Geography of South Africa

Geography of South Africa
South Africa
Continent Africa
Region Southern Africa
Area Ranked 25th
1,221,037 km2 (471,445.0 sq mi)
Borders Total land borders:
4,862 km
Botswana 1,840 km,
Lesotho 909 km,
Mozambique 491 km,
Namibia 967 km,
Swaziland 430 km,
Zimbabwe 225 km
Highest point Mafadi
3,450 m
Lowest point Sea level
0 m
Longest river Orange River
2,200 km
Largest lake Lake Chrissie

South Africa occupies the southern tip of Africa, its coastline stretching more than 2,500 km (1,553 mi) from the desert border with Namibia on the Atlantic (western) coast southwards around the tip of Africa and then north to the border with Mozambique on the Indian Ocean. The low-lying coastal zone is narrow for much of that distance, soon giving way to a mountainous escarpment (Great Escarpment) that separates the coast from the high inland plateau. In some places, notably the province of KwaZulu-Natal in the east, a greater distance separates the coast from the escarpment. Although most of the country is classified as semi-arid, it has considerable variation in climate as well as topography.

Contents

General information

Area
Maritime claims
Natural resources

gold, chromium, antimony, coal, iron ore, manganese, nickel, phosphates, tin, uranium, gem diamonds, platinum, copper, vanadium, salt, natural gas

Land use
Irrigated land
Natural hazards
Environment - issues as of 2010
Environment - international agreements

General geography

By far South Africa's biggest neighbour is the ocean—or two oceans, which meet at the southwestern corner. Its territory includes Marion and Prince Edward Islands, nearly 2,000 km (1,243 mi) from Cape Town in the Atlantic Ocean.

The cold Benguela current sweeps up from the Antarctic along the Atlantic coast, laden with plankton and providing rich fishing-grounds. The east coast has the north-to-south Mozambique/Agulhas Current, which provide its warm waters. These two currents have a major effect on the country's climate, the ready evaporation of the eastern seas providing generous rainfall while the Benguela current retains its moisture to cause desert conditions in the west.

Several small rivers run into the sea along the coastline, but none are navigable and none provide useful natural harbours. The coastline itself, being fairly smooth, provides only one good natural harbour, at Saldanha Bay north of Cape Town. A lack of fresh water prevented major development here. Nevertheless, busy harbours now exist at Cape Town, Port Elizabeth, East London, Durban, and Richards Bay.

On dry land, going from west to east, the country shares long borders with Namibia and Botswana, touches Zimbabwe, has a longitudinal strip of border with Mozambique to the east, and lastly curves in around Swaziland before rejoining Mozambique's southern border. In the interior, nestled in the curve of the bean-shaped Free State, lies the small mountainous country of Lesotho, completely surrounded by South African territory.

There are only two major rivers: the Limpopo, a stretch of which is shared with Zimbabwe, and the Orange (with its tributary, the Vaal) which runs with a variable flow across the central landscape from east to west, emptying into the Atlantic Ocean at the Namibian border. In so dry a country, dams and irrigation are extremely important: the largest dam is the Gariep on the Orange River.

The total land area of South Africa is slightly more than 1,200,000 km2 (463,000 sq mi), and it measures some 1,600 km (994 mi) from north to south and approximately the same from east to west.

Climate

See also: Climate

Average temperatures in °C
City Summer Winter
Cape Town 20 12.6
Durban 23.6 17
Johannesburg 19.4 11.1
Pretoria 22.4 12.9
Source: Lew Leppan: The South African Book of Records. Cape Town, Don Nelson, 1999.

The Karoo, which occupies a large part of the western Central Plateau, has a climate extremely hot in summer and bitterly cold in winter. In contrast, the eastern coastline on the Indian Ocean is lush, well watered and warmed by the Mozambique Current; patches of Southern Africa mangroves grow along this coast.

The southern coast, part of which is known as the Garden Route, is temperate and green. The Cape of Good Hope has a Mediterranean climate, with cool, wet winters and warm, dry summers (becoming hotter in interior valleys). Snow commonly falls in winter on the higher ground of the Cape Fold Mountains. The Cape has a reputation for its wind - which blows intermittently virtually all year round, either from the south-east or the north-west - and for its sunny summer, when almost no rain falls. The vegetation of the Cape area consists of fynbos grassland and Albany thickets.

The eastern section of the Karoo does not extend as far north as the western part, giving way to the flat landscape of the Free State, which though still semi-arid receives somewhat more rain. North of the Vaal River the Highveld is better watered, its annual rainfall is 760 mm (29.9 in) and due to its high altitude (around 1,750 m/5,741 ft) is saved from extremes of heat. Winters are cold, though snow is rare.

Further north and to the east, especially where a drop in altitude beyond the escarpment gives the Lowveld its name, temperatures rise: the Tropic of Capricorn slices through the extreme north. Here one finds the typical South African Bushveld. There is skiing in winter in the high Drakensberg mountains that form the eastern escarpment, but the coldest place in the country is Sutherland in the western Roggeveld Mountains, with midwinter temperatures as low as −15 degrees Celsius. The deep interior provides the hottest temperatures: in 1948 the mercury hit 51.7 °C (125.06 °F) in the Northern Cape Kalahari near Upington.

The Central Plateau

Satellite image of left, generated from raster graphics data supplied by The Map Library.
Topography of South Africa

The Central Plateau has a large range of landscape. It is drained by two major rivers, the Orange and the Limpopo, and is made up of 10 smaller geographic regions. The altitude varies from 600 to 2,500 m and the rainfall varies from 200 to 1200 mm annually. It is ringed in the east, south and west by the Great Escarpment. In general the Great Escarpment slowly loses altitude into the northwestern areas of the Central Plateau. In the west it is very dry, merging with the Kalahari in the northwest. In the central areas the arid scrubland gives way to dry grasslands which become better watered further to the east. These grasslands extend northeastward until they reach the Witwatersrand and Magaliesberg, which are the main watershed between the Orange and Limpopo Rivers. The Witwatersrand and Magaliesberg also form part of an area of low mountain ranges surrounding a basin called the Bushveld. To the north of that the semi-arid savanna loses altitude towards the Limpopo River valley. The regions are outlined in more detail below.

Regions of higher elevation

Southern Africa seen from Aqua and Terra satellites

Low-lying regions

Extreme points

South Africa's cities and main towns

This is a list of the extreme points of South Africa, the points that are farther north, south, east or west than any other location in the country.

South Africa

South Africa (mainland)

See also

References