Gullies on Mars: Clues to Their Formation Timescale from Possible Analogs from Devon Island, Nunavut, Arctic Canada

Details Gullies on Mars: Clues to Their Formation Timescale from Possible Analogs from Devon Island, Nunavut, Arctic Canada Gullies on Mars: Clues to Their Formation Timescale from Possible Analogs from Devon Island, Nunavut, Arctic Canada

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.2050l&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.2050

Physics

11

Scientific paper

The origin and evolution of the youthful gully features on Mars remain
enigmatic. Field investigations of possible analogs from Devon Island,
Arctic, suggest that the terrestrial features are <104
years old and result from melting of surface ice.

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