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Lecture-13-Study of Lake Sediments and its Significance.

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dc.contributor.author Gill, G. S.
dc.date.accessioned 2026-01-23T10:43:19Z
dc.date.available 2026-01-23T10:43:19Z
dc.date.issued 2007
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/7980
dc.description.abstract Lake like any body of standing water, serves as the repository for materials carried into it by water, wind, ice, and the activities of living creatures. These materials include: Fine particles of minerals, rock fragments, and organics referred as sediments. Sunken boats, bottles, cans, tires, fishing lures, etc. also found on the lake bottom are not considered sediments. Sediments of lake are studied in their varied aspects i.e. mineralogy, texture, structure and clay content. While minerals, especially heavy minerals, are direct indicators of source of material (Chaudhri and Gill, 1983), the texture and structures bear imprints of environments during and after the deposition. In this study, the sedimentation pattern of lake sediments worked out with help of textural analyses is described as a case study of lake Agassiz, Canada (Gill & Teller, 1989) en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.subject Lake Sediment en_US
dc.title Lecture-13-Study of Lake Sediments and its Significance. en_US
dc.type Technical Report en_US


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