We codify previously published means of calculating exposure ages and erosion rates from
10Be and 26Al concentrations in rock surfaces, and present a single complete and …

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 …

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 …

Over the last decades, cosmogenic exposure dating has permitted major advances in many
fields of Earth surface sciences and particularly in paleoglaciology. Yet, exposure age …

The major uncertainty in relating cosmogenic-nuclide exposure ages to ages measured by
other dating methods comes from extrapolating nuclide production rates measured at …

ABSTRACT We present a Baffin Bay 10Be production‐rate calibration derived from glacial
deposits in western Greenland and Baffin Island, and test our results against published …

Chlorine-36 production rates obtained from different geological calibration studies (eg
Evans et al., 1997; Phillips et al., 2001; Schimmelpfennig et al., 2011; Stone et al., 1996; …

We present a 10Be production-rate calibration derived from an early Holocene debris-flow
deposit at about 1000m above sea level in the central Southern Alps, New Zealand, in the …

During the last deglaciation, warming over Antarctica was interrupted by a return to colder
conditions from about 14,540 to 12,760 yr ago. This period, known as the Antarctic Cold …

Rainfall scavenges meteoric cosmogenic 10Be from the atmosphere. 10Be falls to the
Earth's surface, where it binds tightly to sediment particles in non-acidic soils over the life …