Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Geology  





2 References  














TaurusLittrow






Català
Deutsch
Eesti
Español
Français
Italiano
Bahasa Melayu

Português
Tiếng Vit

 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 




Print/export  







In other projects  



Wikimedia Commons
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


This is an old revision of this page, as edited by Tyrol5 (talk | contribs)at18:05, 29 August 2010 (created article). The present address (URL) is a permanent link to this revision, which may differ significantly from the current revision.
(diff)  Previous revision | Latest revision (diff) | Newer revision  (diff)

Astronaut Harrison Schmitt is seen next to a large boulder in the Taurus Littrow valley on the Apollo 17 mission in 1972.

Taurus-Littrow is a lunar valley located on the Lunar near side at the coordinates 20°00′N 31°00′E / 20.0°N 31.0°E / 20.0; 31.0 that served as the landing site for the American Apollo 17 mission, the last manned mission to the Moon to date.[1][2]

The valley is located on the southeastern edge of Mare Serenitatis along a ring of mountains formed between 3.8 and 3.9 billion years ago when a large object impacted the Moon, forming Mare Serenitatis and pushing rock outward and upward. Taurus-Littrow is located in the Taurus mountain range and south of Littrow crater, features after which the valley received its name. The valley was named by the crew of Apollo 17, and was subsequently adopted by the IAU in 1973.[1]

Geology

The Taurus-Littrow valley is geologically diverse in that during its formation, lavas welled upward from the Moon's interior. As a result of this, rock and soil samples from the area that were collected by astronauts Eugene Cernan and Harrison Schmitt gave insight to the natural history and geologic timeline of the Moon.

Somewhere between 100 and 200 million years after the Serenitatis basin and Taurus-Littrow formed, the lavas that began to seep through the lunar crust began to flood the low-lying areas. These lava flows were often accompanied by fire fountains that blanketed the surrounding area with tiny glass beads. These beads were sometimes colored orange, explaining the orange soil discovered by the Apollo 17 astronauts. Most of these beads, however, where darkly colored, resulting in the dark appearance of the Serenitatis basin from Earth.

The valley itself is elongated along an axis that points toward the center of Mare Serenitatis. Large massifs are located on either side of the valley, called the North and South Massifs, respective to their geographic location in relation to each other. The height of these massifs give the valley a depth greater than that of the Grand Canyon in the United States. Along the South Massif lies Bear Mountain, named after a mountain of the same name near Harrison Schmitt's hometown of Silver City, New Mexico. The sculptured hills make up the east edge of the valley. To the west, the North and South massifs funnel into the main outlet of the valley into Mare Serenitatis, partially blocked by Family mountain.[1]

References


Retrieved from "https://en.wikipedia.org/w/index.php?title=Taurus–Littrow&oldid=381730169"

Category: 
LQ12 quadrangle
Hidden category: 
Pages using gadget WikiMiniAtlas
 



This page was last edited on 29 August 2010, at 18:05 (UTC).

This version of the page has been revised. Besides normal editing, the reason for revision may have been that this version contains factual inaccuracies, vandalism, or material not compatible with the Creative Commons Attribution-ShareAlike License.



Privacy policy

About Wikipedia

Disclaimers

Contact Wikipedia

Code of Conduct

Developers

Statistics

Cookie statement

Mobile view



Wikimedia Foundation
Powered by MediaWiki