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68-576: The Kalahari Basin , also known as the Kalahari Depression , Okavango Basin or the Makgadikgadi Basin , is an endorheic basin and large lowland area covering approximately 725,293 km (280,037 sq mi) — mostly within Botswana and Namibia , but also parts of Angola , South Africa , Zambia , and Zimbabwe . The outstanding physical feature in the basin, and occupying the centre,
136-426: A balance of surface inflows, evaporation and seepage) are often called sinks. Endorheic lakes are typically located in the interior of a landmass, far from an ocean, and in areas of relatively low rainfall. Their watersheds are often confined by natural geologic land formations such as a mountain range, cutting off water egress to the ocean. The inland water flows into dry watersheds where the water evaporates, leaving
204-573: A high concentration of minerals and other inflow erosion products. Over time this input of erosion products can cause the endorheic lake to become relatively saline (a " salt lake "). Since the main outflow pathways of these lakes are chiefly through evaporation and seepage, endorheic lakes are usually more sensitive to environmental pollutant inputs than water bodies that have access to oceans, as pollution can be trapped in them and accumulate over time. Endorheic regions can occur in any climate but are most commonly found in desert locations. This reflects
272-788: A large portion of Europe drains to the endorheic Caspian Sea, Europe's wet climate means it contains relatively few terminal lakes itself: any such basin is likely to continue to fill until it reaches an overflow level connecting it with an outlet or erodes the barrier blocking its exit. There are some seemingly endorheic lakes, but they are cryptorheic, being drained either through manmade canals , via karstic phenomena, or other subsurface seepage. A few minor true endorheic lakes exist in Spain (e.g. Laguna de Gallocanta , Estany de Banyoles ), Italy , Cyprus ( Larnaca and Akrotiri salt lakes) and Greece . Many small lakes and ponds in North Dakota and
340-536: A limit of the erosion and deposition processes of nearby areas. Endorheic water bodies include the Caspian Sea , which is the world's largest inland body of water. The term endorheic derives from the French word endoréisme , which combines endo- ( Ancient Greek : ἔνδον éndon 'within') and ῥεῖν rheîn 'flow'. Endorheic lakes (terminal lakes) are bodies of water that do not flow into an ocean or
408-614: A merging of populations in East and South Africa . Homo naledi likely coexisted with modern humans in Africa about 300,000 years ago. The Kingdom of Mapungubwe (c. 1075–c. 1220) was one of the earliest state in the South African region. It was located at between the Shashe and Limpopo Rivers. The name is derived from either TjiKalanga and Tshivenda . The kingdom is thought to have existed as
476-470: A redistribution of water from these hydrologically landlocked basins such that endorheic water loss has contributed to sea level rise , and it is estimated that most of the terrestrial water lost ends up in the ocean. In regions such as Central Asia, where people depend on endorheic basins and other surface water sources to satisfy their water needs, human activity greatly impacts the availability of that water. Large endorheic regions in Africa are located in
544-401: A robust mining sector and comparatively developed secondary and tertiary sectors . Additionally many countries (with the exception of Mozambique and Malawi in particular) have relatively well developed infrastructure. Some of its main exports including platinum , diamonds , gold , copper , cobalt , chromium and uranium , Southern Africa still faces some of the problems that the rest of
612-715: A saline lake, and into Lake Xau and the western end of the Makgadikgadi Pan via the Boteti distributary. The Mopipi Dam [ ceb ] was built on the Boteti to provide water to the Orapa diamond mine . The Selinda Spillway, also known as the Magweqana, Magwekwana or Magweggana, is a distributary channel that connects the Okavango Delta to the Cuando River , a tributary of
680-420: A sea. Most of the water that falls to Earth percolates into the oceans and the seas by way of a network of rivers, lakes, and wetlands . Analogous to endorheic lakes is the class of bodies of water located in closed watersheds (endorheic watersheds) where the local topography prevents the drainage of water into the oceans and the seas. These endorheic watersheds (containing water in rivers or lakes that form
