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Volta is a lunarimpact crater near the northwest limb of the Moon. It is located south-southeast of the crater Xenophanes, and due north of the smaller Galvani. The crater Regnault lies across the western rim of Volta. Attached to the southwest rim of Volta and the southern rim of Regnault is Stokes. The worn Langley is lying between Volta and Stokes in the north and Galvani in the south.
The outer rim of Volta is heavily worn and irregular, with small craters overlying the rim crest, a chain of craters along the east, and Regnault along the west rim. Even the northern rim is irregular, with a gouging valley extending through the north-northeast rim towards Xenophanes. In contrast the interior floor is relatively level and flat, other than some fractures.[1] Volta B is in the northeast interior, and Volta D is on the southeast rim.
^The geologic history of the Moon, 1987, Wilhelms, Don E.; with sections by McCauley, John F.; Trask, Newell J. USGS Professional Paper: 1348. (online)
^Volta, Gazetteer of Planetary Nomenclature International Astronomical Union (IAU) Working Group for Planetary System Nomenclature (WGPSN)
Andersson, L. E.; Whitaker, E. A. (1982). NASA Catalogue of Lunar Nomenclature. NASA RP-1097.
Menzel, D. H.; Minnaert, M.; Levin, B.; Dollfus, A.; Bell, B. (1971). "Report on Lunar Nomenclature by the Working Group of Commission 17 of the IAU". Space Science Reviews. 12 (2): 136–186. Bibcode:1971SSRv...12..136M. doi:10.1007/BF00171763. S2CID122125855.