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• W2133187844 abstract "Research Article| June 01, 2005 What sets topographic relief in extensional footwalls? Alexander L. Densmore; Alexander L. Densmore 1Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Nancye H. Dawers; Nancye H. Dawers 2Department of Earth and Environmental Sciences, Tulane University, New Orleans, Louisiana 70118, USA Search for other works by this author on: GSW Google Scholar Sanjeev Gupta; Sanjeev Gupta 3Department of Earth Science and Engineering, Imperial College, London SW7 2AZ, UK Search for other works by this author on: GSW Google Scholar Roman Guidon Roman Guidon 4Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Author and Article Information Alexander L. Densmore 1Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland Nancye H. Dawers 2Department of Earth and Environmental Sciences, Tulane University, New Orleans, Louisiana 70118, USA Sanjeev Gupta 3Department of Earth Science and Engineering, Imperial College, London SW7 2AZ, UK Roman Guidon 4Department of Earth Sciences, ETH Zürich, CH-8092 Zürich, Switzerland Publisher: Geological Society of America Received: 06 Dec 2004 Revision Received: 25 Feb 2005 Accepted: 28 Feb 2005 First Online: 03 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 The Geological Society of America, Inc. Geology (2005) 33 (6): 453–456. https://doi.org/10.1130/G21440.1 Article history Received: 06 Dec 2004 Revision Received: 25 Feb 2005 Accepted: 28 Feb 2005 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Alexander L. Densmore, Nancye H. Dawers, Sanjeev Gupta, Roman Guidon; What sets topographic relief in extensional footwalls?. Geology 2005;; 33 (6): 453–456. doi: https://doi.org/10.1130/G21440.1 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 use three large normal fault arrays in the northeastern Basin and Range Province, western United States, to document catchment development and relief production during fault growth. Fault slip and slip rates increase systematically along strike from zero at the fault tips. Catchment relief and across-strike range width both increase as slip accumulates but reach maximum values at a distance of ∼15 km from the fault tips and remain uniform along strike over much of the footwalls. Catchment outlet spacing also increases away from the fault tips but does not reach a uniform value and may vary by a factor of 5–6 along strike. We infer that catchments first elongate in the across-strike direction as slip accumulates and the range half-width increases. Once the half-width reaches its maximum value, continued catchment growth is possible only by along-strike capture, which increases outlet spacing but not relief. The close correspondence between catchment relief and range half-width suggests that geomorphically limited hillslope and channel gradients are achieved within the 15 km tip zone. Thus, the limiting factor in footwall development is the width of the range, which is controlled by two external agents: the geometry and spacing of the major faults, and the elevations of base level on both flanks. 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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• W2133187844 title "What sets topographic relief in extensional footwalls?" @default.
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