Beach ridge (original) (raw)
浜堤(ひんてい、英語: beach ridge)とは、波によって洗われたり、波によって移動してきた物が堆積したりすることによって、主に海岸とほぼ平行に形成される低い峰のことである。湖にも形成する場合もある。このため、浜堤は世界中の陸上のあちこちで見られる。なお浜堤は、その上を砂丘が覆ったり、砂丘とくっついてしまうこともある。浜堤がよく発達した平野を浜堤平野という。
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dbo:abstract | A beach ridge is a wave-swept or wave-deposited ridge running parallel to a shoreline. It is commonly composed of sand as well as sediment worked from underlying beach material. The movement of sediment by wave action is called littoral transport. Movement of material parallel to the shoreline is called longshore transport. Movement perpendicular to the shore is called on-offshore transport. A beach ridge may be capped by, or associated with, sand dunes. The height of a beach ridge is affected by wave size and energy. A fall in water level (or an uplift of land) can isolate a beach ridge from the body of water that created it. Isolated beach ridges may be found along dry lakes in the western United States and inland of the Great Lakes of North America, where they formed at the end of the last ice age when lake levels were much higher due to glacial melting and obstructed outflow caused by glacial ice. Some isolated beach ridges are found in parts of Scandinavia, where glacial melting relieved pressure on land masses and resulted in subsequent crustal lifting or post-glacial rebound. A rise in water level can submerge beach ridges created at an earlier stage, causing them to erode and become less distinct. Beach ridges can become routes for roads and trails, like in the case of the west coast in the Netherlands, where isolated beach ridges were formed early on in the Holocene, during the Atlanticum, behind newly formed dunes. Both the old and the new beach ridges are the only dry routes in the mids of wet peatland. Numerous settlements emerged here, some of them developed in large populous centres, like The Hague, Haarlem and Alkmaar. (en) 浜堤(ひんてい、英語: beach ridge)とは、波によって洗われたり、波によって移動してきた物が堆積したりすることによって、主に海岸とほぼ平行に形成される低い峰のことである。湖にも形成する場合もある。このため、浜堤は世界中の陸上のあちこちで見られる。なお浜堤は、その上を砂丘が覆ったり、砂丘とくっついてしまうこともある。浜堤がよく発達した平野を浜堤平野という。 (ja) Een strandwal is een door de branding opgeworpen, boven het zeeniveau liggende, zandbank. Een strandwal is langgerekt, enkele meters hoog en ligt evenwijdig aan de kust. Oudere strandwallen zijn in Nederland gevormd tijdens het Holoceen, gedurende het Atlanticum. Als gevolg van hogere temperaturen in deze periode steeg de zeespiegel, waardoor de vorming van zandbanken en strandwallen mogelijk was. De ophoging van de zeebodem ging in deze periode sneller dan de stijging van de zeespiegel. Achter deze wallen ontstond een waddengebied, waar oude zeeklei kon bezinken. Het droog geworden zand van de strandwallen werd later door de wind opgeblazen tot kleine duintjes. Door vegetatie werd uiteindelijk duinvorming een feit. Dit zijn nu de oude duinen. In het natte westen van Nederland boden de hoger gelegen strandwallen gelegenheid tot de eerste transportroutes over land en werden er al snel nederzettingen gesticht. (nl) |
dbo:thumbnail | wiki-commons:Special:FilePath/NorthSaaremaaCoast.jpg?width=300 |
dbo:wikiPageExternalLink | http://www.great-lakes.net/teach/geog/shoreline/shore_2.html https://web.archive.org/web/20060304054241/http:/www.great-lakes.net/teach/geog/shoreline/shore_2.html https://web.archive.org/web/20070924203512/http:/www.state.in.us/dnr/water/water_availability/maumee/pdf/p191-235.pdf http://www.state.in.us/dnr/water/water_availability/maumee/pdf/p191-235.pdf https://kb.osu.edu/bitstream/handle/1811/80361/1/OGS_1959_IC-25.pdf |
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dcterms:subject | dbc:Cliffs dbc:Coastal_and_oceanic_landforms dbc:Beaches |
gold:hypernym | dbr:Ridge |
rdf:type | dbo:Place yago:WikicatBeaches yago:Beach109217230 yago:GeologicalFormation109287968 yago:Object100002684 yago:PhysicalEntity100001930 yago:YagoGeoEntity yago:YagoPermanentlyLocatedEntity |
rdfs:comment | 浜堤(ひんてい、英語: beach ridge)とは、波によって洗われたり、波によって移動してきた物が堆積したりすることによって、主に海岸とほぼ平行に形成される低い峰のことである。湖にも形成する場合もある。このため、浜堤は世界中の陸上のあちこちで見られる。なお浜堤は、その上を砂丘が覆ったり、砂丘とくっついてしまうこともある。浜堤がよく発達した平野を浜堤平野という。 (ja) A beach ridge is a wave-swept or wave-deposited ridge running parallel to a shoreline. It is commonly composed of sand as well as sediment worked from underlying beach material. The movement of sediment by wave action is called littoral transport. Movement of material parallel to the shoreline is called longshore transport. Movement perpendicular to the shore is called on-offshore transport. A beach ridge may be capped by, or associated with, sand dunes. The height of a beach ridge is affected by wave size and energy. (en) Een strandwal is een door de branding opgeworpen, boven het zeeniveau liggende, zandbank. Een strandwal is langgerekt, enkele meters hoog en ligt evenwijdig aan de kust. Oudere strandwallen zijn in Nederland gevormd tijdens het Holoceen, gedurende het Atlanticum. Als gevolg van hogere temperaturen in deze periode steeg de zeespiegel, waardoor de vorming van zandbanken en strandwallen mogelijk was. De ophoging van de zeebodem ging in deze periode sneller dan de stijging van de zeespiegel. Achter deze wallen ontstond een waddengebied, waar oude zeeklei kon bezinken. Het droog geworden zand van de strandwallen werd later door de wind opgeblazen tot kleine duintjes. Door vegetatie werd uiteindelijk duinvorming een feit. Dit zijn nu de oude duinen. (nl) |
rdfs:label | Beach ridge (en) 浜堤 (ja) Strandwal (nl) |
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