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Geomorphological mapping of ice-free areas using polarimetric RADARSAT-2 data on Fildes Peninsula and Ardley Island, Antarctica
ArticleAbstract: Satellite-borne Synthetic Aperture Radar (SAR) has been used for characterizing and mapping in two rPalabras claves:geomorphology, Ice-free areas, periglacial, polarimetry, RADARSAT-2, South Shetland IslandsAutores:D'Hondt O., Durán Valsero J.J., Enrique Serrano, Guillaso S., Koch M., Lopez-Martinez J., Maestro A., Mink S., Nieto A., O'Neill T., Schmid T.Fuentes:scopusInsights into deglaciation of the largest ice-free area in the South Shetland Islands (Antarctica) from quantitative analysis of the drainage system
ArticleAbstract: A quantitative geomorphic analysis of the drainage system on Byers Peninsula, Livingston Island, hasPalabras claves:Byers Peninsula, FLUVIAL, Glacial Geomorphology, Permafrost, Quaternary, Relief evolutionAutores:Durán Valsero J.J., Enrique Serrano, Garrote J., Lopez-Martinez J., Maestro A., Mink S., Ortega J.A., Schmid T.Fuentes:scopusPeriglacial processes and landforms in the South Shetland Islands (northern Antarctic Peninsula region)
ArticleAbstract: Periglacial processes and landforms together with the presence of permafrost are among the most relePalabras claves:Antarctica, geomorphology, Periglacial environment, Periglacial landforms, Permafrost, South Shetland IslandsAutores:Enrique Serrano, Linés C., Lopez-Martinez J., Mink S., Schmid T.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 glacier dynamics in a marginal periglacial high mountain environment: Flow, movement (1991-2000) and structure of the Argualas rock glacier, the Pyrenees
ArticleAbstract: The Argualas rock glacier is located on the southern side of the Central Pyrenees (Argualas massif).Palabras claves:Creep flow, High mountain environment, Periglacial processes, Pyrenees, Rock glacierAutores:Agudo C., Enrique Serrano, San José J.Fuentes:scopusRock glaciers in the South Shetland Islands, Western Antarctica
ArticleAbstract: Rock glaciers are found in the peripheral regions of Antarctica particularly in the Antarctic PeninsPalabras claves:Antarctica, geomorphology, Holocene, Periglacial environment, Rock glaciers, South Shetland IslandsAutores:Enrique Serrano, Lopez-Martinez J.Fuentes:scopusSoils and landforms from Fildes Peninsula and Ardley Island, Maritime Antarctica
ArticleAbstract: Fildes Peninsula (F.P.) and Ardley Island (A.I.) are among the first ice-free areas in Maritime AntaPalabras claves:geomorphology, Ornithogenic soils, periglacial, Permafrost, SoilsAutores:Bockheim J.G., Enrique Serrano, Haus N.W., Lopez-Martinez J., Michel R.F.M., Schaefer C.E.R., Simas F.N.B.Fuentes:scopus