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 …

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 …

The Younger Dryas (YD) was a period of rapid climate cooling that occurred at the end of the
last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD …

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 …

In this study, we document deglaciation in a sector of the southern–central Pyrenees (the
Panticosa massif and the upper Gállego and Ossau valleys) using cosmic-ray exposure …

The main objective of this research is to improve knowledge of the deglaciation stages in
Sierra Nevada (southern Spain) by applying 36 Cl cosmogenic exposure dating to 28 …

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 Comparison of selected, well-dated, lacustrine, speleothem and terrestrial pollen
records spanning the Holocene onset and the Early Holocene (ca. 11.7–8 cal kyrs BP) in the …

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 …