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Geology of the Apollo 17 siteThe Apollo 17 landing site was unique in several aspects: (1) it was the only site that was not selected from telescopic-based geologic interpretation--interest in the site was generated by the visual observations of Al Worden, Apollo 15 Command Module pilot, who interpreted dark-haloed craters as possible cinder cones; (2) instead of 20-m-resolution photographs, as was the norm for all earlier missions, this site had Apollo 15 panoramic camera photography coverage that had 2-m resolution; and (3) it had a geologist-astronaut aboard who was intimately involved in all stages of planning and mission operation, and was also instrumental in the design of a long-handled sample bag holder that eliminated the need for crew to dismount before collecting a sample, which then permitted sampling between major stations. Details of site geology, sample description, and geologic synthesis of the site as viewed from studies through 1976 are summarized.
Document ID
19930009614
Acquisition Source
Legacy CDMS
Document Type
Other
Authors
Muehlberger, W. R.
(Texas Univ. Austin, TX, United States)
Date Acquired
September 6, 2013
Publication Date
December 2, 1992
Publication Information
Publication: Lunar Science Inst., Workshop on Geology of the Apollo 17 Landing Site
Subject Category
Lunar And Planetary Exploration
Accession Number
93N18803
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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