Research in landscape evolution over millions to tens of millions of years slowed
considerably in the mid‐20th century, when Davisian and other approaches to …

The most recent deglaciation of the North American Ice Sheet Complex (NAISC: comprising
the Innuitian, Cordilleran, and Laurentide ice sheets) offers a broad perspective from which …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Cosmogenic exposure dating has greatly enhanced our ability to define glacial chronologies
spanning several global cold periods, and glacial boulder exposure ages are now routinely …

In the last decades surface exposure dating using cosmogenic nuclides has emerged as a
powerful tool in Quaternary geochronology and landscape evolution studies. Cosmogenic …

Climatic changes over the last 50 years resulted in a decrease of permafrost extent, an
increase of permafrost temperature, and deepening of the active layer in numerous locations …

Fjords commonly punctuate continental edges formerly occupied by Quaternary ice sheets,
reaching kilometre depths and extending many tens of kilometres inland,. These features …

Periglacial trimlines separating glacially eroded lower slopes from blockfield-covered
plateaus on British and Irish mountains have been interpreted either (1) in terms of …

At the largest time and space scales, the pace of erosion and chemical weathering is
determined by tectonic uplift rates. Deviations from equilibrium arise from the transient …

Abstract Over 160 10Be and 36Cl exposure ages pertaining to the extent and chronology of
the last British–Irish Ice Sheet (BIIS) are critically reviewed. Despite uncertainties inherent in …