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Structure of the large glacial basins in the Northern Iberian Peninsula, a comparison study: Andorra (Eastern Pyrenees), Gállego (Central Pyrenees) and Trueba valley (Cantabric Range)
ArticleAbstract: Valley glaciers between 16 and 50 km in length developed during Pleistocene glacial maxima in the soPalabras claves:Cantabrian mountains, Geoelectrical units, Glacial consolidation, Glaciated valleys, Overdeepened valleys, Pressurometer tests, Pyrenees, Seismic refraction survey, Vertical electrical soundingsAutores:Bordonau i Ibern J., Boulton G.S., Constante-Orrios A., Enrique Serrano, Garcia-Ruiz J.M., Herrero i Simón R., Martí i Bono C., Palomar i Molins J., Peña-Monné J.L., Pous i Fàbregas J., Ros i Visus X., Sancho-Marcén C., Trueba J.J.G., Turu V.Fuentes:scopusThe glaciers of the Central-Western Pyrenees
Book PartAbstract: The action of the Quaternary glaciers in the Central-Western Pyrenees is responsible for the variousPalabras claves:Central-western pyrenees, Deglaciation, Glacial asynchrony, Glacial landformsAutores:Enrique Serrano, Garcia-Ruiz J.M.Fuentes:scopus