95-604: The Chongwe River is a river in Zambia . The river begins to the north east of the capital Lusaka , and alongside the larger Kafue River , drains into the Zambezi River . 15°42′57″S 29°20′22″E / 15.71583°S 29.33944°E / -15.71583; 29.33944 This article related to a river in Zambia is a stub . You can help Misplaced Pages by expanding it . Zambia Zambia , officially
190-536: A Luba hunter named Chibinda Ilunga , son of Ilunga Mbidi Kiluwe , introduced the Luba model of statecraft to the Lunda sometime around 1600 when he married a local Lunda princess named Lueji and was granted control of her kingdom. Most rulers who claimed descent from Luba ancestors were integrated into the Luba empire. The Lunda kings, however, remained separate and actively expanded their political and economic dominance over
285-535: A chief or headman and worked as a community and helped each other in times of field preparation for their crops. Villages moved around frequently as the soil became exhausted as a result of the slash-and-burn technique of planting crops. The people also kept large herds of cattle, which formed an important part of their societies. The first Bantu communities in Zambia were highly self-sufficient. Early European missionaries who settled in Southern Zambia noted
380-591: A different impact on the ecosystems of the delta from today, as it brought nutrient-rich fresh water down to the Indian Ocean coastal wetlands. The lower Zambezi experienced a small flood surge early in the dry season as rain in the Gwembe catchment and north-eastern Zimbabwe rushed through while rain in the upper Zambezi, Kafue, and Lake Malawi basins, and Luangwa to a lesser extent, is held back by swamps and floodplains. The discharges of these systems contribute to
475-534: A distance from the vices and modus vivendi of ordinary people. Nkongolo Mwamba symbolizes the embodiment of tyranny, whereas Mbidi Kiluwe remains the admired caring and compassionate kin. In the same region of Southern Congo, the Lunda people were made into a satellite of the Luba empire and adopted forms of Luba culture and governance, thus becoming the Lunda Empire to the south. According to Lunda genesis myths,
570-416: A haven for migratory waterbirds, including pintails , garganey , African openbill ( Anastomus lamelligerus ), saddle-billed stork ( Ephippiorhynchus senegalensis ), wattled crane ( Bugeranus carunculatus ), and great white pelican ( Pelecanus onocrotalus ). Reptiles include Nile crocodile ( Crocodylus niloticus ), Nile monitor lizard ( Varanus niloticus ), African rock python ( Python sebae ),
665-657: A millennia-long expansion into much of the continent. This event has been called the Bantu expansion ; it was one of the largest human migrations in history. The Bantu are believed to have been the first to have brought iron working technology into large parts of Africa. The Bantu Expansion happened primarily through two routes: a western one via the Congo Basin and an eastern one via the African Great Lakes. The first Bantu people to arrive in Zambia came through
760-469: A much larger flood in March or April, with a mean monthly maximum for April of 6,700 m (240,000 cu ft) per second at the delta. The record flood was more than three times as big, 22,500 m (790,000 cu ft) per second being recorded in 1958. By contrast, the discharge at the end of the dry season averaged just 500 m (18,000 cu ft) per second. In the 1960s and 1970s,
855-549: A reputation as great cloth traders throughout the region. In a curious note, Goese-born Portuguese trader Manuel Caetano Pereira, who traveled to the Bisa homelands in 1796, was surprised to be shown a second, separate river referred to as the "Zambezi". This "other Zambezi" that puzzled Pereira is most likely what modern sources spell the Chambeshi River in northern Zambia. The Monomatapa notion (reported by Santos) that
950-575: A result of both Atlantic slave trade in the west and Indian Ocean slave trade in the east and wars with breakaway factions of the kingdoms. The Chokwe , a group that is closely related to the Luvale and formed a Lunda satellite state, initially suffered from the European demand for slaves, but once they broke away from the Lunda state, they themselves became notorious slave traders, exporting slaves to both coasts. The Chokwe eventually were defeated by
1045-580: A result, they grew a diverse economy trading fish, copper and iron items and salt for goods from other parts of Africa, like the Swahili coast and, later on, the Portuguese. From these communities arose the Luba Kingdom in the 14th century. The Luba Kingdom was a large kingdom with a centralised government and smaller independent chiefdoms . It had large trading networks that linked the forests in
SECTION 10
#17327762727081140-534: Is joined by sizeable tributaries such as the Luena and the Chifumage flowing from highlands to the north-west. It turns south and develops a floodplain , with extreme width variation between the dry and rainy seasons. It enters dense evergreen Cryptosepalum dry forest , though on its western side, Western Zambezian grasslands also occur. Where it re-enters Zambia, it is nearly 400 m (1,300 ft) wide in
