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Deglaciation in the Cantabrian Mountains: Pattern and evolution
ArticleAbstract: The last deglaciation of the Cantabrian Mountain began later than 30 ka ago, after a local glacier mPalabras claves:Cantabrian mountains, Deglaciation, Glaciations, QuaternaryAutores:Enrique Serrano, Gómez-Lende M., Pellitero-Ondicol R., Trueba J.J.G.Fuentes:scopusGlacial chronology, environmental changes and implications for human occupation during the upper Pleistocene in the eastern Cantabrian Mountains
ArticleAbstract: Interest in the evolution of Pleistocene glaciers, environmental change and human occupation in soutPalabras claves:Cantabrian mountains, Glaciations, Human occupation, Late quaternary, MIS3Autores:Enrique Serrano, Gómez-Lende M., González-Amuchastegui M.J., González-García M., Pellitero-Ondicol R., Rico I., Trueba J.J.G.Fuentes:scopusGlaciations in the Cantabrian Divide: The Quaternary glacial evolution in the Sierra de Cebolleda (León)
ArticleAbstract: The Sierra de Cebolleda (León province, Castilla y León) is a 10 km length part of tha Cantabrian DiPalabras claves:Cantabrian mountains, geomorphology, Glaciers landforms, Quaternary glaciationsAutores:Enrique Serrano, González-García M., Lende M.G., Trueba J.J.G.Fuentes:scopusGround temperatures, landforms and processes in an Atlantic mountain. Cantabrian Mountains (Northern Spain)
ArticleAbstract: Ground temperatures determine significant geomorphological processes in a wet and temperate mountainPalabras claves:Cantabrian mountains, geomorphology, Ground thermal regime, Snow cover, Temperate high mountainAutores:Enrique Serrano, Gómez-Lende M., Pellitero-Ondicol R., Pisabarro A., Trueba J.J.G.Fuentes:scopusQuaternary glacial evolution in the Central Cantabrian Mountains (Northern Spain)
ArticleAbstract: The glacial evolution of the Cantabrian Mountains is not well known. Previous studies have focused oPalabras claves:Cantabrian mountains, ELA, geochronology, Glaciation, Late quaternaryAutores:Enrique Serrano, Gómez-Lende M., González-García M., Pellitero-Ondicol R., Trueba J.J.G.Fuentes:scopusRock glaciers in the central cantabrian mountains: Palaeoenvironmental indicators
ArticleAbstract: Rock glaciers are considered reliable indicators of permafrost occurrence, developed in environmentsPalabras claves:Cantabrian mountains, Cryogenic phases, Periglacial environments, Relict rock glaciersAutores:Enrique Serrano, Pellitero-Ondicol R., Trueba J.J.G.Fuentes:scopusStructure 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:scopus