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Degas (crater)

Coordinates:37°30′N127°00′W/ 37.5°N 127°W/37.5; -127
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Degas
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Degas crater,MESSENGERspacecraft image, 2011. Inset isMariner 10image from 1974.
Feature typeCentral-peak impact crater
LocationShakespeare quadrangle,Mercury
Coordinates37°30′N127°00′W/ 37.5°N 127°W/37.5; -127
Diameter54 km (34 mi)
DiscovererMariner 10
EponymEdgar Degas

Degasis arayedcrateronMercuryat latitude 37.5 N, longitude 127 W. Its diameter is 54 kilometres (34 mi). It was named after the French impressionist painterEdgar Degasin 1979.[1]The rays consist of light colored material blasted out during the crater's formation. Craters older than Degas are covered by the ray material, while younger craters are seen superimposed on the rays.[2]Degas forms a crater pair withBrontëto the north. Both lie near the center ofSobkou Planitia.[3]

The crater's floor contains cracks that formed as the pool ofimpact meltcooled and shrank. The high-reflectance material on the walls and in the central portion of the crater probably has a composition distinct from that of the crater floor and surroundings. The illumination conditions and down-slope movement of eroded material exposing fresh rock also contribute to the bright appearance.[4]The floor of Degas exposed low-reflectance material (LRM).[5]

Degas is one of the largest craters of theKuiperiansystem on Mercury. The largest isBartókcrater.[6]

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References[edit]

  1. ^"Degas (crater)".Gazetteer of Planetary Nomenclature.USGS Astrogeology Research Program.
  2. ^Nemiroff, R.; Bonnell, J., eds. (16 December 2000)."Degas Ray Crater on Mercury".Astronomy Picture of the Day.NASA.
  3. ^Sobkou Planitia,at eSky
  4. ^Degas CraterArchived2014-09-14 at theWayback Machineat NASA Messenger website. This article incorporatespublic domaintext from thisUS governmentwebsite.
  5. ^Denevi, B. W., Ernst, C. M., Prockter, L. M., and Robinson, M. S., 2018. The Geologic History of Mercury. InMercury: The View AfterMESSENGERedited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 6.4.4.
  6. ^Denevi, B. W., Ernst, C. M., Prockter, L. M., and Robinson, M. S., 2018. The Geologic History of Mercury. InMercury: The View AfterMESSENGERedited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 6, Table 6.4.

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