot near the lower right) and "Tracks" from Bradbury LandingtoJohn KleininYellowknife Bay - as viewed from Space (MRO; HiRISE; 27 June 2013).

Other 2013 events[edit]

Argon isotope ratios are used to estimate atmospheric lossonMars. (Curiosity rover, April, 2013)

On 28 February 2013, NASA was forced to switch to the backup computer due to an issue with the then active computer's flash memory which resulted in the computer continuously rebooting in a loop. The backup computer was turned on in safe mode and was converted to operational status on 19 March 2013.[94][95]

On 18 March 2013, NASA reported evidence of mineral hydration, likely hydrated calcium sulfate, in several rock samples including the broken fragments of "Tintina" rock and "Sutton Inlier" rock as well as in veins and nodules in other rocks like "Knorr" rock and "Wernicke" rock.[96][97][98] Analysis using the rover's DAN instrument provided evidence of subsurface water, amounting to as much as 4% water content, down to a depth of 60 cm (2.0 ft), in the rover's traverse from the Bradbury Landing site to the Yellowknife Bay area in the Glenelg terrain.[96]

Composition of "Yellowknife Bay" rocks - rock veins are higher in calcium and sulfur than "Portage" soil - APXS results - Curiosity rover (March, 2013).

Between 4 April – 1 May 2013, Curiosity operated autonomously due to a Martian solar conjunction with Earth. While Curiosity transmitted a beep to Earth each day and the Odyssey spacecraft continued to relay information from the rover, no commands were sent from mission control since there was a possibility of data corruption due to interference from the Sun. Curiosity continued to perform stationary science at Yellowknife Bay for the duration of the conjunction.[89][99]

On 5 June 2013, NASA announced that Curiosity will soon begin a 8 km (5.0 mi) journey from the Glenelg area to the base of Mount Sharp. The trip is expected to take nine months to a year with stops along the way to study the local terrain.[100][101][102]

On 16 July 2013, the Curiosity rover reached a milestone in its journey across Mars, having traveled 1 km (0.62 mi), since its landing in 2012;[103] on 1 August 2013, the rover traveled over one mile: 1.686 km (1.048 mi).[104]

On 6 August 2013, NASA celebrated Curiosity's first year on Mars (6 August 2012 to 5 August 2013) by programming the rover to perform the "Happy Birthday" song to itself.[105][106] NASA also released several videos (video-1, video-2) summarizing the rover's accomplishments over the year.[107][108] Primarily, the mission found evidence of "ancient environments suitable for life" on Mars. The rover drove over one-mile across the Martian terrain, transmitted more than 190 gigabits of data to Earth, including 70,000 images (36,700 full images and 35,000 thumbnails), and the rover's laser fired more than 75,000 times at 2,000 targets.[109]

On 27 August 2013, Curiosity used autonomous navigation (or"autonav"- the ability of the rover to decide for itself how to drive safely) over unknown Martian ground for the first time.[110]

Curiosity rover - view of "Sheepbed" mudstone (lower left) and surroundings (February 14, 2013).

On 19 September 2013, NASA scientists, on the basis of further measurements by Curiosity, reported no detection of atmospheric methane with a measured value of 0.18±0.67 ppbv corresponding to an upper limit of only 1.3 ppbv (95% confidence limit) and, as a result, conclude that the probability of current methanogenic microbial activity on Mars is reduced.[111][112][113]

On 26 September 2013, NASA scientists reported the Mars Curiosity rover detected "abundant, easily accessible" water (1.5 to 3 weight percent) in soil samples at the Rocknest regionofAeolis PalusinGale Crater.[114][115][116][117][118][119] In addition, NASA reported that the Curiosity rover found two principal soil types: a fine-grained mafic type and a locally derived, coarse-grained felsic type.[116][118][120] The mafic type, similar to other Martian soils and Martian dust, was associated with hydration of the amorphous phases of the soil.[120] Also, perchlorates, the presence of which may make detection of life-related organic molecules difficult, were found at the Curiosity rover landing site (and earlier at the more polar site of the Phoenix lander) suggesting a "global distribution of these salts".[119] NASA also reported that Jake M rock, a rock encountered by Curiosity on the way to Glenelg, was a mugearite and very similar to terrestrial mugearite rocks.[121]

On 17 October 2013, NASA reported, based on analysis of argon in the Martian atmosphere, that certain meteorites found on Earth thought to be from Mars are confirmed to be from Mars.[122]

Scarp retreatbywindblown sand over time on Mars (Yellowknife Bay, December 9, 2013).

