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• W2081770676 abstract "Research Article| April 01, 2011 ‘Cape capture’: Geologic data and modeling results suggest the Holocene loss of a Carolina Cape E. Robert Thieler; E. Robert Thieler 1U.S. Geological Survey, 384 Woods Hole Road, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Andrew D. Ashton Andrew D. Ashton 2Woods Hole Oceanographic Institution, 360 Woods Hole Road, MS 22, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Author and Article Information E. Robert Thieler 1U.S. Geological Survey, 384 Woods Hole Road, Woods Hole, Massachusetts 02543, USA Andrew D. Ashton 2Woods Hole Oceanographic Institution, 360 Woods Hole Road, MS 22, Woods Hole, Massachusetts 02543, USA Publisher: Geological Society of America Received: 04 Aug 2010 Revision Received: 27 Oct 2010 Accepted: 09 Nov 2010 First Online: 09 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 © 2011 Geological Society of America Geology (2011) 39 (4): 339–342. https://doi.org/10.1130/G31641.1 Article history Received: 04 Aug 2010 Revision Received: 27 Oct 2010 Accepted: 09 Nov 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 E. Robert Thieler, Andrew D. Ashton; ‘Cape capture’: Geologic data and modeling results suggest the Holocene loss of a Carolina Cape. Geology 2011;; 39 (4): 339–342. doi: https://doi.org/10.1130/G31641.1 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 For more than a century, the origin and evolution of the set of cuspate forelands known as the Carolina Capes—Hatteras, Lookout, Fear, and Romain—off the eastern coast of the United States have been discussed and debated. The consensus conceptual model is not only that these capes existed through much or all of the Holocene transgression, but also that their number has not changed. Here we describe bathymetric, lithologic, seismic, and chronologic data that suggest another cape may have existed between Capes Hatteras and Lookout during the early to middle Holocene. This cape likely formed at the distal end of the Neuse-Tar-Pamlico fluvial system during the early Holocene transgression, when this portion of the shelf was flooded ca. 9 cal (calibrated) kyr B.P., and was probably abandoned by ca. 4 cal kyr B.P., when the shoreline attained its present general configuration. Previously proposed mechanisms for cape formation suggest that the large-scale, rhythmic pattern of the Carolina Capes arose from a hydrodynamic template or the preexisting geologic framework. Numerical modeling, however, suggests that the number and spacing of capes can be dynamic, and that a coast can self-organize in response to a high-angle-wave instability in shoreline shape. In shoreline evolution model simulations, smaller cuspate forelands are subsumed by larger neighbors over millennial time scales through a process of ‘cape capture.’ The suggested former cape in Raleigh Bay represents the first interpreted geological evidence of dynamic abandonment suggested by the self-organization hypothesis. Cape capture may be a widespread process in coastal environments with large-scale rhythmic shoreline features; its preservation in the sedimentary record will vary according to geologic setting, physical processes, and sea-level history. 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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• W2081770676 title "'Cape capture': Geologic data and modeling results suggest the Holocene loss of a Carolina Cape" @default.
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• W2081770676 doi "https://doi.org/10.1130/g31641.1" @default.
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