The geology of the Tiati Hills, Rift Valley Province, Kenya
The area lies between the Kerio and Suguta Rivers in southern Turkana. Metamorphic basement rocks are exposed along the axis of an anticlinal arch which is overlain by a succession of volcanics and associated sediments, up to 2,000 ft. (610 m.) in thickness west of it, and up to 11,000 ft. (3,400 m....
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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.704166 |