This paper reviews current understanding of deglaciation in North, Central and South
America from the Last Glacial Maximum to the beginning of the Holocene. Together with …

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

Rock glaciers are an important geomorphic element of glaciated mountain landscapes, but
our understanding of their distribution and ages, controls on their development, and their …

Temperate glaciers are very sensitive to changes in the global climate system and provide
an excellent opportunity to obtain information on the timing and magnitude of palaeoclimatic …

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 …

Holocene glacial chronostratigraphies in glaciated valleys spread throughout the Himalayan-
Tibetan orogen, including the Himalaya, Tibet, Pamir, and Tian Shan, are developed using a …

Rock glaciers are common in alpine landscapes, but their evolution over time and their
significance as agents of debris transport are not well‐understood. Here, we assess the …

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 …

Piedmont glaciers (lobes), typically found in high latitudes and large mountainous regions,
extend from ice sheets and ice caps to lower altitudes. However, they can also occur …

The aim of this research is to improve our current understanding of the deglaciation stages
in the southeastern Pyrenees and integrate it into reconstructions of the long‐term …