Mostrando 5 resultados de: 5
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:scopusDynamic, evolution and structure of Pyrenean rock glaciers
ArticleAbstract: The paper analyzes the fourteen rock glaciers inventoried in the Pyrenees. The genesis, surface morpPalabras claves:Periglacial processes, Pyrenees, Rock glacierAutores:Enrique Serrano, Sanjosé J.J., 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:scopusSurface dynamic and current status of the madaleta rock glacier (Pyrenees)
ArticleAbstract: The Maladeta Occidental rock glacier is located in the Maladetas massif (Central Pyrenees). A geomorPalabras claves:High mountain, Maladeta, Periglacial processes, Pyrenees, Rock glacierAutores:Enrique Serrano, González-García M., Sanjosé J.J., Trueba J.J.G.Fuentes:scopusThe snow in the Picos de Europa: Geomorphological and environmental implications
ArticleAbstract: The Picos de Europa massif is the maximun exponent of the Atlantic High Mountain of SW Europe. The pPalabras claves:Atlantic high mountain environment, Cordillera Cantábrica, Nival processes, Picos de Europa, SnowAutores:Enrique Serrano, Trueba J.J.G.Fuentes:scopus