Geological Chronicle
Crommelin lies near the Moon’s south pole, on the far side and within the South Pole-Aitken basin. Zeeman lies to its south, Numerov to the west-southwest and Lemaître to the north. The crater dates to the Pre-Nectarian period.
Subsequent impacts have almost completely degraded the formation, leaving little more than a crater-riddled depression. An equally worn crater lies across the northern rim, and Crommelin X is attached to the outward-bulging northwest perimeter.
The largest craterlets inside Crommelin form a pair near the southern rim. At the center is a slight peak, little more than a low rise. Its spectra fit an olivine-bearing gabbroic norite mineralogy, which was excavated from depths of 3.5 to 9.4 km.
Crommelin is named for British astronomer Andrew C. D. Crommelin, an expert on comets. The International Astronomical Union formally adopted the crater’s designation in 1970.