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Autor:
Agata Pyrda
Publikováno v:
Geology, Geophysics and Environment. 49:19-36
In the Western Carpathians, clear evidence of the Pleistocene glaciations only occurs in two mountain massifs – the Tatra and Low Tatra Mountains. The Low Tatra Mountains (2043 m a.s.l.), contrary to the higher and more strongly glaciated Tatra Mou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9bd01069ccddec2356ede1f9eed8fb6f
https://doi.org/10.7494/geol.2023.49.1.19
https://doi.org/10.7494/geol.2023.49.1.19
