The geological evolution of the northern Kamasia Hills Baringo District, Kenya
The Kamasia Hills are formed essentially by a line of 'en echelon' tilted blocks within the main rift valley in northern Kenya. The metamorphic basement crops out locally at the foot of the eastern fault-scarps of the range and is overlain by the thickest sequence of the late Miocene plate...
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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.704175 |