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Sources of Conflict in Southern Africa, c. 1800–30: The ‘Mfecane’ Reconsidered*
Published online by Cambridge University Press: 22 January 2009
Extract
The so-called ‘mfecane’ has been explained in many ways by historians, but never adequately. Julian Cobbing has absolved the Zulu of culpability for ongoing regional conflicts, but his work is severely flawed in its use of evidence. Cobbing is incorrect to argue that the Delagoa Bay slave trade existed on a large scale prior to the disruptions beginning in 1817, and European slaving therefore cannot have been a root cause of political turmoil and change, as he claims. Cobbing correctly identifies European-sponsored slave-raiding as a major cause of violence across the north-eastern Cape Frontier, but his accusations of missionary involvement are false. Jeff Guy's interpretation of the rise of the Zulu kingdom based on environmental factors is inadequate because he examined only stock-keeping and not arable land use, which led him to false conclusions about demography and politics. In this paper I argue that the socio-political changes and associated demographic turmoil and violence of the early nineteenth century in southern Africa were the result of a complex interaction between factors governed by the physical environment and local patterns of economic and political organization. Increasing inequalities within and between societies coupled with a series of environmental crises transformed long-standing competition over natural resources and trade in south-eastern Africa into violent struggles.
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References
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115 The Nguni had the capacity to store large quantities of food for up to seven years in order to prevent famine in times of drought. Contrary to what Hall states, both grain pits and grain baskets were used by the Nguni for storing huge quantities of grain, and although some would always be lost to rot and pests, the incentives for storing grain to avoid famine were very great in the nineteenth century. Hall, ‘Dendroclimatology’.
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