Szczegóły publikacji
Opis bibliograficzny
The evolution of glacial landforms in the Tatra Mountains during the deglaciation / 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. 157-164. — Bibliogr., Abstr.
Autorzy (3)
- AGHZasadni Jerzy
- Kłapyta Piotr
- Makos Michał
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 142841 |
|---|---|
| Data dodania do BaDAP | 2022-10-12 |
| DOI | 10.1016/B978-0-323-91899-2.00042-5 |
| Rok publikacji | 2023 |
| Typ publikacji | fragment książki |
| Otwarty dostęp |  |
| Wydawca | Elsevier |
Abstract
The post-Last Glacial Maximum (LGM) deglaciation of the Tatra Mountains (~18–15 ka BP) left a sequence of multiple moraine and rock glaciers in the landscape, which marks the transition between valley to cirque glaciation, when c.90% of glacier length was reduced after full glacial conditions. The earliest glacier readvance occurred likely 18–17 ka BP and the latest one just before the Bølling–Allerød (B-A) Interstadial at c.15 ka BP when the largest cirque glaciers achieved only 0.5–1.5 km in length. During deglaciation overdeepening basins located in lower glacial cirques (~1400–1700 m a.s.l.) in the High Tatras were for the first time ice-free and the oldest lacustrine deposits started to accumulate since the final part of Oldest Dryas. The post-LGM deglaciation was strongly affected by a high rate of debris supply to the glacial systems, leading to a complex assemblage of landforms from moraines and debris-covered glaciers to rock glaciers.
