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 …

We correlate Upper Pleistocene glacial and fluvial deposits of the Cinca and Gállego River
valleys (south central Pyrenees and Ebro basin, Spain) using geomorphic position …

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 …

While revolutionary to the geomorphic community, the application of terrestrial cosmogenic
nuclide (TCN) dating is complicated by geological uncertainties, which often lead to skewed …

A sedimentological and geochemical study of the Lago Enol sequence (Cantabrian
Mountains, northern Spain), together with detailed geomorphological mapping, provides a …

The glacial evolution of the Cantabrian Mountains is not well known. Previous studies have
focused on the extent of the glacial maximum and the presence of younger features in …

In this paper we synthesize the research in glacial geomorphology and geochronology in
northern Spain, with special attention to the evidence of local glacier maximum extent earlier …

At the north-western limit of the Mediterranean basin, in the Mediterranean–Oceanic
transition zone, the multidisciplinary study of two palaeolakes: Villaseca and La Mata …