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...

Full description

Bibliographic Details
Main Author: Santos-González, Javier (author)
Other Authors: 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)
Format: article
Language:eng
Published: 2022
Subjects:
Rock glacier
Deglaciation
Paraglacial processes
Cosmic-Ray Exposure dating
Bølling-Allerød interstadial
Cantabrian Mountains
Online Access:http://hdl.handle.net/10451/51443
Country:Portugal
Oai:oai:repositorio.ul.pt:10451/51443

Internet

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

Similar Items