The Origin of Foredunes on the Coast of Victoria, Australia
Foredunes are ridges of wind-deposited sand built at the back of a beach, whereas beach ridges are wave-built features (berms that persist). Evidence of the initiation of foredunes has been obtained from successively surveyed transverse beach profiles at points along the Victorian coastline. Some ha...
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| Veröffentlicht in: | Journal of coastal research 1988, Vol.4 (2), p.181-192 |
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| container_title | Journal of coastal research |
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| creator | BIRD, E. C. F JONES, D. J. B |
| description | Foredunes are ridges of wind-deposited sand built at the back of a beach, whereas beach ridges are wave-built features (berms that persist). Evidence of the initiation of foredunes has been obtained from successively surveyed transverse beach profiles at points along the Victorian coastline. Some have formed where wave-built beach ridges became colonised by strandline veg- etation that trapped wind-blown sand; others were initiated when the seaward margins of back- shore sand terraces or hummocky dune topography were cut back by storm waves. Sand-trapping vegetation may germinate in zones of seed-bearing strand litter on a beach, but these are usually deposited on, or as part of, a wave-built beach ridge. |
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C. F ; JONES, D. J. B</creator><creatorcontrib>BIRD, E. C. F ; JONES, D. J. B</creatorcontrib><description>Foredunes are ridges of wind-deposited sand built at the back of a beach, whereas beach ridges are wave-built features (berms that persist). Evidence of the initiation of foredunes has been obtained from successively surveyed transverse beach profiles at points along the Victorian coastline. Some have formed where wave-built beach ridges became colonised by strandline veg- etation that trapped wind-blown sand; others were initiated when the seaward margins of back- shore sand terraces or hummocky dune topography were cut back by storm waves. Sand-trapping vegetation may germinate in zones of seed-bearing strand litter on a beach, but these are usually deposited on, or as part of, a wave-built beach ridge.</description><identifier>ISSN: 0749-0208</identifier><identifier>EISSN: 1551-5036</identifier><identifier>CODEN: JCRSEK</identifier><language>eng</language><publisher>Lawrence, KS: Coastal Education and Research Foundation (CERF)</publisher><subject>Beaches ; Berms ; Coasts ; Dunes ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; Geomorphology, landform evolution ; Marine ; Poultry litter ; Sand ; Surficial geology ; Swales ; Terraces ; Vegetation ; Victorians</subject><ispartof>Journal of coastal research, 1988, Vol.4 (2), p.181-192</ispartof><rights>Copyright 1988 Coastal Education & Research Foundation [CERF]</rights><rights>1988 INIST-CNRS</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/4297392$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4297392$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>314,776,780,799,4010,57992,58225</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=7643680$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>BIRD, E. C. F</creatorcontrib><creatorcontrib>JONES, D. J. B</creatorcontrib><title>The Origin of Foredunes on the Coast of Victoria, Australia</title><title>Journal of coastal research</title><description>Foredunes are ridges of wind-deposited sand built at the back of a beach, whereas beach ridges are wave-built features (berms that persist). Evidence of the initiation of foredunes has been obtained from successively surveyed transverse beach profiles at points along the Victorian coastline. Some have formed where wave-built beach ridges became colonised by strandline veg- etation that trapped wind-blown sand; others were initiated when the seaward margins of back- shore sand terraces or hummocky dune topography were cut back by storm waves. Sand-trapping vegetation may germinate in zones of seed-bearing strand litter on a beach, but these are usually deposited on, or as part of, a wave-built beach ridge.</description><subject>Beaches</subject><subject>Berms</subject><subject>Coasts</subject><subject>Dunes</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>Geomorphology, landform evolution</subject><subject>Marine</subject><subject>Poultry litter</subject><subject>Sand</subject><subject>Surficial geology</subject><subject>Swales</subject><subject>Terraces</subject><subject>Vegetation</subject><subject>Victorians</subject><issn>0749-0208</issn><issn>1551-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1988</creationdate><recordtype>article</recordtype><recordid>eNo9z81Kw0AUhuFBFIzVO3CRhbgycGYyv7gqwVah0E11G04mE52SZupMsvDujbS4Oov34YNzQTIqBC0ElPKSZKC4KYCBviY3Ke0BqNRcZeR59-XybfSffshDl69CdO00uJSHIR_nVAVM41_58HYM0eNTvpzSGLH3eEuuOuyTuzvfBXlfveyq12KzXb9Vy02BTKixkK0CIxS1UmpDDUKrVdPoRgvOOLWskQxYa2hnO4bArC0poDQCacd1i7pckMfT7jGG78mlsT74ZF3f4-DClGoqpFIg5AwfzhCTxb6LOFif6mP0B4w_tZK8lBpmdn9i-zS_9J85M6o0rPwF489aMg</recordid><startdate>1988</startdate><enddate>1988</enddate><creator>BIRD, E. C. F</creator><creator>JONES, D. J. B</creator><general>Coastal Education and Research Foundation (CERF)</general><general>Coastal Education and Research Foundation</general><scope>IQODW</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>1988</creationdate><title>The Origin of Foredunes on the Coast of Victoria, Australia</title><author>BIRD, E. C. F ; JONES, D. J. B</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a257t-6d709571c668919a0d87bb8b854241c2b6202d91fcf2a02cc310a695a1f48da83</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1988</creationdate><topic>Beaches</topic><topic>Berms</topic><topic>Coasts</topic><topic>Dunes</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>Geomorphology, landform evolution</topic><topic>Marine</topic><topic>Poultry litter</topic><topic>Sand</topic><topic>Surficial geology</topic><topic>Swales</topic><topic>Terraces</topic><topic>Vegetation</topic><topic>Victorians</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>BIRD, E. C. F</creatorcontrib><creatorcontrib>JONES, D. J. B</creatorcontrib><collection>Pascal-Francis</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of coastal research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>BIRD, E. C. F</au><au>JONES, D. J. B</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Origin of Foredunes on the Coast of Victoria, Australia</atitle><jtitle>Journal of coastal research</jtitle><date>1988</date><risdate>1988</risdate><volume>4</volume><issue>2</issue><spage>181</spage><epage>192</epage><pages>181-192</pages><issn>0749-0208</issn><eissn>1551-5036</eissn><coden>JCRSEK</coden><abstract>Foredunes are ridges of wind-deposited sand built at the back of a beach, whereas beach ridges are wave-built features (berms that persist). Evidence of the initiation of foredunes has been obtained from successively surveyed transverse beach profiles at points along the Victorian coastline. Some have formed where wave-built beach ridges became colonised by strandline veg- etation that trapped wind-blown sand; others were initiated when the seaward margins of back- shore sand terraces or hummocky dune topography were cut back by storm waves. Sand-trapping vegetation may germinate in zones of seed-bearing strand litter on a beach, but these are usually deposited on, or as part of, a wave-built beach ridge.</abstract><cop>Lawrence, KS</cop><pub>Coastal Education and Research Foundation (CERF)</pub><tpages>12</tpages></addata></record> |
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| identifier | ISSN: 0749-0208 |
| ispartof | Journal of coastal research, 1988, Vol.4 (2), p.181-192 |
| issn | 0749-0208 1551-5036 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_15677056 |
| source | Jstor Complete Legacy; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals |
| subjects | Beaches Berms Coasts Dunes Earth sciences Earth, ocean, space Exact sciences and technology Geomorphology, landform evolution Marine Poultry litter Sand Surficial geology Swales Terraces Vegetation Victorians |
| title | The Origin of Foredunes on the Coast of Victoria, Australia |
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