Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature, Evolution and Thickness of Lobate Debris Aprons and Lineated Valley Fill

Details Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature, Evolution and Thickness of Lobate Debris Aprons and Lineated Valley Fill Modification of Graben Along the Dichotomy Boundary in Eastern Arabia Terra (Coloe Fossae; 53-59°E, 37-41°N): Nature, Evolution and Thickness of Lobate Debris Aprons and Lineated Valley Fill

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3177d&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3177

Physics

Scientific paper

Coloe Fossae lies on the dichotomy boundary of Mars and shows evidence
for widespread glaciation in its recent history. We use MOC, HRSC and
MOLA data to measure minimum thickness for the initial volume of ice.

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