Book contents
- Quaternary Environmental Change in Southern AfricaPhysical and Human Dimensions
- Quaternary Environmental Change in Southern Africa
- Copyright page
- Contents
- Contributors
- 1 The context of Quaternary environmental change in southern Africa
- 2 A brief geological history of southern Africa
- 3 A continental-scale perspective on landscape evolution in southern Africa during the Cenozoic
- 4 Hominin origins and evolution during the Neogene
- 5 Hominin evolution in Africa during the Quaternary
- 6 Quaternary environmental change on the southern African coastal plain
- 7 Dating the southern African landscape
- 8 Glacial and periglacial geomorphology
- 9 Colluvial deposits and slope instability
- 10 Desert dune environments
- 11 Changes in fluvial systems during the Quaternary
- 12 Wetlands in southern Africa
- 13 Sandy coasts
- 14 Environmental change during the Pleistocene and Holocene: Estuaries and lagoons of southern Africa
- 15 Soils and duricrusts
- 16 Karstic systems
- 17 Terrestrial ecosystem changes in the late Quaternary
- 18 Faunal evidence for mid- and late Quaternary environmental change in southern Africa
- 19 Pollen, charcoal and plant macrofossil evidence of Neogene and Quaternary environments in southern Africa
- 20 Minerogenic microfossil records of Quaternary environmental change in southern Africa
- 21 Development of the archaeological record in southern Africa during the Earlier Stone Age
- 22 Development of the archaeological record during the Middle Stone Age of South Africa
- 23 Later Stone Age hunter-gatherers and herders
- 24 Southernmost Africans, archaeology and the environment during the Holocene
- 25 Landscape–climate–human relations in the Quaternary of southern Africa
- Index
- References
13 - Sandy coasts
Published online by Cambridge University Press: 05 June 2016
- Quaternary Environmental Change in Southern AfricaPhysical and Human Dimensions
- Quaternary Environmental Change in Southern Africa
- Copyright page
- Contents
- Contributors
- 1 The context of Quaternary environmental change in southern Africa
- 2 A brief geological history of southern Africa
- 3 A continental-scale perspective on landscape evolution in southern Africa during the Cenozoic
- 4 Hominin origins and evolution during the Neogene
- 5 Hominin evolution in Africa during the Quaternary
- 6 Quaternary environmental change on the southern African coastal plain
- 7 Dating the southern African landscape
- 8 Glacial and periglacial geomorphology
- 9 Colluvial deposits and slope instability
- 10 Desert dune environments
- 11 Changes in fluvial systems during the Quaternary
- 12 Wetlands in southern Africa
- 13 Sandy coasts
- 14 Environmental change during the Pleistocene and Holocene: Estuaries and lagoons of southern Africa
- 15 Soils and duricrusts
- 16 Karstic systems
- 17 Terrestrial ecosystem changes in the late Quaternary
- 18 Faunal evidence for mid- and late Quaternary environmental change in southern Africa
- 19 Pollen, charcoal and plant macrofossil evidence of Neogene and Quaternary environments in southern Africa
- 20 Minerogenic microfossil records of Quaternary environmental change in southern Africa
- 21 Development of the archaeological record in southern Africa during the Earlier Stone Age
- 22 Development of the archaeological record during the Middle Stone Age of South Africa
- 23 Later Stone Age hunter-gatherers and herders
- 24 Southernmost Africans, archaeology and the environment during the Holocene
- 25 Landscape–climate–human relations in the Quaternary of southern Africa
- Index
- References
Summary
The South African coastline is variable in geomorphic character, but at least two thirds of the coastline is dominated by sandy and part-lithified sandy intertidal shorelines. Part-lithified sandy intertidal shorelines consist of a mosaic of rocky outcrops on dominantly sandy beaches. The rocks on these mixed shores are generally composed of cemented Quaternary deposits. Carbonate cemented Quaternary aeolianite/beachrock complexes are relatively common along the South African coastline and on the continental shelf, where they form prominent reefs. The Quaternary deposits along the coastline are characterised mainly by transgressive dune cordons. These systems record sensitive palaeoenvironmental fluctuations, as archived in their structure, diagenetic history, and relationship to past sea-levels and ancient shorelines.
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- Quaternary Environmental Change in Southern AfricaPhysical and Human Dimensions, pp. 203 - 218Publisher: Cambridge University PressPrint publication year: 2016