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)

Article

Abstract: Valley glaciers between 16 and 50 km in length developed during Pleistocene glacial maxima in the so

Palabras claves:

Cantabrian mountains, Geoelectrical units, Glacial consolidation, Glaciated valleys, Overdeepened valleys, Pressurometer tests, Pyrenees, Seismic refraction survey, Vertical electrical soundings

Autores:

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:

scopus