1235-601: Is lost through evaporation in its swamp systems. The 1940s and 1950s were particularly wet decades in the basin. Since 1975, it has been drier, the average discharge being only 70% of that for the years 1930 to 1958. Up to the Late Pliocene or Pleistocene (more than two million years ago), the upper Zambezi flowed south through what is now the Makgadikgadi Pan to the Limpopo River . The change of
1330-518: Is not included in the figures because it only occasionally overflows to any extent into the Zambezi. Because of the rainfall distribution, northern tributaries contribute much more water than southern ones; for example: The Northern Highlands catchment of the upper Zambezi contributes 25%, Kafue 8%, Luangwa and Shire Rivers 16% each, total 65% of Zambezi discharge. The large Cuando basin in the south-west, though, contributes only about 2 m /s because most
1425-521: Is obstructed by a sand bar . A more northerly branch, called the Chinde mouth, has a minimum depth at low water of 2 metres (6 ft 7 in) at the entrance and 4 metres (13 ft) further in, and is the branch used for navigation. About 100 kilometres (62 mi) further north is a river called the Quelimane , after the town at its mouth. This stream, which is silting up, receives the overflow of
1520-481: Is sandy, and the banks are low and reed-fringed. At places, however, and especially in the rainy season, the streams unite into one broad, fast-flowing river. About 160 kilometres (99 mi) from the sea, the Zambezi receives the drainage of Lake Malawi through the Shire River . On approaching the Indian Ocean, the river splits up into a delta . Each of the primary distributaries, Kongone, Luabo, and Timbwe,
1615-566: Is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers 1,390,000 km (540,000 sq mi), slightly less than half of the Nile 's. The 2,574 km (1,599 mi) river rises in Zambia and flows through eastern Angola , along the north-eastern border of Namibia and
1710-618: Is today Zambia, Malawi, Mozambique and Tanzania and assimilated into neighbouring tribes. In the western part of Zambia, another Southern African group of Sotho-Tswana heritage called the Kololo manage to conquer the local inhabitants who were migrants from the fallen Luba and Lunda states called the Luyana or Aluyi. The Luyana established the Barotse Kingdom on the floodplains of the Zambezi upon their arrival from Katanga. Under
1805-546: Is very uniform, dropping only by another 180 m (590 ft) across a distance of around 800 km (500 mi). The first of its large tributaries to enter the Zambezi is the Kabompo River in the North-Western Province of Zambia. The savanna through which the river flows gives way to a wide floodplain, studded with Borassus fan palms . A little farther south is the confluence with
1900-519: The Arab world . The African traders were later joined by the Portuguese in the 16th century. The decline of Great Zimbabwe, due to increasing trade competition from other Kalanga/Shona kingdoms like Khami and Mutapa , spelt the end of Ingombe Ilede. The second mass settlement of Bantu people into Zambia was of people groups that are believed to have taken the western route of the Bantu migration through
1995-574: The Chikunda . After the decline of the Portuguese the Chikunda made their way to Zambia. It is hypothesised by Julian Cobbing that the presence of early Europeans slave trading and attempts to control resources in various parts of Bantu-speaking Africa caused the gradual militarization of the people in the region. This can be observed with the Maravi's WaZimba warrior caste, who, once defeating
SECTION 20
#17327762727082090-496: The Congo Basin and the mineral-rich plateaus of what is today Copperbelt Province and stretched from the Atlantic coast to the Indian Ocean coast. The arts were also held in high esteem in the kingdom, and artisans were held in high regard. Literature was well developed in the Luba Kingdom. One renowned Luba genesis story that articulated the distinction between two types of Luba emperors goes as follows: Nkongolo Mwamba ,
2185-640: The Congo Basin to Lake Mweru then finally settled around Lake Malawi . These migrants are believed to have been one of the inhabitants around the Upemba area in the Democratic Republic of Congo . By the 1400s these groups of migrants collectively called the Maravi, and most prominently among them was the Chewa people (AChewa), who started assimilating other Bantu groups like the Tumbuka . In 1480
2280-545: The Ikelenge District of North-Western Province , Zambia, at about 1,524 metres (5,000 ft) above sea level . The area around the source is a national monument, forest reserve, and important bird area . Eastward of the source, the watershed between the Congo and Zambezi Basins is a well-marked belt of high ground, running nearly east–west and falling abruptly to the north and south. This distinctly cuts off
2375-736: The Itezhi-Tezhi Dam 's deleterious effects on the Kafue Flats, this has these effects: The Zambezi Delta has extensive seasonally and permanently flooded grasslands, savannas, and swamp forests. Together with the floodplains of the Buzi , Pungwe , and Save Rivers, the Zambezi's floodplains make up the World Wildlife Fund 's Zambezian coastal flooded savanna ecoregion in Mozambique. The flooded savannas lie close to
