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Titlebook: Sea-Ice and Iceberg Sedimentation in the Ocean; Recent and Past Alexander P. Lisitzin Book 2002 Springer-Verlag Berlin Heidelberg 2002 Arct

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Cryogenic Faciesnt and initial stages of diagenesis, etc.). According to G. F. Krasheninnikov (1971), facies are considered as a sedimentary complex which differs from neighbouring deposits of the same stratigraphical level.
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Book 2002lay 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.
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Types of Continental and Marine Glaciations · Preparation and Transportation of Sedimentary MaterialCryosphere is one of the Earth’s spheres where negative temperatures are dominant and water is mainly in solid or supercooled state. The author considers the lithosphere to not only occupy cold regions within land but cold regions within the hydrosphere (the World Ocean in high latitudes).
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Iceberg and Sea-Ice Sedimentation in the North Atlantic — Recent and PastGreenland, the largest centre of the modern glaciation of the Northern Hemisphere, is situated in the North Atlantic. Its white ice cap rising above the sea level to the heights of 2–3 thousand metres is a source of numerous icebergs. Modern glaciation also exists on Spitsbergen, Franz Joseph Land, Novaya Zemlya and arctic Canada (see Table 3.1).
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