Cape Town is a city that will captivate you with its stunning scenery, rich history, and diverse culture. Whether you want to explore the majestic Table Mountain, enjoy the sandy beaches and penguins of the Atlantic coast, or experience the vibrant nightlife and cuisine of the city center, Cape Town has something for everyone. You can also discover the heritage and creativity of the city's many neighborhoods, from the colorful Bo-Kaap to the trendy Woodstock. Cape Town is a city that celebrates its diversity and welcomes visitors with open arms.

Dutch period

 

Jan van Riebeeck and Dutch colonists arriving in Table Bay in 1652.

 

A diorama of Cape Town as it would have appeared in 1800 at the end of Dutch rule by the VOC.

In 1652, Jan van Riebeeck and other employees of the United East India Company (Dutch: Verenigde Oost-indische Compagnie, VOC) were sent to the Cape Colony to establish a way-station for ships travelling to the Dutch East Indies, and the Fort de Goede Hoop (later replaced by the Castle of Good Hope). The settlement grew slowly during this period, as it was hard to find adequate labour. This labour shortage prompted the local authorities to import enslaved people from Indonesia and Madagascar. Many of these people are ancestors of modern-day Cape Coloured communities. Under Van Riebeeck and his successors, as VOC commanders and later governors at the Cape, a wide range of agricultural plants were introduced to the Cape. Some of these, including grapes, cereals, ground nuts, potatoes, apples and citrus, had a large and lasting influence on the societies and economies of the region.Adderley Street in 1897 was an important commercial hub in Cape Town at a time when the city was the most important centre of economic activity in the Southern Africa region. With the Dutch Republic being transformed into Revolutionary France's vassal Batavian Republic, Great Britain moved to take control of Dutch colonies, including the colonial possessions of the VOC. Britain captured Cape Town in 1795, but it was returned to the Dutch by treaty in 1803. British forces occupied the Cape again in 1806 following the Battle of Blaauwberg when the Batavian Republic allied with Britain's rival, France, during the Napoleonic Wars. Following the conclusion of the war Cape Town was permanently ceded to the United Kingdom in the Anglo-Dutch Treaty of 1814. The city became the capital of the newly formed Cape Colony, whose territory expanded very substantially through the 1800s. With expansion came calls for greater independence from the UK, with the Cape attaining its own parliament (1854) and a locally accountable Prime Minister (1872). Suffrage was established according to the non-racial Cape Qualified Franchise.During the 1850s and 1860s, additional plant species were introduced from Australia by the British authorities. Notably rooikrans was introduced to stabilise the sand of the Cape Flats to allow for a road connecting the peninsula with the rest of the African continentand eucalyptus was used to drain marshes. In 1859 the first railway line was built by the Cape Government Railways and a system of railways rapidly expanded in the 1870s. The discovery of diamonds in Griqualand West in 1867, and the Witwatersrand Gold Rush in 1886, prompted a flood of immigration into South Africa. In 1895 the city's first public power station, the Graaff Electric Lighting Works, was opened.Conflicts between the Boer republics in the interior and the British colonial government resulted in the Second Boer War of 1899–1902. Britain's victory in this war led to the formation of a united South Africa. From 1891 to 1901, the city's population more than doubled from 67,000 to 171,000. As the 19th century came to an end, the economic and political dominance of Cape Town in the Southern Africa region during the 19th century started to give way to the dominance of Johannesburg and Pretoria in the 20th century.

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South African period

An aerial photograph of the newly completed Cape Town foreshore in 1945. Visible in this photograph as the large area of empty land between the City Centre and the newly constructed harbour out of reclaimed land from Table Bay.In 1910, Britain established the Union of South Africa, which unified the Cape Colony with the two defeated Boer Republics and the British colony of Natal. Cape Town became the legislative capital of the Union, and later of the Republic of South Africa. By the time of the 1936 census, Johannesburg had overtaken Cape Town as the largest city in the country. In 1945 the expansion of the Cape Town foreshore was completed adding an additional 194 ha (480 acres) to the City Bowl area to the city centre.

