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

The manner by which meltwater drains through a glacier is critical to ice dynamics, runoff
characteristics, and water quality. However, much of the contemporary knowledge relating to …

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 …

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 …

Debris-covered glaciers are common in rapidly eroding alpine landscapes. When thicker
than a few centimeters, surface debris suppresses melt rates. If continuous debris cover is …

Ice-cored lateral–frontal moraines are common at the margins of receding high-Arctic valley
glaciers, but the preservation potential of these features within the landform record is …

For more than a century Alpine glaciers have been retreating dramatically, and they are
expected to shrink even more quickly over the coming decades. This study addresses the …

Controlled moraines are supraglacial debris concentrations that become hummocky
moraine upon de-icing and possess clear linearity due to the inheritance of the former …

The reconstruction and tracing of transport paths in glaciated (and other) environments have
a long tradition in the Earth Sciences. We here present a dataset of clast shape samples …

Twelve glaciers, representing various types, were investigated between 2000 and 2005, in a
region adjacent to the northern reaches of Billefjorden, central Spitsbergen (Svalbard). On …