Cape Peninsula

The Cape Peninsula (Afrikaans: Kaapse Skiereiland) is a generally rocky peninsula that juts out into the Atlantic Ocean at the south-western extremity of the African continent. At the southern end of the peninsula are Cape Point and the Cape of Good Hope. On the northern end is Table Mountain, overlooking Cape Town, South Africa. The peninsula is 52 km long from Mouille point in the north to Cape Point in the south.[1]

Benguela and Agulhas Currents 2
The courses of the warm Agulhas current (red) along the east coast of South Africa, and the cold Benguela current (blue) along the west coast. Note that the Benguela current does not originate from Antarctic waters in the South Atlantic Ocean, but from upwelling of water from the cold depths of the Atlantic Ocean against the west coast of the continent. The two currents do not "meet" anywhere along the south coast of Africa.

The Peninsula has been an island on and off for the past 5 million years, as sea levels fell and rose with the ice age and interglacial global warming cycles of, particularly, the Pleistocene.[2] The last time that the Peninsula was an island was about 1.5 million years ago.[2] Soon afterwards it was joined to the mainland by the emergence from the sea of the sandy area now known as the Cape Flats. The towns and villages of the Cape Peninsula and Cape Flats now form part of the City of Cape Town Metropolitan Municipality.

The Cape of Good Hope is sometimes misquoted as the meeting point of the Atlantic and Indian Oceans. However, according to the International Hydrographic Organization agreement that defines the ocean boundaries, the meeting point is at Cape Agulhas, about 200 km (120 mi) to the southeast.[3][4] The west coast of the Peninsula is referred to as the "Atlantic Coast", "Atlantic Seaboard" or west coast,[5] but the eastern side is generally known as the "False Bay Coast".

Similarly, Cape Point is not the fixed "meeting point" of the cold Benguela Current, running northwards along the west coast of Africa, and the warm Agulhas Current, running south from the equator along the east coast of Africa. In fact the south flowing Agulhas Current swings away from the African coastline between about East London and Port Elizabeth, from where it follows the edge of the Continental shelf roughly as far as the southern tip of the Agulhas Bank, 250 km (155 miles) south of Cape Agulhas.[6] From there it is retroflexed (turned sharply round) in an easterly direction by the South Atlantic, South Indian and Southern Ocean currents, known as the "West Wind Drift", which flow eastwards round Antarctica. The Benguela Current, on the other hand, is an upwelling current which brings cold, mineral-rich water from the depths of the Atlantic Ocean to the surface along the west coast of Southern Africa. Having reached the surface it flows northwards as a result of the prevailing wind and Coriolis forces. The Benguela Current, therefore, effectively starts at Cape Point, and flows northwards from there,[6][7] although further out to sea it is joined by surface water that has crossed the South Atlantic from South America as part of the South Atlantic Gyre.[7] Thus the Benguela and Agulhas currents do not strictly "meet" anywhere, although eddies from the Agulhas current do from time to time round the Cape to join the Benguela Current.[6][7]

Cape of Good Hope (Zaian 2008)
The Cape of Good Hope; looking towards the west, from the coastal cliffs above Cape Point.
Cape Peninsula
Map showing the Cape Peninsula, illustrating the positions of the Cape Town City Centre, Table Mountain, the main mountains and peaks that make up the Peninsula, and the Cape of Good Hope.

Ecology

Table Mountain National Park, previously known as the Cape Peninsula National Park, was proclaimed on 29 May 1998, for the purpose of protecting the natural environment of the Table Mountain Chain, and in particular the rare fynbos vegetation. The park comprises a large part of the undeveloped area of the Cape Peninsula, and is managed by South African National Parks Board. The coastal waters surrounding the Cape Peninsula were proclaimed as a marine protected area in 2004, include several no-take zones, and are part of the national park. The waters of this marine protected area are unusual in that they are parts of two fairly distinct marine bioregions, namely the Agulhas bioregion and the South-western Cape bioregion. The boundary is at Cape Point.

