Rapid deglaciation during the Bølling-Allerød Interstadial in the Central Pyrenees and associated glacial and periglacial landforms

The Central Pyrenees hosted a large ice cap during the Late Pleistocene. The cirques under relatively low-altitude peaks (2200–2800 m) include the greatest variety of glacial landforms (moraines, fossil debris-covered glaciers and rock glaciers), but their age and formation process are poorly known....

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Detalhes bibliográficos
Autor principal: Oliva, Marc (author)
Outros Autores: Fernandes, Marcelo (author), Palacios, D. (author), Fernández-Fernández, Jose M. (author), Schimmelpfennig, I. (author), Antoniades, D. (author), Aumaître, Georges (author), Bourlès, Didier (author), Keddadouche, Karim (author)
Formato: article
Idioma:eng
Publicado em: 2021
Assuntos:
Central Pyrenees
Bølling-Allerød
Deglaciation
Cosmic-ray exposure dating
Moraines
Polished bedrock
Paraglacial processes
Texto completo:http://hdl.handle.net/10451/48917
País:Portugal
Oai:oai:repositorio.ul.pt:10451/48917

Texto Completo

http://hdl.handle.net/10451/48917

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