By David G Schrunk; et al
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Additional info for The Moon : resources, future development, and settlement
Example text
The material below this seismic boundary is probably chemically similar to the surrounding highlands rocks. The ®rst few Apollo landings had primarily been engineering experiments. The details of how to land safely on the Moon and survive there for a very short time were of paramount importance. It was only in the last few Apollo missions that scienti®c questions predominated over engineering questions with respect to choice of landing site, EVA activities, and so on. Many important scienti®c discoveries resulted from the Apollo missions to the Moon.
MALEO LHB-1 mass summary . . . . . . . . . . . . . . . . Vehicle payload mass during cislunar transportation . . . . . . . . . Acronyms . . . . . . . . . . . . . . . . . . . . . . . . Speci®cations for Nomad Explorer . . . . . . . . . . . . . . . Primary metallic materials set targeted for fabrication technologies development . . . . . . . . . . . . . . . . . . . . . .
Sec. 4. Orientale Basin. 5. Imbrium Basin (upper middle), is easily seen from Earth with the unaided eye. 7 8 Lunar origins and physical features [Ch. 1 The South Pole±Aitken Basin is a large impact crater with a diameter of 2,500 kilometers and a maximum depth of 12 to 13 kilometers. It extends from the south polar region to the Aitken Crater on the far side of the Moon, and is the largest known impact crater in the solar system. The extent of the basin was not known until it was photographed by the Lunar Orbiter Satellite.