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Bushveld
Bushveld in the Waterberg Biosphere
Bushveld in the Waterberg Biosphere
Higher altitude bushveld near Mookgophong, Limpopo
Higher altitude bushveld near Mookgophong, Limpopo
Low altitude bushveld in the Limpopo valley
Low altitude bushveld in the Limpopo valley
Flora and Fauna
Flora and Fauna
The Southern African Central Plateau edged by the Great Escarpment.
The Southern African Central Plateau edged by the Great Escarpment.
Panorama of the Giant's Castle region of the Drakensberg, the highest section of the Great Escarpment. Here the Escarpment is capped by a 1,400 m laye
Panorama of the Giant's Castle region of the Drakensberg, the highest section of the Great Escarpment. Here the Escarpment is capped by a 1,400 m layer of erosion-resistant lava, which once covered most of Southern Africa 182 million years ago. Only a small remnant of this lava layer remains on the plateau, covering only part of Lesotho, and accounting for the Great Escarpment's great height on the Lesotho/KwaZulu-Natal border.
An approximate SW-NE cross section through South Africa with the Cape Peninsula (with Table Mountain) on left, and north-eastern KwaZulu-Natal on the
An approximate SW-NE cross section through South Africa with the Cape Peninsula (with Table Mountain) on left, and north-eastern KwaZulu-Natal on the right. Diagrammatic and only roughly to scale. It shows the major geological structures (coloured layers) that dominate the southern and eastern parts of the country, as well as the relationship between the Central Plateau, the Cape Fold Mountains, and the Drakensberg escarpment.
A diagrammatic 400 km north–south cross-section through the southern portion of the country near Calitzdorp in the Little Karoo (approximately 21° 30'
A diagrammatic 400 km north–south cross-section through the southern portion of the country near Calitzdorp in the Little Karoo (approximately 21° 30' E), showing the relationship between the Cape Fold Mountains (and their geological structure) and the geology of the Little and Great Karoo, as well as the position of the Great Escarpment. The colour code for the geological layers is the same as those used in the diagram on the left. The heavy black line flanked by opposing arrows is the fault that runs for nearly 300