What geographical feature is located on the Zambezi River. Regime of the Zambezi River. Where does the Zambezi River flow? Zambezi and nutritional features

Zambezi in the heart of Africa great river controls life ancient continent. The Zambezi River is the fourth longest river in the country. The basin area is 1,570,000 km², length is 2,574 km. The source of the river is in Zambia, the river flows through Angola and flows into the Indian Ocean. ( 11 photos)

1. The name Zambezi was given to the river by its European discoverer, David Livingstone, and comes from a corruption of Kasambo Wayzi, a name in one of the local dialects. From the source to the waterfall, for 1200 km, the river flows along a gently sloping, sometimes heavily swampy plain. At exit points hard rocks there are rapids and waterfalls.

4. The Zambezi is a habitat large quantity wild animal populations. There are many living in calm sections of the river. Monitor lizards, special species of birds including heron, pelican, white heron and the African eagle.

5. River floods and drought, which affect animals, depend on the change of seasons. Water may be in short supply, or it may be in excess. But for more than a million years, animals have adapted.

7. In its course, the river often passes through rapids, thus, through navigation on it is impossible. However, for short distances it is much more convenient to move along the river by boat than to travel along regularly washed out floods dirt roads, and some villages are even possible to get to only by water.

The Zambezi is one of the four great rivers of Africa after the Nile, Congo (Zaire) and Niger. The source of the Zambezi is born in a swampy area in northern Zambia on the Lunda plateau at an altitude of 1500 m and rushes to the southwest, and after about 240 km it makes a smooth turn to the south, absorbing small rivers along the way and being fed by groundwater. Her entire path in the upper reaches, like faithful guards, is accompanied by thick deciduous forests. Having left them on the territory of Angola, the Zambezi then flows among tall grass savannah and miombo dry light forest: the trees in it stand at a considerable distance from each other, low bushes and vines grow between them. At the Chavuma Falls, the Zambezi, after passing through the rapids, returns to Zambia. The height of the plateau here is already about 1100 m, and the width of the river is more than 350 m (during the rainy season). From Chavuma Falls to Ngwambe Falls, the Zambezi receives large tributaries Kabombo and Lungwebungd, and the Barotse floodplain begins, and after another 30 km the landscape of the Zambezi banks becomes flat, the flow here slows down and turns to the southeast. 80 km downstream, the Luanginga River flows into the Zambezi from the west. Barotse floods during the rainy season and then the Zambezi can reach 25 km in width. Below begins a series of rapids and rapids, ending with the Ngonye waterfall. This section of the Zambezi is suitable for navigation. After it flows into the Zambezi deep river Kwando (Chobe). In this area, it runs along the border between Angola and Zambia, then a short border with Namibia, the end of a narrow corridor of this country, wedged between Angola. Botswana and Zimbabwe back in 1891 under an agreement between the British Cape Colony and the German protectorate of German South-West Africa. Having merged with the Quando, the Zambezi flows already at an altitude of 920 m above sea level, turns east and slows down, as if preparing to collapse with Victoria Falls - the most famous natural asset, powerful and beautiful.
The waterfall, which the aborigines call Mosioatunya (“thundering smoke”), was the first European to see the famous African explorer David Livingstone (1813-1873). This happened on November 17, 1855 during his journey along the Zambezi.
He gave the waterfall the name of the British queen. And he wrote about it this way: “Angels in flight must have looked at places so beautiful.” The width of the waterfall is about 1800 m, the height of the water fall is from 80 to 108 m, during the rainy season it throws down 9100 m 3 of water per second. Spray and fog above the falling stream rise to 400 m and higher. The sound can be heard 30 km away, hence the “thundering smoke”. For the next 200 km, the Zambezi flows between hills 200-250 m high, basalt cliffs 20-60 m high, accelerating on rapids and rapids. Another attraction and most important hydraulic structure on the Zambezi, the Kariba dam and its reservoir, which arose in 1959 in the Caribbean Gorge. The Itezhi-Tezhi Dam on the Kafue River, the largest left tributary of the middle Zambezi, adds its share of energy. At the