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Conway, S. J.; Balme, M. R.; Towner, M. C. and Murray, J. B.
(2010).
URL: http://www.lpi.usra.edu/meetings/lpsc2010/pdf/1894...
Abstract
We describe experiments designed to study sediment transport by liquid water under the current low temperature and low pressure conditions on Mars. We show that water flowing over unconsolidated material on Mars causes as much erosion as water flowing under ambient terrestrial conditions, propagates faster and further and produces unique sedimentary features due to the combination of boiling and freezing.
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- Item ORO ID
- 35451
- Item Type
- Conference or Workshop Item
- Academic Unit or School
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Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM)
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences - Copyright Holders
- © 2010 Lunar and Planetary Institute
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- Susan Conway