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The Cape Fold Belt is a fold and thrust belt of late Paleozoic age, which affected the sequence of sedimentary rock layers of the Cape Supergroup in the southwestern corner of South Africa. [1] It was originally continuous with the Ventana Mountains near Bahía Blanca in Argentina , the Pensacola Mountains (East Antarctica), the Ellsworth ...
Matroosberg (Afrikaans for 'Sailor Mountain') is a peak in the South African Hex River Mountains, which belong to the Cape Fold Belt. With a height of 2,247 m (7,372 ft) [3] above sea level, it is the highest mountain in the Cape Winelands District Municipality. The mountain is located in the Witzenberg Local Municipality in the Western Cape.
Eastern Cape: Part of the Cape Fold Belt system Langeberg: Long Mountains: Western Cape: 2,075 m (6,808 ft) Part of the Cape Fold Belt system Langkloof Mountains: Long Valley/Gap Mountains: Western Cape: Part of the Cape Fold Belt system Lebombo Mountains: Big nose (in Zulu) from KwaZulu-Natal to Limpopo: Magaliesberg: Mogale's Mountain: North ...
Table Mountain is the northernmost end of a 50-kilometre-long (30 mi) and roughly six-to-ten-kilometre-wide (4 to 6 mi) Cape Fold Mountain range that forms the backbone of the Cape Peninsula, stretching from the Cape of Good Hope in the south to Table Mountain and its flanking Devil's Peak (to the east) and Lion's Head and Signal Hill (to the ...
The formation of the Cape Fold Belt is the result of a collision of tectonic plates that ended over 200 million years ago The accumulated strata of the Cape Supergroup and the older granites and Malmesbury group were raised and deformed by the pressure of the South American, Antarctic and African continental plates slowly moving together. The ...
The Drakenstein mountain is a mountain range in the Western Cape province of South Africa. It lies opposite Simonsberg Mountain and is part of the Cape Fold Belt. It is named after ex-soldier Hendrik Adriaan van Rheede tot Drakenstein, who was Colonial administrator of the Dutch East India Company.
The Cape orogeny formed the Cape Fold Belt and the mountains that range along the Cape and the southern parts of South Africa. [3] An additional geological formation, the Msikaba Formation, found north of Port St. Johns in the Eastern Cape is considered to correlate with the Witteberg Group of the Cape Supergroup. [4]
The Kaapvaal Craton covers an area of approximately 1,200,000 km 2 (460,000 sq mi) and is joined to the Zimbabwe Craton to the north by the Limpopo Belt.To the south and west, the Kaapvaal Craton is flanked by Proterozoic orogens, and to the east by the Lebombo monocline that contains Jurassic igneous rocks associated with the break-up of Gondwana.