Contemporary chic meets gracious history at this hotel: for sale

The earliest known remnants of human occupation in the region were found at Peers Cave in Fish Hoek in the late 1920s. Subject to much debate, earlier estimations as to an upper Pleistocene origin have since been revised. At their most generous and conservative estimates, D. D. Stynder et al. radiocarbon date SAM-AP 4692 to the mid-Holocene at 5448 and 5136 BCE (or 7457 and 7145 cal BP) respectively.

Bartolomeu Dias, the first European to reach the area, arrived in 1488 and named it "Cape of Storms" (Cabo das Tormentas). It was later renamed by John II of Portugal as "Cape of Good Hope" (Cabo da Boa Esperança) because of the great optimism engendered by the opening of a sea route to the Indian subcontinent and East Indies. In 1497, Portuguese explorer Vasco da Gama recorded a sighting of the Cape of Good Hope.

In 1510, at the Battle of Salt River, the Portuguese admiral Francisco de Almeida and sixty-four of his men were killed and his party was defeated by the "Goringhaiqua" (in Dutch approximate spelling) using cattle that were specially trained to respond to whistles and shouts.

The Gorinaiqua were one of the Khoikhoi clans who inhabited the area. In the late 16th century French, Danish, Dutch, and English, but mainly Portuguese, ships regularly continued to stop over in Table Bay en route to the Indies. They traded tobacco, copper, and iron with the Khoikhoi clans of the region in exchange for fresh meat and other essential traveling provisions.

Dutch period

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 and Cape Malay 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.

British period

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, partially as a result of numerous wars with the amaXhosa on the colony's eastern frontier. In 1833 slavery was abolished in the colony freeing over 5500 slaves in the city, almost a third of the city's population at the time. The Convict Crisis of 1849, marked by substantial civil upheaval, bolstered the push for self-governance in the Cape.

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 continent and 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.

South African period

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 Cape Town CBD, and by extension, the City Bowl region.

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 Atlantis, Bellville, Blouberg, Brackenfell, Durbanville, Goodwood, Gordon's Bay, Hout Bay, Khayelitsha, Kraaifontein, Kuilsrivier, Macassar, Melkbosstrand, Milnerton, Muizenberg, Noordhoek, Parow, Philadelphia, 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,^[73] 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.

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.

The coastline of Cape Town is roughly 307 km long, from Silwerstroomstrand at 33°34′14.994″S 18°20′34.959″E on the west coast to slightly south of Kogelbaai at 34°16′10.554″S 18°50′44.905″E on the east coast of False Bay.