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 …

Glacial cirques are armchair-shaped erosional hollows, typified by steep headwalls and,
often, overdeepened floors. They reflect former regions of glacier initiation, and their …

This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …

Glacial landforms are a significant element of landscape in many regions of Earth. The
increasing availability of high-resolution digital elevation models (DEMs) provides an …

Ground surface temperature (GST, depth of 5 cm) is essential for understanding the climate-
induced impacts in the Earth Critical Zone, especially in cold regions. This work aims to …

Cirques are emblematic landforms of alpine landscapes. The statistical distribution of cirque-
floor elevations is used to infer glacial equilibrium-line altitude, and the age of their frontal …

It has been proposed that most cirques are source‐area depressions of large, deep‐seated
rock‐slope failures. Yet the close relation between cirques and climate is convincing …

This first overview of large‐scale rock slope failure (RSF) in the yrenees addresses the
eastern third of the range. Around 30 principal RSFs greater than 0.25 km2 and 20 lesser or …

Three Iberian mountain ranges encompassed glaciers during the Little Ice Age (LIA): the
Pyrenees, Cantabrian Mountains, and Sierra Nevada. The gradual warming trend initiated …

Three themes in global mountain geomorphology have been defined and reinforced over
the past decade:(a) new ways of measuring, sensing, and analyzing mountain …