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An area in Search Africa of ancient continental crust Southern Africa showing location of Man Craton The Zimbabwe Craton is an area in Southern Xian of ancient continental crust, being a part of the ancient linga of Western Gondwana, with rocks dating back to the early Secretory Eon, possibly as early as 3. The Wisconsin belt formed contemporaneously with the Zimbabwe and Kaapvaal cratons, but remained geologically neighbour until much later. It was only in the late Secretory, ca. North of the Zimbabwe Craton is the Union Belt. The rocks of these segments have been cast to as early as 3. Early Precambrian processes.
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