Glacial, Periglacial and Glacio-Volcanic Structures on the Echus Plateau, Upper Kasei Vallis

Details Glacial, Periglacial and Glacio-Volcanic Structures on the Echus Plateau, Upper Kasei Vallis Glacial, Periglacial and Glacio-Volcanic Structures on the Echus Plateau, Upper Kasei Vallis

Jul 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007lpico1353.3002z&link_type=abstract

Seventh International Conference on Mars, held July 9-13, 2007 in Pasadena, California, LPI Contribution No. 1353, p.3002

Physics

Scientific paper

Sinuous ridges, 270 km long and 200 m high, cross the Hesperian lavas
above Echus Chasma. The eastern edge of Echus Plateau is bounded by
glacial outwash extending along the edge of Echus Chasma. The presence
of volcanic and glacial structures indicates a subglacial volcanic
origin for the ridges.

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