On 13 November 2013, NASA announced the names of two features on Mars important to two active Mars exploration rovers in honor of planetary scientist Bruce C. Murray (1931-2013): "Murray Buttes", an entryway the Curiosity rover will traverse on its way to Mount Sharp and "Murray Ridge", an uplifted crater that the Opportunity rover is exploring.[123]

On 25 November 2013, NASA reported that Curiosity has resumed full science operations, with no apparent loss of capability, after completing the diagnosis of an electrical problem first observed on 17 November. Apparently, an internal short in the rover's power source, the Multi-Mission Radioisotope Thermoelectric Generator, caused an unusual and intermittent decrease in a voltage indicator on the rover.[124][125]

On 27 November 2013, an overview (titled, "The World of Mars") of current and proposed Mars exploration by John Grotzinger, chief scientist of the Curiosity rover mission, was published in the New York Times.[126]

On 9 December 2013, NASA reported that the planet Mars had a large freshwater lake (which could have been a hospitable environment for microbial life) based on evidence from the Curiosity rover studying Aeolis Palus near Mount SharpinGale Crater.[127][128]

Clay mineral structure of mudstone.
The Curiosity rover examines mudstone near Yellowknife Bay on Mars (May 2013).

On 9 December 2013, NASA researchers described, in a series of six articles in the journal Science, many new discoveries from the Curiosity rover. Possible organics were found that could not be explained by contamination.[129][130] Although the organic carbon was probably from Mars, it can all be explained by dust and meteorites that have landed on the planet.[131][132][133] Because much of the carbon was released at a relatively low temperature in Curiosity's Sample Analysis at Mars (SAM) instrument package, it probably did not come from carbonates in the sample. The carbon could be from organisms, but this has not been proven. This organic-bearing material was obtained by drilling 5 centimeters deep in a site called Yellowknife Bay into a rock called "Sheepbed mudstone". The samples were named John Klein and Cumberland. Microbes could be living on Mars by obtaining energy from chemical imbalances between minerals in a process called chemolithotrophy which means "eating rock."[134] However, in this process only a very tiny amount of carbon is involved — much less than was found at Yellowknife Bay.[135][136]

Using SAM's mass spectrometer, scientists measured isotopesofhelium, neon, and argon that cosmic rays produce as they go through rock. The fewer of these isotopes they find, the more recently the rock has been exposed near the surface. The 4-billion-year-old lakebed rock drilled by Curiosity was uncovered between 30 million and 110 million years ago by winds which sandblasted away 2 meters of overlying rock. Next, they hope to find a site tens of millions of years younger by drilling close to an overhanging outcrop.[137]

The absorbed dose and dose equivalent from galactic cosmic rays and solar energetic particles on the Martian surface for ~300 days of observations during the current solar maximum was measured. These measurements are necessary for human missions to the surface of Mars, to provide microbial survival times of any possible extant or past life, and to determine how long potential organic biosignatures can be preserved. This study estimates that a 1-meter depth drill is necessary to access possible viable radioresistant microbe cells. The actual absorbed dose measured by the Radiation Assessment Detector (RAD) is 76 mGy/yr at the surface. Based on these measurements, for a round trip Mars surface mission with 180 days (each way) cruise, and 500 days on the Martian surface for this current solar cycle, an astronaut would be exposed to a total mission dose equivalent of ~1.01 sievert. Exposure to 1 sievert is associated with a 5 percent increase in risk for developing fatal cancer. NASA's current lifetime limit for increased risk for its astronauts operating in low-Earth orbit is 3 percent.[138] Maximum shielding from galactic cosmic rays can be obtained with about 3 meters of Martian soil.[139]

The samples examined were probably once mud that for millions to tens of millions of years could have hosted living organisms. This wet environment had neutral pH, low salinity, and variable redox states of both iron and sulfur species.[131][140][141][142] These types of iron and sulfur could have been used by living organisms.[143] C, H, O, S, N, and P were measured directly as key biogenic elements, and by inference, P is assumed to have been there as well.[134][136] The two samples, John Klein and Cumberland, contain basaltic minerals, Ca-sulfates, Fe oxide/hydroxides, Fe-sulfides, amorphous material, and trioctahedral smectites (a type of clay). Basaltic minerals in the mudstone are similar to those in nearby aeolian deposits. However, the mudstone has far less Fe-forsterite plus magnetite, so Fe-forsterite (type of olivine) was probably altered to form smectite (a type of clay) and magnetite.[144] A Late Noachian/Early Hesperian or younger age indicates that clay mineral formation on Mars extended beyond Noachian time; therefore, in this location neutral pH lasted longer than previously thought.[140]

On 20 December 2013, NASA reported that Curiosity has successfully upgraded, for the third time since landing, its software programs and is now operating with version 11. The new software is expected to provide the rover with better robotic arm and autonomous driving abilities. Due to wheel wear, a concern to drive more carefully over the rough terrain the rover is currently traveling on to Mount Sharp, was also reported.[145]

