Difference between revisions of "July 21, 2004"
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<td><p align="center" class="main_titles"><b>Author & Editor:</b><br> | <td><p align="center" class="main_titles"><b>Author & Editor:</b><br> | ||
[mailto:tychocrater@yahoo.com Charles A. Wood]</p> | [mailto:tychocrater@yahoo.com Charles A. Wood]</p> | ||
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===COMMENTS?=== | ===COMMENTS?=== | ||
Register, and click on the <b>Discussion</b> tab at the top of the page. | Register, and click on the <b>Discussion</b> tab at the top of the page. | ||
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| + | Contributions to http://www2.lpod.org/ are licensed under a Creative Commons Attribution No-Derivative-Works Non-Commercial 3.0 License. [http://www.creativecommons.org/licenses/by-nc-nd/3.0 http://www.wikispaces.com/i/creativecommons/by-nc-nd_3.0_80x15.png]<br> | ||
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Revision as of 12:16, 1 February 2015
Taurus-Littrow Route Map
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Image Credit: Ralph Aeschliman |
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Taurus-Littrow Route Map With the use of a rover, astronauts on the last three Apollo missions could travel so far that a route map was need before the mission and afterwards to get a geographical (or selenographical for purists) understanding of their explorations. Apollo 17, humanity's last lunar visit, was the most daring - the Lunar Module Challenger came in low over the Taurus Mountains for a pin-point landing on a small flat plain surrounded by mountains, and the astronauts drove the rover a record 36 km. The two main science goals were to sample ancient rocks, hopefully older than the Imbrium impact, and the dark volcanic deposits that might be young. The long trips to North (12 km) and South (20 km) Massifs allowed sampling of rocks that proved to be greater than 4.2 billion years old, but the hoped for young volcanism - the dark mantle material including orange glass at Shorty Crater: Station 4) - was also ancient: 3.64 billion years. Apollo 17 provided evidence for explosive volcanism, but not youthful volcanism on the Moon. Technical Details: Related Links: Tomorrow's LPOD: Huge Fractures |
Author & Editor: |
COMMENTS?
Register, and click on the Discussion tab at the top of the page.
Contributions to http://www2.lpod.org/ are licensed under a Creative Commons Attribution No-Derivative-Works Non-Commercial 3.0 License. 
