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Ice Age Earth : Late Quaternary Geology and Climate - Alastair G. Dawson

Ice Age Earth

Late Quaternary Geology and Climate

By: Alastair G. Dawson

Paperback | 19 December 1991 | Edition Number 1

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The reconstruction of past climatic change is dependent upon the application of reliable dating techniques and an understanding of the context of these methods. The study of Quarternary palaeoenvironments must draw from a range of disciplines. In an areas of increasing interest and specialisation, Ice Age Earth combines a summary of research and a synthetic description of the Late Quarternary. It focuses on changes in the Earth's geology and climate between the last interglacial and the final melting of the last great ice sheets: 130 000 to 7 000 year ago. The book describes the study of ocean sediments and ice cores and the value of these findings to the development of advance circulation models. Emphasis is placed on regional variability in glacial history, the rapidity of past climate change and the complexity of environmental responses to widespread deglaciation. Periglacial environmnents - lakes, rivers, mires, volcanic and aeolian activity, crustal and sea-level movement - are also considered. The book closes with a contextual discussion on Milankovitch insolation theory. Ice Age Earth provides the first detailed review of global environmental change in the Late Quaternary. It should prove essential reading for all students interested in Quaternary environments.
Industry Reviews
"This volume will serve as an excellent text for advanced undergraduates in geology and physical geography . . . The book is wide-ranging in both its subject and geographic coverage. It is far broader in scope than equivalent texts on glacial landscapes or glacial processes . . . All-in-all this volume will serve as an up-to-date text on the variety of Ice Age associated environments that resulted in the present global landscape."-Palaeogeography, Palaeoclimatology, Palaeoecology ""Ice Age Earth is a bold effort to review a bewildering array of different datasets, methods and theories. . . . [it] succeeds and provides an interesting read."-"New Scientist

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