Geological Chronicle
Coulomb lies behind the Moon’s northwestern limb, on the far side. It sits west-southwest of Poczobutt and northeast of Sarton, within the Coulomb-Sarton Basin. The basin is a 530-kilometer-wide impact crater of Pre-Nectarian age.
Coulomb dates to the Late Imbrian period. Its rim is mildly eroded but retains a well-defined edge, with old terraces on the wide inner walls. The floor is remarkably level and nearly featureless, at least compared with the more rugged terrain around it. Only a few tiny craterlets mark the interior plain. Another small crater lies near the south-southeast inner wall.
An outer rampart extends for about a third of the crater’s diameter. Satellite crater Coulomb V lies just beyond the west-northwest limb; Coulomb J sits a short distance from the outer rim on the opposite side, making a nearly symmetric pattern. The inner walls have only a few small impacts, including one near each of those satellite craters.
Coulomb is named for French physicist Charles A. Coulomb (1736–1806). The International Astronomical Union formally adopted the crater’s designation in 1970.