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Hokusai (crater)

Coordinates:58°18′N342°18′W / 58.3°N 342.3°W /58.3; -342.3
From Wikipedia, the free encyclopedia
Crater on Mercury
Hokusai
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Photo of Hokusai byMESSENGER
Feature typePeak-ring impact basin
LocationHokusai quadrangle,Mercury
Coordinates58°18′N342°18′W / 58.3°N 342.3°W /58.3; -342.3
Diameter95 km (59 mi)
EponymKatsushika Hokusai[1]

Hokusai is a rayedimpact crater onMercury, which was discovered in 1991 by ground-basedradar observations conducted atGoldstone Observatory.[2] The crater was initially known asfeature B. Its appearance was so dissimilar to other impact craters that it was once thought to be ashield volcano. However, improved radar images by theArecibo Observatory obtained later in 2000–2005 clearly showed that feature B is an impact crater with an extensiveray system. The bright appearance of rays in the radio images indicates that the crater is geologically young; fresh impact ejecta has a rough surface, which leads to strong scattering of radio waves.[2]

Hokusai is named afterKatsushika Hokusai (1760–1849), a Japanese artist and printmaker of theEdo period.[3][1] The name Hokusai was suggested by radar astronomer John K. Harmon.[4] The crater has a diameter of about 100 km; the rays extend for thousands kilometers, covering much of the northern hemisphere.[5]

Hokusai is the fourth-largest crater of theKuiperian system on Mercury. The largest isBartók crater.[6] Hokusai is one of 110peak ring basins on Mercury.[7]


  • The rays of Hokusai crater (near central horizon) extend across much of the planet
    The rays of Hokusai crater (near central horizon) extend across much of the planet
  • The ray system close to the crater
    The ray system close to the crater
  • MESSENGER WAC image
    MESSENGER WAC image
  • Mosaic of MESSENGER NAC images
    Mosaic of MESSENGER NAC images
  • Another mosaic of the interior
    Another mosaic of the interior

References

[edit]
  1. ^ab"Ten Craters On Mercury Receive New Names". SpaceDaily. RetrievedMarch 29, 2010.
  2. ^abHarmon, John K.; Slade, Martin A.; Butler, Bryan J.; Head, James W.; Rice, Melissa S.; Campbell, Donald B. (2007). "Mercury: Radar images of the equatorial and midlatitude zones".Icarus.187 (2):374–405.Bibcode:2007Icar..187..374H.doi:10.1016/j.icarus.2006.09.026.
  3. ^"Hokusai (crater)".Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
  4. ^"Hokusai Paints a Wave of Rays". NASA/Johns Hopkins University Applied Physics Laboratory/Carnegie Institution of Washington. 11 May 2010. Archived fromthe original on 5 October 2013. Retrieved13 May 2012.
  5. ^"PIA11356: Looking Back to the Source". NASA. October 6, 2008. RetrievedMarch 29, 2010.
  6. ^Denevi, B. W., Ernst, C. M., Prockter, L. M., and Robinson, M. S., 2018. The Geologic History of Mercury. InMercury: The View AfterMESSENGER edited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 6, Table 6.4.
  7. ^Chapman, C. R., Baker, D. M. H., Barnouin, O. S., Fassett, C. I., Marchie, S., Merline, W. J., Ostrach, L. R., Prockter, L. M., and Strom, R. G., 2018. Impact Cratering of Mercury. InMercury: The View AfterMESSENGER edited by Sean C. Solomon, Larry R. Nittler, and Brian J. Anderson. Cambridge Planetary Science. Chapter 9.

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