2470-731: The Kafue Flats and the Lukanga Twa who lived around the Lukanga Swamp . Many examples of ancient rock art in Zambia, like the Mwela Rock Paintings , Mumbwa Caves , and Nachikufu Cave, are attributed to these early hunter-gatherers. The Khoisan and especially the Twa formed a patron-client relationship with farming Bantu peoples across central and southern Africa but were eventually either displaced by or absorbed into
2565-579: The Kuomboka . After Lealui, the river turns south-southeast. From the east, it continues to receive numerous small streams, but on the west, it is without major tributaries for 240 km. Before this, the Ngonye Falls and subsequent rapids interrupt navigation. South of Ngonye Falls, the river briefly borders Namibia's Caprivi Strip . Below the junction of the Cuando River and the Zambezi,
2660-786: The Lamba , Bisa , Senga , Kaonde , Swaka, Nkoya and Soli , formed integral parts of the Luba Kingdom in Upemba part of the Democratic Republic of Congo and have a strong relation to the BaLuba people . The area which the Luba Kingdom occupied has been inhabited by early farmers and iron workers since the 300s C.E. Over time, these communities learned to use nets and harpoons, make dugout canoes, clear canals through swamps and make dams as high as 2.5 meters (8 ft 2 in). As
2755-610: The Lungwebungu River . This is the beginning of the Barotse Floodplain , the most notable feature of the upper Zambezi, but this northern part does not flood so much and includes islands of higher land in the middle. About 30 km below the confluence of the Lungwebungu, the country becomes very flat, and the typical Barotse Floodplain landscape unfolds, with the flood reaching a width of 25 km in
2850-597: The Maravi Empire was founded by the kalonga (paramount chief of the Maravi) from the Phiri clan, one of the main clans, with the others being Banda, Mwale and Nkhoma. The Maravi Empire stretched from the Indian Ocean through what today is Mozambique to Zambia and large parts of Malawi . The political organization of the Maravi resembled that of the Luba and is believed to have originated from there. The primary export of
2945-528: The Quelimane or Quá-Qua, a small river on the northern end of the delta, which at that time was connected by navigable channels to the Zambezi River proper (the connection silted up by the 1830s). In a few of the oldest maps, the entire river is denoted as such. By the 16th century, a new name emerged, the Cuama River (sometimes "Quama" or "Zuama"). Cuama was the local name given by the dwellers of
Chongwe River - Misplaced Pages Continue
3040-579: The Republic of Zambia , is a landlocked country at the crossroads of Central , Southern and East Africa . It is typically referred to being in South-Central Africa or Southern Africa. It is bordered to the north by the Democratic Republic of the Congo , Tanzania to the north-east, Malawi to the east, Mozambique to the southeast, Zimbabwe and Botswana to the south, Namibia to
3135-679: The Swahili coast for an outpost located on one of the southerly islands of the delta (near the Luabo channel). Most old nautical maps denote the Luabo entry as Cuama, the entire delta as the "rivers of Cuama", and the Zambezi proper as the "Cuama River". In 1552, Portuguese chronicler João de Barros noted that the same Cuama River was called Zembere by the inland people of Monomatapa . The Portuguese Dominican friar João dos Santos , visiting Monomatapa in 1597 reported it as Zambeze (Bantu languages frequently shifts between z and r) and inquired into
3230-717: The World Bank named Zambia among the top 10 reformers in the World Bank's Ease of doing business index . As of the latest estimate in 2018, 47.9 percent of the population is affected by multidimensional poverty . The Common Market for Eastern and Southern Africa (COMESA) is headquartered in Lusaka. The territory of Zambia was known as Northern Rhodesia from 1911 to 1964. It was renamed Zambia in October 1964 on its independence from British rule. The name Zambia derives from
3325-555: The Yao . As Great Zimbabwe was in decline, one of its princes, Nyatsimba Mutota , broke away from the state forming a new empire called Mutapa . The title of Mwene Mutapa, meaning "Ravager of the Lands", was bestowed on him and subsequent rulers. The Mutapa Empire ruled territory between the Zambezi and Limpopo rivers, in what is now Zambia, Zimbabwe and Mozambique, from the 14th to
3420-672: The Zambezi River (Zambezi may mean "the grand river"). Archaeological excavation work on the Zambezi Valley and Kalambo Falls shows a succession of human cultures. Ancient camp site tools near the Kalambo Falls have been radiocarbon dated to more than 36,000 years ago. The fossil skull remains of the Broken Hill Man (also known as Kabwe Man), dated between 300,000 and 125,000 years BC, further shows that
