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Drainage basins and Channel incision on Mars Aharonson, Zuber, Rothman, Schorghofer, Whipple Robert I. Davies San Francisco State University
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Channels on Mars Material squished out by impact
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What are the evidences of Free water on Mars? Was there a climate on Mars that supported rainfall? How are channels formed? What is the hydrology of Mars?
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Channel Incision Results from Surface Runoff Groundwater sapping –Erosion along the base of a cliff, and allowing the rocks above to fall in large blocks –Erosion around a spring at the headwaters of a spring –Undercutting along the headwall of a cirque, owing to frost action at the bottom of the bergschrund
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Terrestrial Analog East & West arms of the Escalante River –East- Channel incision progressed via headward erosion aided by seepage of groundwater at its base –West - Tributaries evolved primarily by runoff
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Comparison of Stream Profiles Al-Qahria Vallis Ma’adim Vallis Browns Canyon The geometry of the profile is characteristic of groundwater sapping, rather than overland flow.
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Calculations Comparison of Stream gradients on Earth and Mars, given that S A - =.02 for Mars =.07 for Earth
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Graph comparing concavity of streams on Earth and Mars
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Conclusions Slope-area relations show no evidence for fluvial sculpting Topographic measurements suggest that sapping is the primary method of channel incision
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Question #6 What role does gravity play in all this? Mars’ gravitational acceleration is only 3.745 m/s/s
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