The only glaciers existing today in the Iberian Peninsula are small features located in the
Pyrenees, though their number and extension has undergone significant changes over the …

The relatively warm climate conditions prevailing today in the Mediterranean region limit
cold geomorphological processes only to the highest mountain environments. However …

A multi-proxy characterization of the uppermost sedimentary infill of an Iberian alpine lake
(Cimera, 2140 m asl) was performed to establish the climatic and environmental conditions …

Throughout the last cold stage, the North Atlantic region was punctuated by abrupt climate
shifts and atmospheric processes propagated their effects to adjacent continents. During …

Active periglacial processes are currently marginal in the Iberian Peninsula, spatially limited
to the highest mountain ranges. However, a wide variety of periglacial deposits and …

Mountain glaciers respond directly to changes in precipitation and temperature, thus their
margin extent is a high-sensitivity climate proxy. Here, we present a robust 10Be chronology …

We review the evolution of glaciers in the Iberian Mountains during the Younger Dryas (12.9–
11.7 ka, following the chronology of Greenland Stadial 1–GS1) and compare with available …

Abstract The Cuerpo de Hombre paleoglacier occupies the upper sector of the Cuerpo de
Hombre river basin, located on the northwest slope of the Sierra de Béjar Mountains (Iberian …

The mountain ranges of the Iberian Peninsula preserve a valuable record of past glaciations
that may help reconstruct past atmospheric circulation patterns in response to cooling events …

This paper examines glacial evolution in the La Pera and Malniu cirques, and Arànser, La
Llosa and Duran valleys, in the Cerdanya massifs on the south-facing slopes of the eastern …