Glinka (crater) explained

Glinka
Location:Beethoven quadrangle, Mercury
Type:Impact crater
Coordinates:14.83°N -112.55°W
Eponym:Mikhail Glinka

Glinka is a pit-floored crater on Mercury, which was discovered in 1974 by Mariner 10 spacecraft. It was named by the IAU in 2008, after Russian composer Mikhail Glinka.[1]

Its floor is covered by the smooth plain material and displays a kidney-shaped collapse feature, which is also called a central pit. The size of the pit, which was first noticed in MESSENGER images obtained in January 2008, is . It is surrounded by a bright pyroclastic deposit. Such a feature may have resulted from collapse of a magma chamber underlying the central part of the crater. The collapse feature is an analog of Earth's volcanic calderas.[2]

Notes and References

  1. Web site: Glinka . . Gazetteer of Planetary Nomenclature . 25 September 2022 . 28 September 2022 . https://web.archive.org/web/20220928131019/https://planetarynames.wr.usgs.gov/Feature/14509 . live .
  2. Gillis-Davis. Jeffrey J.. Blewett. David T.. Gaskell. Robert W.. Denevi. Brett W.. Robinson. Mark S.. Strom. Robert G.. Solomon. Sean C.. Sprague. Ann L.. Pit-floor craters on Mercury: Evidence of near-surface igneous activity. 2009. Earth and Planetary Science Letters. 285. 3-4. 243–250. 10.1016/j.epsl.2009.05.023. 2009E&PSL.285..243G.