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Glacial sediments: Processes, environments and facies

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Encyclopedia of Sediments and Sedimentary Rocks

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Introduction

Significance of glacial deposits

The importance of glacial sediments can be gauged from the fact that 10 percent of the Earth's land surface currently is covered by glacier ice, a figure that exceeded 30 percent during the Quaternary glaciations of the last 2 Ma. Glacier ice has left a complex, often patchy, record of deposition on land, and offshore has contributed substantially to the build up of continental shelves. In earlier geological history, the Earth experienced several continental-scale glaciations, some of them even more extensive than those of the Quaternary Period. Glacial deposition is intimately associated with a wide range of other processes, including fluvial, mass flowage, eolian, lacustrine, and marine. The resulting facies associations are highly variable, and without detailed investigation can be subject to a wide range of interpretations. It is only within the last three decades that studies of glacial processes in modern settings have made it...

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© 1978 Dowden, Hutchinson & Ross, Inc.

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Hambrey, M.J., Glasser, N.F. (1978). Glacial sediments: Processes, environments and facies. In: Middleton, G.V., Church, M.J., Coniglio, M., Hardie, L.A., Longstaffe, F.J. (eds) Encyclopedia of Sediments and Sedimentary Rocks. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-3609-5_99

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  • DOI: https://doi.org/10.1007/978-1-4020-3609-5_99

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