Compilation
Coordinates: 48 ° 30 ′ 1.1 ″ N , 10 ° 34 ′ 25 ″ E
The Zusamplatte is a natural area of the Danube-Iller-Lech-Platte . It is bounded by the Donauried in the north, Schmutter and the Stauffenberg series in the east, Reischenau in the south and Mindel in the west.
Natural space
According to the structure of the manual of the natural spatial structure of Germany by Meynen / Schmithüsen (1953–1962) and the refinements of the single sheets No. 180 Augsburg and No. 172 Nördlingen , it is the natural area 046.6 of the Iller-Lech gravel plates in the foothills of the Alps . It belongs to the natural spatial main unit 04 - Donau-Iller-Lech-Platte .
geology
The term “plate” describes a gravel body that was deposited periglacial in the Quaternary in the Alpine foothills . The gravel of the composite slab can be classified relatively in the Danube complex ( Calabrium ). At Roßhaupten and Lauterbrunn, the Brunhes-Matuyama reversal of the earth's magnetic field could be detected in solifluctive loess loam .
The low mountain ranges remaining on the composite plate after the Ice Age are recorded in maps as the northern wood angle .
Individual evidence
- ↑ cf. Bavarian State Office for the Environment: Shale coal at Uhlenberg accessed on September 15, 2015.
- ↑ Penck, Albrecht; Brückner, Eduard (1909): The Alps in the Ice Age. Leipzig.
- ↑ Strattner, Monika; Rolf, Christian (1995): Magnetostratigraphic investigations on Pleistocene cover layer profiles in the Bavarian Alpine foothills. In: Geologica Bavarica (99), pp. 55-101.
- ↑ northern compilation on Bavaria Atlas