Stauchmoränengenese durch die Entwicklung eines Gletscherfusses am Kotlujokull, Südisland. (Push-moraine genesis through the formation of a glacier-foot at the Kotlujokull, South Iceland)
The advancement of the lower parts of the glacier-foot into and across the sands of the foreland implies the following genesis of push-moraines: Shoving off a place of sand, folding it and pushing it over the foreland at average rates of up to 7,2
by decreasing bottom current and increasing sedimentation rates| 4active bottom current, decreasing dissolution and markel increase of the sedimentation rates in the early Pliocene, that contributed to active building of a sedimentary ridge at the foot
Doline Karst occurs in the upper catchments of the Tsondab, Gaub and Kuiseb rivers in the central Namib. The karst extends from the Escarpment foot westwards decreasing in density and altitude for 40 to 50 km. The existence of this well-developed