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

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 …

In the geological record, hummocky dead-ice moraines represent the final product of the
melt-out of dead-ice. Processes and rates of dead-ice melting in ice-cored moraines and at …

This book is a comprehensive overview of the ever-captivating field of glaciation from the
perspective of glacial landsystems. This approach models the many processes, forms and …

Irregular mounds of glacial debris, commonly referred to as' hummocky moraine', until
recently were linked to ice stagnation during rapid climatic amelioration. However, recent …

Over large areas of the western interior plains of North America, hummocky moraine (HM)
formed at the margins of Laurentide Ice Sheet (LIS) lobes that flowed upslope against …

Clast-supported boulder gravel in outwash-fans along the glacial-maximum margin of the
Laurentide Ice Sheet in Wisconsin indicates the occurrence of outburst floods. These …

Pleistocene permafrost had a major but generally unappreciated effect on the landscape of
Wisconsin, second only to glaciation. Evidence for continuous permafrost during the last part …

An extensive dead‐ice area has developed at the stagnant snout of the Holmströmbreen
glacier, Svalbard, following its last advance during the Little Ice Age (LIA). The most common …