Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/39174
Full metadata record
DC FieldValueLanguage
dc.contributor.authorVora, K H-
dc.contributor.authorGujar, A R-
dc.contributor.authorKarisiddaiah, S M-
dc.date.accessioned2016-12-26T06:36:11Z-
dc.date.available2016-12-26T06:36:11Z-
dc.date.issued1980-06-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/39174-
dc.description90-93en_US
dc.description.abstractIn the Gulf of Khambhat (Gujarat, India) the best formed sandwaves are seen in the west close to the Eastern Sand Bank. With increasing clay content and clay cover of the sea bed, the sandwaves become poorly formed. In the southern part of the Gulf the sandwaves are nearly symmetrical <2 m height and 100-200 m wavelength. In the northern part of Gulf the sandwaves are asymmetrical, 3-4 m high and 300-400 m wavelength. The sediments in the crest are finer than those in the troughs. The extensive development of the sandwaves in the Gulf is related to the abundant coarse sediment from the rivers Narmada and Tapti. High energy hydrodynamic conditions primarily, due to large tidal range in the funnel shaped Gulf appear to be responsible for the formation of these sandwaves.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.09(2) [June 1980]en_US
dc.titleSandwaves of the Gulf of Khambhaten_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.09(2) [June 1980]

Files in This Item:
File Description SizeFormat 
IJMS 9(2) 90-93.pdf1.24 MBAdobe PDFView/Open


Items in NOPR are protected by copyright, with all rights reserved, unless otherwise indicated.