Geomorphological evidence and 10Be exposure ages for the Last Glacial Maximum and deglaciation of the Velká and Malá Studená dolina valleys in the High Tatra Mountains, central Europe
Geomorphological evidence and 10Be exposure ages for the Last Glacial Maximum and deglaciation of the Velká and Malá Studená dolina valleys in the High Tatra Mountains, central Europe
Authors
Keywords
Quaternary, Glaciation chronology, Glacier retreat, Thinning rate, Paraglacial, High Tatra Mts., Western Carpathians
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