Millennial climate oscillations of the glacial interval are interrupted by extreme events, the so‐
called Heinrich events of the North Atlantic. Their near‐global footprint is a testament to …

The Late Wisconsinan advance of the Laurentide Ice Sheet started from a Middle
Wisconsinan interstadial minimum 27–30 14C ka BP when the ice margin approximately …

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 …

High-resolution studies of North Atlantic deep sea cores demonstrate that prominent
increases in iceberg calving recurred at intervals of 2000 to 3000 years, much more …

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 …

Ice‐rafted debris in sediment cores from the North Atlantic suggests that the Laurentide ice
sheet (LIS) periodically disgorged icebergs in brief but violent episodes which occurred …

Fine sediment size (< 63 µm) is best measured by a sedimentation technique which records
the whole size distribution. Repeated size measurement with intermediate steps of removal …

XRF core scanners, with their rapid and non-destructive analytical capability, have now
been used for two decades in the analysis of marine sediments. Initially they were used to …

The location and behaviour of ice streams is one of the most important controls on ice sheet
configuration and stability. In order to reconstruct former ice sheets we need to know ice …

This paper presents a comprehensive review and synthesis of ice streams in the Laurentide
Ice Sheet (LIS) based on a new map** inventory that includes previously hypothesised ice …