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Swiss Journal of Geosciences
Fig. 6 | Swiss Journal of Geosciences

Fig. 6

From: Alpine overdeepenings and paleo-ice flow changes: an integrated geophysical-sedimentological case study from Tyrol (Austria)

Fig. 6

Ice flow model from the ice build-up phase to the climax of the LGM. a Early ingression of the Inn glacier into the basin of Hopfgarten and early impediment of Windau and Kelchsau glacier (dashed lines). b Advanced phase of ice-build up with the blockade of ice flow towards the east by the Achen glacier. c Ice flow during the climax of the LGM, when the ice transfluences (locations A and B in Figs. 1, 2) from the Salzach valley to the Windau and Kelchsau valley were active. Ice surface around Hopfgarten in 1,900 m asl

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