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Camelot (crater)

Lunar impact crater From Wikipedia, the free encyclopedia

Camelot (crater)
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Camelot is a feature on Earth's Moon, a crater in Taurus-Littrow valley. Astronauts Eugene Cernan and Harrison Schmitt visited it in 1972, on the Apollo 17 mission, during EVA 2. Geology Station 5 was along the south rim of Camelot.

Quick Facts Coordinates, Diameter ...

Camelot is due 700 meters west of the landing site. The smaller Horatio crater is to the southwest, and Victory is to the northwest. Powell and Trident are to the southeast.

The crater was named by the astronauts after the castle Camelot of Arthurian legend.[2]

Thumb
Panorama taken by Eugene Cernan from the south rim of Camelot, at Geology Station 5 (part of the "West pan" in the map below")
Thumb
Planimetric map of station 5
Thumb
Apollo 17 panoramic camera image
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Samples

The following samples were collected from Camelot crater (Station 5), as listed in Table 7-I of the Apollo 17 Preliminary Science Report.[3] The "Rock Type" is from the table, and the "Lithology" is from the Lunar Sample Compendium of the Lunar and Planetary Institute or NASA's Lunar Sample Catalog.

SampleIn Situ PhotoRock TypeLithologyPhoto
75015Coarse basaltIlmenite Basalt[4]
75035Medium basaltIlmenite Basalt[5]
75055Coarse basaltIlmenite Basalt[6]
75065-Medium basaltHigh-Ti Mare Basalt[7]-
75066-Dark-gray basaltGlassy Breccia[8]-
75075Medium basaltVuggy Ilmenite Basalt[9]
75085-Medium basaltHigh-Ti Basalt (from soil sample 75080)[10]-
75086-Medium basaltHigh-Ti Basalt (from soil sample 75080)[11]-
75087-Medium basaltHigh-Ti Basalt (from soil sample 75080)[12]-
75088-Fine basaltHigh-Ti Basalt (from soil sample 75080)[13]-
75089-Fine basaltHigh-Ti Basalt (from soil sample 75080)[14]-
75115-Fine basaltHigh-Ti Basalt-
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References

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