Flora

Peninsula Sandstone Fynbos - Table Mountain Cape Town 4
A king protea growing in Peninsula Sandstone Fynbos on Table Mountain
4 Silvertrees on Lions Head - Cape Town
Silver trees (Leucadendron argenteum) only occur naturally on the granite and clay soils of the Cape Peninsula, surrounding Table Mountain and the Back Table.[8][9] A few tiny patches, possibly planted there by early European settlers, occur near Stellenbosch, Paarl and Somerset West.[8] This photo was taken on Lion's Head, looking towards the Twelve Apostles.
RedDisa
The Disa uniflora, also known as the Pride of Table Mountain is a showy orchid that blooms under waterfalls, along streamlets and seeps on the top and upper slopes of Table Mountain and the Back Table, in January–March.[10]
5 Indigenous Afrotemperate Forest on Devils Peak - Cape Town
Indigenous forest on Table Mountain, with Devil's Peak visible in the distance

The Cape Peninsula has an unusually rich biodiversity. Its vegetation consists predominantly of several different types of the unique and rich Cape Fynbos. The main vegetation type is endangered Peninsula Sandstone Fynbos, but critically endangered Peninsula Granite Fynbos, Peninsula Shale Renosterveld and Afromontane forest occur in smaller portions on the mountain ranges of the Peninsula. On the sandy Cape Flats lowlands there are a few pockets of protected Cape Flats Sand Fynbos.

The Peninsula's vegetation types form part of the Cape Floral Region protected areas. These protected areas are a World Heritage Site, and an estimated 2,200 species of plants are confined to Table Mountain range - which are at least as many as occur in the whole of the United Kingdom.[11][12] Many of these species, including a great many types of proteas, are endemic to these mountains and can be found nowhere else. The Disa uniflora, despite its restricted range within the Western Cape, is relatively common in the perennially wet areas (waterfalls, streamlets and seeps) on Table Mountain and the Back Table, but hardly anywhere else on the Cape Peninsula.[10][13] It is a very showy orchid that blooms from January to March on the Table Mountain Sandstone regions of the mountain. Although they are quite widespread on the Back Table, the best (most certain, and close-up) place to view these beautiful blooms is in the "Aqueduct" off the Smuts Track, halfway between Skeleton Gorge and Maclear's Beacon.

Remnant patches of indigenous forest persist in the wetter ravines. However, much of the indigenous forest was felled by the early European settlers for fuel for the lime kilns needed during the construction of the Castle.[14] The exact extent of the original forests is unknown, though most of it was probably along the eastern slopes of Devil's Peak, Table Mountain and the Back Table where names such as Rondebosch, Kirstenbosch, Klaassenbosch and Witteboomen survive (in Dutch "bosch" means forest; and "boomen" means trees) . Hout Bay (in Dutch "hout" means wood) was another source of timber and fuel as the name suggests.[14] In the early 1900s commercial pine plantations were planted on these slopes all the way from the Constantiaberg to the front of Devil’s Peak, and even on top of the mountains, but these have now been largely cleared allowing fynbos to flourish in the regions where the indigenous Afromontane forests have not survived, or never existed.

Fynbos is a fire adapted vegetation, and evidence suggests that in the absence of regular fires all but the drier fynbos would become dominated by trees.[11][15] Regular fires have dominated fynbos for at least the past 12 000 years largely as a result of human activity.[12][16] In 1495 Vasco da Gama named the South African coastline Terra de Fume because of the smoke he saw from numerous fires.[15] This was originally probably to maintain a productive stock of edible bulbs (especially watsonians)[15] and to facilitate hunting, and later, after the arrival of pastoralists,[17] to provide fresh grazing after the rains.[15][16] Thus the plants that make up fynbos today are those that have been subjected to a variety of fire regimes over a very long period time, and their preservation now requires regular burning. The frequency of the fires obviously determines precisely which mix of plants will dominate any particular region,[18] but intervals of 10–15 years between fires[11] are considered to promote the proliferation of the larger Protea species, a rare local colony of which, the Aulax umbellata (Family: Proteaceae), was wiped out on the Peninsula by more frequent fires,[18] as have been the silky-haired pincushion, Leucospermum vestitum, the red sugarbush, Protea grandiceps and Burchell's sugarbush, Protea burchellii, although a stand of a dozen or so plants has recently been "rediscovered" in the saddle between Table Mountain and Devil's Peak.[15] Some bulbs may similarly have become extinct as a result of a too rapid sequence of fires.[18] The fires that occur on the mountains today are still largely due to unregulated human activity. Fire frequency is therefore a matter of chance rather than conservation.

Despite intensive conservation efforts the Table Mountain range has the highest concentration of threatened species of any continental area of equivalent size in the world.[11][19] The non-urban areas of the Cape Peninsula (mainly on the mountains and mountain slopes) have suffered particularly under a massive onslaught of invasive alien plants for well over a century, with perhaps the worst invader being the cluster pine, partly because it was planted in extensive commercial plantations along the eastern slopes of the mountains, north of Muizenberg. Considerable efforts have been made to control the rapid spread of these invasive alien trees. Other invasive plants include black wattle, blackwood, Port Jackson and rooikrans (All Australian members of the acacia family), as well as several Hakea species and bramble.[11][18][20]

Dassie 2
The Cape hyrax or "dassie" as it is known in South Africa. It is the Verreaux's eagle's favourite and almost exclusive prey on the Cape Peninsula.