Search for ancient life[edit]

On 24 January 2014, NASA reported that current studies by the Curiosity and Opportunity rovers will now be searching for evidence of ancient life, including a biosphere based on autotrophic, chemotrophic and/or chemolithoautotrophic microorganisms, as well as ancient water, including fluvio-lacustrine environments (plains related to ancient riversorlakes) that may have been habitable.[146][147][148][134] The search for evidence of habitability, taphonomy (related to fossils), and organic carbon on the planet Mars is now a primary NASA objective.[146]

Arrival at Mount Sharp[edit]

On 11 September 2014 (Sol 746), Curiosity reached the slopes of Aeolis Mons (orMount Sharp), the rover mission's long-term prime destination[149][150] and where the rover is expected to learn more about the history of Mars.[109] Curiosity had traveled an estimated linear distance of 6.9 km (4.3 mi)[151] to the mountain slopes since leaving its "start" point in Yellowknife Bay on 4 July 2013.[151]

Geology map - from the crater floor in Aeolis Palus up the Slopes of Mount Sharp
(11 September 2014).
Rocks in "Hidden Valley" near the "Pahrump Hills" on the slopes of Mount Sharp as viewed from the Curiosity Rover
(11 September 2014; white balanced).

Detection of organics[edit]

On 16 December 2014, NASA reported the Curiosity rover detected a "tenfold spike", likely localized, in the amount of methane in the Martian atmosphere. Sample measurements taken "a dozen times over 20 months" showed increases in late 2013 and early 2014, averaging "7 parts of methane per billion in the atmosphere." Before and after that, readings averaged around one-tenth that level.[152][153]

Detecting organics on Mars is a challenge.
Methane measurements in the atmosphereofMars by the Curiosity rover (August 2012 to September 2014).
Methane (CH4) on Mars - potential sources and sinks.

In addition, high levels of organic chemicals, particularly chlorobenzene, were detected in powder drilled from one of the rocks, named "Cumberland", analyzed by the Curiosity rover.[152][153]

Comparison of OrganicsinMartian rocks - Chlorobenzene levels were much higher in the "Cumberland" rock sample.
Detection of Organics in the "Cumberland" rock sample.
Spectral Analysis (SAM) of "Cumberland" rock.

Other 2014 events[edit]

On 6 February 2014, the Curiosity rover, in order to reduce wear on its wheels by avoiding rougher terrain,[154] successfully crossed (image) the "Dingo Gap" sand dune and is now expected to travel a smoother route to Mount Sharp.[155]

NOV-2013 - Curiosity's wheel - dents & holes - 3 miles on Mars (30 November 2013).
FEB-2014 - Curiosity's wheel - dents & holes - 3 miles on Mars (18 February 2014).

On 19 May 2014, scientists announced that numerous microbes, like Tersicoccus phoenicis, may be resistant to methods usually used in spacecraft assembly clean rooms. It's not currently known if such resistant microbes could have withstood space travel and are present on the Curiosity rover now on Mars.[156]

On 25 May 2014, Curiosity discovered an iron meteorite, and named it "Lebanon" (image).

On 3 June 2014, Curiosity observed the planet Mercury transiting the Sun, marking the first time a planetary transit has been observed from a celestial body besides Earth.[157]

On 24 June 2014, Curiosity completed a Martian year—687 Earth days—after finding that Mars once had environmental conditions favorable for microbial life.[158]

On 27 June 2014, Curiosity crossed the boundary line of its "3-sigma safe-to-land ellipse" and is now in territory that may get even more interesting, especially in terms of Martian geology and landscape (view from space).[159]

On 12 July 2014, Curiosity imaged the first laser spark on Mars (related image; video (01:07).)

On 6 August 2014, Curiosity celebrated its second anniversary since landing on Mars in 2012.[160]

On 11 September 2014, a panel of NASA scientists announced (video (01:25)) the arrival of CuriosityatMount Sharp and discussed future rover plans.[150]

First extended mission (October 2014 - September 2016)[edit]

On 19 October 2014, the Curiosity rover viewed the flyby of Comet C/2013 A1.

On 8 December 2014, a panel of NASA scientists discussed (archive 62:03) the latest observations of Curiosity, including findings about how water may have helped shape the landscape of Mars and had a climate long ago that could have produced long-lasting lakes at many Martian locations.[161][162][163]

On 16 December 2014, NASA reported detecting an unusual increase, then decrease, in the amounts of methane in the atmosphere of the planet Mars; in addition, organic chemicals were detected in powder drilled from a rock by the Curiosity rover. Also, based on deuteriumtohydrogen ratio studies, much of the wateratGale Crater on Mars was found to have been lost during ancient times, before the lakebed in the crater was formed; afterwards, large amounts of water continued to be lost.[152][153][164]

CuriosityatThe Kimberley
Curiosity rover (lower left quadrant of image) and "Tracks" near The Kimberley - as viewed from Space (MRO; HiRISE; 11 April 2014).
Curiosity at Mount Sharp
Curiosity rover (within rectangle) in the Pahrump HillsofMount Sharp - as viewed from Space (MRO; HiRISE; 13 December 2014).
Pahrump Hills as viewed by the Curiosity rover (2014).

