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==Geology== |
==Geology== |
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Mare Serenitatis is located within the Serenitatis basin, which is of the [[Nectarian]] [[epoch (geology)|epoch]]. The material surrounding the mare is of the [[Lower Imbrian]] epoch, while the mare material is of the [[Upper Imbrian]] epoch. The mare [[basalt]] covers a majority of the basin and overflows into [[Lacus Somniorum]] to the northeast. The most noticeable feature is the crater [[Posidonius (crater)|Posidonius]] on the northeast rim of the mare.<ref name="ccastronomy">{{cite web|title=Lunar Map |publisher=[http://www.ccastronomy.org/ Central Coast Astronomical Society] |url=http://www.ccastronomy.org/photo_tour_Moon_Map.jpg |access-date=2009-07-04 |url-status = dead|archive-url=https://web.archive.org/web/20070128013417/http://www.ccastronomy.org/photo_tour_Moon_Map.jpg |archive-date=January 28, 2007 }}</ref> The ring feature to the west of the mare is indistinct, except for [[Montes Haemus]]. Mare Serenitatis connects with [[Mare Tranquillitatis]] to the southeast and borders [[Mare Vaporum]] to the southwest. Mare Serenitatis is an example of a [[mass concentration (astronomy)|mascon]], an anomalous gravitational region on the moon. |
Mare Serenitatis is located within the Serenitatis basin, which is of the [[Nectarian]] [[epoch (geology)|epoch]].<ref>[https://pubs.er.usgs.gov/publication/pp1348 The geologic history of the Moon]. [[USGS]] Professional Paper 1348. By [[Don Wilhelms|Don E. Wilhelms]], John F. McCauley, and Newell J. Trask. U.S. Government Printing Office, Washington: 1987. Table 9-3.</ref> The material surrounding the mare is of the [[Lower Imbrian]] epoch, while the mare material is of the [[Upper Imbrian]] epoch. The mare [[basalt]] covers a majority of the basin and overflows into [[Lacus Somniorum]] to the northeast. The most noticeable feature is the crater [[Posidonius (crater)|Posidonius]] on the northeast rim of the mare.<ref name="ccastronomy">{{cite web|title=Lunar Map |publisher=[http://www.ccastronomy.org/ Central Coast Astronomical Society] |url=http://www.ccastronomy.org/photo_tour_Moon_Map.jpg |access-date=2009-07-04 |url-status = dead|archive-url=https://web.archive.org/web/20070128013417/http://www.ccastronomy.org/photo_tour_Moon_Map.jpg |archive-date=January 28, 2007 }}</ref> The ring feature to the west of the mare is indistinct, except for [[Montes Haemus]]. Mare Serenitatis connects with [[Mare Tranquillitatis]] to the southeast and borders [[Mare Vaporum]] to the southwest. Mare Serenitatis is an example of a [[mass concentration (astronomy)|mascon]], an anomalous gravitational region on the moon. |
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A [[mass concentration (astronomy)|mass concentration]] (mascon), or gravitational high, was identified in the center of Mare Serenitatis from Doppler tracking of the five [[Lunar Orbiter program|Lunar Orbiter]] spacecraft in 1968.<ref>{{cite journal | doi = 10.1126/science.161.3842.680 | title = Mascons: Lunar Mass Concentrations | year = 1968 | author = P. M. Muller, W. L. Sjogren | journal = Science | volume = 161 | issue = 3842 | pages = 680–684 | pmid=17801458| bibcode = 1968Sci...161..680M | s2cid = 40110502 }}</ref> The mascon was confirmed and mapped at higher resolution with later orbiters such as [[Lunar Prospector]] and [[Gravity Recovery and Interior Laboratory|GRAIL]]. |
A [[mass concentration (astronomy)|mass concentration]] (mascon), or gravitational high, was identified in the center of Mare Serenitatis from Doppler tracking of the five [[Lunar Orbiter program|Lunar Orbiter]] spacecraft in 1968.<ref>{{cite journal | doi = 10.1126/science.161.3842.680 | title = Mascons: Lunar Mass Concentrations | year = 1968 | author = P. M. Muller, W. L. Sjogren | journal = Science | volume = 161 | issue = 3842 | pages = 680–684 | pmid=17801458| bibcode = 1968Sci...161..680M | s2cid = 40110502 }}</ref> The mascon was confirmed and mapped at higher resolution with later orbiters such as [[Lunar Prospector]] and [[Gravity Recovery and Interior Laboratory|GRAIL]]. |
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Photograph of Mare Serenitatis
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Coordinates | 28°00′N 17°30′E / 28.0°N 17.5°E / 28.0; 17.5 |
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Diameter | 674 km (419 mi)[1][2] |
Eponym | Sea of Serenity |
Mare Serenitatis /sɪˌrɛnɪˈteɪtɪs/ (Latin serēnitātis, the "Sea of Serenity") is a lunar mare located to the east of Mare Imbrium on the Moon. Its diameter is 674 km (419 mi).[1]
Mare Serenitatis is located within the Serenitatis basin, which is of the Nectarian epoch.[3] The material surrounding the mare is of the Lower Imbrian epoch, while the mare material is of the Upper Imbrian epoch. The mare basalt covers a majority of the basin and overflows into Lacus Somniorum to the northeast. The most noticeable feature is the crater Posidonius on the northeast rim of the mare.[4] The ring feature to the west of the mare is indistinct, except for Montes Haemus. Mare Serenitatis connects with Mare Tranquillitatis to the southeast and borders Mare Vaporum to the southwest. Mare Serenitatis is an example of a mascon, an anomalous gravitational region on the moon.
Amass concentration (mascon), or gravitational high, was identified in the center of Mare Serenitatis from Doppler tracking of the five Lunar Orbiter spacecraft in 1968.[5] The mascon was confirmed and mapped at higher resolution with later orbiters such as Lunar Prospector and GRAIL.
Like most of the other maria on the Moon, Mare Serenitatis was named by Giovanni Riccioli, whose 1651 nomenclature system has become standardized.[6] Previously, William Gilbert had cited it as within the Regio Magna Occidentalis ("Large Western Region") in his map of c.1600.[7] Pierre Gassendi had included it as part of the 'Homuncio' ('little man'), referring to a small humanoid figure that he could see among the maria; Gassendi also referred to it as 'Thersite' after Thersites, the ugliest warrior in the Trojan War.[8] Michael van Langren had labelled it the Mare Eugenianum ("Eugenia's Sea") in his 1645 map,[9] in honour of Isabella Clara Eugenia, queen of the Spanish Netherlands.[10] And Johannes Hevelius included it within Pontus Euxinus (after the classical name for the Black Sea) in his 1647 map.
Both Luna 21 and Apollo 17 landed near the eastern border of Mare Serenitatis, in the area of the Montes Taurus range. Apollo 17 landed specifically in the Taurus-Littrow valley, and Luna 21 landed in Le Monnier crater. SpaceIL's Beresheet lunar lander was planned to land in Mare Serenitatis, but crashed into the surface on 11 April 2019. Its final resting place was about 33°N, 19°E, near to the centre of the mare.[11]
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