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HIV/AIDS in South Africa - Wikipedia
A comparison between communal and freeholdtenure systems in a similar area (approximately 15 000 ha) of the Peddiedistrict, Eastern Cape, South Africa.
The natural flora, comprising some 24 000 taxa, is one of therichest floras in the world and creates many opportunities for developing theecotourism industry. Regions of particular significance include Namaqualand,which attracts visitors to its unique floral displays during September of eachyear. The diverse Cape floral kingdom, with its estimated 8 000 taxa andassociated avifauna, also provides the visitor with a glimpse of uniqueevolutionary forces driving speciation in the region. The southern Cape and itsgarden route, with a high structural diversity (Afromontane forests,coastal thicket, lowland and mountain ), attractsmany international visitors.
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Tanser, F.C. & Palmer, A.R. 1999. The applicationof a remotely-sensed diversity index to monitor degradation patterns in a semi-arid, heterogeneous, South African landscape. 43(4): 477-484.
Grossman, D., Holden, P.L. & Collinson, R.F.H.1999. Veld management on the game ranch. N.M. Tainton (ed).Pietermaritzburg, South Africa:University of Natal Press.
South African Political Geography
The grassland resources of South Africa have been extensivelyreported, with four important publications appearing recently (Cowling,Richardson and Pierce, 1997; Dean and Milton 1999; Tainton, 1999, 2000). Theseprovide exhaustive information on types of range land resources; their generalecology, including history, biodiversity, species composition and associatedenvironmental conditions; dynamics; productivity; and land-use and managementoptions available to their peoples.
In addition, information applicable to the management ofgrasslands in southern Africa is provided in the approximately 980 researchpublications that have appeared since 1966 in the and its predecessors. Other peer-reviewed scientificjournals that provide exhaustive information on the natural resources of SouthAfrica include the and . Researchers are stronglyencouraged to publish in the wider international literature and many importantresearch articles appear in peer-reviewed journals published elsewhere. Thischapter does not attempt to synthesize or review all this available information,but provides a brief summary of the current status of our understanding ofsouthern African grassland ecosystems.
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Voyages - Trans-Atlantic Slave Trade Database
The Great Escarpment and the Drakensberg mountains provide thephysical barriers that largely determine the climate and vegetation of much ofthe livestock growing regions of South Africa. The combination of moderate tohigh rainfall and high elevation associated with these features means that thelargest area of native grasslands occurs here. In geological time, severalphases of uplifting, erosion and deposition have created complex landformsdetermined by the underlying geology. The country has five main physiographicalregions at differing elevations (Figure 3.3).
africa - Directory of Open Access Repositories
The grasslands (see Figure 3.2) adjoin a number of othereconomically important biomes (savannah, thicket and Nama-karoo) and grasslandpatches are found within these biomes. It is important to include these biomesin this chapter, as their ecology is strongly interlinked, and to consider therole that all grasslands and their associated biota play in the economy of SouthAfrica. In this chapter, grasslands in South Africa will have a wider definitionthan at the biome level.
Latest articles - SA Journal of Human Resource Management
South Africa is thus characterized by a high interior plateau,surrounded on three sides by the Great Escarpment and the Drakensberg mountains,which provide the physical barriers that largely determine the climate andvegetation. The plateau is intruded by several mountain massifs, with thehighlands of Lesotho exceeding 3 000 m in places. The northern and westernsections of the plateau contain two large basins, namely the Kalahari and theTransvaal Bushveldt (Partridge, 1997). Adjacent to the Great Escarpment lies acoastal plinth that varies in width from 50 to 200 km. This plinth is incised bydeep riverine gorges.
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The relatively young South Africa n geology gives rise tosoils of high nutrient status. The Nama-karoo biome of the central regionscomprise predominantly mudstones and sandstones of the Karoo Supergroup, whichgive rise to shallow (
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Hominids have occupied southern Africa for three million years(Volman, 1984), and although the ancestral forms used fire (Thackeray ., 1990), there are no artefacts that enable us to quantify the extent oftheir impact. They undoubtedly burnt large tracts of land in the interior,thereby promoting the development of grasslands, and early hominids must beregarded as a significant agent in the evolution of grasslands in SouthAfrica.
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