Moseley (crater)
Encyclopedia
Moseley is a worn lunar
Moon
The Moon is Earth's only known natural satellite,There are a number of near-Earth asteroids including 3753 Cruithne that are co-orbital with Earth: their orbits bring them close to Earth for periods of time but then alter in the long term . These are quasi-satellites and not true moons. For more...

 impact crater
Impact crater
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 a larger body...

 that lies along the western limb of the Moon
Moon
The Moon is Earth's only known natural satellite,There are a number of near-Earth asteroids including 3753 Cruithne that are co-orbital with Earth: their orbits bring them close to Earth for periods of time but then alter in the long term . These are quasi-satellites and not true moons. For more...

. It lies just to the south of the crater Bartels
Bartels (crater)
Bartels is a lunar crater located along the western perimeter of the Moon's visible face. At this location the crater is viewed from the side, and visibility is affected by libration. The crater can be viewed in its entirety only from lunar orbit...

, and near the north-northeastern rim of Einstein
Einstein (crater)
Einstein is a large lunar crater that lies along the western limb of the Moon, making it difficult to observe from the Earth. The visibility of this formation is affected by libration effects, but even under the best conditions not much detail can be observed except from lunar orbit...

. Due to its location, this crater is viewed side-on from Earth, and not much detail can be seen. It can also become hidden from sight due to the effects of libration
Libration
In astronomy, libration is an oscillating motion of orbiting bodies relative to each other, notably including the motion of the Moon relative to Earth, or of Trojan asteroids relative to planets.-Lunar libration:...

.

The outer rim of this feature has been worn and eroded due to subsequent impacts. Little of the original rim remains intact, and the perimeter is generally an irregular circular ridge surrounding the interior floor. In contrast the floor of the crater is relatively level and featureless. There are only a few tiny craterlets marking the surface.
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