Pseudokarstic Subsidences Induced by Subsurface Melting of Tephra-covered Firn -- Analogues for Martian Subsidences in the Dyngjufjöll Massif, Iceland

Details Pseudokarstic Subsidences Induced by Subsurface Melting of Tephra-covered Firn -- Analogues for Martian Subsidences in the Dyngjufjöll Massif, Iceland Pseudokarstic Subsidences Induced by Subsurface Melting of Tephra-covered Firn -- Analogues for Martian Subsidences in the Dyngjufjöll Massif, Iceland

Mar 2009

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2009lpi....40.2353g&link_type=abstract

40th Lunar and Planetary Science Conference, (Lunar and Planetary Science XL), held March 23-27, 2009 in The Woodlands, Texas, i

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The subsidences from the selected area of Iceland can aid to understand
more about the newly discovered ice shields on Mars and their
morphological features and climatic environments.

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