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Chapter 1 - High Africa: Eroding Surfaces

from Part I - The Physical Cradle: Land Forms, Geology, Climate, Hydrology and Soils

Published online by Cambridge University Press:  09 September 2021

Norman Owen-Smith
Affiliation:
University of the Witwatersrand, Johannesburg
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Summary

This chapter establishes how mantle plumes elevated the interior of eastern and southern Africa and generated predominantly eroding land surfaces. Depositional basins were restricted mainly to the Congo, Kalahari, interior South Africa and offshore. It outlines the origins of the African rift valley and its propagation southward. This sets the tectonic context for climates, river flow, geological substrates, volcanism and soil fertility.

Type
Chapter
Information
Only in Africa
The Ecology of Human Evolution
, pp. 5 - 13
Publisher: Cambridge University Press
Print publication year: 2021

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References

Suggested Further Reading

Burke, K; Gunnell, Y. (2008) The African erosion surface: a continental-scale synthesis of geomorphology, tectonics, and environmental change over the past 180 million years. Geological Society of America Memoirs 201:166.Google Scholar
Macgregor, D. (2015) History of the development of the East African Rift System: a series of interpreted maps through time. Journal of African Earth Sciences 101:232252.CrossRefGoogle Scholar

References

Partridge, TC. (2010) Tectonics and geomorphology of Africa during the Phanerozoic. In Werdelin, L; Sanders, WJ (eds) Cenozoic Mammals of Africa. University of California Press, Berkeley, pp. 317.CrossRefGoogle Scholar
Burke, K; Gunnell, Y. (2008) The African erosion surface: a continental-scale synthesis of geomorphology, tectonics, and environmental change over the past 180 million years. Geological Society of America Memoirs 201:166.Google Scholar
Mathu, EM; Davies, TC. (1996) Geology and the environment in Kenya. Journal of African Earth Sciences 23:511539.Google Scholar

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