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Typus
KomplettPlagiat
Bearbeiter
Graf Isolan
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Untersuchte Arbeit:
Seite: 18, Zeilen: 1-10
Quelle: Wikipedia Landslide 2010
Seite(n): 1 (Internetsource), Zeilen:
[For instance if] there is a slope with silt and sand as its top soil and bedrock as its bottom soil, during an intense rainstorm, the bedrock will keep the rain trapped in the top soils of silt and sand. As the topsoil becomes saturated and heavy, it can start to slide over the bedrock and become a shallow landslide. Studies on shallow landslides prove that if permeability decreases with depth, a perched water table may develop in soils at intense precipitation. When pore water pressures are sufficient to reduce effective normal stress to a critical level, failure occurs.

Landslides in which the sliding surface is mostly deeply located below the maximum rooting depth of trees, typically to depths greater than ten meters are called deep seated landslides. Deep-seated landslides usually involve deep regolith, weathered rock, and/or bedrock and include large slope failure associated with translational, rotational, or complex movement.

Say there is a slope with silt and sand as its top soil and bedrock as its bottom soil. During an intense rainstorm, the bedrock will keep the rain trapped in the top soils of silt and sand. As the topsoil becomes saturated and heavy, it can start to slide over the bedrock and become a shallow landslide. R. H. Campbell did a study on shallow landslides on Santa Cruz Island California. He notes that if permeability decreases with depth, a perched water table may develop in soils at intense precipitation. When pore water pressures are sufficient to reduce effective normal stress to a critical level, failure occurs.[5]

Deep-seated landslide

Landslides in which the sliding surface is mostly deeply located below the maximum rooting depth of trees (typically to depths greater than ten meters). Deep-seated landslides usually involve deep regolith, weathered rock, and/or bedrock and include large slope failure associated with translational, rotational, or complex movement.


5. Renwick,W., Brumbaugh,R. & Loeher,L. 1982. Landslide Morphology and Processes on Santa Cruz Island California. Geografiska Annaler. Series A, Physical Geography, Vol. 64, No. 3/4, pp. 149-159

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