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- W4297904532 abstract "During the final part of the Oldest Dryas cold stadial (~15 ka), the glaciers in the Tatra Mountains were already confined to sheltered areas below high cirque walls and likely disappeared completely responding to Bølling–Allerød Interstadial (B-A) warming. In the High Tatras ice-moulded bedrocks or moraine boulders located in the direct neighbourhood of Younger Dryas (YD) moraines or rock glacier fronts above 2100 m a.s.l. were ice-free already at 14.8–14.2 ka and there is no evidence for moraines left by glaciers during the B-A retreat. In the lower elevated cirques in the Western Tatras, the stabilisation of debris-covered glaciers and rock glaciers was prolonged until the B-A Interstadial (13–14 ka) or even to the YD – Holocene transition (11.9 ka)." @default.
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- W4297904532 date "2023-01-01" @default.
- W4297904532 modified "2023-09-30" @default.
- W4297904532 title "The evolution of glacial landforms in the Tatra Mountains during the Bølling–Allerød Interstadial" @default.
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- W4297904532 doi "https://doi.org/10.1016/b978-0-323-91899-2.00035-8" @default.
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