Zimbabwe, officially the Republic of Zimbabwe, is a landlocked country in Southeast Africa, bordered by South Africa to the south, Botswana to the southwest, Zambia to the north, and Mozambique to the east. A country of roughly 16.9 million people as per 2024 estimates, Zimbabwe's largest ethnic group are the Shona, who make up 80% of the population, followed by the Northern Ndebele and other smaller minorities. Zimbabwe has 16 official languages, with English, Shona, and Ndebele the most common.
The name "Zimbabwe" stems from a Shona term for Great Zimbabwe, a medieval city (Masvingo) in the country's south-east. Many sources hold that "Zimbabwe" derives from dzimba-dza-mabwe, translated from the Karanga dialect of Shona as "houses of stones" (dzimba = plural of imba, "house"; mabwe = plural of ibwe, "stone"). The Karanga-speaking Shona people live around Great Zimbabwe in the modern-day Masvingo province. Zimbabwe was formerly known as Southern Rhodesia (1898), Rhodesia (1965), and Zimbabwe Rhodesia (1979). Like those of many African countries that gained independence during the Cold War, Zimbabwe is an ethnically neutral name.
Let's delve into some key aspects of this nation, focusing on its capital, Harare.
I Didn't Expect Zimbabwe's Capital To Look Like This - Harare (the most underrated African city) 🇿🇼
Location of Zimbabwe in Africa
Historical Overview
Archaeological records date archaic human settlement of present-day Zimbabwe to at least 500,000 years ago. Zimbabwe's earliest known inhabitants were most likely the San people, who left behind a legacy of arrowheads and cave paintings. Societies speaking proto-Shona languages first emerged in the middle Limpopo River valley in the 9th century before moving on to the Zimbabwean highlands. The Zimbabwean plateau became the centre of subsequent Shona states, beginning around the 10th century. Around the early 10th century, trade developed with Arab merchants on the Indian Ocean coast, helping to develop the Kingdom of Mapungubwe in the 13th century.
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This was the precursor to the Shona civilisations that dominated the region from the 13th century, evidenced by ruins at Great Zimbabwe, near Masvingo, and by other smaller sites. The main archaeological site used a unique dry stone architecture. The Kingdom of Mapungubwe was the first in a series of trading states which had developed in Zimbabwe by the time the first European explorers arrived from Portugal. By 1300, the Kingdom of Zimbabwe eclipsed Mapungubwe. This Shona state further refined and expanded upon Mapungubwe's stone architecture.
From c. 1450 to 1760, the Kingdom of Mutapa ruled much of the area of present-day Zimbabwe, plus parts of central Mozambique. It is known by many names including the Mutapa Empire, also known as Mwene Mutapa or Monomotapa as well as "Munhumutapa", and was renowned for its strategic trade routes with the Arabs and Portugal. As a direct response to increased European presence in the interior a new Shona state emerged, known as the Rozwi Empire. Relying on centuries of military, political and religious development, the Rozwi (meaning "destroyers") expelled the Portuguese from the Zimbabwean plateau in 1683.
Around 1821 the Zulu general Mzilikazi of the Khumalo clan successfully rebelled against King Shaka and established his own clan, the Ndebele. The Ndebele fought their way northwards into the Transvaal, leaving a trail of destruction in their wake and beginning an era of widespread devastation known as the Mfecane. When Dutch trekboers converged on the Transvaal in 1836, they drove the tribe even further northward, with the assistance of Tswana Barolong warriors and Griqua commandos. After losing their remaining South African lands in 1840, Mzilikazi and his tribe permanently settled in the southwest of present-day Zimbabwe in what became known as Matabeleland, establishing Bulawayo as their capital. Mzilikazi then organised his society into a military system with regimental kraals, similar to those of Shaka, which was stable enough to repel further Boer incursions.
In the 1880s, European colonists arrived with Cecil Rhodes's British South Africa Company (chartered in 1889). In 1888, Rhodes obtained a concession for mining rights from King Lobengula of the Ndebele peoples. He presented this concession to persuade the government of the United Kingdom to grant a royal charter to the company over Matabeleland, and its subject states such as Mashonaland as well. Rhodes used this document in 1890 to justify sending the Pioneer Column, a group of Europeans protected by well-armed British South Africa Police (BSAP) through Matabeleland and into Shona territory to establish Fort Salisbury (present-day Harare), and thereby establish company rule over the area.
In 1893 and 1894, with the help of their new Maxim guns, the BSAP would go on to defeat the Ndebele in the First Matabele War. In 1895, the BSAC adopted the name "Rhodesia" for the territory, in honour of Rhodes. In 1898, "Southern Rhodesia" became the official name for the region south of the Zambezi river, which later adopted the name "Zimbabwe". The region to the north, administered separately, was later termed Northern Rhodesia (present-day Zambia).
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Shortly after the disastrous Rhodes-sponsored Jameson Raid on the South African Republic, the Ndebele rebelled against white rule, led by their charismatic religious leader, Mlimo. The Second Matabele War of 1896-1897 lasted in Matabeleland until 1896, when Mlimo was assassinated by American scout Frederick Russell Burnham. The United Kingdom annexed Southern Rhodesia on 12 September 1923. Shortly after annexation, on 1 October 1923, the first constitution for the new Colony of Southern Rhodesia came into force. Under the new constitution, Southern Rhodesia became a self-governing British colony, subsequent to a 1922 referendum.
