Surface composition of Hyperion

  • D. P. Cruikshank
  • , J. B. Dalton
  • , C. M.Dalle Ore
  • , J. Bauer
  • , K. Stephan
  • , G. Filacchione
  • , A. R. Hendrix
  • , C. J. Hansen
  • , A. Coradini
  • , P. Cerroni
  • , F. Tosi
  • , F. Capaccioni
  • , R. Jaumann
  • , B. J. Buratti
  • , R. N. Clark
  • , R. H. Brown
  • , R. M. Nelson
  • , T. B. McCord
  • , K. H. Baines
  • , P. D. Nicholson
  • C. Sotin, A. W. Meyer, G. Bellucci, M. Combes, J. P. Bibring, Y. Langevin, B. Sicardy, D. L. Matson, V. Formisano, P. Drossart, V. Mennella

Research output: Contribution to journalArticlepeer-review

48 Scopus citations

Abstract

Hyperion, Saturn's eighth largest icy satellite, is a body of irregular shape in a state of chaotic rotation. The surface is segregated into two distinct units. A spatially dominant high-albedo unit having the strong signature of H2O ice contrasts with a unit that is about a factor of four lower in albedo and is found mostly in the bottoms of cup-like craters. Here we report observations of Hyperion's surface in the ultraviolet and near-infrared spectral regions with two optical remote sensing instruments on the Cassini spacecraft at closest approach during a fly-by on 25-26 September 2005. The close fly-by afforded us the opportunity to obtain separate reflectance spectra of the high- and low-albedo surface components. The low-albedo material has spectral similarities and compositional signatures that link it with the surface of Phoebe and a hemisphere-wide superficial coating on Iapetus.

Original languageEnglish (US)
Pages (from-to)54-56
Number of pages3
JournalNature
Volume448
Issue number7149
DOIs
StatePublished - Jul 7 2007

ASJC Scopus subject areas

  • General

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