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 …

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 …

The Seymareh landslide, detached∼ 10 ka from the northeastern flank of the Kabir-kuh fold
(Zagros Mts., Iran), is recognized worldwide as the largest rock slope failure (44 Gm 3) ever …

Fluvial terraces are valuable records to study and characterize landscape evolution and
river response to base level lowering, and to decipher coupled responses between fluvial …

Constraining the ages of fluvial terraces is essential to understanding fluvial responses to
climate and sea-level changes and estimating uplift/incision. Luminescence dating of sand …

The rise of large mountain ranges is considered to be driven by tectonics potentially coupled
with climate driven-erosion, although the role of this coupling remains uncertain. The arid …

The end of the Middle Stone Age in southern Africa, often called the final MSA (∼ 40–28 ka),
represents one of the most understudied technocomplexes in this part of the world …

The cumulative incision rates of~ 50–70 m/Ma integrating over the last~ 3 Ma have been
derived from published terrace-chronological data of the Danube river in the Western …

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 …

The stream length-gradient (SL) index is widely used in geomorphological studies aimed at
detecting knickzones, which are extensive along-stream deviations from the typical concave …