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Possible liquid water origin for Atacama Desert mudflow and recent gully deposits on Mars |
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| Authors: | JL Heldmann CA Conley AJ Brown L Fletcher CP McKay |
| Institution: | a NASA Ames Research Center, Moffett Field, CA 94035, USA b NASA Headquarters, Washington, DC 20546, USA c SETI Institute, Mountain View, CA 94043, USA |
| Abstract: | Evidence of recent gully activity on Mars has been reported based on the formation of new light toned deposits within the past decade, the origin of which remains controversial. Analogous recent light toned gully features have formed by liquid water activity in the Atacama Desert on Earth. These terrestrial deposits leave no mineralogical trace of water activity but rather show an albedo difference due to particle size sorting within a fine-grained mudflow. Therefore, spectral differences indicating varying mineralogy between a recent gully deposit and the surrounding terrain may not be the most relevant criteria for detecting water flow in arid environments. Instead, variation in particle size between the deposit and surrounding terrain is a possible discriminator to identify a water-based flow. We show that the Atacama deposit is similar to the observed Mars gully deposits, and both are consistent with liquid water activity. The light-toned Mars gully deposits could have formed from dry debris flows, but a liquid water origin cannot be ruled out because not all liquid water flows leave hydrated minerals behind on the surface. Therefore, the Mars deposits could be remnant mudflows that formed on Mars within the last decade. |
| Keywords: | Mars Mars Surface Geological processes |
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