Deposition and degradation of a volatile-rich layer in Utopia Planitia and implications for climate history on Mars

Details Deposition and degradation of a volatile-rich layer in Utopia Planitia and implications for climate history on Mars Deposition and degradation of a volatile-rich layer in Utopia Planitia and implications for climate history on Mars

Jun 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007jgre..11206010m&link_type=abstract

Journal of Geophysical Research, Volume 112, Issue E6, CiteID E06010

Mathematics

Logic

33

Planetary Sciences: Solar System Objects: Mars, Planetary Sciences: Solar System Objects: Comparative Planetology, Cryosphere: Thermokarst, Cryosphere: Permafrost (0475), Cryosphere: Periglacial Processes

Scientific paper

We investigate the surface morphology of a study area in western Utopia Planitia, Mars, which is characterized by a variety of landforms that resemble those of terrestrial periglacial landscapes. Polygonally fractured ground and thermokarst-like depressions are found to be located in a young mantling deposit with a thickness of several tens of meters. We observe a latitudinal dependence of the degradation of this mantling deposit. Larger depressions, whose floors reveal the underlying basement rocks, cover a higher fraction of the total terrain in the southern part of the study area than in the northern part, indicating a more intense degradation of the mantle in the south. All depressions have an asymmetric cross section in north-south direction, interpreted to be the result of the different solar radiation on differently oriented slopes. On the basis of our morphological observations, we develop a conceptual model for landscape evolution in western Utopia Planitia. It involves subaerial deposition of a layered, ice-rich mantle and its subsequent degradation by polygon formation and sublimation. A terrestrial analog to the polygonally fractured mantling deposit and its thermokarst-like depressions is the Siberian Ice Complex or ``Yedoma,'' which consists of subaerial ice-rich deposits and is connected to nonglaciated landscapes with highly continental cold-climatic environmental conditions. Our comparison suggests that no unusual or exotic processes need to be invoked to explain the current morphology of western Utopia. However, the young age of the deposition and degradation implies climatic excursions in the very recent past on Mars.

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