3515-463: The "Espirito Santo" Rivers converging deep in the interior, at the same lake. However, the Bisa-derived etymology is not without dispute. In 1845, W.D. Cooley, examining Pereira's notes, concluded the term "Zambezi" derives not from the Bisa people, but rather from the Bantu term "mbege"/"mbeze" ("fish"), and consequently it probably means merely "river of fish". David Livingstone , who reached
3610-569: The 17th century. By its, peak Mutapa had conquered the Dande area of the Tonga and Tavara. The Mutapa Empire predominately engaged in the Indian Ocean transcontinental trade with and via the WaSwahili . The primary exported gold and ivory for silk and ceramics from Asia. Like their contemporaries in Maravi, Mutapa had problems with the arriving Portuguese traders. The peak of this uneasy relationship
3705-638: The 18th century, the British colonised the region into the British protectorates of Barotziland–North-Western Rhodesia and North-Eastern Rhodesia towards the end of the 19th century. These were merged in 1911 to form Northern Rhodesia . For most of the colonial period, Zambia was governed by an administration appointed from London with the advice of the British South Africa Company . On 24 October 1964, Zambia became independent of
3800-484: The Bantu groups. The Bantu people or Abantu (meaning people) are an enormous and diverse ethnolinguistic group that comprise the majority of people in much of eastern, southern and central Africa. Due to Zambia's location at the crossroads of Central Africa, Southern Africa, and the African Great Lakes , the history of the people that constitute modern Zambians is a history of these three regions. Many of
3895-445: The Batoka Gorge, the current being continually interrupted by reefs. It has been described as one of the world's most spectacular whitewater trips, a tremendous challenge for kayakers and rafters alike. Beyond the gorge are a succession of rapids that end 240 km (150 mi) below Victoria Falls. Over this distance, the river drops 250 m (820 ft). At this point, the river enters Lake Kariba , created in 1959 following
Chongwe River - Misplaced Pages Continue
3990-431: The Congo Basin. These Bantu people spent the majority of their existence in what is today the Democratic Republic of Congo and are ancestors of the majority of modern Zambians. While there is some evidence that the Bemba people or AbaBemba have a strong ancient connection to the Kongo Kingdom through BaKongo ruler Mwene Kongo VIII Mvemba , this is not well documented. The Bemba, along with other related groups like
4085-411: The East African Swahili coast . Ingombe Ilede was one of the most important trading posts for rulers of Great Zimbabwe, others being the Swahili port cities like Sofala . The goods traded at Ingombe Ilede included fabrics, beads, gold, and bangles. Some of these items came from what is today southern Democratic Republic of Congo and Kilwa Kisiwani while others came from as far away as India, China and
4180-455: The Indian Ocean coast. Mangroves fringe the delta's shoreline. Although the dams have stemmed some of the annual flooding of the lower Zambezi and caused the area of floodplain to be greatly reduced, they have not removed flooding completely. They cannot control extreme floods, and they have only made medium-level floods less frequent. When heavy rain in the lower Zambezi combines with significant runoff upstream, massive floods still happen, and
4275-478: The Indian Ocean is navigable, although the river is shallow in many places during the dry season. This shallowness arises as the river enters a broad valley and spreads out over a large area. Only at one point, the Lupata Gorge , 320 kilometres (200 mi) from its mouth, is the river confined between high hills. Here, it is scarcely 200 metres (660 ft) wide. Elsewhere it is from 5 to 8 kilometres (3 to 5 mi) wide, flowing gently in many streams. The river bed
4370-438: The Kololo, the Kololo language was imposed upon the Luyana until the Luyana revolted and overthrew the Kololo by this time the Luyana language was largely forgotten and a new hybrid language emerged, SiLozi and the Luyana began to refer to themselves as Lozi . At the end of the 18th century, some of the Mbunda migrated to Barotseland , Mongu upon the migration of among others, the Ciyengele . The Aluyi and their leader,
4465-401: The Litunga Mulambwa, especially valued the Mbunda for their fighting ability. By the late 18th century, most of the various peoples of Zambia were established in their current areas. One of the earliest recorded Europeans to visit the area was the Portuguese explorer Francisco de Lacerda in the late 18th century. Lacerda led an expedition from Mozambique to the Kazembe region in Zambia (with
4560-422: The Maravi was ivory, which was transported to Swahili brokers. Iron was also manufactured and exported. In the 1590s the Portuguese endeavoured to take monopoly over Maravi export trade. This attempt was met with outrage by the Maravi of Lundu, who unleashed their WaZimba armed force. The WaZimba sacked the Portuguese trade towns of Tete, Sena and various other towns. The Maravi are also believed to have brought
