Bhabha (crater)
Encyclopedia
Bhabha is a 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 is located in the southern part 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...

's far side. It is nearly attached to the southeast rim of the larger crater Bose
Bose (crater)
Bose is a lunar impact crater that is located on the far side of the Moon, in the southern hemisphere. It lies just to the northwest of the smaller crater Bhabha, and southeast of Alder....

, and the outer rampart of that crater has produced a slight inward bulge along the northwest face of Bhabha. Other nearby craters of note include Stoney
Stoney (lunar crater)
Stoney is a lunar impact crater that is located in the southern part of the Moon's far side. It lies to the southeast of the crater Baldet and to the east of Bhabha....

 to the east, and Bellinsgauzen
Bellinsgauzen (crater)
Bellinsgauzen is a lunar impact crater that lies in the southern part of Moon, on the far side from the Earth. It is attached to the northern rim of the larger crater Berlage, and within a half crater diameter of Cabannes to the west. North of Bellinsgauzen is the crater Bhabha.The outer rim of...

 to the south.

This is a relatively fresh crater with a nicely terraced inner wall. This terracing is most notable along the southeastern half of the crater, and nearly disappears along the north-northwest rim where the inner wall is at its minimum extent. The rim and inner wall have not been significantly eroded, and there are no craterlets of note along the rim.

The interior floor has a formation of central peaks that forms a semicircle with the concave interior open to the north. The remainder of the floor is relatively level, with a single small craterlet in the northern part.
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