South Africa
In South Africa, one finds the world's strangest and most dramatic landscapes, a unique wealth of animal and plant life, a treasure of gold, diamonds and other minerals, and a kaleidoscope of fascinating cultures. Nature's tools of creation, the wind, sun, ice and rain, have worked a special magic. There are extremes of deserts, savannas, snow-covered mountains, grasslands, high forests and tropical mangrove swamps. Within these climatic zones, earth's most diverse plant population flourishes. South Africa is also the home of big game, and hosts birds as varied as the vast range of habitats and foods that nature has prepared for them.

The land
The Republic of South Africa occupies the southernmost part of the African continent, stretching latitudinally from 22° to 35° S and longitudinally from 17° to 33° E. Its surface area is 1 219 090 km2. It has common boundaries with the republics of Namibia, Botswana and Zimbabwe, while the Republic of Mozambique and the Kingdom of Swaziland lie to the north-east. Completely enclosed by South African territory in the south-east is the mountain kingdom of Lesotho. To the west, south and east, South Africa borders on the Atlantic and Indian oceans. Isolated, 1 920 km southeast of Cape Town in the Atlantic, lie Prince Edward and Marion islands, annexed by South Africa in 1947.

The seas
South Africa is surrounded by the ocean on three sides ¬ to the west, south and east ¬ and has a long coastline of about 3 000 km. This coastline is swept by two major ocean currents ¬ the warm south-flowing Mozambique-Agulhas Current and the cold Benguela. The former skirts the east and south coasts as far as Cape Agulhas, while the Benguela Current flows northwards along the west coast as far as southern Angola. The contrast in temperature between these two currents partly accounts for important differences in climate and vegetation between the east and west coasts of South Africa. It also causes big differences in marine life. The cold waters of the west coast are much richer in oxygen, nitrates, phosphates and plankton than those of the east coast. Consequently, the South African fishing industry is centred on the west coast.

Relief features
The surface area of South Africa falls into two major physiographic features: the interior plateau, and the land between the plateau and the coast. Forming the boundary between these two areas is the Great Escarpment, the most prominent and continuous relief feature of the country. Its height above sea level varies from approximately 1 500 m in the dolerite-capped Roggeveld scarp in the south-west to a height of 3 482 m in the KwaZulu-Natal Drakensberg. Inland from the Escarpment lies the interior plateau, which is the southern continuation of the great African plateau stretching north to the Sahara Desert. The plateau itself is characterised by wide plains with an average height of 1 200 m above sea level. Surmounting the plateau in places are a number of well-defined upland blocks. The dissected Lesotho plateau, which is more than 3 000 m above sea level, is the most prominent. In general, the Escarpment forms the highest parts of the plateau. Between the Great Escarpment and the coast lies an area which varies in width from 80 to 240 km in the east and south to a mere 60 to 80 km in the west. At least three major subdivisions can be recognised: the eastern plateau slopes, the Cape folded belt and adjacent regions, and the western plateau slopes.

Climatic features
The subtropical location, on either side of 30? S, accounts for the warm temperate conditions so typical of South Africa, making it a popular destination for foreign tourists. The country also falls squarely within the subtropical belt of high pressure, making it dry, with an abundance of sunshine. The wide expanses of ocean on three sides of South Africa have a moderating influence on its climate. More apparent, however, are the effects of the warm Agulhas and cold Benguela currents along the east and west coasts respectively. While Durban (east coast) and Port Nolloth (west coast) lie more or less on the same latitude, there is a difference of at least 6?C in their mean annual temperatures. Gale-force winds are frequent on the coasts, especially in the south-western and southern coastal areas.

Rainfall
South Africa has an average annual rainfall of 464 mm, compared with a world average of 860 mm. About 20% of the country has a total annual rainfall of less than 200 mm, 48% between 200 and 600 mm, while only about 30% records more than 600 mm. In total, 65% of the country has an annual rainfall of less than 500 mm ¬ usually regarded as the absolute minimum for successful dry-land farming. In Cape Town, the capital city of the Western Cape, the average rainfall is highest in the winter months, while in the capital cities of the other eight provinces, the average rainfall is highest during summer. South Africa's rainfall is unreliable and unpredictable. Large fluctuations in the average annual figure are the rule rather than the exception in most areas of the country. Years when a below-average figure is recorded are more common than years with an above-average total. South Africa is periodically afflicted by drastic and prolonged droughts, which often end in severe floods.

Temperatures
Temperature conditions in South Africa are characterised by three main features. Firstly, temperatures tend to be lower than in other regions at similar latitudes, for example Australia. This is due primarily to the greater elevation above sea level of the subcontinent. Secondly, despite a latitudinal span of 13 degrees, average annual temperatures are remarkably uniform throughout the country. Owing to the increase in the height of the plateau towards the northeast, there is hardly any increase in temperature from south to north as might be expected. The third feature is the striking contrast between temperatures on the east and west coasts. Temperatures above 32°C are fairly common in summer, and frequently exceed 38°C in the lower Orange River valley and the Mpumalanga Lowveld.

Frost, humidity and fog
Frost often occurs on the interior plateau during cold, clear winter nights, with ice forming on still pools and in water-pipes. The frost season is longest (from April to October) over the eastern and southern plateau areas bordering on the Escarpment. Frost decreases to the north, while the coast is virtually frost-free. Average annual relative humidity readings show that, in general, the air is driest over the western interior and over the plateau. Along the coast, the humidity is much higher and at times may rise to 85%. Low stratus clouds and fog frequently occur over the cool west coast, particularly during summer. The only other area that commonly experiences fog is the 'mist belt' along the eastern foothills of the Escarpment.

Sunshine
South Africa is famous for its sunshine. Generally speaking, April and May are the most pleasant months. The rainy season over the summer-rainfall region has then ended, while it has not yet really sarted in the winter-rainfall area. The hot summer weather has abated, and the winds are lighter than during the rest of the year. In certain areas, however, notably the hot, humid KwaZulu-Natal coast, Mpumalanga and the Northern Province, June and July are the ideal holiday months.

Religion: Religious groups in South Africa
Almost 80% of South Africa's population adheres to the Christian faith. Other major religious groups are the Hindus, Muslims and Jews. A minority of South Africa's population does not belong to any of the major religions, but regard themselves as traditionalists or of no specific religious affiliation. Freedom of worship is guaranteed by the Constitution, and official policy is one of noninterference in religious practices.