Apartheid era

Prior to the mid-twentieth century, Cape Town was one of the most racially integrated cities in South Africa. In the 1948 national elections, the National Party won on a platform of apartheid (racial segregation) under the slogan of "swart gevaar" (Afrikaans for "black danger"). This led to the erosion and eventual abolition of the Cape's multiracial franchise. In 1950, the apartheid government first introduced the Group Areas Act, which classified and segregated urban areas according to race. Formerly multi-racial suburbs of Cape Town were either purged of residents deemed unlawful by apartheid legislation, or demolished. The most infamous example of this in Cape Town was the suburb of District Six. After it was declared a whites-only area in 1965, all housing there was demolished and over 60,000 residents were forcibly removed. Many of these residents were relocated to the Cape Flats. The earliest of the Cape Flats forced removals saw the expulsion of Black South Africans to the Langa, Cape Town's first and oldest township, in line with the 1923 Native Urban Areas Act.

Under apartheid, the Cape was considered a "Coloured labour preference area", to the exclusion of "Bantus", i.e. Black Africans. The implementation of this policy was widely opposed by trade unions, civil society and opposition parties. It is notable that this policy was not advocated for by any Coloured political group, and its implementation was a unilateral decision by the apartheid government. During the student-led Soweto Uprising of June 1976, school students from Langa, Gugulethu and Nyanga in Cape Town reacted to the news of the protests against Bantu Education by organising gatherings and marches of their own. A number of school buildings were burnt down and the protest action was met with forceful resistance from the police.

Cape Town has been home to many leaders of the anti-apartheid movement. In Table Bay, 10 km (6 mi) from the city is Robben Island. This penitentiary island was the site of a maximum security prison where many famous apartheird-era political prisoners served long prison sentences. Famous prisoners include activist, lawyer and future president Nelson Mandela who served 18 of his 27 years of imprisonment on the island, as well as two other future presidents, Kgalema Motlanthe and Jacob Zuma. In one of the most famous moments marking the end of apartheid, Nelson Mandela made his first public speech since his imprisonment, from the balcony of Cape Town City Hall, hours after being released on 11 February 1990. His speech heralded the beginning of a new era for the country. The first democratic election, was held four years later, on 27 April 1994. Nobel Square in the Victoria & Alfred Waterfront features statues of South Africa's four Nobel Peace Prize winners: Albert Luthuli, Desmond Tutu, F. W. de Klerk and Nelson Mandela.

Geography and the natural environment

Devil's Peak, Table Mountain and Lion's Head Satellite image of Cape Town showing the Cape Peninsula (left), Cape Flats and False Bay Satellite image 3D of the City Bowl and Table Mountain

Cape Town is located at latitude 33.55° S (approximately the same as Sydney and Buenos Aires and equivalent to Casablanca and Los Angeles in the northern hemisphere) and longitude 18.25° E. Table Mountain, with its near vertical cliffs and flat-topped summit over 1,000 m (3,300 ft) high, and with Devil's Peak and Lion's Head on either side, together form a dramatic mountainous backdrop enclosing the central area of Cape Town, the so-called City Bowl. A thin strip of cloud, known colloquially as the "tablecloth" ("Karos" in Afrikaans), sometimes forms on top of the mountain. To the immediate south of the city, the Cape Peninsula is a scenic mountainous spine jutting 40 km (25 mi) southward into the Atlantic Ocean and terminating at Cape Point. There are over 70 peaks above 300 m (980 ft) within Cape Town's official metropolitan limits. Many of the city's suburbs lie on the large plain called the Cape Flats, which extends over 50 km (30 mi) to the east and joins the peninsula to the mainland. The Cape Town region is characterised by an extensive coastline, rugged mountain ranges, coastal plains and inland valleys.

Extent

The extent of Cape Town has varied considerably over time. It originated as a small settlement at the foot of Table Mountain and has grown beyond its city limits as a metropolitan area to encompass the entire Cape Peninsula to the south, the Cape Flats, the Helderberg basin and part of the Steenbras catchment area to the east, and the Tygerberg hills, Blouberg and other areas to the north. Robben Island in Table Bay is also part of Cape Town. It is bounded by the Atlantic Ocean to the west, and False Bay to the south. To the north and east, the extent is demarcated by boundaries of neighbouring municipalities within the Western Cape province. The official boundaries of the city proper extend between the City Bowl and the Atlantic Seaboard to the east and the Southern Suburbs to the south. The City of Cape Town, the metropolitan municipality that takes its name from the city covers the Greater Cape Town metropolitan area, known as the Cape Metropole, extending beyond the city proper itself to include a number of satellite towns, suburbs and rural areas such as Milnerton, Atlantis, Bellville, Brackenfell, Durbanville, Goodwood, Gordon's Bay, Hout Bay, Kraaifontein, Kuilsrivier, Muizenberg, Simon's Town, Somerset West and Strand among others.

