Erosion by flowing Martian lava

New insights for Hecates Tholus from Mars express and MER data

David Williams, Ronald Greeley, Ernst Hauber, Klaus Gwinner, Gerhard Neukum

Research output: Contribution to journalArticle

34 Citations (Scopus)

Abstract

We have used new compositional i nformation on Martian basaltic rocks from the Mars Exploration Rover Spirit and data from new stereo imaging by the High Resolution Stereo Camera (HRSC) on the Mars Express orbiter to constrain an existing analytical-numerical computer model to assess the potential of Martian lavas to form lava channels by erosion of substrate. The basaltic rocks studied in Gusev crater by Spirit have compositions consistent with lavas of higher liquidus temperature and lower dynamic viscosity than terrestrial tholeiitic basalts, suggesting that they had a greater potential for turbulent flow and erosion of substrate during flow emplacement than terrestrial basalts, more similar to lunar mare basalts. We modeled a specific case to determine whether these lavas could have formed part of a >66 km long channel on the Martian shield volcano Hecates Tholus. This channel formed on relatively steep slopes (∼2-8°), based on measurements from the HRSC Digital Terrain Model. Our results suggest that erosion rates were of the order of tens to hundreds of centimeters/day, depending on flow rate and ice content of the substrate. Eruption durations required to erode the Hecates channel (∼100-30 m deep over the first ∼20 km, depth decreasing downstream) range from weeks to months, which are consistent with the known eruption durations of terrestrial basaltic lavas and the previous modeling of Wilson and Mouginis-Mark (2004). Any Hecates lava channels formed from erosion by lava could have served as conduits for later fluvial activity, as recently described by Fassett and Head (2004, 2005).

Original languageEnglish (US)
Pages (from-to)1-13
Number of pages13
JournalJournal of Geophysical Research E: Planets
Volume110
Issue number5
DOIs
StatePublished - May 20 2005

Fingerprint

Mars Express
lava
erosion
Mars
Erosion
basalt
Substrates
substrate
volcanic eruptions
Rocks
volcanic eruption
Volcanoes
rocks
Ice
Digital cameras
mare basalt
Mars exploration
shield volcano
tholeiitic basalt
digital cameras

ASJC Scopus subject areas

  • Oceanography
  • Astronomy and Astrophysics
  • Atmospheric Science
  • Space and Planetary Science
  • Earth and Planetary Sciences (miscellaneous)
  • Geophysics
  • Geochemistry and Petrology

Cite this

Erosion by flowing Martian lava : New insights for Hecates Tholus from Mars express and MER data. / Williams, David; Greeley, Ronald; Hauber, Ernst; Gwinner, Klaus; Neukum, Gerhard.

In: Journal of Geophysical Research E: Planets, Vol. 110, No. 5, 20.05.2005, p. 1-13.

Research output: Contribution to journalArticle

Williams, David ; Greeley, Ronald ; Hauber, Ernst ; Gwinner, Klaus ; Neukum, Gerhard. / Erosion by flowing Martian lava : New insights for Hecates Tholus from Mars express and MER data. In: Journal of Geophysical Research E: Planets. 2005 ; Vol. 110, No. 5. pp. 1-13.
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