The rim of this crater is heavily worn by impacts, and several small craterlets lie along the southern edge. The inner wall is somewhat wider on the western side when compared to the east and southeast. The interior floor is relatively level and featureless.
Albedo Anomaly
To the northeast of Dufay is a bright albedo anomaly that does not correlate with any topographic features. The lunar surface at the anomaly is not atypical under low sun angles.[1] The albedo anomaly is associated with an enhancement in Thorium.[2]
Dufay is at center, and the elongate white patch above right of center is the anomaly. The bright feature to the left is Mandel'shtam F crater and its ray system.
The albedo anomaly is visible above center in this view from Apollo 11
Satellite craters
Map of satellite craters
By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Dufay.
↑N. E. Petro. Association Between Small Thorium Enhancements, Silicic Volcanism, and Enhanced OH/H2O as Measured by the Moon Mineralogy Mapper. Annual Meeting of the Lunar Exploration Analysis Group, 2014. [1]
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 Reviews12 (2): 136–186. doi:10.1007/BF00171763. Bibcode: 1971SSRv...12..136M.