Glacial - periglacial transition in the Ratera Cirque (Central Pyrenees) from the Younger Dryas to the Holocene

The transition from glacial to deglacial environments in mid-latitude mountains leaves a wide range of landforms of glacial, periglacial and paraglacial origin, of which the chronology and evolution are still debated. This work provides geomorphological and geochronological evidence for the last pha...

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Egile Nagusiak:	Josep Ventura, Marc Oliva, José M. Fernández-Fernández, Marcelo Fernandes, David Palacios, Tancrède Leger, Vincent Jomelli, Aster Team
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Elsevier 2025-12-01
Saila:	Quaternary Science Advances
Gaiak:	Deglaciation, Heinrich 1, Bølling-Allerød Younger dryas Early holocene Debris-covered glaciers Rock glaciers Paraglacial processes
Sarrera elektronikoa:	http://www.sciencedirect.com/science/article/pii/S2666033425000437
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