The Cape Peninsula is 52 km (30 mi) long from Mouille Point in the north to Cape Point in the south, with an area of about 470 km2 (180 sq mi), and it displays more topographical variety than other similar sized areas in southern Africa, and consequently spectacular scenery. There are diverse low-nutrient soils, large rocky outcrops, scree slopes, a mainly rocky coastline with embayed beaches, and considerable local variation in climatic conditions.[45] The sedimentary rocks of the Cape Supergroup, of which parts of the Graafwater and Peninsula Formations remain, were uplifted between 280 and 21S million years ago, and were largely eroded away during the Mesozoic. The region was geologically stable during the Tertiary, which has led to slow denudation of the durable sandstones. Erosion rate and drainage has been influenced by fault lines and fractures, leaving remnant steep-sided massifs like Table Mountain surrounded by flatter slopes of deposits of the eroded material overlaying the older rocks, There are two internationally notable landmarks, Table Mountain and Cape Point, at opposite ends of the Peninsula Mountain Chain, with the Cape Flats and False Bay to the east and the Atlantic Ocean to the west. The landscape is dominated by sandstone plateaux and ridges, which generally drop steeply at their margins to the surrounding debris slopes, interrupted by a major gap at the Fish Hoek–Noordhoek valley. In the south much of the area is a low sandstone plateau with sand dunes. Maximum altitude is 1113 m on Table Mountain. The Cape Flats (Afrikaans: Kaapse Vlakte) is a flat, low-lying, sandy area, area to the east the Cape Peninsula, and west of the Helderberg much of which was wetland and dunes within recent history. To the north are the Tygerberg Hills and the Stellenbosch district.

The Helderberg area of Greater Cape Town, previously known as the "Hottentots-Holland" area, is mostly residential, but also a wine-producing area east of the Cape Flats, west of the Hottentots Holland mountain range and south of the Helderberg mountain, from which it gets its current name. The Helderberg consists of the previous municipalities of Somerset West, Strand, Gordons Bay and a few other towns. Industry and commerce is largely in service of the area. After the Cape Peninsula, Helderberg is the next most mountainous part of Greater Cape Town, bordered to the north and east by the highest peaks in the region along the watershed of the Helderberg and Hottentots Holland Mountains, which are part of the Cape Fold Belt with Cape Supergroup strata on a basement of Tygerberg Formation rocks intruded by part of the Stellenbosch granite pluton. The region includes the entire catchment of the Lourens and Sir Lowry's rivers, separated by the Schapenberg hill, and a small part of the catchment of the Eerste River to the west. The Helderberg is ecologically highly diverse, rivaling the Cape Peninsula, and has its own endemic ecoregions and several conservation areas. To the east of the Hottentots Holland mountains is the valley of the Steenbras River, in which the Steenbras Dam was built as a water supply for Cape Town. The dam has been supplemented by several other dams around the western Cape, some of them considerably larger. This is almost entirely a conservation area, of high biodiversity. Bellville, Brackenfell, Durbanville, Kraaifontein, Goodwood and Parow are a few of the towns that make up the Northern Suburbs of Cape Town. In current popular culture these areas are often referred to as being beyond the "boerewors curtain," a play on the term "iron curtain." UNESCO declared Robben Island in the Western Cape a World Heritage Site in 1999. Robben Island is located in Table Bay, some 6 km (3.7 mi) west of Bloubergstrand, a coastal suburb north of Cape Town, and stands some 30m above sea level. Robben Island has been used as a prison where people were isolated, banished, and exiled for nearly 400 years. It was also used as a leper colony, a post office, a grazing ground, a mental hospital, and an outpost. Cape Town's "City Bowl" viewed from Lion's Head in May (late autumn)

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Geology

Main article: Geology of Cape Town

Geological map of the Cape Peninsula and False Bay

The Cape Peninsula is a rocky and mountainous peninsula that juts out into the Atlantic Ocean at the south-western extremity of the continent. At its tip is Cape Point and the Cape of Good Hope. The peninsula forms the west side of False Bay and the Cape Flats. On the east side are the Helderberg and Hottentots Holland mountains. The three main rock formations are the late-Precambrian Malmebury group (sedimentary and metamorphic rock), the Cape Granite suit, comprising the huge Peninsula, Kuilsrivier-Helderberg, and Stellenbosch batholiths, that were intruded into the Malmesbury Group about 630 million years ago, and the Table Mountain group sandstones that were deposited on the eroded surface of the granite and Malmesbury series basement about 450 million years ago.