4655-499: The Portuguese succumbed to disease along the Zambezi river. In the 1600s internal disputes and civil war began the decline of Mutapa. The weakened kingdom was finally conquered by the Portuguese and was eventually taken over by rival Shona states. The Portuguese also had vast estates, known as Prazos, and they used slaves and ex-slaves as security guards and hunters. They trained the men in military tactics and gave them guns. These men became expert elephant hunters and were known as
4750-410: The Portuguese, remained quite militaristic afterwards. The Portuguese presence in the region was also a major reason for the founding of the Rozvi Empire , a breakaway state of Mutapa. The ruler of the Rozvi, Changamire Dombo, became one of the most powerful leaders in South-Central Africa's history. Under his leadership, the Rozvi defeated the Portuguese and expelled them from their trading posts along
4845-422: The Swahili (and later Portuguese) upriver trade station at Sena . In 1752, the Zambezi Delta, under the name "Rivers of Sena" ( Rios de Sena ) formed a colonial administrative district of Portuguese Mozambique , but common usage of "Zambezi" led eventually to a royal decree in 1858 officially renaming the district " Zambézia ". The Zambezi region was known to medieval geographers as the Empire of Monomotapa , and
SECTION 50
#17327762727084940-404: The United Kingdom and prime minister Kenneth Kaunda became the inaugural president . Kaunda's socialist United National Independence Party (UNIP) maintained power from 1964 until 1991 with him playing a key role in regional diplomacy, cooperating closely with the United States in search of solutions to conflicts in Southern Rhodesia (Zimbabwe), Angola, and Namibia. From 1972 to 1991, Zambia
5035-418: The Zambezi in the rainy season. Average, minimum and maximum discharge of the Zambezi River at Marromeu (Lower Zambezi). Period from 1998 to 2022. The delta of the Zambezi is today about half as broad as it was before the construction of the Kariba and Cahora Bassa dams controlled the seasonal variations in the flow rate of the river. Before the dams were built, seasonal flooding of the Zambezi had quite
5130-435: The Zambezi river. But perhaps the most notable instance of this increased militarization was the rise of the Zulu under the leadership of Shaka . Pressures from the English colonialists in the Cape and increased militarization of the Zulu resulted in the Mfecane (the crushing). The Zulu expanded by assimilating the women and children of tribes they defeated, if the men of these Nguni tribes escaped slaughter, they used
5225-413: The Zambezi was sourced from a great internal lake might be a reference to one of the African Great Lakes . One of the names reported by early explorers for Lake Malawi was "Lake Zambre" (probably a corruption of "Zambezi"), possibly because Lake Malawi is connected to the lower Zambezi via the Shire River. The Monomatapa story resonated with the old European notion, drawn from classical antiquity, that all
5320-424: The area was inhabited by early humans. Broken Hill Man was discovered in Zambia in Kabwe District . Modern Zambia once was inhabited by the Khoisan and Batwa peoples until around AD 300, when migrating Bantu began to settle the areas. It is believed the Khoisan people originated in East Africa and spread southwards around 150,000 years ago. The Twa people were split into two groups: the Kafwe Twa lived around
5415-418: The basin of the Lualaba (the main branch of the upper Congo) from the Zambezi. In the neighborhood of the source, the watershed is not as clearly defined, but the two river systems do not connect. The region drained by the Zambezi is a vast, broken-edged plateau 900–1,200 m high, composed in the remote interior of metamorphic beds and fringed with the igneous rocks of the Victoria Falls. At Chupanga , on
5510-406: The building of dams changed that pattern completely. Downstream, the mean monthly minimum–maximum was 500 to 6,000 m (18,000 to 212,000 cu ft) per second; now it is 1,000 to 3,900 m (35,000 to 138,000 cu ft) per second. Medium-level floods especially, of the kind to which the ecology of the lower Zambezi was adapted, happen less often and have a shorter duration. As with
5605-445: The calm stretches of the river, as well as Nile crocodiles. Monitor lizards are found in many places. Birds are abundant, with species including heron , pelican , egret , lesser flamingo , and African fish eagle present in large numbers. Riverine woodland also supports many large animals, such as buffalo, zebras , giraffes , and elephants . The Zambezi also supports several hundred species of fish, some of which are endemic to
5700-410: The completion of the Kariba Dam . The lake is one of the largest man-made lakes in the world, and the hydroelectric power-generating facilities at the dam provide electricity to much of Zambia and Zimbabwe. The Luangwa and Kafue rivers are the two largest left-hand tributaries of the Zambezi. The Kafue joins the main river in a quiet, deep stream about 180 m (590 ft) wide. From this point,
