Large Grooves in the South Polar Layered Deposits: Insights from Spacecraft Data and Terrestrial Analogs

Details Large Grooves in the South Polar Layered Deposits: Insights from Spacecraft Data and Terrestrial Analogs Large Grooves in the South Polar Layered Deposits: Insights from Spacecraft Data and Terrestrial Analogs

Aug 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000mpse.conf...12b&link_type=abstract

International Conference on Mars Polar Science and Exploration, p. 12

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Mars (Planet), Polar Regions, Climatology, Deposits, Mars Environment, Mars Polar Lander, Viking Mars Program, Mars Global Surveyor, Landing Sites, Sediments, Morphology, Topography, Wind Effects, Grooves

Scientific paper

The Martian polar layered deposits (PLD) are probably the best source of information about the recent climate history of Mars, but their origin and the mechanisms of accumulation are still a mystery. The polar layers are sedimentary deposits that most planetary scientists believe are composed of water ice and varying amounts of wind-blown dust, although their composition is poorly constrained. Interpretation of the observed polar stratigraphy in terms of global climate changes is complicated by the significant difference in surface ages between the north and south PLD inferred from crater statistics. The study reported here was undertaken as part of the landing site selection effort for the Mars Polar Lander (MPL) and Deep Space 2 (DS2) missions that made use of all available data. We used Mariner 9, Viking, and Mars Global Surveyor images of the south PLD in the area accessible to MPL and DS2 to evaluate the topography and morphology of grooves, terraced layers, and other features. Here we report on results from grooves that appear to have been carved by strong winds. Because these features are found throughout the interior of the PLD, where MPL and DS2 were targeted to land, their topographic characteristics were judged as important input for landing site safety assessment. The characteristics of the grooves also provide constraints and insights into aeolian processes in the polar regions and the effects these have on PLD ablation. Our results indicate that these grooves do not represent landing hazards at the scale of the images (approx. 80 m/pixel). Their topography and shape do not seem correlated with south PLD layering. No Earth analog of suitable scale exists, although the grooves bear some resemblance to smaller terrestrial deflation hollows found in soft sediment and ice. Additional information is contained in original extended abstract.

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