Michael J. Hambrey – författare

Considering that glaciers and ice sheets cover about 10% of the Earth’s land surface in a world where human civilization is increasingly impacted by the effects of changing glacial activity, Colour Atlas of Glacial Phenomena presents itself as an indispensable guide for students, professionals, and researchers who want to be better informed while studying and tracking the future influences of glaciers and ice sheets on the global environment. While stressing both the beauty and utility of glaciers, the authors cover critical features of glaciers and their landforms and provide useful explanations of the key concepts in glaciology and glacial geology. The authors expand to demonstrate how our lives are influenced by the Cryosphere, a key component of the Earth system and how this heightens the vulnerability of glaciers and ice sheets to deterioration. This illustrated book also helpfully maps out regions of mountain glaciers and ice caps around the world for a practical reference and discusses the products of glacial erosion and deposition integral to understanding rising global sea levels.

Associating ice masses with the transport and deposition of sediments has long formed a central theme in glaciology and glacial geomorphology. The reason for this focus is clear, in that ice masses are responsible for much of the physical landscape which characterizes the Earth's glaciated regions. This association also holds at a variety of scales, for example, from the grain-size characteristics of small-scale moraines to the structural architecture of large-scale, glacigenic sedimentary sequences in both surface and subaqueous environments.This volume brings numerous state-of-the-art research contributions together, each relating to a different physical setting, spatial scale, process or investigative technique. The result is a diverse and interesting collection of papers by glaciologists, numerical modellers and glacial geologists, which are all linked by the theme of investigating the relationships between the behaviour of ice masses and their resulting sedimentary sequences.