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• W1978573630 abstract "Research Article| September 01, 2010 Retreat of a giant cataract in a long-lived (3.7–2.6 Ga) martian outflow channel Nicholas H. Warner; Nicholas H. Warner * 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK *E-mail: n.warner@imperial.ac.uk. Search for other works by this author on: GSW Google Scholar Sanjeev Gupta; Sanjeev Gupta 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK Search for other works by this author on: GSW Google Scholar Jung-Rack Kim; Jung-Rack Kim 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK Search for other works by this author on: GSW Google Scholar Shih-Yuan Lin; Shih-Yuan Lin 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK Search for other works by this author on: GSW Google Scholar Jan-Peter Muller Jan-Peter Muller 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK Search for other works by this author on: GSW Google Scholar Author and Article Information Nicholas H. Warner * 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK Sanjeev Gupta 1Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK Jung-Rack Kim 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK Shih-Yuan Lin 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK Jan-Peter Muller 2Mullard Space Science Laboratory, Department of Space and Climate Physics, University College London, Holmbury St Mary, Surrey RH5 6NT, UK *E-mail: n.warner@imperial.ac.uk. Publisher: Geological Society of America Received: 31 Mar 2010 Revision Received: 08 Apr 2010 Accepted: 09 Apr 2010 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2010 Geological Society of America Geology (2010) 38 (9): 791–794. https://doi.org/10.1130/G31268.1 Article history Received: 31 Mar 2010 Revision Received: 08 Apr 2010 Accepted: 09 Apr 2010 First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Nicholas H. Warner, Sanjeev Gupta, Jung-Rack Kim, Shih-Yuan Lin, Jan-Peter Muller; Retreat of a giant cataract in a long-lived (3.7–2.6 Ga) martian outflow channel. Geology 2010;; 38 (9): 791–794. doi: https://doi.org/10.1130/G31268.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract We describe the evolution of an ∼600-m-deep tributary outflow channel to Ares Vallis, Mars. High-resolution topography, image analysis, and crater statistics indicate that this tributary canyon developed by the upstream migration of a large, ∼300-m-tall cataract during multiple flood events that span ∼1 b.y. of Mars history (3.7–2.6 Ga). Issuing from Hydapsis Chaos, these floods were initiated at a similar time and occurred over a similar time range to flooding in Ares Vallis, suggesting a potential regional control on flood initiation and chaos formation. In addition, we provide evidence that cataract retreat and significant incision within the tributary canyon occurred only after a series of downcutting events within Ares Vallis. Topography data and crater statistics taken from the floor of Ares Vallis indicate an ∼300 m base-level drop that coincides temporally with an Early Amazonian (ca. 2.6 Ga) flood event and cataract formation within the tributary canyon. The results both confirm the hypothesis of long-term, multiple flood events within martian outflow channels and demonstrate the influence of base-level change on their incision. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W1978573630 title "Retreat of a giant cataract in a long-lived (3.7–2.6 Ga) martian outflow channel" @default.
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