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 increase in aridity, mainly by decreases in precipitation but also by higher temperatures,
is likely the main threat to the diversity and survival of Mediterranean forests. Changes in …

It is widely accepted that future environmental changes will affect rainfall-induced shallow
slides in high-mountain areas. In this study, the Val d'Aran region located in the Central …

The effects of land use and land cover (LULC) dynamics on landslide susceptibility are not
fully understood. This study evaluates the influence of LULC on landslide susceptibility 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 …

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

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

Recent research in the mountains of the Mediterranean has attempted to establish the timing
of the maximum extent of glaciers during the last cold stage. Several dating methods have …

Little Ice Age'(LIA) glacier advance has been registered in three of the main Iberian high
mountain areas: Pyrenees, Picos de Europa and Sierra Nevada. During the LIA, three …