Fauna

The most common mammal on the mountain was the dassie (the South African name, from Afrikaans, pronounced "dussy"), or rock hyrax. Between about 2000 and 2004 (no one is certain about the exact year or years) their numbers suddenly plummeted for unknown reasons. They used to cluster around the restaurant at the upper cable station, near areas where tourists discarded or (inadvisably supplied) food. The population crash of the dassies was in all probability responsible for the decline in the Verreaux's eagle population on the Peninsula, which is believed to have consisted of 3 breeding pairs during the period 1950 to 1990, with only 2 pairs, maximally, ever having been reported to fledge a chick each in any given year.[21] With the commencement of formal monitoring in 1993, two breeding pairs were recorded on the Cape Peninsula Mountain Chain in 2004: one below the upper cable station at the western end of Table Mountain, in Blinkwater Ravine, the other on the cliffs below Noordhoek Peak.[22] The nest near the cable station was abandoned in 2006, leaving only the Noordhoek pair, which continued to fledge chicks reasonably regularly till 2013, at which point one member of the pair disappeared. From 2013 till January 2017 only a single Verreaux's Eagle, presumed to be a female, remained on the Peninsula. She continued to maintain the nest under Noordhoek Peak, but seemed unable to attract a mate. But in early 2017 a pair of eagles was seen by at least 7 independent observers during the course of 10 days (27 January - 5 February). It remains to be seen whether they will breed later in the year. Dassies are an important part the Verreaux's eagle's prey on the Peninsula.[23] (See Foot note[nb 1])

Table Mountain is also home to porcupines, mongooses, snakes, lizards, tortoises, and a rare endemic species of amphibian that is only found on Table Mountain, the Table Mountain ghost frog. The last lion in the area was shot circa 1802. Leopards persisted on the mountains 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 Southern African wildcat) were once common in the mountains and the mountain slopes. The rooikat continues to be seen on rare occasions by mountaineers but the status of the vaalboskat is uncertain. The mountain cliffs are home to several raptors species, apart from the Verreaux's eagle. They include the jackal buzzard, booted eagle (in summer), African harrier-hawk, peregrine falcon and the rock kestrel.[23][24] In 2014 three pairs of African fish eagles were believed to be breeding on the Peninsula, but they nest in trees generally as far away from human habitation as is possible on the Peninsula. Their number in 2017 is unknown.

Up until the late 1990s baboons occurred on all the mountains of the Peninsula, including the Back Table immediately behind Table Mountain. Since then they have abandoned Table Mountain and the Back Table, and only occur on the Constantiaberg, and the mountains to the south. They have also abandoned the tops of many of the mountains, in favour of the lower slopes, particularly when these were covered in pine plantations which seemed to provide them with more, or higher quality food than the fynbos on the mountain tops. However these new haunts are also within easy reach of Cape Town's suburbs, which brings them into conflict with humans and dogs, and the risk of traffic accidents. In 2014 there were a dozen troops on the Peninsula, varying in size from 7 to over 100 individuals, scattered on the mountains from the Constantiaberg to Cape Point.[25][26] The baboon troops are the subject of intense research into their movements (both of individuals and of the troops), their physiology, genetics, social interactions and habits. In addition, their sleeping sites are noted each evening, so that monitors armed with paint ball guns can stay with the troop all day, to ward them off from wandering into the suburbs. From when this initiative was started in 2009 the number of baboons on the Peninsula has increased from 350 to 450, and the number of baboons killed or injured by residents has decreased.[26]

Rau Quagga on Devils Peak
Rau quagga in the animal camp on the slopes of Devil's Peak, above Groote Schuur Hospital.

Himalayan tahrs, fugitive descendants of tahrs that escaped from Groote Schuur Zoo near the University of Cape Town, 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. These animals may still be seen occasionally despite efforts to eliminate or relocate them.

On the lower slopes of Devil's Peak, above Groote Schuur Hospital, an animal camp bequeathed to the City of Cape Town by Cecil John Rhodes has been used in recent years as part of the Quagga Project.[27] The quaggas used to roam the Cape Peninsula, the Karoo and the Free State in large numbers, but were hunted to extinction during the early 1800s. The last quagga died in an Amsterdam zoo in 1883. In 1987 a project was launched by Reinhold Rau to back-breed the quagga, after it had been established, using mitochondrial DNA obtained from museum specimens, that the quagga was closely related to the plains zebra, and on 20 January 2005 a foal considered to be the first quagga-like individual because of a visible reduced striping was born. These quagga-like zebras are officially known as Rau quaggas, as no one can be certain that they are anything more than quagga look-alikes. The animal camp above Groote Schuur Hospital has several good looking Rau quaggas, but they are unfortunately not easily seen except from within the game camp, which is quite large and undulating, and the animals are few. The animal camp is not open to the public.

