Direct response of small non-glaciated headwater catchments to Late Quaternary climate change: The Valle de la Fueva, southern Pyrenees
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DOI: 10.1016/j.geomorph.2018.06.008
Abstract: Abstract Topographic depressions in mountain regions function as sediment traps and their morpho-sedimentary archives provide important insight into erosion and sediment dynamics in mountain ranges. In order to establish the (direct) drivers and timing of… read more here.
Keywords: valle fueva; climate; erosion; small non ... See more keywords