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Insights 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:scopusSoil characteristics on varying lithological substrates in the South Shetland Islands, maritime Antarctica
ArticleAbstract: Soils in ice-free areas of Livingston Island have been forming since the last deglaciation in a mariPalabras claves:Antarctica, Byers Peninsula, geochemistry, Hurd Peninsula, Permafrost, Properties, Soils, South Shetland IslandsAutores:Casas J., Cuchi J.A., Durán Valsero J.J., Enrique Serrano, Lopez-Martinez J., Machín J., Mink S., Navas A.Fuentes:scopus