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Statements

Subject Item
dbr:Prim_(Neckar)
dbo:wikiPageWikiLink
dbr:Klinge_(landform)
Subject Item
dbr:Murr_(river)
dbo:wikiPageWikiLink
dbr:Klinge_(landform)
Subject Item
dbr:Klinge_(geomorphology)
dbo:wikiPageWikiLink
dbr:Klinge_(landform)
dbo:wikiPageRedirects
dbr:Klinge_(landform)
Subject Item
dbr:Klinge_(disambiguation)
dbo:wikiPageWikiLink
dbr:Klinge_(landform)
dbo:wikiPageDisambiguates
dbr:Klinge_(landform)
Subject Item
dbr:Klinge_(landform)
rdf:type
dbo:Place
rdfs:label
Klinge (landform) Klinge (Geomorphologie)
rdfs:comment
Klingen are small, narrow, steep V-shaped valleys formed by the erosive forces of water and suspended abrasive particles, gravel and pebbles. They are usually side valleys without a discernible valley floor that lead into a main valley. Further incision through ablation and headward erosion is mainly caused by the waters of small, steep, fast flowing, streams or becks and their processes are still visible today. Erosion, sedimentation and transport are mutually dependent. The term klinge is German and is used to refer to European stream landforms, especially in southern Germany and eastern France. Klingen sind durch Wasser- und Schutt-Erosion entstandene kleine Kerbtäler und in der Regel Seitentäler größerer Täler. Sie bilden kurze, schmale, aber gefällestarke Tälchen ohne Talboden. Die weitere Eintiefung durch Abtragung und rückschreitende Erosion wird im Wesentlichen durch die Wasser von Rinnsalen und Bächen und deren Gefälle bewirkt und ist auch heute beobachtbar. Erosion, Sedimentation und Transport bedingen sich dabei gegenseitig.
foaf:depiction
n12:Schwälblesklinge_4.jpg n12:Loue_Source_02.jpg n12:Erosion_Klingen+Quellnischen.jpg
dcterms:subject
dbc:Valleys
dbo:wikiPageID
48088739
dbo:wikiPageRevisionID
1099535539
dbo:wikiPageWikiLink
n4:Loue_Source_02.jpg dbr:Marl dbr:White_Jurassic dbr:Muschelkalk dbr:Erosion dbr:Loue dbr:Sedimentation dbr:V-shaped_valley n4:Erosion_Klingen+Quellnischen.jpg dbr:Limestone n4:Schwälblesklinge_4.jpg dbr:Valley dbr:Side_valley dbr:Jura_Mountains dbr:Ablation dbr:Karst_spring dbr:Heubach dbr:Valley_floor dbr:Albtrauf dbr:Spawn_(biology) dbr:Swabian_Jura dbr:Headward_erosion dbc:Valleys dbr:Teufelsklinge dbr:Clay dbr:Gravel dbr:Pebble dbr:Common_midwife_toad dbr:Franconian_Jura
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dbpedia-de:Klinge_(Geomorphologie) wikidata:Q1727788 n17:go2G yago-res:Klinge_(landform)
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dbt:Reflist dbt:ISBN dbt:Italic_title
dbo:thumbnail
n12:Schwälblesklinge_4.jpg?width=300
dbo:abstract
Klingen sind durch Wasser- und Schutt-Erosion entstandene kleine Kerbtäler und in der Regel Seitentäler größerer Täler. Sie bilden kurze, schmale, aber gefällestarke Tälchen ohne Talboden. Die weitere Eintiefung durch Abtragung und rückschreitende Erosion wird im Wesentlichen durch die Wasser von Rinnsalen und Bächen und deren Gefälle bewirkt und ist auch heute beobachtbar. Erosion, Sedimentation und Transport bedingen sich dabei gegenseitig. Klingen are small, narrow, steep V-shaped valleys formed by the erosive forces of water and suspended abrasive particles, gravel and pebbles. They are usually side valleys without a discernible valley floor that lead into a main valley. Further incision through ablation and headward erosion is mainly caused by the waters of small, steep, fast flowing, streams or becks and their processes are still visible today. Erosion, sedimentation and transport are mutually dependent. The term klinge is German and is used to refer to European stream landforms, especially in southern Germany and eastern France.
gold:hypernym
dbr:V-
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wikipedia-en:Klinge_(landform)?oldid=1099535539&ns=0
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4181
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wikipedia-en:Klinge_(landform)
Subject Item
dbr:Siepen
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dbr:Klinge_(landform)
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wikipedia-en:Klinge_(landform)
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dbr:Klinge_(landform)