Unraveling paraglacial activity on Sierra de Gredos, Central Spain: A study based on geomorphic markers, stratigraphy and OSL


Por: Munoz-Salinas, E, Castillo, M, Sanderson, D, Kinnaird, T

Publicada: 1 nov 2013
Categoría: Earth-Surface Processes

Resumen:
We study the paraglacial activity in Gredos Gorge, a glaciated valley of Sierra de Gredos (Central Spain), using geomorphic markers, stratigraphy and an approach based on OSL. We use luminescence signals from debris flow and fluvial deposits as well as OSL dating of three deposits to detect the main paraglacial processes in Gredos Gorge. We identify two major phases of paraglacial activity during and after the retreat of Last Glacial Maximum (LGM) glaciers. The first phase consisted of high discharge debris flows, sourced up-valley, triggered during the deglaciation. The second phase started similar to 11 ka and is characterized by two processes: (1) the triggering of low discharge debris flows sourced on the flanks of moraines, and (2) the reworking of paraglacial deposits by rivers. Our results of OSL signals, stratigraphy markers and sediment volume indicate that during and after the deglaciation of Gredos Gorge, paraglacial sediment was depleted as theory predicts. However, glacigenic sediments have not been transferred to sediment sinks as long as similar to 70% of glacial deposits are still stored in the valley. The transition of the environmental conditions prevailing during the LGM to current Mediterranean climate seems to play an important role in delaying the exhaustion model of glacially-conditioned sediment release. We propose that the poor coverage of vegetation driven by the Mediterranean climate prevents the stabilization of glacigenic sediment that is only mobilized during high discharge events responding to extreme rainfalls. (c) 2013 Elsevier B.V. All rights reserved.

Filiaciones:
Munoz-Salinas, E:
 Univ Nacl Autonoma Mexico, Dept Reg Geol, Inst Geol, Mexico City, DF, Mexico

Castillo, M:
 Univ Nacl Autonoma Mexico, Dept Reg Geol, Inst Geol, Mexico City, DF, Mexico
ISSN: 03418162
Editorial
Elsevier, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS, Países Bajos
Tipo de documento: Article
Volumen: 110 Número:
Páginas: 207-214
WOS Id: 000323405600020