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Titel    Landslide
Herausgeber    Wikipedia
Datum    24. June 2010
URL    http://en.wikipedia.org/w/index.php?title=Landslide&oldid=369975528

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[1.] Analyse:Hja/Fragment 017 16 - Diskussion
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Landslide in which the sliding surface is located within the soil mantle or weathered bed rock, typically to a depth from few decimeters to some meters are called shallow landslides. They usually include debris slides, debris flows, and failures of road cut-slopes.

Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low permeable bottom soils. The low permeable, bottom soils trap the water in the shallower, high permeable soils creating high water pressure in the top soils. As the top soils are filled with water and become heavy, slopes can turn out to be very unstable and slide over the low permeable bottom soils.

Shallow landslide

Landslide in which the sliding surface is located within the soil mantle or weathered bedrock (typically to a depth from few decimetres to some metres). They usually include debris slides, debris flow, and failures of road cut-slopes. Landslides occurring as single large blocks of rock moving slowly down slope are sometimes called block glides.

Shallow landslides can often happen in areas that have slopes with high permeable soils on top of low permeable bottom soils. The low permeable, bottom soils trap the water in the shallower, high permeable soils creating high water pressure in the top soils. As the top soils are filled with water and become heavy, slopes can become very unstable and slide over the low permeable bottom soils.

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[2.] Analyse:Hja/Fragment 018 01 - Diskussion
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[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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