On 21 January 2015, NASA announced a collaborative effort with Microsoft that developed a software project called OnSight which allows scientists to perform virtual work on Mars based on data from the Curiosity rover.[165]

CuriosityatMount Sharp
Self-portrait of the Curiosity rover at the Mojave site (31 January 2015).

On 6 March 2015, NASA reported performing tests on the rover to help uncover the reason for intermittent problems with the robotic arm used for rock drilling and analysis.[166] Results of preliminary tests suggest the intermittent short-circuit problem may be related to the percussion mechanism of the drill. Further tests are planned to verify and adjust to the problem.[167]

On 24 March 2015, NASA reported the first detection of nitrogen released after heating surface sediments on the planet Mars. The nitrogen, in the form of nitric oxide, was detected by the SAM instrument on the Curiosity rover and can be used by living organisms. The discovery supports the notion that ancient Mars may have been habitable for life.[168]

On 27 March 2015, NASA reported that the landing site was fading from view in the two-and-a-half years since landing in 2012, as shown in the following animation:

Landing site fading from view after first several years.

On 4 April 2015, NASA reported studies, based on measurements by the Sample Analysis at Mars (SAM) instrument on the Curiosity rover, of the Martian atmosphere using xenon and argon isotopes. Results provided support for a "vigorous" loss of atmosphere early in the history of Mars and were consistent with an atmospheric signature found in bits of atmosphere captured in some Martian meteorites found on Earth.[169]

On 19 August 2015, NASA scientists reported that the Dynamic Albedo of Neutrons (DAN) instrument on the Curiosity rover detected an unusual hydrogen-rich area, at "Marias Pass," on Mars. The hydrogen found seemed related to water or hydroxyl ions in rocks within three feet beneath the rover, according to the scientists.[170]

Hydrogen-rich area detected at 'Marias Pass" on Mars by Curiosity.[170]

On 5 October 2015, possible recurrent slope lineae, wet brine flows, were reported on Mount Sharp near Curiosity.[171] In addition, on 5 October 2015, NASA reported an estimated 20,000 to 40,000 heat-resistant bacterial spores were on Curiosity at launch, as much as 1,000 times more than that may not have been counted.[171]

On 8 October 2015, NASA confirmed that lakes and streams existed in Gale crater 3.3 - 3.8 billion years ago delivering sediments to build up the lower layers of Mount Sharp.[172][173]

Namib sand dune (downwind side) on Mars
(Curiosity rover; December 17, 2015).

On 17 December 2015, NASA reported that as Curiosity climbed higher up Mount Sharp, the composition of rocks were changing substantially. For example, rocks found higher up the mountain contained much higher levels of silica than the basaltic rocks found earlier. After further analysis, the silica-rich rocks on Mars were found to be tridymite, a mineral that is not commonly found on Earth. Opal-A, another form of silica, was also found on Mars.[174]

Second extended mission (October 2016 - September 2019)[edit]

The second extended mission began on 1 October 2016.[175] The rover explored a ridge known as the Murray Formation for most of the mission.

As of 3 October 2016, NASA summarized the findings of the mission, thus far, as follows: "The Curiosity mission has already achieved its main goal of determining whether the landing region ever offered environmental conditions that would have been favorable for microbial life, if Mars has ever hosted life. The mission found evidence of ancient rivers and lakes, with a chemical energy source and all of the chemical ingredients necessary for life as we know it."[176] Plans for the next two years, up to September 2018, include further explorations of the uphill slopes of Mount Sharp, including a ridge rich in the mineral hematite and a region of clay-rich bedrock.[176]

"Egg Rock" Meteorite (27 October 2016)[177]
Context view
Close-up view

On 13 December 2016, NASA reported further evidence supporting habitability on Mars as the Curiosity rover climbed higher, studying younger layers, on Mount Sharp.[178] Also reported, the very soluble element boron was detected for the first time on Mars.[178] Since landing on Mars in August 2012, Curiosity has driven 15.0 km (9.3 mi) and climbed 165 m (541 ft) in elevation.[179]

Curiosity rover view of Mount Sharp (November 10, 2016).
Summary of the Curiosity rover mission (14-fold exaggerated elevation; 13 December 2016)[179]
Curiosity rover - Mudstone Mineralogy - 2013 to 2016 on Mars (CheMin; December 13, 2016)[180]

On 17 January 2017, NASA released an image of a rock slab, named "Old Soaker", which may contain mud cracks. Also, somewhat later, it released an animation of sand moving in a nearby area.

