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dc.contributor.authorRajamanickam, G.V.
dc.contributor.authorVethamony, P.
dc.contributor.authorGujar, A.R.
dc.date.accessioned1995-06-17T10:01:22Z
dc.date.accessioned2017-09-29T13:48:18Z
dc.date.available1995-06-17T10:01:22Z
dc.date.available2017-09-29T13:48:18Z
dc.date.issued1986
dc.identifier.citationProceedings of the Indian Academy of Sciences (Earth and Planetary Sciences), vol.95; 1986; 237-244
dc.identifier.issn0253-4126
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/6190
dc.description.abstractFrom the wave refraction diagrams it is delineated that the Jaigad Head and Warori Bluff are the zones of wave energy convergence and the Narvan and Ambwah bays the areas of wave energy divergence. The presence of two distinct mineral phases noticed at the Jaigad, Ambwah and Varvade bays shows that there are two different circulations of sediment movements. The presence of natural barriers restricts the movement of sediment along the coast. The sand bar at the mouth of the Jaigad Bay has different orientations during the monsoon and non-monsoon periods causing obstruction to navigation during the former period
dc.languageen
dc.publisherIndian Academy of Sciences, Bangalore
dc.relation.ispartofP Indian As-Earth
dc.relation.isreferencedbySCI
dc.subjectGeology and Geophysics
dc.subject.othernearshore bars
dc.subject.othersand
dc.subject.othersediment movement
dc.subject.othercoastal erosion
dc.subject.othersediments
dc.subject.otherISW, India, West Coast
dc.titleEffect of waves in the redistribution of sediments along the Konkan coast
dc.typeJournal Article


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