748-407: A small population of European ( Afrikaner , British , Portuguese Africans , etc.) and Asian descent ( Cape Malays , Indian South Africans , etc.) people in many southern African countries. Further information in the sections of Architecture of Africa : Further information in the sections of History of science and technology in Africa : Some key factors affecting the food security within
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#1732845438216816-491: Is a major food producer and exporter in the region. Data on agricultural production trends and food insecurity especially in term of food availability for Southern Africa is readily available through the Famine Early Warning Systems Network ( FEWS NET ) and Southern African Development Community ( SADC ) - Food, Agriculture and Nature Resource Directorate (FARN). However, this data might not fully capture
884-683: Is joined just above its confluence with the Cuito by the Omatako River, which flows northeast from its origin in the Damaraland region of central Namibia . The Okavango continues through the Caprivi Strip of Namibia into Botswana , where it splits into a number of distributaries to form the Okavango Delta , a large inland delta that becomes a seasonally flooded grassland . After the Okavango Delta,
952-692: Is one of the largest waterfalls in the world and a major tourist attraction for the region. Southern Africa includes both subtropical and temperate climates, with the Tropic of Capricorn running through the middle of the region, dividing it into its subtropical and temperate halves. Countries commonly included in Southern Africa include Angola , Botswana , the Comoros , Eswatini , Lesotho , Madagascar , Malawi , Mauritius , Mozambique , Namibia , South Africa , Zambia , and Zimbabwe . In cultural geography ,
1020-403: Is one such case, with annual precipitation of 850 mm (33 in) and characterized by waterlogged soils that require draining. Endorheic regions tend to be far inland with their boundaries defined by mountains or other geological features that block their access to oceans. Since the inflowing water can evacuate only through seepage or evaporation, dried minerals or other products collect in
1088-495: Is set apart from other Sub-Saharan African regions because of its mineral resources, including copper, diamonds, gold, zinc, chromium, platinum, manganese, iron ore, and coal. Countries in Southern Africa are larger in geographic area, except three smaller landlocked states: Lesotho, Swaziland, and Malawi. The larger states- South Africa, Botswana, Mozambique, Zimbabwe, Zambia, Namibia, and Angola—all have extensive mineral deposits. These widespread mineral resources make this one of
1156-563: Is the dominant economy of the region. Generally, mining, agriculture, the public sector and tourism dominate the economies of Southern African countries, apart from South Africa which has mature and flourishing financial, retail, and construction sectors. Zimbabwe maintains a smaller banking and real estate sector along with what remains of its manufacturing industry, despite a protracted economic crisis . Most global banks have their regional offices for Southern Africa based in Johannesburg . Over
1224-607: Is the large Kalahari Desert . The perennial river bifurcation of Selinda Spillway (or Magweggana River), on the Cuando River , connects the Kalahari basin to the Zambezi Basin . The Okavango River is the chief stream in the basin. It is formed by the confluence of the Cubango and Cuito rivers, which originate on the Bié Plateau of central Angola and flow southeast. The Cubango
1292-610: The Bonneville flood . The Malheur / Harney lake system in Oregon is normally cut off from drainage to the ocean, but has an outflow channel to the Malheur River . This is presently dry, but may have flowed as recently as 1,000 years ago. Examples of relatively humid regions in endorheic basins often exist at high elevation. These regions tend to be marshy and are subject to substantial flooding in wet years. The area containing Mexico City
1360-585: The Bushveld basin into South Africa. This extends southwest through the Witwatersrand and Northern Cape of South Africa toward the southern coast. Mining activity exists across the eastern region. Diamond mining is found in parts of Botswana and along the Namibian coast. Coal can also be found in central Mozambique, Zimbabwe and northeast South Africa. The climate of the region is broadly divided into subtropical in
1428-642: The Makgadikgadi Pans of Botswana . This area, for example, supports numerous halophilic species and, in the rainy season tens of thousands of flamingos visit these pans. The source of the Okavango Delta's waters in Angola and Namibia remain unaffected by any upstream dams or significant water abstraction and the three riparian states have established a protocol under the Permanent Okavango River Basin Water Commission (OKACOM) for
