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

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