Ohm is a lunar impact crater that is located on the far side of the Moon. It lies to the south of the crater Comrie, and the satellite crater Comrie K is attached to Ohm's northeastern rim. To the northwest is the larger Shternberg, and to the southwest is Kamerlingh Onnes. It is named after the German physicist Georg Simon Ohm. This formation dates to the Copernican period and has a meteoritic iron-rich impact melt. It is located at the origin of a ray system that extends for several hundred kilometers across the surrounding lunar terrain. The exterior surface for about 20–30 km is relatively free of the ray material, but beyond that perimeter is a skirt of higher albedo, with streaks extending to the northwest, east-northeast, and southwards. The outer rim of Ohm is sharply defined, except at the southern end where the edge is somewhat irregular. The inner surface drops down to an interior blanket of slumped material that slopes down to the floor. The crater has a modest central peak. The spectra of this rise fits a gabbro mineralogy, which was excavated from a depth of 6.4 to 9.9 km. Prior to formal naming by the IAU in 1970, Ohm was called Crater 253.
Artemis II The view of Ohm and its surroundings was first captured by human eyes during the lunar flyby of Artemis II in April 2026. The typical chevron-shaped system of Ohm's bright rays was easily noticeable during the approach of the gibbous moon, which was gradually showing its western hemisphere and the far side regions beyond 90° west.
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External links Media related to Ohm (lunar crater) at Wikimedia Commons





