Tidal disruption of Phobos as the cause of surface fractures

T. A. Hurford, E. Asphaug, J. N. Spitale, D. Hemingway, A. R. Rhoden, W. G. Henning, B. G. Bills, S. A. Kattenhorn, M. Walker

Research output: Contribution to journalArticle

21 Scopus citations

Abstract

Phobos, the innermost satellite of Mars, displays an extensive system of grooves that are mostly symmetric about its sub-Mars point. Phobos is steadily spiraling inward due to the tides it raises on Mars lagging behind Phobos’ orbital position and will suffer tidal disruption before colliding with Mars in a few tens of millions of years. We calculate the surface stress field of the deorbiting satellite and show that the first signs of tidal disruption are already present on its surface. Most of Phobos’ prominent grooves have an excellent correlation with computed stress orientations. The model requires a weak interior that has very low rigidity on the tidal evolution time scale, overlain by an ~10–100 m exterior shell that has elastic properties similar to lunar regolith as described by Horvath et al. (1980).

Original languageEnglish (US)
Pages (from-to)1054-1065
Number of pages12
JournalJournal of Geophysical Research E: Planets
Volume121
Issue number6
DOIs
StatePublished - Jun 1 2016

Keywords

  • satellites
  • tectonics
  • tides

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geophysics
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

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    Hurford, T. A., Asphaug, E., Spitale, J. N., Hemingway, D., Rhoden, A. R., Henning, W. G., Bills, B. G., Kattenhorn, S. A., & Walker, M. (2016). Tidal disruption of Phobos as the cause of surface fractures. Journal of Geophysical Research E: Planets, 121(6), 1054-1065. https://doi.org/10.1002/2015JE004943