It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …

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 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 …

The Mediterranean mountains were repeatedly glaciated during the Pleistocene. Glaciers
were present in most of the major mountains areas from Morocco in the west to the Black …

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

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 …

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 …

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 …

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 …