soil resources (Subject) / erosion mechanisms and badland formation (Lesson)

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This lesson was created by tinalinea92.

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  • def erosion transport of soil particles along the soil surface dependin on tranport medium either fluvial erosion or aeolian erosion
  • fluvial erosion rainfall and surface runoff rivers and streams  floods
  • aeolian erosion geomorphical force in arid and semi arid regions deflation abrasion
  • erosion by human activities intensive agricultre deforestation roads and urbanization
  • which flow energy vertical erosion and lateral erosion resistance of the materia is crucial factor variation of different particles
  • Hjulström curve shows a rivers speed- affects to erode particles of different sizes 1. critical erosion speed - > minimum speed to transport and erode particles  2. mean setting velocity -> minimum speed needed to deposit particles
  • badland formation arid regions source of sediment for dryland rivers gullysystems by wind and water erosion gullly landscape with high drainage desities are called badlands manifestation of desertificaion
  • badland characteristica loess  smectite-rich  and mudstones  vulcanic ash sandy conglomerates with clay and weakly cmented sandstones
  • badland characterisitis important dry terrain soft sediment rocks and clay rich soils eroded by wind and water minimal vegetation and steep slopes - steile abhänge  lack of regolith layer -> covering solid rocks  canyons and ullied are common in badlands
  • how to prevent erosion crop rotation  vegetation  terracing and windbeaks rows of trees and shrubs