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Glacial evolution of Sierra Nevada (Spain) and the origin of rock glaciares
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Orientador(es)
Resumo(s)
In spite of considerable advances in the knowledge and understanding of the glacial
chronology of southern Europe, some very significant mountains still have to be studied.
These include the Sierra Nevada, the highest mountain range in the Iberian Peninsula, located
in the extreme south-east, only 170 km from Africa, where the last glaciers disappeared last
century. The aim of this paper is to present a chronology of deglaciation from the Sierra
Nevada based on geomorphological analysis of glacial and periglacial landforms and on 36Cl
surface exposure dating, then to relate it to the historical Little Ice Age (LIA) deglaciation
process reconstructed from field data and historical documentary sources.
Descrição
Palavras-chave
Glacial Evolution Sierra Nevada Spain Rock Glaciares
Contexto Educativo
Citação
Ortiz, A. G., Palacios, D., Palade, B. Selem, L. V., Franch, F. S., García, L. M. T., Oliva, M. (2013). Glacial evolution of Sierra Nevada (Spain) and the origin of rock glaciares. Boletín de la Asociación de Geógrafos Españoles, 61, 391-393. https://bage.age-geografia.es/ojs/index.php/bage/article/view/1558