The Characteristics, Classification and Land Use Significance of Swell-Shrink Soils East of Lake Victoria, Kenya

dc.contributor.authorGatahi, M.M.
dc.contributor.authorGachene, C.K.K.
dc.contributor.corpauthorKenya Soil Survey
dc.date.accessioned2015-09-22T11:43:03Z
dc.date.available2015-09-22T11:43:03Z
dc.date.issued1988en
dc.description.abstractThe eastern gulf shores of Lake Victoria is an old lacustrine valley of Pleistocene period which has since been filled with alluvial and colluvial sediments derived from the surrounding volcanic hills and scaps to form a major plain. This plain slopes very gently into the lake. It is surrounded by Nandi Escarpment to the north Nyabando Escarpment to the south and volcanic hills to the east and North West.en
dc.format.pages6en
dc.identifier.citationGatahi, M. M., Gachene, C. K. K. (1988). The Characteristics, Classification and Land Use Significance of Swell-Shrink Soils East of Lake Victoria, Kenya. p.5
dc.identifier.urihttp://kalroerepository.kalro.org/handle/0/13303
dc.language.isoenen
dc.publisherKenya Soil Surveyen
dc.publisher.placeNairobien
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/en
dc.subject.agrovocAlluvial soilsen
dc.subject.agrovocTopographyen
dc.subject.agrovocCropsen
dc.subject.agrovocIrrigationen
dc.titleThe Characteristics, Classification and Land Use Significance of Swell-Shrink Soils East of Lake Victoria, Kenyaen
dc.typeBook*
dc.type.refereedRefereeden
dc.type.specifiedArticleen

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