As promised in last post , here's the full chapter from Gareis (1978). The crucial paragraphs to Tütensee found only on the last pages. But in order to understand his concept of ballasting the dead ice blocks, you should also read the first pages.
Who careful reading finds even more 'details' that the CIRT has on their homepage probably 'forget' mitabzudrucken, for example. Gareis cite as follows:
. "internal structure and shape of the terrace, to speak particularly of the edge line against an origin by glacial or glaciofluvial ... ... Processes"
Gareis but writes:
"Internal structure and format of Terrace, especially the edges course, speak for a generation of Tüttenseeumrahmung by glacial (moraine) or glaciofluvial (erosion remnants of a larger terrace) processes.
Because that time, he turned to his sedimentological Methods: To distinguish between moraine and terrace material.
Gareis: The Eiszerfall within the Chiemsee
Gareis, J. (1978): The Toteisfluren of the Bavarian Alps as a testament to the type of spätwürmzeitlichen Eisschwundes, Wurzburg Geographical work Würzburg, 101 pages
0 comments:
Post a Comment