5795-445: The confluence with the Luanginga is Lealui , one of the capitals of the Lozi people , who populate the Zambian region of Barotseland in the Western Province. The chief of the Lozi maintains one of his two compounds at Lealui; the other is at Limulunga , which is on high ground and serves as the capital during the rainy season. The annual move from Lealui to Limulunga is a major event, celebrated as one of Zambia's best-known festivals,
SECTION 60
#17327762727085890-544: The eastern route via the African Great Lakes. They arrived around the first millennium C.E, and among them were the Tonga people (also called Ba-Tonga, "Ba-" meaning "men") and the Ba-Ila and Namwanga and other related groups, who settled around Southern Zambia near Zimbabwe. Ba-Tonga oral records indicate that they came from the east near the "big sea". They were later joined by the Ba-Tumbuka who settled around Eastern Zambia and Malawi. These first Bantu people lived in large villages. They lacked an organised unit under
5985-442: The endemic Pungwe worm snake ( Leptotyphlops pungwensis ), and three other snakes that are nearly endemic - floodplain water snake ( Lycodonomorphus whytei obscuriventris ), dwarf wolf snake ( Lycophidion nanus ), and swamp viper ( Proatheris ). Several butterfly species are endemic. The north of the Zambezi basin has mean annual rainfall of 1100 to 1400 mm, which declines towards the south, reaching about half that figure in
6080-428: The falls are known as "Mosi-o-Tunya" or "thundering smoke" in the Lozi or Kololo dialect. The town of Livingstone , near the Falls, is named after him. Highly publicised accounts of his journeys motivated a wave of European visitors, missionaries and traders after his death in 1873. Zambezi (Period: 1971–2000)4,256.1 m /s (150,300 cu ft/s) The Zambezi (also spelled Zambeze and Zambesi )
6175-421: The goal of exploring and to crossing Southern Africa from coast to coast for the first time), and died during the expedition in 1798. The expedition was from then on led by his friend Francisco Pinto. This territory, located between Portuguese Mozambique and Portuguese Angola , was claimed and explored by Portugal in that period. Other European visitors followed in the 19th century. The most prominent of these
6270-405: The great African rivers—the Nile, the Senegal , the Congo, and the Zambezi—were all sourced from the same great internal lake. The Portuguese were also told that the Mozambican Espirito Santo "river" (actually an estuary formed by the Umbeluzi , Matola , and Tembe Rivers) was sourced from a lake (hence its outlet became known as Delagoa Bay ). As a result, several old maps depict the Zambezi and
6365-464: The historical events in these three regions happened simultaneously. Thus, Zambia's history, like that of many African nations, cannot be presented perfectly chronologically. The early history of the peoples of modern Zambia is deduced from oral records, archaeology, and written records, mostly from non-Africans. The Bantu people originally lived in West and Central Africa around what is today Cameroon and Nigeria. Approximately 5000 years ago, they began
6460-404: The independence of these Bantu societies. One of these missionaries noted: "[If] weapons for war, hunting, and domestic purposes are needed, the [Tonga] man goes to the hills and digs until he finds the iron ore. He smelts it and with the iron thus obtained makes axes, hoes, and other useful implements. He burns wood and makes charcoal for his forge. His bellows are made from the skins of animals and
6555-440: The lower Zambezi, thin strata of grey and yellow sandstones , with an occasional band of limestone , crop out on the bed of the river in the dry season, and these persist beyond Tete , where they are associated with extensive seams of coal. Coal is also found in the district just below Victoria Falls. Gold-bearing rocks occur in several places. The river flows to the southwest into Angola for about 240 km (150 mi), then
6650-467: The military tactics of the Zulu to attack other groups. This caused mass displacements, wars and raids throughout Southern, Central and Eastern Africa as Nguni or Ngoni tribes made their way throughout the region and is referred to as the Mfecane. The arriving Nguni under the leadership of Zwagendaba crossed the Zambezi river moving northwards. The Ngoni were the final blow to the already weakened Maravi Empire. Many Nguni eventually settled around what
6745-407: The native idea of this magnificent stream being the main drain of the country". Other historical records show that the river was called Kasambabezi by the Tonga people, which means “only those who know the river can bath in it.” a name which is still in use to this day. In Portuguese records, the "Cuama River" term disappeared and gave way to the term "Sena River" ( Rio de Sena ), a reference to
6840-473: The northern border of Botswana , then along the border between Zambia and Zimbabwe to Mozambique , where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls . Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on