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#17328454382161496-906: The Sahara Desert , the Sahel , the Kalahari Desert , and the East African Rift : Endorheic lakes exist in Antarctica's McMurdo Dry Valleys , Victoria Land , the largest ice-free area. Much of Western and Central Asia is a giant endorheic region made up of a number of contiguous closed basins. The region contains several basins and terminal lakes, including: Other endorheic lakes and basins in Asia include: Australia , being very dry and having exceedingly low runoff ratios due to its ancient soils, has many endorheic drainages. The most important are: Though
1564-701: The Southern African Bird Atlas Project , and Mammals of the Southern African Subregion . It is not used in political, economic, or human geography contexts because the definition cuts Mozambique in two. In the United Nations geoscheme for Africa, five states constitute Southern Africa: This definition excludes other countries in the region, and instead includes the Comoros, Madagascar, Malawi, Mauritius, Mayotte, Mozambique, Réunion,
1632-901: The Zambezi . In periods of very high water in the Okavango, the water flows eastward towards the Cuando-Linyanti-System. The last time this happened was in August 2009 after 30 years of falling dry. In times of high water in the Kwando, the water can flow west from the Cuando towards the Okavango Delta, but often evaporates before it reaches the delta. Other streams in the basin include the Eiseb , an intermittent stream that originates in Namibia's Herreroland and flows east into
1700-514: The colonial territories led to the independence of new states of Angola and Mozambique as well as Southern Rhodesia , which declared independence as Zimbabwe in 1980. The denouement of South West Africa achieved independence as Namibia in 1990 and the black majority in South Africa took power after the democratic elections in 1994 , therefore ending the Apartheid regime. From the end of
1768-565: The physical geography definition based on the physical characteristics of the land. Defined by physical geography , Southern Africa is home to a number of river systems; the Zambezi River is the most prominent. The Zambezi flows from the northwest corner of Zambia and western Angola to the Indian Ocean on the coast of Mozambique . Along the way, it flows over Victoria Falls on the border between Zambia and Zimbabwe . Victoria Falls
1836-653: The 1820s between Shaka's half-brothers Dingane and Mhlangana due to a succession dispute. Boer settlers began arriving northwards of the Orange River in the 1830s, which led to conflicts between the two peoples and resulted in the Battle of Blood River in 1838. The kingdom fell during the Anglo-Zulu War of the late 19th-century. In the aftermath of World War II , the colonial powers came under international pressure to decolonize. The transfer to an African majority, however,
1904-454: The 1990s these industries have struggled in the face of globalization and cheaper imports from China , leading to job losses particularly in heavy industry , gold mining and textiles . Zimbabwe in particular has seen significant deindustrialization as a result of factors both domestic and foreign. While colonialism has left its mark on the development over the course of history, today poverty , corruption , and HIV / AIDS are some of
1972-774: The June–August rainfall maximum in the western cape. Year-to-year variability in rainfall, including drought, is associated with changes in global and regional sea surface temperatures . These include the El Nino Southern Oscillation , the Subtropical Indian Ocean Dipole , and changes in the Benguela Current region in the southeast Atlantic. Future climate projections suggest that much of southern Africa will get hotter and drier in response to global climate change. East and southern Africa are among
2040-520: The Northern Great Plains are endorheic, and some have salt encrustations along their shores. Some of Earth's ancient endorheic systems and lakes include: Southern Africa Southern Africa is the southernmost region of Africa . No definition is agreed upon, but some groupings include the United Nations geoscheme , the intergovernmental Southern African Development Community , and
2108-534: The Okavango Delta, and the Nata River , which originates in western Zimbabwe to flow into the eastern end of the Makgadikgadi Pan . Despite its aridity, the Kalahari Basin supports a variety of fauna and flora on soils known as Kalahari sands. The native flora includes acacia trees, African rosewood and a large number of herbs and grasses. Some of the areas within the Kalahari are seasonal wetlands , such as
