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Autor:
Gerit E.U. Griesmeier, Sandra M. Braumann, Jürgen M. Reitner, Stephanie M. Neuhuber, Daniel P. Le Heron, Oscar Marchhart, Alexander Wieser
During the Last Glacial Maximum (LGM), large glacier tongues reached far into the alpine foreland and formed piedmont lobes. Common deposits are moraine “amphitheatres” directly connected to glaciofluvial deposits, which are both suitable for (di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0e92e9901f928757f8f0314515668f2
https://doi.org/10.5194/egusphere-egu23-5525
https://doi.org/10.5194/egusphere-egu23-5525