Geology

Geology of Cape Peninsula 1
Geology of the Cape Peninsula, showing where the Malmesbury Group and Cape Granite rocks and weathered soils are exposed, and overlain by the Cape Supergroup. The hard, erosion resistant Cape Supergroup form the mountains of the Peninsula.
West-East cross section through Cape Peninsula
Schematic West-East geological cross section through the Cape Peninsula to illustrate its general structure. It closely resembles a W–E section through the Back Table, immediately south of Table Mountain, but is not to scale. The height of the "plateau" varies from 1000 m on Table Mountain, in the north, to about 150 m close to Cape Point, 50 km to the south. The colour-coding is the same as on the geological map on the left. Kirstenbosch Botanical Gardens, and all the major wines estates on the Peninsula are situated on the fertile (weathered) granite slopes on the east side of the mountain.
Ou Kaapse weg
A view of the cutting at the second hairpin bend on Ou Kaapse Weg, as it winds on to the Silvermine Plateau. The transition between the lowermost layer of the Table Mountain Group on the Cape Peninsula - the Graafwater Formation - and the layer above it, the Table Mountain Sandstone or Peninsula Formation, can be clearly seen. The photograph was taken at an elevation of 250 m.
Newlands Graafwater
A view of the eastern crags (or cliffs) of Table Mountain and Devils Peak as seen from Newlands Forest, above the University of Cape Town. The two layers of the Table Mountain Group which are represented on the Cape Peninsula, namely the Graafwater Formation and the Table Mountain Sandstone or Peninsula Formation, can readily be distinguished. The remaining layer, the Pakhuis Formation, occurs as a tiny remnant at Maclear's Beacon on the top of Table Mountain, not visible in the photograph. The granite basement on which the Table Mountain Group rests on the Cape Peninsula is obscured by the forest in the foreground.
Erosion A5
A west-east (left to right) geological cross section through Table Mountain on the Cape Peninsula, the Cape Flats (the isthmus connecting the Peninsula to the African mainland) and the Hottentots-Holland Mountains on the mainland. It indicates how the Cape Fold Mountains have been eroded in this region, leaving what was once the bottom of a valley to form Table Mountain with its flat table-top structure.[2]

The Cape Peninsula is underlain by the oldest rocks in the area, the Malmesbury Group, and the granite intrusions of the Peninsula pluton.

The Malmesbury Group has been dated from between 830 and 980 Mya, and was deformed during the Saldanian orogenic cycle, both before and during the granite intrusions of 630 to 500 Mya, and there are minor intrusions which precede the granite. The base of this group has not been exposed.[28] The basal rocks were eroded to a relatively featureless peneplain with exposed granites covering most of the peninsula south of Lion's Head and Devil's Peak. The Sea-Point contact zone, described by Charles Darwin is a well known region of metamorphic rocks formed by the (originally very hot) granite intrusion into the Malmesbury rocks.[2]

These rocks were later unconformably covered by the Cape Supergroup. The Cape Supergroup is divided into eight formations, the three oldest of which are present on the Peninsula. The lowest present is the reddish Graafwater formation which consist of shales and sandstone. The Graafwater Formation can be clearly seen in the cutting on the second hairpin bend as the Ou Kaapse Weg (road) goes up the slope from Westlake on to the Silvermine plateau. In the cutting one can also see the abrupt and obvious transition into the Table Mountain Sandstone (or, as it is currently known, the Peninsula Formation Sandstone) above it. Looking up the slope from below to the first hairpin bend, the granite basement on which the Graafwater formation rests is visible. And in the cutting at the first hairpin bend, the ocher-colored, gritty clay into which the granite weathers is clearly displayed. The relatively thin Graafwater layer (no more than about 60–70 m thick on the Cape Peninsula) is overlain by the prominent Peninsula Formation, which consist mainly of hard, erosion resistant, quartzitic sandstone, which form the high, prominent, almost vertical cliffs of the Cape Peninsula. At the very top of Table Mountain, at Maclear's Beacon, is a small remnant of the Pakhuis Diamictites, better represented in the Cederberg Mountains, 200 km to the north of Cape Town.[28]

Foot note

  1. ^ In 2011-2012 dassies began to be seen in Bakoven, on the Atlantic coast, below the Twelve Apostles Mountains. They were then seen in the Silvermine region of the Table Mountain National Park, and in 2015 at the restaurant on the top of the western end of Table Mountain, as well as elsewhere in the mountains. But even in 2017 dassies are still not as abundant as they were on the Peninsula Mountain Chain in the 1990s.

