A.E. MOORE, F.P.D (WOODY) COTTERILL, T. BRODERICK AND D. PLOWES 65 Landscape evolution in Zimbabwe from the Permian to present, with implications for kimberlite prospecting A.E. Moore Department of Geology, Rhodes University, Grahamstown. Somabula Explorations (Pvt.) Limited, Box CH399, Chisipite, Harare, Zimbabwe. e-mail:
[email protected] F.P.D. (Woody) Cotterill AEON - Africa Earth Observatory Network and Department of Geological Sciences, University of Cape Town, Rondebosch 7701, South Africa. e-mail:
[email protected] T. Broderick 19 Jenkinson Road, Chisipite, Harare, Zimbabwe e-mail:
[email protected] D. Plowes 49 Arcadia Road, Tigers Kloof, Mutare, Zimbabwe. e-mail:
[email protected] © 2009 March Geological Society of South Africa ABSTRACT Evidence is presented to model drainage evolution across Zimbabwe since the Permian. This provides the framework to understand the marked difference in character of the rivers to the north and south of the modern central Zimbabwe watershed, which separates the Zambezi and Limpopo drainage basins. North-flowing tributaries of the Zambezi rising off this river divide have low gradients and senile characteristics. The northwest orientation of the upper sections of many of these rivers is unusual for tributaries of a major east- flowing drainage, but is in accord with the west-orientated fluvial system that deposited the Triassic sediments of the Karoo Supergroup in the Cabora Bassa basin of the Zambezi Valley. The modern drainage system to the north of the central Zimbabwe watershed is thus largely controlled by a surface that has existed since pre-Karoo times. Headwaters of the Zambezi tributaries were originally located well to the south of the modern divide, with high ground extending to the present-day Chimanimani and Nyanga mountainland in eastern Zimbabwe.