Features
The main feature of
The highest point on
The cliffs of the main plateau are split by Platteklip Gorge ("Flat Stone Gorge"), which provides an easy and direct ascent to the summit and was the route taken by Antonio de Saldanha on the first recorded ascent of the mountain in 1503.
The flat top of the mountain is often covered by clouds/mist/fog spilling over the top to form the "table cloth".
Geology
The upper part of the mountain mesa consists of Ordovician quartzitic sandstone, commonly referred to as Table Mountain Sandstone (TMS), which is highly resistant to erosion and forms characteristic steep grey crags. Below the sandstone is a layer of micaceous basal shale, which weathers quite readily and is therefore not readily visible. The basement consists of heavily folded and altered late precambrian Malmesbury shale, which has been intruded by
Flora
The main vegetation of the mountain is the unique and rich
Fauna
The most common animal on the mountain is the dassie, or rock hyrax. They especially cluster around the upper cable station, near areas where tourists may discard or (illegally) supply food. There are also porcupines, mongooses, snakes and tortoises. The last lion in the area was shot circa 1802. Leopards persisted on the mountain until perhaps the 1920s but are now extinct locally. Two smaller, secretive, nocturnal carnivores, the rooikat (caracal) and the vaalboskat (also called the vaalkat or African Wild Cat) were once common on the mountain. The rooikat continues to be seen on rare occasions by mountaineers but the status of the vaalboskat is uncertain.
Himalayan tahrs, fugitive descendants of tahrs that escaped from Groote Schuur zoo in 1936, used to be common on the less accessible upper parts of the mountain. As an exotic species, they were almost eradicated through a culling programme initiated by the South African National Parks to make way for the reintroduction of indigenous klipspringers. Until recently there were also small numbers of fallow deer of European origin and sambar deer from southeast Asia. These were mainly in the Rhodes Memorial area but during the 1960s they could be found as far afield as Signal Hill. The animals may by now have been eliminated or relocated.
History
The original name given to the mountain by the first Khoi inhabitants was Hoeri 'kwaggo ("sea mountain").
Prehistoric people first left evidence here more than 600,000 years ago. Evidence tools of these Early Stone Age hunter-gatherers were found in a depression near the
San (or Bushmen) hunter-gatherers relied on the seashore for most of their food. This resulted in the Dutch naming, Strandlopers (beach combers). About 2000 years ago the Khoikhoi migrated from the north, displacing the San, bringing with them their herds of cattle and sheep. It was the Khoikhoi who were the dominant tribe when the Europeans sailed into
Antonio de Saldanha was the first European to land in
Between 1896 and 1907, five dams, the Woodhead, Hely-Hutchinson, De Villiers,
The mountain became part of the new
Fires are common on the mountain. The most recent major fire came in January 2006, destroying large amounts of vegetation and resulting in the death of a tourist. A charge of arson and culpable homicide was laid against a British man who was suspected of starting the blaze.
credited to wikipedia and flickr:der~Jens,Reisezeitland,joachimhim,Dennis de Grauw


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