References

  1. ^ 1:250,000 Geological Series map 3318:Cape Town, Government Printer, Pretoria, 1990.
  2. ^ a b c d Compton, John S. (2004) The Rocks & Mountains of Cape Town. Cape Town: Double Story. ISBN 978-1-919930-70-1
  3. ^ http://ioc.unesco.org/oceanteacher/OceanTeacher2/01_GlobOcToday/03_GeopolOc/s23_1953.pdf
  4. ^ http://www.southafrica.info/about/geography/oceansmeet.htm
  5. ^ http://www.discoverthecape.com/atlantic-coast.html
  6. ^ a b c Branch, M & Branch G. (1981). The Living Shores of Southern Africa. pp. 14-18. Struik Publishers, Cape Town.
  7. ^ a b c Tyson, P.D., Preston-Whyte, R.A. (2000) The Weather and Climate of Southern Africa. pp. 221-223. Oxford University Press, Cape Town
  8. ^ a b Manning, John (2007). "Cone Bush, Tolbos". In: Field Guide to Fynbos. Cape Town: Struik Publishers. p. 258. ISBN 9781770072657.
  9. ^ http://www.proteaatlas.org.za/cpldarge.htm
  10. ^ a b Trinder-Smith, Terry (2006). "Orchidaceae". In: Wild Flowers of the Table Mountain National Park. Kirstenbosch, Claremont: Botanical Society of South Africa. pp. 104–105. ISBN 1874999600.
  11. ^ a b c d e Manning, John (2007). "The World of Fynbos". In: Field Guide to Fynbos. Cape Town: Struik Publishers. pp. 8–23. ISBN 9781770072657.
  12. ^ a b Trinder-Smith, Terry (2006). "Introduction". In: Wild Flowers of the Table Mountain National Park. Cape Town: Botanical Society of South Africa. pp. 19–35. ISBN 1874999600.
  13. ^ Manning, John (2007). "Disa". In: Field Guide to Fynbos. Cape Town: Struik Publishers. pp. 162–163. ISBN 9781770072657.
  14. ^ a b Sleigh, Dan (2002). Islands. London: Secker & Warburg. p. 429. ISBN 0436206323.
  15. ^ a b c d e Pauw, Anton; Johnson, Steven (1999). "The Power of Fire". in: Table Mountain. Vlaeberg, South Africa: Fernwood Press. pp. 37–53. ISBN 1 874950 43 1.
  16. ^ a b Kraaij, Tineke; van Wilgen, Brian W. (2014). "Drivers, ecology, and management of fynbos fires.". In Allsopp, Nicky; Colville, Jonathan F.; Verboom, G. Anthony. Fynbos, Ecology, Evolution and Conservation of a Megadiverse Region. Oxford: Oxford University Press. p. 47. ISBN 9780199679584.
  17. ^ Saunders, Christopher; Bundy, Colin (eds.), eds. (1992). "A way of life perfected". Readers’ Digest Illustrated History of South Africa. Cape Town: Reader’s Digest Association Ltd. pp. 20–25. ISBN 0-947008-90-X.CS1 maint: Extra text: editors list (link)
  18. ^ a b c d Maytham Kid, Mary (1983). "Introduction". In: Cape Peninsula. South African Wild Flower Guide 3. Kirstenbosch, Claremont: Botanical Society of South Africa. p. 27. ISBN 0620067454.
  19. ^ "Perceval" (PDF). Archived from the original (PDF) on 2013-08-25.
  20. ^ "Brochures, booklets and posters". Capetown.gov.za. Archived from the original on 2012-12-23. Retrieved 2013-01-12.
  21. ^ Information gleaned from reports in the Cape Bird Club's newsletters from the 1950s onwards
  22. ^ Jenkins, A.R.; van Zyl, A.J. (2005). "Conservation status and community structure of cliff-nesting raptors and ravens on the Cape Peninsula, South Africa". Ostrich. 76: 175–184. doi:10.2989/00306520509485490. ISSN 0030-6525.
  23. ^ a b Hockey, P. A. R.; Dean, W. R. J.; Ryan, P. G., eds. (2005). Roberts Birds of Southern Africa (Seventh ed.). Cape Town: John Voelcker Bird Book Fund. pp. 531–532. ISBN 0-620-34053-3.
  24. ^ Jenkins, Andrew; van Zyl, Anthony (2002). "Home on the range. Raptor riches of the Cape Peninsula". Africa Birds & Birding. 7: 38–46.
  25. ^ "Archived copy". Archived from the original on 2014-08-11. Retrieved 2014-06-10.CS1 maint: Archived copy as title (link) Cape Peninsula Baboon Research Unit
  26. ^ a b http://www.ncc-group.co.za/case-studies/managing-baboon-human-conflict-city-cape-town Managing Baboon-human conflict: City of Cape Town
  27. ^ http://www.quaggaproject.org/ The Quagga Project South Africa
  28. ^ a b Theron, J.N. Gresse, P.G. Siegfried, H.P. and Rogers, J. Explanation sheet 3318 – The Geology of the Cape Town Area. Geological Survey, Department of Mineral and Energy Affairs, Government Printer, Pretoria 1992. ISBN 978-0-621-14284-6

