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...
| Main Author: | |
|---|---|
| Published: |
Royal Holloway, University of London
1971
|
| Subjects: | |
| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.704175 |