Alpentore during the Würm glaciation
During the Würm glaciation, where several glaciers from different Alpine valleys met or flowed through narrow passages at the edge of the Alps, ice was piled up. Such bottlenecks had a significant impact on the level of the ice sheet which meant that it eventually flowed over low mountain passes and ridges and the glaciers were combined into a network of ice streams.
Alpentore, through which particularly large masses of ice poured into the surrounding plains, were mainly located at the mouths of large longitudinal valleys such as Inn, Rhine or Salzach valleys. These glaciers penetrated up to 50 kilometres (31 mi) into the lowlands. Even valleys that appear rather insignificant today such as those of the Isar, Loisach and Ammer rivers, were able to produce large tongues of ice when their glaciers were fed by larger ones, such as the Inn Valley Glacier (e.g. via the Fern Pass). By contrast with such large glaciers, quite isolated valleys, such as those of the Iller or the Lech, could only produce much smaller glacial tongues.
A further prerequisite for glaciers extending into the Alpine foreland are high mountains. East of the Salzach, glacier tongues hardly reached the edge of the Alps, because the mountains of the Low Tauern, unlike those of the High Tauern did not produce enough ice. So the alpentore were found mainly in the Bavarian Alpine Foreland. One of the few examples at the southern edge of the Alps was the comparatively small alpentor of today's Tagliamento valley.[1]