Coordinates: 34°12′18″S 18°24′14″E / 34.205°S 18.404°E

Bakoven

Bakoven is a residential suburb on the west coast of the Cape Peninsula, south of Camps Bay.

It is the last suburb out of Cape Town on Victoria Road past Camps Bay, positioned between Camps Bay and the wild Nature Reserve. Thereafter the coastline is protected, with thousands of acres of mountain Nature Reserve. This scenic drive from Bakoven to Llandudno and Hout bay is one of the most visited in the Cape.

It has views of the Atlantic Ocean, is surrounded by a fynbos nature reserve and has a backdrop of the Twelve Apostle mountains.

As of 2017 it is the 4th most expensive suburb in Cape Town. Named "Baking oven", possibly after an off shore rock of that shape; the name is Dutch in origin.Bakoven has two popular beaches, Beta Beach and Oudekraal - which were an old settlement of Khoi San people there, the original people in the Cape.

Beaches of Cape Town

Cape Town has a wide variety of beaches divided into three regions by the Cape Peninsula:

False Bay, including the long sandy beach running from Gordon's Bay to Muizenberg, and the smaller beaches along the East side of the Cape Peninsula

Atlantic Seaboard, along the West (Atlantic) side of the Cape Peninsula

West Coast, along the West coast running Northwards from Cape TownThe sea in False Bay is about 6 degrees warmer than the Atlantic Seaboard and the West Coast.

In 2011, Lonely Planet listed Cape Town second in its list of the world's top 10 beach cities.

Bobtail squid

Bobtail squid (order Sepiolida) are a group of cephalopods closely related to cuttlefish. Bobtail squid tend to have a rounder mantle than cuttlefish and have no cuttlebone. They have eight suckered arms and two tentacles and are generally quite small (typical male mantle length being between 1 and 8 cm).Sepiolids live in shallow coastal waters of the Pacific Ocean and some parts of the Indian Ocean and Atlantic Ocean as well as in shallow waters on the west coast of the Cape Peninsula off South Africa.

Like cuttlefish, they can swim by either using the fins on their mantle or by jet propulsion. They are also known as dumpling squid (owing to their rounded mantle) or stubby squid.

Cape Fold Belt

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. It was originally continuous with the Ventana Mountains near Bahía Blanca in Argentina, the Pensacola Mountains (East Antarctica), the Ellsworth Mountains (West Antarctica) and the Hunter-Bowen orogeny in eastern Australia. The rocks involved are generally sandstones and shales, with the shales (Bokkeveld Group) persisting in the valley floors while the erosion resistant sandstones (belonging to the Peninsula Formation) form the parallel ranges, the Cape Fold Mountains, which reach a maximum height of 2325 m at Seweweekspoortpiek (‘Seven Weeks Defile Peak’ in Afrikaans).

The Cape Fold Mountains form a series of parallel ranges that run along the south-western and southern coastlines of South Africa for 850 km from the Cederberg 200 km to the north of the Cape Peninsula, and then along the south coast as far as Port Elizabeth, 650 km to the east (see the two maps one above the other on the right).

Cape Peninsula University of Technology

Cape Peninsula University of Technology, a university in Cape Town, South Africa, is the only university of technology in the Western Cape province, and is also the largest university in the province, with over 32,000 students. It was formed by merging the Cape Technikon and a various independent colleges.

