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 …

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 …

The study of glacial geomorphology in the Cantabrian Mountains, a mountain range that
extends 460 km along the northern coast of the Iberian Peninsula (SW Europe), started late …

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 …

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 …

Abstract The Western Massif of the Picos de Europa (latitude 43° N, longitude 4–5° W)
includes some of the highest peaks in the Cantabrian Mountains. This massif was heavily …

The aim of this research is to improve our current understanding of the deglaciation stages
in the southeastern Pyrenees and integrate it into reconstructions of the long‐term …

Deglaciation processes in the upper Gállego Valley, central–southern Pyrenees, were
studied using geomorphological mapping and 36Cl cosmogenic dating of moraine and rock …