Rhodesians of all races served on behalf of the United Kingdom during the two World Wars in the early-20th century. The 1930 Land Apportionment Act restricted black land ownership to certain segments of the country, setting aside large areas solely for the purchase of the white minority. This act, which led to rapidly rising inequality, became the subject of frequent calls for subsequent land reform.
In 1953, in the face of African opposition, Britain consolidated the two Rhodesias with Nyasaland (Malawi) in the ill-fated Central African Federation, which Southern Rhodesia essentially dominated. Growing African nationalism and general dissent, particularly in Nyasaland, persuaded Britain to dissolve the union in 1963, forming three separate divisions. Following Zambian independence (effective from October 1964), Ian Smith's Rhodesian Front government in Salisbury dropped the designation "Southern" in 1964 (once Northern Rhodesia had changed its name to Zambia, having the word Southern before the name Rhodesia became unnecessary and the country simply became known as Rhodesia afterwards).
Intent on effectively repudiating the recently adopted British policy of "no independence before majority rule", Smith issued a Unilateral Declaration of Independence (UDI) from the United Kingdom on 11 November 1965. The United Kingdom deemed the Rhodesian declaration an act of rebellion but did not re-establish control by force. The British government petitioned the United Nations for sanctions against Rhodesia pending unsuccessful talks with Smith's administration in 1966 and 1968.
A civil war ensued when Joshua Nkomo's Zimbabwe African People's Union (ZAPU) and Robert Mugabe's Zimbabwe African National Union (ZANU), supported actively by communist powers and neighbouring African nations, initiated guerrilla operations against Rhodesia's predominantly white government. ZAPU was supported by the Soviet Union, the Warsaw Pact and associated nations such as Cuba, and adopted a Marxist-Leninist ideology; ZANU meanwhile aligned itself with Maoism and the bloc headed by the People's Republic of China. Smith declared Rhodesia a republic in 1970, following the results of a referendum the previous year, but this went unrecognised internationally.
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In March 1978, Smith reached an accord with three African leaders, led by Bishop Abel Muzorewa, who offered to leave the white population comfortably entrenched in exchange for the establishment of a biracial democracy. As a result of the Internal Settlement, elections were held in April 1979, concluding with the United African National Council (UANC) carrying a majority of parliamentary seats. On 1 June 1979, Muzorewa, the UANC head, became prime minister and the country's name was changed to Zimbabwe Rhodesia.
Following the fifth Commonwealth Heads of Government Meeting, held in Lusaka, Zambia, from 1 to 7 August in 1979, the British government invited Muzorewa, Mugabe, and Nkomo to participate in a constitutional conference at Lancaster House. The purpose of the conference was to discuss and reach an agreement on the terms of an independence constitution, and provide for elections supervised under British authority allowing Zimbabwe Rhodesia to proceed to legal independence. With Lord Carrington, Secretary of State for Foreign and Commonwealth Affairs of the United Kingdom, in the chair, these discussions were mounted from 10 September to 15 December in 1979, producing a total of 47 plenary sessions.
On 21 December 1979, delegations from every major interest represented reached the Lancaster House Agreement, effectively ending the guerrilla war. On 11 December 1979, the Rhodesian House of Assembly voted 90 to nil to revert to British colonial status. With the arrival of Christopher Soames, the new governor on 12 December 1979, Britain formally took control of Zimbabwe Rhodesia as the Colony of Southern Rhodesia. Britain lifted sanctions on 12 December and the United Nations on 16 December.
During the 1980 Southern Rhodesian general election, Mugabe and the ZANU party secured a landslide victory. On 11 April 1980, Southern Rhodesia became the independent nation of Zimbabwe. Zimbabwe's first president after its independence was Canaan Banana in what was originally a mainly ceremonial role as head of state.
Opposition to what was perceived as a Shona takeover immediately erupted around Matabeleland. During the 1990s, students, trade unionists, and other workers often demonstrated to express their growing discontent with Mugabe and ZANU-PF party policies. In 1996, civil servants, nurses, and junior doctors went on strike over salary issues. The general health of the population also began to significantly decline; by 1997 an estimated 25% of the population had been infected by HIV in a pandemic that was affecting most of southern Africa.
Land redistribution re-emerged as the main issue for the ZANU-PF government around 1997. President Mugabe and the ZANU-PF party leadership found themselves beset by a wide range of international sanctions. In 2002, the nation was suspended from the Commonwealth of Nations due to the reckless farm seizures and blatant election tampering. The following year, Zimbabwean officials voluntarily terminated its Commonwealth membership. In 2001, the United States enacted the Zimbabwe Democracy and Economic Recovery Act (ZDERA).
By 2003, the country's economy had collapsed. It is estimated that up to a quarter of Zimbabwe's 11 million people had fled the country. On 29 March 2008, Zimbabwe held a presidential election along with a parliamentary election. The results of this election were withheld for two weeks, after which it was generally acknowledged that the Movement for Democratic Change - Tsvangirai (MDC-T) had achieved a majority of one seat in the lower house of parliament.
