Topographic mapping of pluto and charon using new horizons data

  • P. M. Schenk
  • , R. A. Beyer
  • , J. M. Moore
  • , J. R. Spencer
  • , W. B. McKinnon
  • , A. D. Howard
  • , O. M. White
  • , O. M. Umurhan
  • , K. Singer
  • , S. A. Stern
  • , H. A. Weaver
  • , L. A. Young
  • , K. Ennico Smith
  • , C. Olkin

Research output: Contribution to journalConference articlepeer-review

1 Scopus citations

Abstract

New Horizons 2015 flyby of the Pluto system has resulted in high-resolution topographic maps of Pluto and Charon, the most distant objects so mapped. DEM's over ∼30% of each object were produced at 100-300 m vertical and 300-800 m spatial resolutions, in hemispheric maps and high-resolution linear mosaics. Both objects reveal more relief than was observed at Triton. The dominant 800-km wide informally named Sputnik Planum bright ice deposit on Pluto lies in a broad depression 3 km deep, flanked by dispersed mountains 3-5 km high. Impact craters reveal a wide variety of preservation states from pristine to eroded, and long fractures are several km deep with throw of 0-2 km. Topography of this magnitude suggests the icy shell of Pluto is relatively cold and rigid. Charon has global relief of at least 10 km, including ridges of 2-3 km and troughs of 3-5 km of relief. Impact craters are up to 6 km deep. Vulcan Planum consists of rolling plains and forms a topographic moat along its edge, suggesting viscous flow.

Keywords

  • Charon
  • Pluto
  • Spatial databases
  • Topographic mapping

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