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The Du Toitskloof Mountains (Dutoitsberge[2]) are a range in the Cape Fold Belt in the Western Cape Province of South Africa. The highest point is Du Toits Peak (Dutoitspiek[3]) (1,995 m or 6,545 ft) which is the highest seaward facing peak in the Cape Fold Belt ranges, i.e. the highest peak in the Western Cape within direct sight of the ocean.
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| Du Toits Peak | |
|---|---|
| Dutoitspiek | |
 Du Toitskloof Mountains from Du Toitskloof Pass | |
| Highest point | |
| Elevation | 1,995 m (6,545 ft)[1] |
| Prominence | 1,730 m (5,680 ft)[1] |
| Listing | Ultra List of mountains in South Africa |
| Coordinates | 33°45′18″S 19°11′12″E[1] |
| Geography | |
  Du Toits Peak Location in South Africa | |
| Location | Western Cape, South Africa |
| Parent range | Du Toitskloof Mountains |
Located between Paarl and Worcester in the south-west of South Africa, 70 kilometres (43 mi) to the north-east of the provincial capital of Cape Town, the mountains form a formidable barrier between Cape Town and the rest of Africa. The N1 highway, also called the Cape to Cairo Road crosses them at the Du Toitskloof Pass. The old route culminated at 820 metres (2,690 ft); however, the new Huguenot Tunnel, of 3.7 kilometres (2.3 mi) in length, cuts out the old mountain pass.[4] Sometimes the Du Toitskloof Mountains together with the Wemmershoek Mountains and others are called the Klein Drakenstein, but it is more usually considered part of the greater Boland mountain range.
Structurally, the mountains form part of the Cape Syntaxis, a complex portion of the Cape Fold Belt where the north-south trending ranges meet the east-west trending ranges in a complex series of folds and thrusts.[5] The range mostly consists of Table Mountain sandstone, an erosion-resistant quatzitic sandstone. Vegetation is almost exclusively montane fynbos of the Cape floristic region. The rest of the mountains are barren rocks and steep cliffs. Precipitation occurs primarily in the winter months as rain on the lower slopes and as snow higher up, usually above 1000m. Climate varies dramatically, with the surrounding valleys being up to 10°C (18°F) warmer than the mountains. The climate falls within the Mediterranean type.
The Limietberg Nature Reserve, known for its mountain fynbos, is located in the Du Toitskloof Mountains.[6]
See also
References
- Africa Ultra-Prominences Listed as "Dutoitspiek" Peaklist.org. Retrieved 2012-01-30.
- Dutoitsberge (Approved - N) at GEOnet Names Server, United States National Geospatial-Intelligence Agency
- Dutoitspiek (Approved - N) at GEOnet Names Server, United States National Geospatial-Intelligence Agency
- De Villiers, P. A. (1988). "History of the Du Toitskloof Pass and Tunnel". Civil Engineering = Siviele Ingenieurswese. 30 (4): 145–148.
- De Beer, C. H. (1990). "Simultaneous folding in the western and southern branches of the Cape Fold Belt". South African Journal of Geology. 93 (4): 583–591.
- "Limietberg Nature Reserve". CapeNature.
External links
- "Gliding Du Toits Kloof Adventure". South Africa's official tourism website. Retrieved 3 March 2010.
- "Du Toits Peak, South Africa" on Peakbagger
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На других языках
- [en] Du Toits Peak
[es] Pico Du Toits
El Pico Du Toits (1995m) ("Du Toits Peak ") es el pico más alto que da al mar de los montes del Cinturón de Pliegue del Cabo (Cape Fold Belt), i.e. el pico más alto en la Provincia Occidental del Cabo con una vista directa del océano. Situado entre Paarl y Worcester en el suroeste de Sudáfrica, 70 km el noreste de la capital provincial de Ciudad del Cabo. Las montañas constituyen una formidable barrera entre la Ciudad del Cabo y el resto de África. La cadena está compuesta en su mayoría de Arenisca de la Montaña de la Mesa, una arenisca cuarzítica resistente a la erosión. La vegetación es casi exclusivamente fynbos montano del Reino florístico del Cabo. El resto de las montañas son rocas yermas y acantilados escarpados. La precipitación ocurre primariamente en los meses de invierno como lluvia en las laderas bajas y nieve en las partes superiores, usualmente encima de los 1000m. El clima varía dramáticamente, con los valles circundantes siendo de hasta 10 °C más cálidos que las montañas. El clima cae dentro del tipo mediterráneo. Las montañas forman parte de la Sintaxis del Cabo, una porción compleja del Cinturón de Pliegue del Cabo donde los montes en dirección norte-sur se encuentran con los de orientación este-oeste en una serie compleja de pliegues, corrimientos y líneas de fallas.Другой контент может иметь иную лицензию. Перед использованием материалов сайта WikiSort.org внимательно изучите правила лицензирования конкретных элементов наполнения сайта.
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