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Proceedings Anniversary Event – 10 International Alpine Workshop ...

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anch basins contain lakes (Ammersee, Starnberger See, Kochelsee, Chiemsee). Lech,<br />

Isar, Inn and Salzach River have already lost their lakes. The borders of ancient glaciers<br />

are marked by the end moraine walls which surround the basins in a large arrow.<br />

Altitude (average 500 m NN) and distance to the Alpes determine the climate of the <strong>Alpine</strong><br />

forelands. Referring to the latitude the typical west weather conditions of Central Europe<br />

are strongly modified by the nearness of the high mountains in the <strong>Alpine</strong> foreland. During<br />

a southwest stream the Foehn wind conditions arise with dry and warm weather; during a<br />

northwest stream there are strong cloud accumulations as well as heavier and longer rain<br />

intensity. The cold snaps thereby hold in southern Bavaria twice as long as in alpinedistant<br />

areas (WESTERMANN 1962).<br />

Fig. 11: Europe during the last glacial age (from Westermann 1991)<br />

11

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