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2176-518: The SADC members. The terrain of Southern Africa is varied, ranging from forest and grasslands to deserts . The region has both low-lying coastal areas, and mountains. In terms of natural resources, the region has the world's largest resources of platinum and the platinum group elements, chromium , vanadium , and cobalt , as well as uranium , gold , copper , titanium , iron , manganese , silver , beryllium , and diamonds . Southern Africa
2244-746: The SADC region and ensures sustainable energy developments through sound economic, environmental and social practices. The main objective of the power pool is to develop a world class, robust and safe interconnected electrical system across the Southern African Region. According to a report by Southern Africa Power Pool, the three largest producers of electricity in Southern Africa as at 2017, include Eskom in South Africa with an estimated 46,963MW, Zesco in Zambia with 2,877MW and SNL of Angola with 2,442MW. Whilst moderately successful by African standards,
2312-877: The Scattered Islands in the Indian Ocean (as a part of the French Southern Territories ), Zambia, and Zimbabwe in Eastern Africa , Angola in Middle Africa (or Central Africa), and Saint Helena, Ascension, and Tristan da Cunha (under the name Saint Helena) in Western Africa , instead. Some atlases include Malawi, Zambia, and Zimbabwe in Central Africa instead of Southern or Eastern Africa. The Southern African Customs Union , created in 1969, also comprises
2380-706: The South African border. There are numerous environmental issues in Southern Africa , including air pollution and desertification . Southern Africa is home to many people. It was initially populated by San , Hottentots and Pygmies in widely dispersed concentrations. Due to the Bantu expansion , the majority of African ethnic groups in this region, including the Xhosa , Zulu , Tsonga , Swazi , Northern Ndebele , Southern Ndebele , Tswana , Sotho , Pedi , Mbundu , Ovimbundu , Shona , Chaga and Sukuma , speak Bantu languages . The process of colonization and settling resulted in
2448-584: The Western Cape in South Africa, the major rainfall season is during the southern-hemisphere summer, from December to February. In the Western Cape , the rainfall maximum occurs from June through August. There are a number of important rainfall-producing weather systems in southern Africa. These include tropical-extra-tropical cloud bands, tropical lows, and tropical cyclones , cut-off lows , and mesoscale convective systems . Winter midlatitude storms account for
2516-509: The Zambezi and Limpopo river valleys, probably due to the lower altitude. The Western Cape has a Mediterranean vegetation and climate, including the unique fynbos , grading eastward into an oceanic climate along the Garden Route to Gqeberha and East London . The Namib and Kalahari deserts form arid lands in the centre-west, separating the highlands, woodlands, croplands, and pastures of
2584-493: The balance between tectonic subsidence and rates of evaporation and sedimentation. Where the basin floor is dropping more rapidly than water and sediments can accumulate, any lake in the basin will remain below the sill level (the level at which water can find a path out of the basin). Low rainfall or rapid evaporation in the watershed favor this case. In areas where rainfall is higher, riparian erosion will generally carve drainage channels (particularly in times of flood), or cause
2652-456: The basin, eventually making the water saline and also making the basin vulnerable to pollution. Continents vary in their concentration of endorheic regions due to conditions of geography and climate. Australia has the highest percentage of endorheic regions at 21 per cent while North America has the least at five per cent. Approximately 18 per cent of the Earth's land drains to endorheic lakes or seas,
2720-491: The biggest factors impeding economic growth. In addition, South Africa and Zimbabwe in particular, face high emigration among their skilled workers leading to a significant brain drain to western economies and billions lost in human capital flight . The pursuit of economic and political stability is an important part of the region's goals, as demonstrated by the SADC, however complete regional integration remains an elusive target. In terms of economic strength, South Africa
