Eijkman (crater)

Eijkman
Oblique view of Eijkman (LRO)
Coordinates63°06′S 141°30′W / 63.1°S 141.5°W / -63.1; -141.5
Diameter54 km
DepthUnknown
Colongitude144° at sunrise
FormationNectarian[1]
EponymChristiaan Eijkman

Eijkman is a lunar impact crater that is located on the far side of the Moon's southern hemisphere.[2] It lies about a half crater diameter to the southeast of the larger crater Lemaître. To the south-southwest is the crater Crommelin, and to the northeast is Fizeau.

On the lunar geologic timescale, Eijkman dates to the Nectarian period.[1] The rim of this crater is well-defined and has not been significantly worn down by impacts. Nevertheless, there are a few tiny craterlets along the edge and a small craterlet along the northern inner wall.[3] The inner walls display some minor terracing along the northwestern edge. Near the midpoint of the crater interior floor is a horseshoe-shaped central peak formation, with the open end pointing towards the south. The spectra of the central peak fits an olivine-bearing gabbroic norite mineralogy, which originated from a depth of 5.4 to 8.2 km.[4]

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 Eijkman.

Eijkman Latitude Longitude Diameter
D 62.3° S 136.9° W 25 km

References

  1. 1 2 Moriarty, D. P.; Pieters, C. M. (March 2018). "The Character of South Pole-Aitken Basin: Patterns of Surface and Subsurface Composition". Journal of Geophysical Research: Planets. 123 (3): 729–747. Bibcode:2018JGRE..123..729M. doi:10.1002/2017JE005364.
  2. ↑ Moore, Patrick (2000). The Data Book of Astronomy. CRC Press. p. 67. ISBN 978-1-4200-3344-1.
  3. ↑ "What Color Is The Moon?". LunarSail.com. 2022-04-18. Retrieved 2023-06-03.
  4. ↑ Cahill, J. T. S.; et al. (September 2009). "Compositional variations of the lunar crust: Results from radiative transfer modeling of central peak spectra". Journal of Geophysical Research. 114 (E9) E09001. Bibcode:2009JGRE..114.9001C. doi:10.1029/2008JE003282.

Sources