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Crater characteristics
Coordinates 40. Selenographic coordinates are used to refer to locations on the surface of Earth 's Moon. 4° N, 153. 2° E
Diameter 78 km
Depth Unknown
Colongitude 209° at sunrise
Eponym John Von Neumann

Von Neumann is a lunar impact crater that lies on the far side of the Moon, in the northern hemisphere. Geometry, a diameter of a Circle is any straight Line segment that passes through the center of the circle and whose Endpoints are on the The depth of any crater in a solid Planet or moon - whether it is an Impact crater, a Volcanic crater, or a Subsidence crater - may Selenographic coordinates are used to refer to locations on the surface of Earth 's Moon. In the broadest sense the term impact crater can be applied to any depression natural or manmade resulting from the high velocity impact of a projectile with larger body Far Side of the Moon, in original French, La face cachée de la lune, is a 2003 film by Robert Lepage. "Globose" redirects here See also Globose nucleus. A sphere (from Greek σφαίρα - sphaira, "globe It is nearly attached to the south-southeastern rim of the Campbell walled plain. Campbell is a large lunar crater that is located in the Northern hemisphere on the far side of the Moon. Ley crater is attached to the northeastern rim of Von Neumann, and is somewhat overlain by the outer rampart. Ley is a lunar Impact crater that is located across the southern rim of the much larger Campbell impact basin. To the west is the prominent Wiener crater, and to the south-southwest is the Nikolayev crater. Wiener is a lunar Impact crater that lies on the Moon 's far side from the Earth. Nikolaev is a crater on the far side of the Moon. It is located north of the Mare Moscoviense and south of the larger Von Neumann crater

This crater has a wide inner wall with multiple terraces. The width of the inner wall varies around the perimeter, with the widest section to the south. There is some slumping along the inner wall to the northwest where the rim makes its closest approach to Campbell, and the narrow terrain between these two craters is rugged and irregular. But, of course, the remaining terrain that surrounds the crater is almost equally rugged. The rim appears somewhat straighter along the southwest side, but is roughly circular elsewhere.

The interior floor is nearly flat and level along the western side. There is a small range of ridges running from the south to the northern edge of the floor, and the ground is more irregular in the eastern half. There are no significant impacts within the crater interior and the sides are generally unworn.

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