Cape of Good Hope

upright=1.6|right|The Cape of Good Hope looking towards the west, from the coastal cliffs above Cape Point, overlooking Dias beach]]

The Cape of Good Hope (Afrikaans: Kaap die Goeie Hoop [ˌkɑːp di ˌχujə ˈɦʊəp], Dutch: Kaap de Goede Hoop [ˌkaːb də ˌɣudə ˈɦoːp] (listen), Portuguese: Cabo da Boa Esperança [ˈkaβu ðɐ ˈβoɐ ʃpɨˈɾɐ̃sɐ]) is a rocky headland on the Atlantic coast of the Cape Peninsula in South Africa.

A common misconception is that the Cape of Good Hope is the southern tip of Africa. This misconception was based on the misbelief that the Cape was the dividing point between the Atlantic and Indian Oceans. Contemporary geographic knowledge instead states the southernmost point of Africa is Cape Agulhas about 150 kilometres (90 mi) to the east-southeast. The currents of the two oceans meet at the point where the warm-water Agulhas current meets the cold-water Benguela current and turns back on itself. That oceanic meeting point fluctuates between Cape Agulhas and Cape Point (about 1.2 kilometres (0.75 mi) east of the Cape of Good Hope).

When following the western side of the African coastline from the equator, however, the Cape of Good Hope marks the point where a ship begins to travel more eastward than southward. Thus, the first modern rounding of the cape in 1488 by Portuguese explorer Bartolomeu Dias was a milestone in the attempts by the Portuguese to establish direct trade relations with the Far East (although Herodotus mentioned a claim that the Phoenicians had done so far earlier). Dias called the cape Cabo das Tormentas ("Cape of Storms"; Dutch: Stormkaap), which was the original name of the "Cape of Good Hope".As one of the great capes of the South Atlantic Ocean, the Cape of Good Hope has long been of special significance to sailors, many of whom refer to it simply as "the Cape". It is a waypoint on the Cape Route and the clipper route followed by clipper ships to the Far East and Australia, and still followed by several offshore yacht races.

The term Cape of Good Hope is also used in three other ways:

It is a section of the Table Mountain National Park, within which the cape of the same name, as well as Cape Point, falls. Prior to its incorporation into the national park, this section constituted the Cape Point Nature Reserve.

It was the name of the early Cape Colony established by the Dutch in 1652, on the Cape Peninsula.

Just before the Union of South Africa was formed, the term referred to the entire region that in 1910 was to become the Cape of Good Hope Province (usually shortened to the Cape Province).

Clovelly, Cape Town

Clovelly is a suburb in the Cape Peninsula area of Cape Town in South Africa.

In biology, Clovelly is home to several seaweeds found only around the Cape Peninsula, including Chaetomorpha, Cladophora and Laurenciophila minima.

Derrick America

Derrick America is a South African politician who has served as a Member of the National Assembly of South Africa since May 2014 representing the Democratic Alliance.

False Bay

False Bay (Afrikaans Valsbaai) is a body of water defined by Cape Hangklip (Dutch/Afrikaans for "Hang(ing)-rock") and the Cape Peninsula in the extreme south-west of South Africa.

Kommetjie

Kommetjie (Afrikaans for "small basin," approximately pronounced cawma-key) is a small town near Cape Town, in the Western Cape province of South Africa. It lies about halfway down the west coast of the Cape Peninsula, at the southern end of the long wide beach that runs northwards towards Chapman's Peak and Noordhoek.

The area is a popular spot for surfing, since powerful waves from the Atlantic Ocean rise up over rocky reefs formed by hard sandstones of the Table Mountain Group. Wherever the bottom is rocky, the shallower waters are thick with giant kelp forests.

Kommetjie is famous for its excellent crayfishing despite recent changes in fishing quotas which have seen a drastic reduction in the daily catch allowed.

It is the hometown of the South African singer-songwriter Jeremy Loops.

List of marine animals of the Cape Peninsula and False Bay

The list of marine animals of the Cape Peninsula and False Bay is a list of marine and shore-based species that form a part of the fauna of South Africa. This list includes animals which either live entirely marine lives, or which spend critical parts of their lives at sea.

The geographical range is from Bloubergstrand at the north of Table Bay to Cape Hangklip, the south eastern limit of False Bay, in the Western Cape province of South Africa and includes the Table Mountain National Park Marine Protected Area and the Helderberg Marine Protected Area.

List of seaweeds of the Cape Peninsula and False Bay

This is a list of seaweeds recorded from the oceans bordering The Cape Peninsula in South Africa from Melkbosstrand on the West Coast to Cape Hangklip on the South Coast.

This list comprises locally used common names, scientific names with author citation and recorded ranges. Ranges specified may not be the entire known range for the species, but should include the known range within the waters surrounding the Republic of South Africa.

