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Geologic Setting of the Apollo 14 Samples

G. A. Swann, N.J. Trask, Milan Hait, R. L. Sutton

Abstract

The Apollo 14 lunar module landed in a region of the lunar highlands that is part of a widespread blanket of ejecta surrounding the mare Imbrium basin. Samples were collected from the regolith developed on a nearly level plain, a ridge 100 meters high, and a blocky ejecta deposit around a young crater. Large boulders in the vicinity of the landing site are coherent fragmental rocks as are some of the returned samples.

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Key concepts: Ejecta, Regolith, Impact crater, Apollo, Geology, Lunar mare, Lunar craters, Astrobiology