Geologic Exploration of Taurus-Littrow: Apollo 17 Landing Site

Science
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Abstract

Apollo 17 landed in a deep graben valley embaying the mountainous highlands southeast of the Serenitatis basin. Impact-generated breccias underlie the massifs adjacent to the valley, and basalt has flooded and leveled the valley floor. The dark mantle inferred from orbital photographs was not recognized as a discrete unit; the unusually thick regolith of the valley floor contains a unique high concentration of dark glass beads that may cause the low albedo of much of the surface.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Geologic Exploration of Taurus-Littrow: Apollo 17 Landing Site
Series title Science
DOI 10.1126/science.182.4113.672
Volume 182
Issue 4113
Year Published 1973
Language English
Publisher American Association for the Advancement of Science
Contributing office(s) Geology, Minerals, Energy, and Geophysics Science Center
Description 9 p.
First page 672
Last page 680
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