Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/38259
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dc.contributor.authorSundaresan, J-
dc.date.accessioned2016-12-07T10:32:34Z-
dc.date.available2016-12-07T10:32:34Z-
dc.date.issued1991-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/38259-
dc.description127-129en_US
dc.description.abstractSediment texture in the Cochin harbour shows fine sediment in the inner channels and coarse fraction in the approach channel. In the inner channels the sediment transport is mostly by suspension, while it is due to graded suspension and saltation in the approach channel. The sediment size indicates that maximum deposition occurs during premonsoon (February-May). The littoral transport plays a major role in the sedimentation in the Cochin harbour.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.20(2) [June 1991]en_US
dc.titleTextural distribution of surficial sediments of the Cochin harboren_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.20(2) [June 1991]

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