2788-444: The continent does. Despite this, diamond production has fueled the economies of Botswana and Namibia, for example. Over the 20th century, the region developed a robust manufacturing sector, focused on South Africa and Zimbabwe, which allowed greater prosperity and investments into infrastructure, education and healthcare that elevated both nations into middle income economies and captured growing markets across Africa. However, since
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2856-564: The degree that a lake no longer forms. Even most permanent endorheic lakes change size and shape dramatically over time, often becoming much smaller or breaking into several smaller parts during the dry season. As humans have expanded into previously uninhabitable desert areas, the river systems that feed many endorheic lakes have been altered by the construction of dams and aqueducts. As a result, many endorheic lakes in developed or developing countries have contracted dramatically, resulting in increased salinity, higher concentrations of pollutants, and
2924-440: The disruption of ecosystems. Even within exorheic basins, there can be "non-contributing", low-lying areas that trap runoff and prevent it from contributing to flows downstream during years of average or below-average runoff. In flat river basins, non-contributing areas can be a large fraction of the river basin, e.g. Lake Winnipeg 's basin. A lake may be endorheic during dry years and can overflow its basin during wet years, e.g.,
2992-414: The earliest regions where modern humans (Homo sapiens) and their predecessors are believed to have lived. In September 2019, scientists reported the computerized determination, based on 260 CT scans , of a virtual skull shape of the last common human ancestor to modern humans , representative of the earliest modern humans, and suggested that modern humans arose between 350,000 and 260,000 years ago through
3060-600: The expansion of supermarkets in the region, which is changing the way people obtain food in the city, rural-to-urban migration, unemployment, and poverty. The issue of food insecurity in general and urban food insecurity in particular in the region is also characterized by an increased consumption of caloric junk food and processed foods leading to potential increase in the co-existence of undernutrition and dietary-related chronic diseases such as obesity and hypertension. In South Africa for example, while over 50% experience hunger, 61% are overweight or morbidly obese. There
3128-482: The first class-based social system within the region. Society was mainly centered around family and farming. The kingdom would culminate to the Kingdom of Zimbabwe in the 13th century. And at its height the capital's population was about 5000 people. There are no written records from the kingdom and what historians and archeologists know of the state is from the remains of buildings. The Kingdom of Zimbabwe (c. 1220–1450)
3196-771: The five states in the UN subregion of Southern Africa. The Southern African Development Community (SADC) was established in 1980 to facilitate co-operation in the region. It includes: Other than the UN subregion, these countries and territories are often included in Southern Africa: The Democratic Republic of the Congo is generally included in Central Africa, while Seychelles and Tanzania are more commonly associated with Eastern Africa, but these three countries have occasionally been included in Southern Africa, as they are
3264-774: The former Tulare Lake . Because the Earth's climate has recently been through a warming and drying phase with the end of the Ice Ages, many endorheic areas such as Death Valley that are now dry deserts were large lakes relatively recently. During the last ice age, the Sahara may have contained lakes larger than any now existing. Climate change coupled with the mismanagement of water in these endorheic regions has led to devastating losses in ecosystem services and toxic surges of pollutants. The desiccation of saline lakes produces fine dust particles that impair agriculture productivity and harm human health. Anthropogenic activity has also caused
3332-629: The island country of Madagascar is often not included due to its distinct language and cultural heritage. In physical geography , the geographical delineation for the subregion is the portion of Africa south of the Cunene and Zambezi Rivers: Botswana, Eswatini, Lesotho, Namibia, South Africa, Zimbabwe, and the part of Mozambique that lies south of the Zambezi River. That definition is most often used in South Africa for natural sciences and particularly in guidebooks such as Roberts' Birds of Southern Africa ,
