To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the
form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we …

A global overview of glacier advances and retreats (grouped by regions and by millennia)
for the Holocene is compiled from previous studies. The reconstructions of glacier …

We present a new time‐slice reconstruction of the Eurasian ice sheets (British–Irish,
Svalbard–Barents–Kara Seas and Scandinavian) documenting the spatial evolution of these …

Accurate calculation of the environmental radiation dose rate (Ḋ) is an essential part of
trapped charge dating methods, such as luminescence and electron spin resonance dating …

Abstract Models of the production of cosmogenic nuclides typically incorporate an
adjustable production rate parameter that is scaled for variations in production with latitude …

Several models have been proposed for scaling in situ cosmogenic nuclide production rates
from the relatively few sites where they have been measured to other sites of interest. Two …

The ongoing debate about the nature of coupling between climate and tectonics in mountain
ranges derives, in part, from an imperfect understanding of how topography, climate …

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

For more than a century, geologists have sought to measure the distribution of erosion rates
on Earth's dynamic surface. Since the mid-1980s, measurements of in situ 10Be, a …

It has long been known that mountain glaciers and continental ice sheets around the globe
reached their respective maximum extent at different times during the last glacial cycle, often …