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Sediment dynamics of a major piedmont glacier: the Salzach Glacier in the North Alpine Foreland

Title data

Salcher, Bernhard ; Starnberger, Reinhard ; Pollhammer, Thomas ; Götz, Joachim:
Sediment dynamics of a major piedmont glacier: the Salzach Glacier in the North Alpine Foreland.
In: DEUQUA Special Publications. Vol. 5 (2024) . - pp. 31-39.
ISSN 2625-8137
DOI: https://doi.org/10.5194/deuquasp-5-31-2024

Abstract in another language

The foreland basins of the European Alps were repeatedly covered by major piedmont glaciers during Quaternary glacial maxima. The Salzach Glacier was the easternmost of a series of large Pleistocene piedmont glaciers entering the North Alpine Foreland through major Alpine valleys. It covered an area of more than 1000 km2 during at least four glacial maxima. The slightly elevated molasse bedrock provides a high potential for preservation of glacial landforms and offers an ideal setting to explore the erosional and depositional dynamics of a major glacier piedmont lobe. This field excursion guide leads to some selected key sites representing deposits of glacial advance, relative equilibrium, and ice lobe collapse.

Further data

Item Type: Article in a journal
Refereed: Yes
Institutions of the University: Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Chair Geomorphology
Faculties > Faculty of Biology, Chemistry and Earth Sciences > Department of Earth Sciences > Chair Geomorphology > Chair Geomorphology - Univ.-Prof. Dr. Oliver Sass
Result of work at the UBT: Yes
DDC Subjects: 500 Science > 550 Earth sciences, geology
900 History and geography > 910 Geography, travel
Date Deposited: 27 Jun 2025 04:57
Last Modified: 27 Jun 2025 04:57
URI: https://eref.uni-bayreuth.de/id/eprint/93999