Glazialtektonik als Wirkungsfeld exogener Dynamik

Gerhard Keller
The glacial tectonics connected with the ice sheet are comparable to other tectonics in tectonik and phenomenological respect. Since 40 years they has been looked at as a result of exogenetic agents. Glacial tectonics extend to the depth of 200 ms. and are advanced by soil dynamics of the geological substratum. 100 years and 50 years ago the glacial tectonics were conceived as endodynamics. In periods when orogenetic opinions dominated it got the grade of...