6935-547: The northward bend of the Zambezi is checked, and the stream continues due east. At the confluence of the Luangwa (15°37' S), it enters Mozambique. The middle Zambezi ends where the river enters Lake Cahora Bassa , formerly the site of dangerous rapids known as Kebrabassa; the lake was created in 1974 by the construction of the Cahora Bassa Dam. The lower Zambezi's 650 kilometres (400 mi) from Cahora Bassa to
7030-576: The origins of the name; he was told it was named after a people. "The River Cuama is by them called Zambeze; the head whereof is so farre within Land that none of them know it, but by tradition of their Progenitors say it comes from a Lake in the midst of the continent which yeelds also other great Rivers, divers ways visiting the Sea. They call it Zambeze, of a Nation of Cafres dwelling neere that Lake which are so called." —J. Santos Ethiopia Oriental , 1609 Thus,
7125-478: The other ethnic groups and the Portuguese. This instability caused the collapse of the Luba-Lunda states and a dispersal of people into various parts of Zambia from the Democratic Republic of the Congo. The majority of Zambians trace their ancestry to the Luba-Lunda and surrounding Central African states. In the 1200s, before the founding of the Luba-Lunda states, a group of Bantu people started migrating from
7220-561: The pipes are clay tile, and the anvil and hammers are also pieces of the iron he has obtained. He moulds, welds, shapes, and performs all the work of the ordinary blacksmith." These early Bantu settlers also participated in the trade at the site Ingombe Ilede (which translates to sleeping cow in Chi-Tonga because the fallen baobab tree appears to resemble a cow) in Southern Zambia. At this trading site they met numerous Kalanga / Shona traders from Great Zimbabwe and Swahili traders from
7315-532: The rainy season and flows rapidly, with rapids ending in the Chavuma Falls , where the river flows through a rocky fissure. The river drops about 400 m (1,300 ft) in elevation from its source at 1,500 m (4,900 ft) to the Chavuma Falls at 1,100 m (3,600 ft), over a distance of about 400 km (250 mi). From this point to the Victoria Falls, the level of the basin
7410-549: The rainy season. For more than 200 km downstream, the annual flood cycle dominates the natural environment and human life, society, and culture. About 80 km further down, the Luanginga , which with its tributaries drains a large area to the west, joins the Zambezi. A short distance higher up on the east, the main stream is joined in the rainy season by overflow of the Luampa / Luena system. A short distance downstream of
7505-499: The red king, and Ilunga Mbidi Kiluwe , a prince of legendary black complexion. Nkongolo Mwamba is the drunken and cruel despot, Ilunga Mbidi Kiluwe the refined and gentle prince. Nkongolo the Red is a man without manners, a man who eats in public, gets drunk, and cannot control himself, whereas [Ilunga] Mbidi Kiluwe is a man of reservation, obsessed with good manners; he does not eat in public, controls his language and his behaviour, and keeps
7600-579: The region. The Lunda, like its parent state Luba, also traded with both coasts, the Atlantic and Indian Oceans. While ruler Mwaant Yaav Naweej had established trade routes to the Atlantic coast and initiated direct contact with European traders eager for slaves and forest products and controlling the regional Copper trade, and settlements around Lake Mweru regulated commerce with the East African coast. The Luba-Lunda states eventually declined as
7695-713: The river are the Kariba Dam , which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa . Additionally, two smaller power stations are along the Zambezi River in Zambia, one at Victoria Falls and the other in Zengamina , near Kalene Hill in the Ikelenge District . The river rises in a black, marshy dambo in dense, undulating miombo woodland 50 km (31 mi) north of Mwinilunga and 20 km (12 mi) south of Ikelenge in
7790-577: The river bends almost due east. Here, the river is broad and shallow and flows slowly, but as it flows eastward towards the border of the great central plateau of Africa, it reaches a chasm into which the Victoria Falls plunge. The Victoria Falls are considered the boundary between the upper and middle Zambezi. Below them, the river continues to flow due east for about 200 km (120 mi), cutting through perpendicular walls of basalt 20 to 60 m (66 to 197 ft) apart in hills 200 to 250 m (660 to 820 ft) high. The river flows swiftly through
7885-549: The river course is the result of epeirogenic movements that lifted up the surface at the present-day water divide between both rivers. Meanwhile, 1,000 km (620 mi) east, a western tributary of the Shire River in the East African Rift 's southern extension through Malawi eroded a deep valley on its western escarpment. At a slow rate, the middle Zambezi started cutting back the bed of its river towards
7980-743: The river. Important species include cichlids , which are fished heavily for food, as well as catfish, tigerfish, yellowfish , and other large species. The bull shark is sometimes known as the Zambezi shark after the river, not to be mistaken with Glyphis freshwater shark genus that inhabit the river, as well. Upper Zambezi: 507,200 km , discharges 1044 m /s at Victoria Falls, comprising: Middle Zambezi cumulatively 1,050,000 km , 2442 m /s, measured at Cahora Bassa Gorge Lower Zambezi cumulatively, 1,378,000 km , 3424 m /s, measured at Marromeu Total Zambezi river basin : 1,390,000 km , 3424 m /s discharged into delta Source: Beilfuss & Dos Santos (2001) The Okavango Basin
