Beyond Drainage Channels: The Characteristics and Global Variations of Colluvium Deposits
Richard
Broschiertes Buch

Beyond Drainage Channels: The Characteristics and Global Variations of Colluvium Deposits

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Periglacial slope deposits also known as cover beds (CB) are an accepted phenomenon in Europe. KLEBER AND TERHORST (2013b) defined: "CBs are deposits that formed by unconcentrated dislocation processes chiefly from upslope materials, but that may contain admixed eolian matter. They cover undifferentiated slopes to a large extent or even completely rather than being restricted to drainage ways, linear discharges, or local failures. CBs typically consist of several layers separated by disconformities." In Europe, CB consist of an upper layer ("Hauptlage", LH), an intermediate layer ("Mittellage"...