Geomorphological evidence of water level changes in Nepenthes Mensae, Mars

Details Geomorphological evidence of water level changes in Nepenthes Mensae, Mars Geomorphological evidence of water level changes in Nepenthes Mensae, Mars

Aug 2008

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2008icar..196..667d&link_type=abstract

Icarus, Volume 196, Issue 2, p. 667-671.

Mathematics

Logic

9

Scientific paper

In the western sector of Nepenthes Mensae, Mars, there are some geomorphological features that could be related to a standing water sheet in the area, such as fluvial terraces, deltas and shorelines. A detailed analysis of these features reveals two variations in water level, probably related to tectonic processes, as suggested by the existence of a fissural volcano at this site.

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