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 …
M Calvet, Y Gunnell, B Laumonier - Earth-Science Reviews, 2021 - Elsevier
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 …
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 …
D Palacios, A Gómez-Ortiz, N Andrés… - Quaternary Science …, 2016 - Elsevier
The main objective of this research is to improve knowledge of the deglaciation stages in Sierra Nevada (southern Spain) by applying 36 Cl cosmogenic exposure dating to 28 …
We review the evolution of glaciers in the Iberian Mountains during the Younger Dryas (12.9– 11.7 ka, following the chronology of Greenland Stadial 1–GS1) and compare with available …
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 …
There exists a transition between rockfalls, large rock mass failures, and rock avalanches. The magnitude and frequency relations (M/F) of the slope failure are increasingly used to …
The 120 km-longTêt River flows out of the Pyrenees to the Mediterranean. By displaying a mappable sequence of Quaternary alluvial units between the Pleistocene frontal moraines …
Much research, especially within the framework of the Fluvial Archives Group, has focused on river response to climate change in mid-latitude non-glaciated areas, but research into …