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Typus
KomplettPlagiat
Bearbeiter
Graf Isolan
Gesichtet
No.png
Untersuchte Arbeit:
Seite: 17, Zeilen: 16-22
Quelle: Wikipedia Landslide 2010
Seite(n): 1 (Internetsource), Zeilen:
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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