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sediment drift

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However, water-column plumes will include a disaggregated, fine-grained sediment fraction that may drift for years and disperse for several hundred to over 1,000 kilometres, depending on the release depth.
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Other areas of basic research included the study of drift pumice in the Basin, relationships between the chemical composition and magnetic susceptibility in sediment cores and petrology.
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In geology, drift is the name for all material of glacial origin found anywhere on land or at sea, including sediment and large rocks (glacial erratic).
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The widespread distribution of Permo-Carboniferous glacial sediments in South America, Africa, Madagascar, Arabia, India, Antarctica and Australia was one of the major pieces of evidence for the theory of continental drift.
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