The sand, silt and mud deposits were lithified by pressure and then folded during the Cape Orogeny to form the Cape Fold Belt, which extends in an arc along the western and southern coasts. The present landscape is due to prolonged erosion having carved out deep valleys, removing parts of the once continuous Table Mountain Group sandstone cover from over the Cape Flats and False Bay, and leaving high residual mountain ridges.

At times the sea covered the Cape Flats and Noordhoek valley and the Cape Peninsula was then a group of islands. During glacial periods the sea level dropped to expose the bottom of False Bay to weathering and erosion, with the last major regression leaving the entire bottom of False Bay exposed. During this period an extensive system of dunes was formed on the sandy floor of False Bay. At this time the drainage outlets lay between Rocky Bank Cape Point to the west, and between Rocky Bank and Hangklip Ridge to the east, with the watershed roughly along the line of the contact zone east of Seal Island and Whittle Rock.

Climate

Llandudno, Western Cape during a sunny day

Cape Town has a warm Mediterranean climate (Köppen: Csb), with mild, moderately wet winters and dry, warm summers. Winter, which lasts from June to September, may see large cold fronts entering for limited periods from the Atlantic Ocean with significant precipitation and strong north-westerly winds. Winter months in the city average a maximum of 18 °C (64 °F) and minimum of 8.5 °C (47 °F). Winters are snow and frost free, except on Table Mountain and on other mountain peaks, where light accumulation of snow and frost can sometimes occur. Total annual rainfall in the city averages 515 mm (20.3 in) although in the Southern Suburbs, close to the mountains, rainfall is significantly higher and averages closer to 1,000 mm (39.4 in). Summer, which lasts from December to March, is warm and dry with an average maximum of 26 °C (79 °F) and minimum of 16 °C (61 °F). The region can get uncomfortably hot when the Berg Wind, meaning "mountain wind", blows from the Karoo interior. Spring and summer generally feature a strong wind from the south-east, known locally as the south-easter or the Cape Doctor, so called because it blows air pollution away. This wind is caused by a persistent high-pressure system over the South Atlantic to the west of Cape Town, known as the South Atlantic High, which shifts latitude seasonally, following the sun, and influencing the strength of the fronts and their northward reach. Cape Town receives about 3,100 hours of sunshine per year. Water temperatures range greatly, between 10 °C (50 °F) on the Atlantic Seaboard, to over 22 °C (72 °F) in False Bay. Average annual ocean surface temperatures are between 13 °C (55 °F) on the Atlantic Seaboard (similar to Californian waters, such as San Francisco or Big Sur), and 17 °C (63 °F) in False Bay (similar to Northern Mediterranean temperatures, such as Nice or Monte Carlo). A 2019 paper published in PLOS One estimated that under Representative Concentration Pathway 4.5, a "moderate" scenario of climate change where global warming reaches ~2.5–3 °C (4.5–5.4 °F) by 2100, the climate of Cape Town in the year 2050 would most closely resemble the current climate of Perth in Australia. The annual temperature would increase by 1.1 °C (2.0 °F), and the temperature of the coldest month by 0.3 °C (0.54 °F), while the temperature of the warmest month would be 2.3 °C (4.1 °F) higher. According to Climate Action Tracker, the current warming trajectory appears consistent with 2.7 °C (4.9 °F), which closely matches RCP 4.5. Moreover, according to the 2022 IPCC Sixth Assessment Report, Cape Town is one of 12 major African cities (Abidjan, Alexandria, Algiers, Cape Town, Casablanca, Dakar, Dar es Salaam, Durban, Lagos, Lomé, Luanda and Maputo) which would be the most severely affected by future sea level rise. It estimates that they would collectively sustain cumulative damages of US$65 billion under RCP 4.5 and US$86.5 billion for the high-emission scenario RCP 8.5 by the year 2050. Additionally, RCP 8.5 combined with the hypothetical impact from marine ice sheet instability at high levels of warming would involve up to US$137.5 billion in damages, while the additional accounting for the "low-probability, high-damage events" may increase aggregate risks to US$187 billion for the "moderate" RCP4.5, US$206 billion for RCP8.5 and US$397 billion under the high-end ice sheet instability scenario. Since sea level rise would continue for about 10,000 years under every scenario of climate change, future costs of sea level rise would only increase, especially without adaptation measures.

