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An integrated hypothesis for regional patterns of shoreline change along the Northern North Carolina Outer Banks, USA

An integrated hypothesis for regional patterns of shoreline change along the Northern North Carolina Outer Banks, USA
An integrated hypothesis for regional patterns of shoreline change along the Northern North Carolina Outer Banks, USA
Combining analyses of plan-view shoreline change and shoreline curvature with existing nearshore geologic and bathymetric data and the results of a recent theoretical, large-scale shoreline-evolution model that couples geologic framework to alongshore sediment transport, we propose an integrated explanation for persistent patterns of shoreline change observed on the northern Outer Banks of North Carolina, USA. Concentrated sources of coarse-grained sediment, derived from relict fluvial stratigraphy or densely grouped relict inlet channels excavated from the shoreface, may both enable persistence of nearshore bathymetric anomolies and control multi-km-scale undulations in shoreline curvature, which in turn affect gradients in wave-driven alongshore sediment transport that drive long-term shoreline change
0025-3227
85-90
Lazarus, Eli
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
Murray, A. Brad
dd93e4dd-ed6c-4cf5-89c6-e1f85cf8f61f
Lazarus, Eli
642a3cdb-0d25-48b1-8ab8-8d1d72daca6e
Murray, A. Brad
dd93e4dd-ed6c-4cf5-89c6-e1f85cf8f61f

Lazarus, Eli and Murray, A. Brad (2011) An integrated hypothesis for regional patterns of shoreline change along the Northern North Carolina Outer Banks, USA. Marine Geology, 281 (1-4), 85-90. (doi:10.1016/j.margeo.2011.02.002).

Record type: Article

Abstract

Combining analyses of plan-view shoreline change and shoreline curvature with existing nearshore geologic and bathymetric data and the results of a recent theoretical, large-scale shoreline-evolution model that couples geologic framework to alongshore sediment transport, we propose an integrated explanation for persistent patterns of shoreline change observed on the northern Outer Banks of North Carolina, USA. Concentrated sources of coarse-grained sediment, derived from relict fluvial stratigraphy or densely grouped relict inlet channels excavated from the shoreface, may both enable persistence of nearshore bathymetric anomolies and control multi-km-scale undulations in shoreline curvature, which in turn affect gradients in wave-driven alongshore sediment transport that drive long-term shoreline change

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More information

Accepted/In Press date: 2 February 2011
e-pub ahead of print date: 9 February 2011
Published date: 15 March 2011
Organisations: Earth Surface Dynamics

Identifiers

Local EPrints ID: 400723
URI: http://eprints.soton.ac.uk/id/eprint/400723
ISSN: 0025-3227
PURE UUID: d5d9788c-d967-42ab-afa7-16e09360c1e4
ORCID for Eli Lazarus: ORCID iD orcid.org/0000-0003-2404-9661

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Date deposited: 23 Sep 2016 14:32
Last modified: 15 Mar 2024 03:57

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Contributors

Author: Eli Lazarus ORCID iD
Author: A. Brad Murray

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