Transient Slope Lineae: Evidence for Summertime Briny Flows on Mars?

Details Transient Slope Lineae: Evidence for Summertime Briny Flows on Mars? Transient Slope Lineae: Evidence for Summertime Briny Flows on Mars?

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.2314m&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.2314

Physics

1

Scientific paper

TSL form on equator-facing rocky slopes in southern summer from
latitudes -32 to -48. This distribution, incremental
formation and fading, and associated morphologies and mineralogies
suggest the flow of brines.

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