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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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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