On 6 February 2017, NASA reported that rock samples analyzed by the rover have not revealed any significant carbonate. This poses a puzzle to researchers: the same rocks that indicate a lake existed also indicate there was very little carbon dioxide in the air to help keep the lake unfrozen.[181]

On 27 February 2017, NASA presented the following mission overview: "During the first year after Curiosity's 2012 landing in Gale Crater, the mission fulfilled its main goal by finding that the region once offered environmental conditions favorable for microbial life. The conditions in long-lived ancient freshwater Martian lake environments included all of the key chemical elements needed for life as we know it, plus a chemical source of energy that is used by many microbes on Earth. The extended mission is investigating how and when the habitable ancient conditions evolved into conditions drier and less favorable for life."[182]

From 3 to 7 May 2017, Curiosity used ChemCam to study what turned out to be manganese oxide deposits on the Sutton Island and Blunts Point layers of the Murray Formation. According to a 2024 paper, the deposits suggest Earth-level amounts of oxygen were present in the very early Martian atmosphere, hinting at microbial life.[183]

On 1 June 2017, NASA reported that the Curiosity rover provided evidence of an ancient lake in Gale crater on Mars that could have been favorable for microbial life; the ancient lake was stratified, with shallows rich in oxidants and depths poor in oxidants, particularly silica; the ancient lake provided many different types of microbe-friendly environments at the same time. NASA further reported that the Curiosity rover will continue to explore higher and younger layers of Mount Sharp in order to determine how the lake environment in ancient times on Mars became the drier environment in more modern times.[184][185][186]

Stratification of an ancient lake in Gale crater.
Curiosity rover (center bright blue) on Mount Sharp viewed from space by MRO (June 5, 2017).[187]

Between 22 July – 1 August 2017, few commands were sent from the Earth to Mars since Mars was in conjunction with the sun.[188]

On 5 August 2017, NASA celebrated the fifth anniversary of the Curiosity rover mission landing, and related exploratory accomplishments, on the planet Mars.[189][190] (Videos: Curiosity's First Five Years (02:07); Curiosity's POV: Five Years Driving (05:49); Curiosity's Discoveries About Gale Crater (02:54))

On 5 September 2017, scientists reported that the Curiosity rover detected boron, an essential ingredient for lifeonEarth, on the planet Mars. Such a finding, along with previous discoveries that water may have been present on ancient Mars, further supports the possible early habitability of Gale Crater on Mars.[191][192]

Curiosity climbed Vera Rubin RidgeonMount Sharp (September 13, 2017).[193]

On 13 September 2017, NASA reported that the Curiosity rover climbed an iron-oxide-bearing ridge called Vera Rubin Ridge (orHematite Ridge) and will now start studying the numerous bright veins embedded in the various layers of the ridge, in order to provide more details about the history and habitability of ancient Mars.[193]

On 30 September 2017, NASA reported radiation levels on the surface of the planet Mars were temporarily doubled, and were associated with an aurora 25-times brighter than any observed earlier, due to a massive, and unexpected, solar storm in the middle of the month.[194]

Curiosity testing its systems in order to better resume the drilling process.[195]

On 17 October 2017, NASA announced the testing of its systems on Curiosity in an attempt to better resume drilling. The drilling system had stopped working reliably in December 2016.[195]

Curiosity's view of Gale Crater from the slopes (at 327 m (1,073 ft) elevation) of Mount Sharp (video (1:53)) (October 25, 2017)

On 2 January 2018, Curiosity captured images of rock shapes that may require further study in order to help better determine whether the shapes are biological or geological.[196][197]

On 22 March 2018, Curiosity had spent 2000 sols (2054 days) on Mars,[198] and prepares to study a region of clay-bearing rocks.

Curiosity views a region of clay-bearing rocks (highlighted) on the slopes of Mount Sharp.

In June 2018, a local dust storm occurred near the Opportunity rover which may affect Curiosity.[199][200] The first signs of the storm, 1,000 km (620 mi) from Opportunity, were discovered on 1 June 2018, in photographs by the Mars Color Imager (MARCI) camera on the Mars Reconnaissance Orbiter (MRO). More weather reports from the MRO and the MARCI team indicated a prolonged storm. Although this was, at that time, still far away from the rover, it influenced the atmospheric permeability (opacity) at the location. Within days, the storm had spread. As of 12 June 2018, the storm spanned an area of 41 million km2 (16 million sq mi) - about the area of North America and Russia combined.[199][201] Although such dust storms are not surprising, they rarely occur. They can arise within a short time and then persist for weeks to months. During the southern season of summer, the sunlight heats dust particles and brings them higher into the atmosphere. This creates wind, which in turn stirs up more dust. This results in a feedback loop that scientists are still trying to understand. NASA reported on 20 June 2018, that the dust storm had grown to completely cover the entire planet.[202][203]

