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 …

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 …

Geomorphological map** is a well-established method for examining earth surface
processes and landscape evolution in a range of environmental contexts. In glacial …

Reconstructing the growth and decay of palaeo-ice sheets is critical to understanding
mechanisms of global climate change and associated sea-level fluctuations in the past …

Recent archaeological and paleoecological work along both interior and coastal routes for
early colonization of the New World has suggested that the interior route was impossible …

Studies of past glacial cycles yield critical information about climate and sea-level (ice-
volume) variability, including the sensitivity of climate to radiative change, and impacts of …

The most recent maximum in global ice volume occurred around 23,000 to 19,000 years
ago, during Marine Isotope Stage 2 (MIS 2;∼ 29-14 ka) according to benthic δ 18 O and sea …

Abstract The timing of Cordilleran Ice Sheet deglaciation along the central coast of British
Columbia, Canada, informs climate forcing and early human migration. Thirty‐two 10Be …

Cosmogenic exposure dating of glacial boulders is commonly used to estimate the timing of
past glaciations because the method enables direct dating of the duration a boulder has …

The Cordilleran Ice Sheet (CIS) once covered an area comparable to that of Greenland.
Previous geologic evidence and numerical models indicate that the ice sheet covered much …