The formation of beaches on shore platforms in microtidal environments

Beaches are common features of many rocky shorelines and can be considered to be constrained by the underlying geology. In mesotidal to macrotidal areas the slope of the substrate and sediment supply are the primary factors in constraining the size and development of beaches on shore platforms. In m...
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Autor*in:	Kennedy, David M [verfasserIn] Milkins, Jemima

Format:	Artikel
Sprache:	Englisch

Erschienen:	2015

Rechteinformationen:	Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd.

Schlagwörter:	beaches rocky coast shore platform evolution abrasion

Übergeordnetes Werk:	Enthalten in: Earth surface processes and landforms - New York, NY [u.a.] : Wiley, 1981, 40(2015), 1, Seite 34-46
Übergeordnetes Werk:	volume:40 ; year:2015 ; number:1 ; pages:34-46

Links:	Volltext Link aufrufen Link aufrufen

DOI / URN:	10.1002/esp.3610

Katalog-ID:	OLC1962505553

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allfields	10.1002/esp.3610 doi PQ20160617 (DE-627)OLC1962505553 (DE-599)GBVOLC1962505553 (PRQ)p1770-bd04ec1880aa6a7e27b5b2182411e5932a4e45fdf38a8044dc3c8147c62934753 (KEY)0004410520150000040000100034formationofbeachesonshoreplatformsinmicrotidalenvi DE-627 ger DE-627 rakwb eng 910 DNB Kennedy, David M verfasserin aut The formation of beaches on shore platforms in microtidal environments 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Beaches are common features of many rocky shorelines and can be considered to be constrained by the underlying geology. In mesotidal to macrotidal areas the slope of the substrate and sediment supply are the primary factors in constraining the size and development of beaches on shore platforms. In microtidal settings it is not known if these factors are wholly responsible for determining the presence of beaches on shore platforms, nor the contribution of other factors such as hydrodynamics. The microtidal coast of Victoria, Australia, is surveyed in this study in order to quantify the morphological boundary conditions that constrain beach development on semi‐horizontal shore platforms. An ample sediment supply indicates that the underlying geology is controlling the presence and absence of beaches. Where beaches occur they always overlie a rock ramp which is the steepest part of the platform. The two most important morphological constraints were platform width and height both of which significantly correlated with beach volume. An elevational threshold exists at just over +1.0 m where beaches cannot accumulate. Below this threshold, platform width appears to be the principle constraining factor in beach accumulation. An evolutionary model is inferred which suggests that dissipation of wave energy associated with platform widening plays an important role in allowing beaches to accumulate. The model suggests beaches on platforms will be particularly sensitive to sea level rise. Copyright © 2014 John Wiley & Sons, Ltd. Nutzungsrecht: Copyright © 2014 John Wiley & Sons, Ltd. beaches rocky coast shore platform evolution abrasion Milkins, Jemima oth Enthalten in Earth surface processes and landforms New York, NY [u.a.] : Wiley, 1981 40(2015), 1, Seite 34-46 (DE-627)130395609 (DE-600)602320-4 (DE-576)015897788 0197-9337 nnns volume:40 year:2015 number:1 pages:34-46 http://dx.doi.org/10.1002/esp.3610 Volltext http://onlinelibrary.wiley.com/doi/10.1002/esp.3610/abstract http://search.proquest.com/docview/1642468879 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO AR 40 2015 1 34-46
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title_auth	The formation of beaches on shore platforms in microtidal environments
abstract	Beaches are common features of many rocky shorelines and can be considered to be constrained by the underlying geology. In mesotidal to macrotidal areas the slope of the substrate and sediment supply are the primary factors in constraining the size and development of beaches on shore platforms. In microtidal settings it is not known if these factors are wholly responsible for determining the presence of beaches on shore platforms, nor the contribution of other factors such as hydrodynamics. The microtidal coast of Victoria, Australia, is surveyed in this study in order to quantify the morphological boundary conditions that constrain beach development on semi‐horizontal shore platforms. An ample sediment supply indicates that the underlying geology is controlling the presence and absence of beaches. Where beaches occur they always overlie a rock ramp which is the steepest part of the platform. The two most important morphological constraints were platform width and height both of which significantly correlated with beach volume. An elevational threshold exists at just over +1.0 m where beaches cannot accumulate. Below this threshold, platform width appears to be the principle constraining factor in beach accumulation. An evolutionary model is inferred which suggests that dissipation of wave energy associated with platform widening plays an important role in allowing beaches to accumulate. The model suggests beaches on platforms will be particularly sensitive to sea level rise. Copyright © 2014 John Wiley & Sons, Ltd.
abstractGer	Beaches are common features of many rocky shorelines and can be considered to be constrained by the underlying geology. In mesotidal to macrotidal areas the slope of the substrate and sediment supply are the primary factors in constraining the size and development of beaches on shore platforms. In microtidal settings it is not known if these factors are wholly responsible for determining the presence of beaches on shore platforms, nor the contribution of other factors such as hydrodynamics. The microtidal coast of Victoria, Australia, is surveyed in this study in order to quantify the morphological boundary conditions that constrain beach development on semi‐horizontal shore platforms. An ample sediment supply indicates that the underlying geology is controlling the presence and absence of beaches. Where beaches occur they always overlie a rock ramp which is the steepest part of the platform. The two most important morphological constraints were platform width and height both of which significantly correlated with beach volume. An elevational threshold exists at just over +1.0 m where beaches cannot accumulate. Below this threshold, platform width appears to be the principle constraining factor in beach accumulation. An evolutionary model is inferred which suggests that dissipation of wave energy associated with platform widening plays an important role in allowing beaches to accumulate. The model suggests beaches on platforms will be particularly sensitive to sea level rise. Copyright © 2014 John Wiley & Sons, Ltd.
abstract_unstemmed	Beaches are common features of many rocky shorelines and can be considered to be constrained by the underlying geology. In mesotidal to macrotidal areas the slope of the substrate and sediment supply are the primary factors in constraining the size and development of beaches on shore platforms. In microtidal settings it is not known if these factors are wholly responsible for determining the presence of beaches on shore platforms, nor the contribution of other factors such as hydrodynamics. The microtidal coast of Victoria, Australia, is surveyed in this study in order to quantify the morphological boundary conditions that constrain beach development on semi‐horizontal shore platforms. An ample sediment supply indicates that the underlying geology is controlling the presence and absence of beaches. Where beaches occur they always overlie a rock ramp which is the steepest part of the platform. The two most important morphological constraints were platform width and height both of which significantly correlated with beach volume. An elevational threshold exists at just over +1.0 m where beaches cannot accumulate. Below this threshold, platform width appears to be the principle constraining factor in beach accumulation. An evolutionary model is inferred which suggests that dissipation of wave energy associated with platform widening plays an important role in allowing beaches to accumulate. The model suggests beaches on platforms will be particularly sensitive to sea level rise. Copyright © 2014 John Wiley & Sons, Ltd.
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title_short	The formation of beaches on shore platforms in microtidal environments
url	http://dx.doi.org/10.1002/esp.3610 http://onlinelibrary.wiley.com/doi/10.1002/esp.3610/abstract http://search.proquest.com/docview/1642468879
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author2	Milkins, Jemima
author2Str	Milkins, Jemima
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doi_str	10.1002/esp.3610
up_date	2024-07-04T03:44:21.110Z
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