Conway, S. J.; Balme, M. R. and Grindrod, P. M.
(2011).
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| URL: | http://meetings.copernicus.org/epsc-dps2011/home.h... |
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Abstract
We have found that debris flows are the main process in forming two gullied crater slopes on Mars. We used 1 m/pix elevation models to derive three topographic indices: slope-area, CAD and DI-25. These indices allow the active slope processes to be identified by comparison to data from Earth analogues. We present data from Meteor Crater together with analogues previsouly presented by Conway et al. [1]. We also compare the signals from the martian gullied slopes with a non-gullied martian example: Zumba crater.
| Item Type: | Conference or Workshop Item |
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| Copyright Holders: | 2011 The Authors |
| Academic Unit/School: | Faculty of Science, Technology, Engineering and Mathematics (STEM) > Physical Sciences Faculty of Science, Technology, Engineering and Mathematics (STEM) |
| Related URLs: | |
| Item ID: | 31394 |
| Depositing User: | Matthew Balme |
| Date Deposited: | 24 Jan 2012 17:05 |
| Last Modified: | 24 Jun 2019 17:22 |
| URI: | http://oro.open.ac.uk/id/eprint/31394 |
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