Mars dust stormoptical depth tau – May to September 2018
(Mars Climate Sounder; Mars Reconnaissance Orbiter)
(1:38; animation; 30 October 2018; file description)

On 4 June 2018, NASA announced that Curiosity's ability to drill has been sufficiently restored by engineers. The rover had experienced drill mechanical problems since December 2016.[204]

Drill bit over a sample inlet on the deck of Curiosity
(31 May 2018/Sol 2068)[204]

On 7 June 2018, NASA announced a cyclical seasonal variation in atmospheric methane, as well as the presence of kerogen and other complex organic compounds. The organic compounds were from mudstone rocks aged approximately 3.5 billion years old, sampled from two distinct sites in a dry lake in the Pahrump Hills of the Gale crater. The rock samples, when pyrolyzed via the Curiosity'sSample Analysis at Mars instrument, released an array of organic molecules; these include sulfur-containing thiophenes, aromatic compounds such as benzene and toluene, and aliphatic compounds such as propane and butene. The concentration of organic compounds are 100-fold higher than earlier measurements. The authors speculate that the presence of sulfur may have helped preserve them. The products resemble those obtained from the breakdown of kerogen, a precursor to oil and natural gas on Earth. NASA stated that these findings are not evidence that life existed on the planet, but that the organic compounds needed to sustain microscopic life were present, and that there may be deeper sources of organic compounds on the planet.[205][206][207][208][209][210][211][212]

Curiosity detected a cyclical seasonal variation in atmospheric methane.
Curiosity – 360° panoroma at Vera Rubin Ridge (9 August 2018/Sol 2137; white balanced)[213]

Since 15 September 2018, a glitch in Curiosity's active computer (Side-B) has prevented Curiosity from storing science and key engineering data.[214] On 3 October 2018, the JPL began operating Curiosity on its backup computer (Side-A).[214] Curiosity will store science and engineering data normally using its Side-A computer until the cause of the glitch in Side-B is determined and remedied.[214]

Rocks viewed by Curiosity - Effect of 2018 dust storm winds[215]
Before dust storm winds (14 September 2018)
After dust storm winds (25 October 2018)

On 4 November 2018, geologists presented evidence, based on studies in Gale Crater by the Curiosity rover, that there was plenty of water on early Mars.[216][217]

Curiosity viewed a shiny object (named "Little Colonsay") on Mars (26 November 2018)[218]

On 26 November 2018, Curiosity viewed a shiny object (named, "Little Colonsay") on Mars.[218] Although possibly a meteorite, further studies are planned to better understand its nature.

On 1 February 2019, NASA scientists reported that the Mars Curiosity rover determined, for the first time, the density of Mount Sharp in Gale crater, thereby establishing a clearer understanding of how the mountain was formed.[219][220]

On 4 April 2019, NASA released images of solar eclipses by the two moons of the planet Mars, Phobos (animation1) and Deimos (animation2), as viewed by the Curiosity rover on the planet Mars in March 2019.[221][222]

Solar eclipses by two moons of Mars viewed by Curiosity (March, 2019)[221][222]
Deimos (17 March 2019)
Phobos (27 March 2019)

On 11 April 2019, NASA announced that the Curiosity rover on the planet Mars drilled into, and closely studied, a "clay-bearing unit" which, according to the rover Project Manager, is a "major milestone" in Curiosity's journey up Mount Sharp.[223]

Curiosity drilled into a "clay-bearing unit".[223]
Curiosity views moving clouds (12 May 2019)
Mars Curiosity rover explores Mount Sharp (15 May 2019)

During June 2019, while still studying the clay-bearing unit, Curiosity detected the highest levels of methane gas, 21 parts per billion, compared to the typical 1 part per billion the rover detects as normal background readings. The levels of methane dropped quickly over a few days, leading NASA to call this event one of several methane plumes that they have observed before but without any observable pattern. The rover lacked the necessary instrumentation to determine if the methane was biological or inorganic in nature.[224][225][226]

Curiosity viewed at Woodland Bay from space (31 May 2019)
Strathdon rock (July 2019)
Overall
CloseUp
Curiosity moves across clay unit (May–July 2019)

Third extended mission (October 2019 - September 2022)[edit]

The third extended mission began on 1 October 2019 - the rover's 2544th sol on Mars.[227]

In October 2019, evidence in the form of magnesium sulfate deposits left behind in ways that suggested evaporation, uncovered by the Curiosity rover on Mount Sharp, was reported of a 150 km (93 mi) wide ancient basin in Gale crater that once may have contained a salty lake.[228][229]