8075-517: The south-west. The rain falls in a 4-to-6-month summer rainy season when the Intertropical Convergence Zone moves over the basin from the north between October and March. Evaporation rates are high (1600 mm-2300 mm), and much water is lost this way in swamps and floodplains, especially in the south-west of the basin. The river supports large populations of many animals. Hippopotamuses are abundant along most of
8170-499: The southwest, and Angola to the west. The capital city of Zambia is Lusaka , located in the south-central part of Zambia. The population is concentrated mainly around Lusaka in the south and the Copperbelt Province to the north, the core economic hubs of the country. Originally inhabited by Khoisan peoples, the region was affected by the Bantu expansion of the thirteenth century. Following European colonizers in
8265-463: The term "Zambezi" is after a people who live by a great lake to the north. The most likely candidates are the "M'biza", or Bisa people (in older texts given as Muisa, Movisa, Abisa, Ambios, and other variations), a Bantu people who live in what is now central-eastern Zambia, between the Zambezi River and Lake Bangweolo (at the time, before the Lunda invasion, the Bisa would have likely stretched further north, possibly to Lake Tanganyika ). The Bisa had
8360-454: The traditions that would become Nyau secret society from Upemba . The Nyau form the cosmology or indigenous religion of the people of Maravi. The Nyau society consists of ritual dance performances and masks used for the dances; this belief system spread around the region. The Maravi declined as a result of succession disputes within the confederacy, attack by the Ngoni and slave raids from
8455-508: The upper Zambezi in 1853, refers to it as "Zambesi", but also makes note of the local name "Leeambye" used by the Lozi people , which he says means "large river or river par excellence". Livingstone records other names for the Zambezi—Luambeji, Luambesi, Ambezi, Ojimbesi, and Zambesi—applied by different peoples along its course, and asserts they "all possess a similar signification and express
8550-399: The west, aided by grabens ( rift valleys ) forming along its course in an east–west axis. As it did so, it captured several south-flowing rivers such as the Luangwa and Kafue. Eventually, the large lake trapped at Makgadikgadi (or a tributary of it) was captured by the middle Zambezi cutting back towards it, and emptied eastwards. The upper Zambezi was captured, as well. The middle Zambezi
8645-644: The wetlands are still an important habitat. The shrinking of the wetlands, though, resulted in uncontrolled hunting of animals such as buffalo and waterbuck during the Mozambican Civil War . Although the region has had a reduction in the populations of the large mammals, it is still home to some, including the reedbuck and migrating eland . Carnivores found here include lion ( Panthera leo ), leopard ( Panthera pardus ), cheetah ( Acinonyx jubatus ), spotted hyena ( Crocuta crocuta ), and side-striped jackal ( Canis adustus ). The floodplains are
8740-534: Was David Livingstone , who had a vision of ending the slave trade through the "3 Cs": Christianity, Commerce, and Civilisation. He was the first European to see the magnificent waterfalls on the Zambezi River in 1855, naming them the Victoria Falls after Queen Victoria of the United Kingdom. He described them thus: "Scenes so lovely must have been gazed upon by angels in their flight". Locally
8835-553: Was a one-party state with UNIP as the sole legal political party under the motto "One Zambia, One Nation" coined by Kaunda. Kaunda was succeeded by Frederick Chiluba of the social-democratic Movement for Multi-Party Democracy in 1991, beginning a period of socio-economic development and government decentralisation. Zambia has since become a multi-party state and has experienced several peaceful transitions of power. Zambia contains abundant natural resources, including minerals, wildlife, forestry, freshwater, and arable land. In 2010,
8930-548: Was about 300 m (980 ft) lower than the upper Zambezi, and a high waterfall formed at the edge of the basalt plateau across which the upper river flows. This was the first Victoria Falls, somewhere down the Batoka Gorge near where Lake Kariba is now. The first European to come across the Zambezi River was Vasco da Gama in January 1498, who anchored at what he called Rio dos Bons Sinais (River of Good Omens), now
9025-489: Was reached when the Portuguese attempted to influence the kingdoms internal affairs by establishing markets in the kingdom and converting the population to Christianity. This action caused outrage by the Muslim WaSwahili living in the capital, this chaos gave the Portuguese the excuse they were searching for to warrant an attack on the kingdom and try to control its gold mines and ivory routes. This attack failed when
#707292