Sea-Ice and Iceberg Sedimentation in the Ocean

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Sea-Ice and Iceberg Sedimentation in the Ocean is written by Alexander P. Lisitzin and published by Springer Science & Business Media. It's available with International Standard Book Number or ISBN identification 3642559050 (ISBN 10) and 9783642559051 (ISBN 13).

In many geological epochs, glacial sediments are widespread. This type of sedimentation results from the interaction between atmosphere, cryosphere, hydrosphere and biosphere under temperatures ranging from 0 to -80. Two types of glacial sediments exists: those from sea-ice and those from icebergs. Both types can be subdivided into various subfacies. Most widespread in the Northern Hemisphere is the Siberian subfacies, characterized by silt and clay and often misinterpreted as sediments of temperate zones. This reference book for researchers working on this kind of sediments provides a complete overview of the various glacial deposits in the ocean.