Bavarian Alpine Foreland
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The Bavarian Alpine Foreland (German: Bayerisches Alpenvorland) refers to a region of plateau and rolling foothills in Southern Germany, stretching from the Danube in the north to the Bavarian Alps in the south.
The Alpine foreland has been shaped under the influence of the ice ages and has a rich variety of landforms. A molasse basin of extensive Tertiary and Quarternary sediments —silt and clay, sand and sedimentary rocks from Alpine erosion— overlay the Alpine nappes. Features such as the morainic hills, gravel sandar and lakes have left a record of various glaciation stages in this region.
The Bavarian Alpine Foreland is crossed by the rivers Iller, Wertach, Lech, Isar and Inn, its western boundary roughly being formed by the border of the Bavarian administrative district of Swabia with the State of Baden-Württemberg, and its eastern boundary being the Salzach river on the border with Austria. The numerous lakes include Lake Constance, Lake Starnberg and Chiemsee. The largest city of the region is Munich, located in the centre of the Alpine Foreland on the River Isar.
- Northern Alpine Foreland:
- Southern Alpine Foreland (D66) at the foot of the Northern Limestone Alps
In the west, the Alpine Foreland stretches along the Danube up to its sources in the Black Forest and beyond Lake Constance continues as the Swiss Plateau. In the east, the Austrian Alpine Foreland comprises the Flachgau region of Salzburg, the adjacent Innviertel, Hausruckviertel and Traunviertel of Upper Austria, as well as the Mostviertel region of Lower Austria up to the Tulln Basin.