Mars rocks - 26 drill holes (1 July 2020)

In January 2020, a report was presented that compared Curiosity at the time of its landing on Mars in 2012, with the rover over seven years later in 2020.[230]

In February 2020, scientists reported the detection of thiophene organic molecules by the Curiosity rover on the planet Mars. It is not currently known if the detected thiophenes — usually associated on Earth with kerogen, coal and crude oil — are the result of biological or non-biological processes.[231][232]

In April 2020, scientists began operating the rover remotely from their homes due to the COVID-19 pandemic.[233]

Curiosity's views (released July 2020)
Pediment top view
Nodules found
Sulfate area
Dust devil on Mars - viewed by the Curiosity rover (9 August 2020)

On 29 August 2020, NASA released several videos taken by the Curiosity rover, including those involving dust devils, as well as very high resolution images of the related local martian terrain.[234]

Housedon Hill distant outcrop mosaic viewed by Curiosity rover between 9 September – 23 October 2020 (posted 21 December 2020)
Mount Mercou − viewed by Curiosity (4 March 2021)
Mont Mercou beneath Martian clouds (19 March 2021)

In June 2021, scientists determined that the methane concentration around Curiosity varied according to the time of sol, with methane present only at night. This explains the difference in methane levels detected by Curiosity and the Trace Gas Orbiter (an open question since 2016), although it does not explain what is creating the methane or why the methane seems to be more short-lived than current models predict.[235] On 3 July 2021, the Curiosity rover viewed the "Rafael Navarro Mountain" area.

Curiosity32 drill holes (17 August 2021)

On 1 November 2021, astronomers reported detecting, in a "first-of-its-kind" process based on SAM instruments, organic molecules, including benzoic acid, ammonia and other related unknown compounds, on the planet Mars by the Curiosity rover.[236][237]

Panorama - viewed by Curiosity (16 November 2021)

On 17 January 2022, scientists reported finding an unusual signal of carbon isotopes on Mars by the Curiosity rover which may (or may not) be associated with ancient Martian life and suggesting, according to the scientists, that microbes residing underground may have emitted the "enriched carbon as methane gas". However, abiotic sources of the unusual carbon signal have not been completely ruled out.[238][239][240]

In April 2022, Mars Science Laboratory was renewed for a fourth extended mission, which will include the exploration of the sulfate-bearing unit.[241]

Mars Curiosity Rover - East Cliffs (noted door-shaped fracture) (7 May 2022)
Curiosity36 drill holes
Panorama of rocks viewed by Curiosity on the slopes of Mount Sharp at Gediz Valles (November 7, 2022).
Panorama of rocks viewed by Curiosity on the slopes of Mount Sharp at Marker Band Valley (December 16, 2022).

Fourth extended mission (October 2022 - Present)[edit]

The rover began its fourth extended mission on 1 October 2022, which will last until October 2025.[242]

In January 2023, the Curiosity Rover viewed and studied the "Cacao" meteorite.

Curiosity views the "Cacao" meteorite (28 January 2023)

In August 2023, Curiosity explored the upper Gediz Vallis Ridge.[243][244] A panoramic view of the ridge is here, and a 3D rendered view is here.

The path of CuriositytoGediz Vallis Ridge and beyond (August 2023)
A Day on Mars (Curiosity rover; 8 November 2023)

In February 2024, Curiosity completed its 40th successful drilling,[245][246] of a rock named "Mineral King" in Gediz Vallis.

Current status[edit]

Weather[edit]

Location and travel statistics[edit]

Distance traveled over time by Curiosity

As of July 10, 2024, Curiosity has been on the planet Mars for 4240 sols (4356 total days) since landing on 6 August 2012. Since 11 September 2014, Curiosity has been exploring the slopes of Mount Sharp,[149][150] where more information about the history of Mars is expected to be found.[109] As of 26 January 2021, the rover has traveled over 24.15 km (15.01 mi) and climbed over 327 m (1,073 ft) in elevation[151][179][249] to, and around, the mountain base since arriving at Bradbury Landing in August 2012.[151][179]

The Curiosity rover is exploring the slopes of Mount Sharp.[149][150]
Close-up map - planned route from "Dingo Gap" to "Kimberley" (KMS-9) (HiRISE image)
(18 February 2014/Sol 547).
Traverse map - Curiosity has traveled over 21.92 km (13.62 mi) since leaving its "start" point in Yellowknife Bay on 4 July 2013 (now beyond the "3-sigma safe-to-land ellipse" border) (HiRISE image)
(3 March 2020/Sol 2692).
Context map - Curiosity's trip to Mount Sharp (star = landing)
(22 August 2019/Sol 2504).
Curiosity traverse path showing location as of June 2021. An up-to-date live link
Credit: NASA/JPL-Caltech/University of Arizona


