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Xenophanes (crater) : ウィキペディア英語版 | Xenophanes (crater)
Xenophanes is a lunar crater that is located along the northwestern limb of the Moon. It is nearly attached to Volta, a similar formation to the south-southwest. To the northeast is the smaller crater Cleostratus. Xenophanes is significantly foreshortened when viewed from the Earth, hindering observation. It is a worn and eroded crater with a battered outer rim that is overlaid by several smaller craters. The rim is a circular range of rugged, irregular ground that is notched in places along the inner wall. A chain of small craters lies along the northern and northeastern rim. At the west end, a pair of clefts in the rim nearly join the floor to the surface beyond. To the northeast, Xenophanes A is an impact crater with a sharp rim and a rough interior. The interior surface is irregular, but sections have been resurfaced by basaltic lava. A pair of flooded crater rims lie along the southern and northeast sections of the interior. The interior is more level and less rough at the eastern end. ==Satellite craters== By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Xenophanes.
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