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- W3217356371 abstract "Detailed geomorphological mapping over several decades has led to the conclusion that the Quaternary glaciation left a strong imprint in the geomorphological landscape of all mountain massifs higher than 2000 m. They are present two main types of geomorphologic landscapes, the Borăscu glacial landscape, with glacial cirques developed at the edge of planation surfaces, and Făgăraș landscape, a typical alpine-style glacial landscape. In Last Glacial Maximum (LGM) phase, in lower mountain areas, glaciers were present only where a sum of local factors favoured their formation, a good example being Apuseni Mountains. For the Rodnei Mountains the highest of Eastern Carpathians, a 5-km long glacier descended to 1000 m on Pietroasa Valley, corresponding to an equilibrium-line altitude (ELA) at 1340 m, the frontal moraines being between 26.6±2.4 and 18.3±1.6 ka. On the volcanic caldera’s walls of Călimani Mountains, small cirque and valley glaciers were present, and the upper conglomeratic structural plateau of Ceahlău Mountains was occupied by a small plateau glacier. In the Southern Carpathians in the Retezat Mountains, around 21±0.8–1.5 ka 10Be ages, the glaciers descended to 1000–1050 m during LGM. The Pietrele glacial complex covering an area of 27.3 km2, and the corresponding ELA was at 1646 m. The planation surfaces, a true peneplain, ubiquitous above 1800 m in Godeanu, Ţarcu, Cindrel, Lotrului, and Şurianu Mountains and the marginal parts of the Retezat, Iezer, and Făgăraş Mountains favoured the development of plateau glaciers associated with conical glaciers and/or small ice caps." @default.
- W3217356371 created "2021-12-06" @default.
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- W3217356371 date "2022-01-01" @default.
- W3217356371 modified "2023-09-25" @default.
- W3217356371 title "The Romanian Carpathians: glacial landforms from the Last Glacial Maximum (29–19 ka)" @default.
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- W3217356371 doi "https://doi.org/10.1016/b978-0-12-823498-3.00013-3" @default.
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