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 …

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 …

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 …

Large glaciers and ice caps formed in the Mediterranean mountains during the cold stages
of the Pleistocene and some small glaciers remain today. Here we review 157 outputs that …

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 …

Alpine caves have attracted considerable geomorphological, paleoenvironmental and
hydrogeological interest since climate, glaciations, relief uplift, fluvial incision and karst …

Abstract The Last Glacial Termination led to major changes in ice sheet coverage that
disrupted global patterns of atmosphere and ocean circulation. Paleoclimate records from …

Abstract Mt Chelmos in the Peloponnesus was glaciated by a plateau ice field during the
most extensive Pleistocene glaciation. Valley glaciers radiated out from an ice field over the …

Sierra Nevada constitutes the southernmost and highest massif in the Iberian Peninsula,
with elevations exceeding 3000 m. Two large glacial advances were recorded during the …