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.
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| - Klinge (Geomorphologie) (de)
- Klinge (landform) (en)
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| - 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. (de)
- 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. (en)
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| - 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. (de)
- 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. (en)
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