Dry season sediment fluxes in the frontwater zone of the mangrove-fridged Mwache Creek, Kenya

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dc.contributor.author Kitheka, Johnson U.
dc.date.accessioned 2015-01-26T09:17:11Z
dc.date.available 2015-01-26T09:17:11Z
dc.date.issued 2002
dc.identifier.citation Land Ocean Interactions Coastal Zone Reports and Studies No. 25, pp 194 - 202 en_US
dc.identifier.uri http://www.loicz.org/imperia/md/content/loicz/print/rsreports/report25.pdf
dc.identifier.uri http://hdl.handle.net/123456789/724
dc.description.abstract Mwache Creek is a typical mangrove creek along the Kenya coast. The creek receives terrigenous sediments on a seasonal basis and there is tremedous tidal influence. The supply of terrigenous sediments increases greatly during periods associated with major flood events. Most of the sediments supplied by the seasonal rivers are trapped in the upper parts of the creek with very little export to the lower frontwater zone of the creek. en_US
dc.language.iso en en_US
dc.title Dry season sediment fluxes in the frontwater zone of the mangrove-fridged Mwache Creek, Kenya en_US
dc.type Other en_US


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