Location map - Curiosity rover at the base of Mount Sharp - as viewed from Space (MRO; HiRISE; 3 March 2020/Sol 2692).
Mars Curiosity Rover - Quadrant Themes (8 June 2023)

Equipment status[edit]

Since early 2015, the percussive mechanism in the drill that helps chisels into rock has had an intermittent electrical short circuit.[250]

In December 2016, the motor inside the drill caused a malfunction that prevented the rover from moving its robotic arm and driving to another location.[251] The fault is in the drill feed motor - internal debris is suspected.[250] The fault was determined to be limited to the drill mechanism and the rover started moving again on 9 December. The robotic arm is functional, and the Curiosity team performed diagnostics on the drill mechanism throughout 2017.[252] On 4 June 2018, NASA announced that Curiosity's ability to drill has been sufficiently restored by changing the drilling methods.[204]

Since 15 September 2018, a glitch in Curiosity's active computer (Side-B) has prevented Curiosity from storing science and key engineering data.[214] On 3 October 2018, the JPL began operating Curiosity on its backup computer (Side-A).[214] Curiosity will store science and engineering data normally using its Side-A computer until the cause of the glitch in Side-B is determined and remedied.[214]

Images[edit]

Self-portraits[edit]

Curiosity roveronMount SharponMars — self-portraits
"Rocknest"
(Oc2012)
"JohnKlein"
(Ma2013)
"Windjana"
(Ma2014)
"Mojave"
(Ja2015)
"Buckskin"
(Aug2015)
"BigSky"
(Oc2015)
"Namib"
(Ja2016)
"Murray"
(Se2016)
"VeraRub"
(Ja2018)
"DustStrm"
(Ju2018)
"VeraRub"
(Ja2019)
"Aberlady"
(Ma2019)
"GlenE"
(Oc2019)
"MaryAnn"
(No2020)
"MtMercou"
(March 2021)
"Greenh"
(No2021)
Curiosity rover self-portrait ("Hutton" Drill Site; 26 February 2020)

Videos[edit]

Curiosity rover mission - One Year on Mars (6 August 2012 – 5 August 2013) (03:58/file)
(2 August 2013).[107][108]
Curiosity rover views - First Year on Mars (6 August 2012 – 5 August 2013) (02:13/file)
(1 August 2013).[107][108]
Curiosity views a Solar EclipsebyPhobos, largest of the two Moons of Mars (01:30/real-time)
(20 August 2013).

Gallery[edit]

Wide images[edit]

Curiosity's view of Mount Sharp (20 September 2012; white balanced; raw color).
Curiosity's view of the Rocknest area - South is center/North at both ends; Mount Sharp at SE horizon (somewhat left-of-center); Glenelg at East (left-of-center); rover tracks at West (right-of-center) (16 November 2012; white balanced; raw color; interactives).
Curiosity's view from Rocknest looking eastward toward Point Lake (center) on the way to Glenelg Intrigue (26 November 2012; white balanced; raw color).
Curiosity's view of Drilling Sites of Rocks at Yellowknife Bay (24 December 2012).
Curiosity's view from the slopes of Mount Sharp (December 1, 2019; video (3:09)).
Curiosity's view of Mount Sharp (9 September 2015).
Curiosity's view of Rafael Navarro Mountain (April 5, 2021).
Curiosity views Marker Band Valley (8 April 2023).
Curiosity's view of Mars skyatsunset (February 2013; Sun simulated by artist).
Curiosity's first view of the Earth and the Moon from the surfaceofMars (31 January 2014).[255]

See also[edit]

  • Astrobiology
  • Composition of Mars
  • ExoMars programme
  • Exploration of Mars
  • Geography of Mars
  • Geology of Mars
  • InSight lander
  • List of missions to Mars
  • List of rocks on Mars
  • Mars Exploration Rover
  • Mars Express orbiter
  • Mars Odyssey Orbiter
  • Mars Orbiter Mission
  • Mars Pathfinder (Sojourner rover)
  • Mars Reconnaissance Orbiter
  • Mars 2020 rover mission
  • MAVEN orbiter
  • Moons of Mars
  • Phoenix lander
  • Robotic spacecraft
  • Scientific information from the Mars Exploration Rover mission
  • Space exploration
  • Timeline of Mars 2020
  • U.S. Space Exploration History on U.S. Stamps
  • Viking program
  • Water on Mars
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  • ^ Revkin, Andrew C. (6 February 2014). "Martian View of Our Pale Dot". New York Times. Retrieved 9 February 2014.
  • External links[edit]

  • icon Biology
  • Solar System
  • Spaceflight

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Timeline_of_Mars_Science_Laboratory&oldid=1231984662"

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