In September 2008, a power-sharing agreement was reached between Morgan Tsvangirai and President Mugabe, permitting the former to hold the office of prime minister. Due to ministerial differences between their respective political parties, the agreement was not fully implemented until 13 February 2009. In July 2016, nationwide protests took place regarding the economic collapse in the country. In November 2017, the army led a coup d'état following the dismissal of Vice-president Emmerson Mnangagwa, placing Mugabe under house arrest.
Geographical Context
Zimbabwe is a landlocked country in southern Africa. It shares a 125-mile (200-kilometre) border on the south with the Republic of South Africa and is bounded on the southwest and west by Botswana, on the north by Zambia, and on the northeast and east by Mozambique. The capital is Harare (formerly called Salisbury).
Zimbabwe lies almost entirely over 1,000 feet (300 metres) above sea level. Its principal physical feature is the broad ridge running 400 miles from southwest to northeast across the entire country, from Plumtree near the Botswana frontier through Gweru (formerly Gwelo) and Marondera (formerly Marandellas) to the Inyanga Mountains, which separate Zimbabwe from Mozambique. About 50 miles wide, this ridge ranges in altitude from 4,000 to 5,000 feet, until it eventually rises to 8,504 feet (2,592 metres) at Mount Inyangani, the highest point in Zimbabwe, in the eastern highlands. This ridge is known as the Highveld and comprises about 25 percent of the country’s total area.
On each side of this central spine, sloping down northward to the Zambezi River and southward to the Limpopo River, lies the wider plateau of the Middleveld, which, at an altitude between about 3,000 and 4,000 feet, makes up roughly 40 percent of Zimbabwe’s area. Beyond this again and mostly in the south, where the Sabi, Lundi, and Nuanetsi rivers drain from the plateau into the Limpopo, lies the Lowveld, which constitutes approximately 23 percent of the country’s total area. The lowest point in Zimbabwe lies at an altitude of 660 feet near Dumela, where the Limpopo flows into Mozambique.
Map of Zimbabwe with regions and cities
Landscape Features
The landscape is characterized by extensive outcroppings of Precambrian rock, which is between about 570 million and 4 billion years old. The most ancient part of this rock formation, known as the basement complex, covers the greater part of the country. About four-fifths of the basement complex consists of granite; the Matopo (Matopos) Hills south of the city of Bulawayo are formed from prolonged erosion of an exposed granite batholith. Some of the hills are surmounted by formations, known as balancing rocks, that have been eroded by wind and water along regular fault lines, leaving some blocks precariously balanced upon others.
Elsewhere are found innumerable small rounded granite hillocks known locally as kopjes. Belts of schist in the basement complex contain the veins and lodes of most of the country’s gold, silver, and other commercial minerals. The Great Dyke, which is up to 8 miles wide and about 330 miles long, is another notable landscape feature. The longest linear mass of mafic and ultramafic rocks in the world, the Great Dyke bisects the country from north to south and contains enormous reserves of chromium, nickel, and platinum. The Alkali Ring complexes near Beitbridge in the Sabi valley are distinctive igneous intrusions.
The Karoo (Karroo) System-a thick layer of sedimentary rocks consisting of shale, sandstone, and grit of Permian and Triassic age (about 200 to 300 million years old)-covers the Zambezi valley and the valleys of its tributaries from Hwange (formerly Wankie) southward to Bulawayo and spreads across parts of the southern Lowveld from Tuli, near the southern border, to the Sabi River.
Drainage and Soils
Major faulting from southwest to northeast formed the middle Zambezi trough, which is now partially flooded by the Lake Kariba reservoir. Other faulting episodes affected the depressions of the Sabi (Save) and Limpopo rivers. Except for a small area of internal drainage in the dry southwest, these three rivers carry the entire runoff of the country to the Indian Ocean via Mozambique.
The light, sandy soils found in most parts of Zimbabwe are residual soils developed largely from the granite parent material. They are highly weathered and leached, even in the areas of lower rainfall, and do not easily retain water because of their coarse texture. Outcrops of basement schists give rise to rich red clays and loams-some of the country’s best soils-but their extent is limited. Since most rain occurs in heavy showers during a few months of the year, rapid runoff and high rates of erosion are common.
The meagre mineral reserves in most soils imply an inherently low fertility; under cultivation, productivity drops rapidly after a few years. The difficulty of cultivating these lighter soils is greatest in the Black farming areas, where population pressure no longer allows land to be temporarily abandoned to rejuvenate after cultivation; Black farmers, because of a lack of capital, are also less able than white farmers to maintain the mineral fertility with manure and chemical fertilizers.
Demographic and Economic Impact
If the rate of population growth in 1980 had been maintained, the population would have been 31 million as of 2018. Instead, it is about 13 million. The discrepancies were believed to be partly caused by death from starvation and disease, and partly due to decreased fertility. The life expectancy has halved, and deaths from politically motivated violence sponsored by the government exceed 200,000 since 1980.
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