Szczegóły publikacji
Opis bibliograficzny
The evolution of glacial landforms in the Tatra Mountains during the Bølling–Allerød Interstadial / Jerzy ZASADNI, Piotr Kłapyta, Michał Makos // W: European glacial landscapes : the last deglaciation / eds. David Palacios [et al.]. — Amsterdam : Elsevier, cop. 2023. — ISBN: 978-0-323-91899-2. — S. 341-346. — Bibliogr., Abstr.
Autorzy (3)
- AGHZasadni Jerzy
- Kłapyta Piotr
- Makos Michał
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 142839 |
|---|---|
| Data dodania do BaDAP | 2022-10-12 |
| DOI | 10.1016/B978-0-323-91899-2.00035-8 |
| Rok publikacji | 2023 |
| Typ publikacji | fragment książki |
| Otwarty dostęp |  |
| Wydawca | Elsevier |
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).
