Geological Chronicle
On the Moon’s far side, Buffon lies a crater diameter south of the walled plain Chebyshev. Langmuir lies to the northeast and Leavitt to the southwest; Buffon is nearly midway among these formations.
Buffon dates to the Nectarian period. Its worn rim can still be traced through rugged terrain, though it is irregular and rounded after a history of lesser impacts. A tiny crater lies across the northern rim, and the satellite crater Buffon D sits along the inner eastern wall.
The floor is generally level but remains rugged and irregular, particularly in the eastern half. An infrared spectrum of pure crystalline plagioclase has been identified on the central peak and the east and southwest floor.
The crater takes its name from French naturalist Georges-Louis Leclerc, Comte de Buffon. The International Astronomical Union formally adopted the designation in 1970.