Hydrology

See also: Cape Peninsula § Drainage, Helderberg § Drainage, and Cape Flats § Drainage

Sea surface temperatures

See also: False Bay § Waves, tides, water circulation and temperature; and Cape Peninsula § Oceanography

Charts of sea surface temperature in and near False Bay in summer and winter

Cape Town's coastal water ranges from cold to mild, and the difference between the two sides of the peninsula can be dramatic. While the Atlantic Seaboard averages annual sea surface temperatures around 13 °C (55 °F), the False Bay coast is much warmer, averaging between 16 and 17 °C (61 and 63 °F) annually. In summer, False Bay water averages slightly over 20 °C (68 °F), with 22 °C (72 °F) an occasional high. Beaches located on the Atlantic Coast tend to have colder water due to the wind driven upwellings which contribute to the Benguela Current which originates off the Cape Peninsula, while the water at False Bay beaches may occasionally be warmer by up to 10 °C (18 °F) at the same time in summer.

In summer False Bay is thermally stratified, with a vertical temperature variation of 5 to 9˚C between the warmer surface water and cooler depths below 50 m, while in winter the water column is at nearly constant temperature at all depths. The development of a thermocline is strongest around late December and peaks in late summer to early autumn. In summer the south easterly winds generate a zone of upwelling near Cape Hangklip, where surface water temperatures can be 6 to 7 °C colder than the surrounding areas, and bottom temperatures below 12 °C.

In the summer to early autumn (January–March), cold water upwelling near Cape Hangklip causes a strong surface temperature gradient between the south-western and north-eastern corners of the bay. In winter the surface temperature tends to be much the same everywhere. In the northern sector surface temperature varies a bit more (13 to 22 °C) than in the south (14 to 20 °C) during the year.

Surface temperature variation from year to year is linked to the El Niño–Southern Oscillation. During El Niño years the South Atlantic high is shifted, reducing the south-easterly winds, so upwelling and evaporative cooling are reduced and sea surface temperatures throughout the bay are warmer, while in La Niña years there is more wind and upwelling and consequently lower temperatures. Surface water heating during El Niño increases vertical stratification. The relationship is not linear. Occasionally eddies from the Agulhas current will bring warmer water and vagrant sea life carried from the south and east coasts into False Bay.

Flora and fauna

Main article: Biodiversity of Cape Town

Peninsula Sandstone Fynbos growing in Table Mountain National Park.

Located in a Conservation International biodiversity hotspot as well as the unique Cape Floristic Region, the city of Cape Town has one of the highest levels of biodiversity of any equivalent area in the world. These protected areas are a World Heritage Site, and an estimated 2,200 species of plants are confined to Table Mountain – more than exist in the whole of the United Kingdom which has 1200 plant species and 67 endemic plant species. Many of these species, including a great many types of proteas, are endemic to the mountain and can be found nowhere else. It is home to a total of 19 different vegetation types, of which several are endemic to the city and occur nowhere else in the world. It is also the only habitat of hundreds of endemic species and hundreds of others which are severely restricted or threatened. This enormous species diversity is mainly because the city is uniquely located at the convergence point of several different soil types and micro-climates. Table Mountain 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.

Rapid population growth and urban sprawl has covered much of these ecosystems with development. Consequently, Cape Town now has over 300 threatened plant species and 13 which are now extinct. The Cape Peninsula, which lies entirely within the city of Cape Town, has the highest concentration of threatened species of any continental area of equivalent size in the world. Tiny remnant populations of critically endangered or near extinct plants sometimes survive on road sides, pavements and sports fields. The remaining ecosystems are partially protected through a system of over 30 nature reserves – including the massive Table Mountain National Park. Cape Town reached first place in the 2019 iNaturalist City Nature Challenge in two out of the three categories: Most Observations, and Most Species. This was the first entry by Capetonians in this annual competition to observe and record the local biodiversity over a four-day long weekend during what is considered the worst time of the year for local observations.[  A worldwide survey suggested that the extinction rate of endemic plants from the City of Cape Town is one of the highest in the world, at roughly three per year since 1900 – partly a consequence of the very small and localised habitats and high endemicity.

