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AGU: Geophysical Research Letters

 

Keywords

  • seasonal processes
  • mass wasting HiRISE

Index Terms

  • Planetary Sciences: Solid Surface Planets: Polar regions
  • Planetary Sciences: Solar System Objects: Mars
  • Planetary Sciences: Solid Surface Planets: Surface materials and properties
  • Planetary Sciences: Solid Surface Planets: Ices
  • Cryosphere: Avalanches

Abstract

Seasonally active frost-dust avalanches on a north polar scarp of Mars captured by HiRISE

Patrick Russell

Department of Space Research and Planetary Sciences, Physikalisches Institut, University of Bern, Bern, Switzerland

Nicolas Thomas

Department of Space Research and Planetary Sciences, Physikalisches Institut, University of Bern, Bern, Switzerland

Shane Byrne

Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona, USA

Kenneth Herkenhoff

U.S. Geological Survey, Flagstaff, Arizona, USA

Kathryn Fishbaugh

Center for Earth and Planetary Studies, Smithsonian Air and Space Museum, Washington, D. C., USA

Nathan Bridges

Jet Propulsion Lab, California Institute of Technology, Pasadena, California, USA

Chris Okubo

U.S. Geological Survey, Flagstaff, Arizona, USA

Moses Milazzo

U.S. Geological Survey, Flagstaff, Arizona, USA

Ingrid Daubar

HiRISE Operations Center, Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona, USA

Candice Hansen

Jet Propulsion Lab, California Institute of Technology, Pasadena, California, USA

Alfred McEwen

HiRISE Operations Center, Lunar and Planetary Laboratory, University of Arizona, Tucson, Arizona, USA

North-polar temporal monitoring by the High Resolution Imaging Science Experiment (HiRISE) orbiting Mars has discovered new, dramatic examples that Mars' CO2-dominated seasonal volatile cycle is not limited to quiet deposition and sublimation of frost. In early northern martian spring, 2008, HiRISE captured several cases of CO2 frost and dust cascading down a steep, polar scarp in discrete clouds. Analysis of morphology and process reveals these events to be similar to terrestrial powder avalanches, sluffs, and falls of loose, dry snow. Potential material sources and initiating mechanisms are discussed in the context of the Martian polar spring environment and of additional, active, aeolian processes observed on the plateau above the scarp. The scarp events are identified as a trigger for mass wasting of bright, fractured layers within the basal unit, and may indirectly influence the retreat rate of steep polar scarps in competing ways.

Received 25 August 2008; accepted 30 October 2008; published 6 December 2008.

Citation: Russell, P., et al. (2008), Seasonally active frost-dust avalanches on a north polar scarp of Mars captured by HiRISE, Geophys. Res. Lett., 35, L23204, doi:10.1029/2008GL035790.

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