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The Ventersdorp boulder beds of the Transvaal may possibly be of early palaeozoic age but as a total the palaeozoic time period in Africa was remarkably totally free from volcanic and igneous disturbances. Up to the near of the palaeozoic period of time the relative positions of the historical land masses and oceans keep on being unsolved but the absence of maritime strata of early palaeozoic age from Central Africa factors to there becoming land in this path. The breaking up of Gondwana Land is typically regarded as to have been prompted by a sequence of blocks of place remaining let down by faulting with the consequent formation of the Indian Ocean. In late Carboniferous occasions Africa and India were without doubt united to type a big continent, known as by Suess Gondwana Land. To the east it arrived at India. In Mozambique and in German East Africa, Cretaceous rocks lengthen from the coastline to a length inland of over 100 m.