The geology of the Ribkwo area, Baringo district, Kenya
The Ribkwo area is divided into two contrasting east and west parts by the Kito Pass fault system, This has upfaulted the area to the west of the Chepanda Hills and Sigatgat Hill exposing 6,000 to 7,000 feet of phonolite and tuffaceous sediments with subordinate basaltic lavas (the Tugen Hills Group...
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Royal Holloway, University of London
1971
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.307548 |