The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: a new study case from the Cantabrian Mountains (Spain)

During the Late Pleistocene, the main mountain ranges of the Iberian Peninsula were covered by small icefields and cirque and alpine glaciers. The deglaciation triggered paraglacial processes that generated landforms, mostly within the ice-free glacial cirques. In this research we analyse the deglac...

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Detalhes bibliográficos
Autor principal: Santos-González, Javier (author)
Outros Autores: González-Gutiérrez, Rosa Blanca (author), Redondo-Vega, José María (author), Gómez-Villar, Amelia (author), Jomelli, Vincent (author), Fernández-Fernández, Jose M. (author), Andrés, Nuria (author), García-Ruiz, José M. (author), Peña-Pérez, Sergio Alberto (author), Melón-Nava, Adrián (author), Oliva, Marc (author), Álvarez-Martínez, Javier (author), Charton, Joanna (author), Palacios, David (author)
Formato: article
Idioma:eng
Publicado em: 2022
Assuntos:
Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
Texto completo:http://hdl.handle.net/10451/51443
País:Portugal
Oai:oai:repositorio.ul.pt:10451/51443

Texto Completo

http://hdl.handle.net/10451/51443

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