Portal:Botswana

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Intro

Botswana, officially the Republic of Botswana, is a landlocked country in Southern Africa. Botswana is topographically flat, with approximately 70 per cent of its territory part of the Kalahari Desert. It is bordered by South Africa to the south and southeast, Namibia to the west and north, Zambia to the north, and Zimbabwe to the northeast. With a population of slightly over 2.4 million people and a comparable land area to France, Botswana is one of the most sparsely populated countries in the world. It is essentially the nation-state of the Tswana people, who constitute nearly 80 per cent of the population.

The Tswana ethnic group are descended mainly from Bantu-speaking peoples who migrated into southern Africa, including modern Botswana, in several waves before AD 600. In 1885, the British colonised the area and declared a protectorate named Bechuanaland. As part of the decolonisation of Africa, Bechuanaland became an independent Commonwealth republic under its current name on 30 September 1966. Since then, it has been a parliamentary republic with a consistent record of uninterrupted democratic elections, though dominated by the Botswana Democratic Party until 2024. As of 2024, Botswana is the least corrupt country in mainland Africa according to the Corruption Perceptions Index published by Transparency International.

Botswana's economy has generally experienced stable growth since independence. It is dominated by tourism and mining; Botswana produces more diamonds than any other country. Its gross national income per capita (purchasing power parity) of about $20,158 as of 2024 (by some estimates the fourth-largest in Africa) gives the country a relatively high standard of living and the second-highest Human Development Index of continental Sub-Saharan Africa, after South Africa. Despite this, Botswana continues to grapple with high unemployment rates. Botswana is a member of the Southern African Customs Union, the Southern African Development Community, the Commonwealth of Nations and the United Nations. (Full article...)


Selected article -

Botswana–Namibia relations refers to the current and historical relationship between Botswana and Namibia. Botswana gained independence from Britain in September 1966. Namibia gained independence from South Africa in 1990 following the Namibian War of Independence, and the two countries soon after established formal diplomatic relations. Botswana has a high commission in Windhoek and Namibia has one in Gaborone. Both countries are members of the Southern African Development Community, African Union, Group of 77, and Commonwealth of Nations. (Full article...)

Did you know -

... that the Motswana ANC activist Fish Keitseng helped anti-Apartheid leaders including Nelson Mandela and Thabo Mbeki to move through Bechuanaland?

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This is a good article, A-class article, featured list, or featured article, one of Wikipedia’s best work.

A desert is a landscape where little precipitation occurs and, consequently, living conditions create unique biomes and ecosystems. The lack of vegetation exposes the unprotected surface of the ground to denudation. About one-third of the land surface of the Earth is arid or semi-arid. This includes much of the polar regions, where little precipitation occurs, and which are sometimes called polar deserts or "cold deserts". Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location.

Deserts are formed by weathering processes as large variations in temperature between day and night strain the rocks, which consequently break in pieces. Although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter, and the resulting fragments and rubble strewn over the desert floor are further eroded by the wind. This picks up particles of sand and dust, which can remain airborne for extended periods – sometimes causing the formation of sand storms or dust storms. Wind-blown sand grains striking any solid object in their path can abrade the surface. Rocks are smoothed down, and the wind sorts sand into uniform deposits. The grains end up as level sheets of sand or are piled high in billowing dunes. Other deserts are flat, stony plains where all the fine material has been blown away and the surface consists of a mosaic of smooth stones, often forming desert pavements, and little further erosion occurs. Other desert features include rock outcrops, exposed bedrock and clays once deposited by flowing water. Temporary lakes may form and salt pans may be left when waters evaporate. There may be underground water sources in the form of springs and seepages from aquifers. Where these are found, oases can occur. (Full article...)

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