3400-422: The largest of these land areas being the interior of Asia. In deserts, water inflow is low and loss to solar evaporation high, drastically reducing the formation of complete drainage systems . In the extreme case, where there is no discernible drainage system, the basin is described as arheic . Closed water flow areas often lead to the concentration of salts and other minerals in the basin. Minerals leached from
3468-439: The north and temperate in the south, but also includes humid-subtropical , Mediterranean-climate , highland-subtropical , oceanic, desert, and semi-arid regions. Except for lower parts of Zambia and interior areas of Namibia and Botswana, the region rarely suffers from extreme heat. In addition, the winter presents mostly as mild and dry, except in the southwest. Cool southeasterly winds and high humidity bring cool conditions in
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#17328454382163536-462: The other in the south ( Kingdom of Butua from 1450–1683) which was a smaller entity than the former two, the kingdom was governed by the Torwa dynasty and its capital was situated at Khami . Both states would eventually be absorbed by the powerful Shona state, the Rozwi Empire by 1683. The economy was based on cattle herding, farming, and gold mining. The empire lasted until 1866, which came after droughts and instability. The Mthethwa Paramountcy
3604-408: The period of colonial rule, imperial interests controlled the economies of the region and South Africa became the dominant economic power in the late 20th century. The 21st century has seen attempts to create unity among nations in Southern Africa. In spite of democracy, violence , inequality and poverty still persist throughout the region. The region is distinct from the rest of Africa, with
3672-782: The reality of a region with large urban populations and where food insecurity goes beyond per-capita availability to issues of access and dietary adequacy. Urban food security has been noted as an emerging area of concern in the region, with recent data showing high levels of food insecurity amongst low-income households. In a study of eleven cities in nine countries: Blantyre , Cape Town , Gaborone , Harare , Johannesburg , Lusaka , Maputo , Manzini , Maseru , Durban , and Windhoek , only 17% of households were categorized as 'food-secure' while more than half (57%) of all households surveyed were found to be 'severely food-insecure'. Some factors affecting urban food insecurity include climate change with potential impact on agricultural productivity,
3740-679: The region largely lags behind their Asian counterparts in innovation, foreign direct investment, STEM sciences and research and development . Southern Africa has a wide diversity of ecoregions including grassland , bushveld , karoo , savannah and riparian zones . Even though considerable disturbance has occurred in some regions from habitat loss due to human population density or export-focused development, there remain significant numbers of various wildlife species, including white rhino , lion , African leopard , impala , kudu , blue wildebeest , vervet monkey and elephant . It has complex Plateaus that create massive mountain structures along
3808-748: The regions including political instability, poor governance, droughts, population growth, urbanisation, poverty, low economic growth, inadequate agricultural policies, trade terms and regimes, resource degradation and the recent increase in HIV/AIDS . These factors vary from country to country. For example, the Democratic Republic of the Congo has favourable climatic and physical conditions, but performs far below its capacity in food provision due to political instability and poor governance. In contrast, semi-arid countries such as Botswana and Namibia, produce insufficient food, but successfully achieve food security through food imports due to economic growth, political stability and good governance. The Republic of South Africa
3876-599: The surrounding rocks are deposited in the basin, and left behind when the water evaporates. Thus endorheic basins often contain extensive salt pans (also called salt flats, salt lakes, alkali flats , dry lake beds, or playas). These areas tend to be large, flat hardened surfaces and are sometimes used for aviation runways , or land speed record attempts, because of their extensive areas of perfectly level terrain. Both permanent and seasonal endorheic lakes can form in endorheic basins. Some endorheic basins are essentially stable because climate change has reduced precipitation to
3944-474: The sustainable management of the entire river system. This Southern African location article is a stub . You can help Misplaced Pages by expanding it . Endorheic basin An endorheic basin ( / ˌ ɛ n d oʊ ˈ r iː . ɪ k / EN -doh- REE -ik ; also endoreic basin and endorreic basin ) is a drainage basin that normally retains water and allows no outflow to other external bodies of water (e.g. rivers and oceans ); instead,
