Shaping Titan's Landscapes by Dissolution and Evaporation: The Case of Ontario Lacus, a High-Latitude Semi-Arid Karst-Playa Landsystem

Details Shaping Titan's Landscapes by Dissolution and Evaporation: The Case of Ontario Lacus, a High-Latitude Semi-Arid Karst-Playa Landsystem Shaping Titan's Landscapes by Dissolution and Evaporation: The Case of Ontario Lacus, a High-Latitude Semi-Arid Karst-Playa Landsystem

Mar 2012

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2012lpi....43.1914c&link_type=abstract

43rd Lunar and Planetary Science Conference, held March 19–23, 2012 at The Woodlands, Texas. LPI Contribution No. 1659, id.1914

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Scientific paper

The comparison between Ontario Lacus (Titan) and the Etosha Pan
(Namibia), a semi-arid karst-playa landsystem, infer that
dissolution/evaporation processes shaped Ontario Lacus' region until the
present day, and perhaps as a whole, other Titan's lakes.

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