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Tourism

Clifton Beach is one of Cape Town's most famous beaches Table Mountain from the Kirstenbosch National Botanical Garden African penguins at Boulders Penguin Colony

The Western Cape is a highly important tourist region in South Africa; the tourism industry accounts for 9.8% of the GDP of the province and employs 9.6% of the province's workforce. In 2010, over 1.5 million international tourists visited the area. Cape Town is not only a popular international tourist destination in South Africa, but Africa as a whole. This is due to its mild climate, natural setting, and well-developed infrastructure. The city has several well-known natural features that attract tourists, most notably Table Mountain, which forms a large part of the Table Mountain National Park and is the back end of the City Bowl. Reaching the top of the mountain can be achieved either by hiking up, or by taking the Table Mountain Cableway. Cape Point is the dramatic headland at the end of the Cape Peninsula. Many tourists also drive along Chapman's Peak Drive, a narrow road that links Noordhoek with Hout Bay, for the views of the Atlantic Ocean and nearby mountains. It is possible to either drive or hike up Signal Hill for closer views of the City Bowl and Table Mountain.

Many tourists also visit Cape Town's beaches, which are popular with local residents. It is possible to visit several different beaches in the same day, each with a different setting and atmosphere. Both coasts are popular, although the beaches in affluent Clifton and elsewhere on the Atlantic Coast are better developed with restaurants and cafés, with a strip of restaurants and bars accessible to the beach at Camps Bay. The Atlantic seaboard, known as Cape Town's Riviera, is regarded as one of the most scenic routes in South Africa, along the slopes of the Twelve Apostles to the boulders and white sand beaches of Llandudno, with the route ending in Hout Bay, a diverse suburb with a fishing and recreational boating harbour near a small island with a breeding colony of African fur seals. This suburb is also accessible by road from the Constantia valley over the mountains to the northeast, and via the picturesque Chapman's Peak drive from the residential suburb Noordhoek in the Fish Hoek valley to the south-east. Boulders Beach near Simon's Town is known for its colony of African penguins. The city has several notable cultural attractions. The Victoria & Alfred Waterfront, built on top of part of the docks of the Port of Cape Town, is the city's most visited tourist attraction. It is also one of the city's most popular shopping venues, with several hundred shops as well as the Two Oceans Aquarium. The V&A also hosts the Nelson Mandela Gateway, through which ferries depart for Robben Island. It is possible to take a ferry from the V&A to Hout Bay, Simon's Town and the Cape fur seal colonies on Seal and Duiker Islands. Several companies offer tours of the Cape Flats, a region of mostly Coloured & Black townships. Within the metropolitan area, the most popular areas for visitors to stay include Camps Bay, Sea Point, the V&A Waterfront, the City Bowl, Hout Bay, Constantia, Rondebosch, Newlands, and Somerset West. In November 2013, Cape Town was voted the best global city in The Daily Telegraph's annual Travel Awards. Cape Town offers tourists a range of air, land and sea-based adventure activities, including helicopter rides, paragliding and skydiving, snorkelling and scuba diving, boat trips, game-fishing, hiking, mountain biking and rock climbing. Surfing is popular and the city hosts the Red Bull Big Wave Africa surfing competition every year, and there is some local and international recreational scuba tourism.

The City of Cape Town works closely with Cape Town Tourism to promote the city both locally and internationally. The primary focus of Cape Town Tourism is to represent Cape Town as a tourist destination. Cape Town Tourism receives a portion of its funding from the City of Cape Town while the remainder is made up of membership fees and own-generated funds[  The Tristan da Cunha government owns and operates a lodging facility in Cape Town which charges discounted rates to Tristan da Cunha residents and non-resident natives. Cape Town's transport system links it to the rest of South Africa; it serves as the gateway to other destinations within the province. The Cape Winelands and in particular the towns of Stellenbosch, Paarl and Franschhoek are popular day trips from the city for sightseeing and wine tasting.