List ordering and taxonomy complies where possible with the current usage in Algaebase, and may differ from the cited source, as listed citations are primarily for range or existence of records for the region.

Sub-taxa within any given taxon are arranged alphabetically as a general rule.

Details of each species may be available through the relevant internal links. Synonyms may be listed where useful.

Llandudno, Cape Town

Llandudno is a residential suburb of Cape Town, South Africa, on the Atlantic seaboard of the Cape Peninsula. There are no street lights, shops or commercial activities, and the suburb has some of the most expensive residential property in South Africa.

Llandudno Beach is one of the Cape's most naturally diverse beaches, surrounded by large granite boulders and overlooked by mountains. It is a popular surfing spot, but the swimming can be treacherous, with rough seas and extremely cold water. Llandudno has lifeguards on duty during the summer season, operated by the Llandudno Surf Lifesaving club. It is also the access point for the walk to Sandy Bay, an isolated beach still popular with nudists.

On 26 September 1903 the valley was declared a township and named Llandudno after the North Wales seaside resort of Llandudno, which means "Parish of Saint Tudno" in the Welsh language. The striking similarities between Kleinkommetjie Bay in which the valley resides and Llandudno in Wales were noted as reasons for choosing this name.

Recreational dive sites

Recreational dive sites are specific places that recreational scuba divers go to enjoy the underwater environment. They include recreational diver training sites and technical diving sites beyond the range generally accepted for recreational diving. In this context all diving done for recreational purposes is included. Professional diving tends to be done where the job is, and with the exception of the recreational diving service industry, does not generally occur at specific sites chosen for their easy access, pleasant conditions or interesting features.

Recreational dive sites may be found in a wide range of bodies of water, and may be popular for various reasons, including accessibility, biodiversity, spectacular topography, historical interest and artifacts (such as shipwrecks), and water clarity. Tropical waters of high biodiversity and colourful sea life are popular recreational diving vacation destinations. South-east Asia, the Caribbean islands, the Red Sea and the Great Barrier Reef of Australia are regions where the clear, warm, waters and colourful and diverse sea life have made recreational diving an economically important tourist industry.

Recreational divers may accept a relatively high level of risk to dive at a site perceived to be of special interest. Wreck diving and cave diving have their adherents, and enthusiasts will endure considerable hardship, risk and expense to visit caves and wrecks where few have been before. Some sites are popular almost exclusively for their convenience for training and practice of skills, such as flooded quarries. They are generally found where more interesting and pleasant diving is not locally available, or may only be accessible when weather or water conditions permit.

Scarborough, Cape Town

Scarborough is a town situated on the Cape Peninsula to the South of Cape Town in South Africa.

This town was designated as a conservation village in April 1996, defined as "a residential area of limited extent, surrounded by a conserved natural landscape, committed to reverse past environmental damage and to avoid future environmental impacts."

Table Bay

Table Bay (Afrikaans Tafelbaai) is a natural bay on the Atlantic Ocean overlooked by Cape Town (founded 1652 by Van Riebeeck) and is at the northern end of the Cape Peninsula, which stretches south to the Cape of Good Hope. It was named because it is dominated by the flat-topped Table Mountain.

Table Mountain

Table Mountain (Khoekhoe: Huri ‡oaxa, mountain rising from the sea; Afrikaans: Tafelberg) is a flat-topped mountain forming a prominent landmark overlooking the city of Cape Town in South Africa. It is a significant tourist attraction, with many visitors using the cableway or hiking to the top. The mountain forms part of the Table Mountain National Park. Table Mountain is home to a large array of fauna and flora, most of which is endemic.

Table Mountain National Park

Table Mountain National Park, previously known as the Cape Peninsula National Park, is a national park in Cape Town, South Africa, proclaimed on 29 May 1998, for the purpose of protecting the natural environment of the Table Mountain Chain, and in particular the rare fynbos vegetation. The park is managed by South African National Parks. The property is included as part of the UNESCO Cape Floral Region World Heritage Site.

The park contains two well-known landmarks: Table Mountain, for which the park is named; and the Cape of Good Hope, the most southwestern extremity of Africa.

Zonnebloem

Zonnebloem (Dutch for sunflower) is a suburb in City of Cape Town metropolitan municipality in the Western Cape province of South Africa, previously part of District Six.

It was a farming estate until the early 19th century, when it became a suburb of Cape Town as the population and city boundaries grew. Zonnebloem became a home to freed slaves, merchants, labourers and immigrants. During apartheid, the area of District Six was declared a white-only area and the previous residents were evicted.

The suburb hosts the District Six Campus of the Cape Peninsula University of Technology.

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