Topographic evidence for shield volcanism on Io

Jeffrey M. Moore, Alfred S. McEwen, Edward F. Albin, Ronald Greeley

Research output: Contribution to journalArticle

15 Scopus citations

Abstract

A shield volcano has been identified on Io, based on photoclinometrically determined slope values and planimetric presentation. The slope values (typically 10°) and 2.5 km height of the volcano imply that it is composed of a material with the mechanical properties of basaltic rock. The height of the volcano may also indicate a minimum value of ∼40 km for the thickness of the local lithosphere.

Original languageEnglish (US)
Pages (from-to)181-183
Number of pages3
JournalIcarus
Volume67
Issue number1
DOIs
StatePublished - Jul 1986
Externally publishedYes

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Space and Planetary Science

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