4012-517: The water drainage flows into permanent and seasonal lakes and swamps that equilibrate through evaporation . Endorheic basins are also called closed basins , terminal basins , and internal drainage systems . Endorheic regions contrast with open lakes (exorheic regions), where surface waters eventually drain into the ocean. In general, water basins with subsurface outflows that lead to the ocean are not considered endorheic; but cryptorheic . Endorheic basins constitute local base levels , defining
4080-428: The water level in the terminal lake to rise until it finds an outlet, breaking the enclosed endorheic hydrological system's geographical barrier and opening it to the surrounding terrain. The Black Sea was likely such a lake, having once been an independent hydrological system before the Mediterranean Sea broke through the terrain separating the two. Lake Bonneville was another such lake, overflowing its basin in
4148-407: The waters of the basin enter a zone of strong evaporation, already within the Kalahari Desert depression. A series of salt pans lie in the lowest points of the basin, including the Nwako Pan south of the Okavango Delta and the vast Makgadikgadi Pan southeast of the Delta. At times of high flow, the Okavango spills into the Nwako Pan via the Xudum and Nhabe distributaries to replenish Lake Ngami ,
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#17328454382164216-422: The wealthiest regions of Africa with the greatest potential for economic growth . A chain of mineral resources in Southern Africa stretches from the rich oil fields in northwest Angola, east through the central diamond-mining region in Huambo Province , and into the Copper Belt region of Zambia and Congo. A region of rich mineral deposits continues to the south called the Great Dyke in central Zimbabwe, through
4284-489: The wetter and higher East from the Atlantic Ocean . In addition, the Drakensberg and Eastern Highlands separate the highland areas and coastal plains centred on Mozambique in the north and KwaZulu-Natal in the south, the latter of which are often prone to flooding every few years. In the east, the river systems of the Zambezi and Limpopo basin form natural barriers and sea lanes between Mozambique, South Africa, and Zimbabwe. Across most of southern Africa, apart from
4352-434: The winter. The Namib Desert is the driest area in the region. Altitude plays an outsize role in moderating the temperatures of the South African Highveld , Lesotho , and much of Zambia and Zimbabwe. The prairie region of central and northeast South Africa, the country of Zimbabwe, and parts of Zambia are known as the veldt , divided into the Bushveld and Highveld . There are high temperatures and low rainfall within
4420-424: The years, some the other Southern African nations have invested in economic diversification, and invested public funds into rail, road and air transportation as part of a concerted effort through SADC to boost regional trade and improve communication and transportation. The countries in this region also belong to the Southern Africa Power Pool, which facilitates the development of a competitive electricity market within
4488-466: Was a Shona ( Karanga ) kingdom in what is today Zimbabwe . The capital, which sits near present-day Masvingo , is located at Great Zimbabwe , which are the largest stone structure in precolonial Southern Africa. This kingdom came after the collapse of the Kingdom of Mapungubwe. During the decline of the Kingdom of Zimbabwe, two powers emerged, one in the north ( Kingdom of Mutapa from 1430–1760) which had improved on Zimbabwe's administrative structure; and
4556-415: Was an African state that emerged in the late 18th-century in the region of present-day KwaZulu-Natal . The state was consolidated and extended under the rule of Dingiswayo who produced a disciplined and highly organised army for the first time in the region. The Zulu Kingdom rose under the leadership of Shaka and covered most of present-day KwaZulu-Natal in the 19th century. Internal conflict arose in
4624-438: Was complicated by the settlement of white peoples . After an initial phase from 1945 to 1958, as a consolidation of white power, decolonization succeeded in its achievement when High Commission territories and overseas departments such as Zambia , Malawi , Botswana , Lesotho , Mauritius , Swaziland , Madagascar and the Comoros became independent states from British and French rule. The brutal struggle for independence in
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