confluence of the next left tributary - the Luangwa - the Zambezi route across Mozambique begins - 650 km, and they are navigable. It is home to another major hydraulic structure, the Cahora Bassa Dam and Reservoir, built in 1974. The Zambezi in Mozambique is between 5 and 8 km wide during the rainy season. Only 320 km from the mouth of the Zambezi it falls into the gorge of the Lupata Canyon, no more than 200 m wide. The Shire River, flowing from Lake Nyasa (Malawi), flows into the Zambezi 160 km from the mouth. The largest branches of the delta, covered with mangrove forests, are Milaimbe, Congoun, Luabo and Timbw. But only one is navigable; Shende is also the location of the only Zambezi port of the same name.
The river valley in its upper and middle reaches is located in climatic zone, in which the trade winds of the Northern and Southern hemispheres. After months of scorching heat, in mid-November the skies over the Zambezi are covered with heavy, thunderous sheets of clouds, from which a wall of rain falls, and the entire animal world rushes towards the water, which on the plains spreads in places over a distance of up to 25 km; only small islands of land protrude to the surface. From the interior of Central and Southern Africa, large herds of black and wildebeest, buffalo, zebra, lion prides, families of elephants and rhinoceroses, countless flocks of spoonbills, herons, cranes different types and pelicans. They are accompanied by hyenas and hyena-like dogs. Monkeys move through the trees, among which the most numerous species- baboons. The shallow waters created by the spill are teeming with juvenile fish, and herds of catfish flock here. Moving upstream from the Indian Ocean gray bull shark, capable of existing in both sea and fresh water. In some areas of the Zambezi, herds of hippopotamuses accumulate at this time.
In full compliance with the laws natural selection On the banks there are life-and-death fights, their progress being closely watched by phlegmatic-looking crocodiles.
And then drought sets in again: the grass dries up, small tributaries of the river dry up, there is almost no food for many species of animals, with the exception of some roots, dried fruits of trees and leaves of succulents. Animals migrate to other places on the continent. But even in this time of heat, the Zambezi will give water to everyone who remains.
Associated with the seasonal cycle is the colorful festival of the Lozi people who live in the Barotse floodplain, or Barotseland. The festival is called Kuomboka, which means “to get out of the river.” The Lozi, led by their leader (litunga), set off from the flooded places. On the front boat is the king, who is taller than the litunga, an elephant, or rather his statue, and next to it is a statue of his “wife” in the form of a crane. The action is accompanied by loud drumming and singing. The Lozi are one of the most ancient peoples of the Bantu group, who settled in the lands near the Zambezi (but not only here) several thousand years ago. Another people who have lived since ancient times near the Zambezi, in the area between the Zambezi and Limpopo rivers and also belong to the Bantu, is the Shona. The empire of their ancestors Monomotapa (Mwene-Mutapa) arose in the 6th century and flourished in the 13th-15th centuries. and fell apart to early XVIII V. as a result of internecine conflicts and wars with the southern Ndebele people. It had an influence far beyond its borders, possessed such a rich oral folklore and such a high culture of agriculture, metallurgy, ceramics and jewelry making that some researchers of Africa are inclined to consider Monomotapa even a separate civilization. Trade links with Arab world this empire had since the 10th century. The ruins of its capital, the fortified city of Great Zimbabwe near the modern city of Masvingo in Zimbabwe, are a monument of world significance. These are mainly the remains of gigantic towers, built from blocks of granite and surrounded by powerful walls.
Even in an almost free environment from technogenic pressure modern civilization The Zambezi Valley cannot escape environmental problems. Reservoirs have made their own adjustments to the biological balance of the river: new species have appeared aquatic plants and fish. The Caribbean reservoir is located in a seismic zone, its water surface area is 5580 km 2, its depth is up to 97 m. Such a mass of water creates serious pressure on volcanic rocks, and it is believed that this was the cause of at least eight recent earthquakes in the south of the continent. There is also the problem of pollution of the Zambezi waters with chemical runoff.

general information

The fourth longest river in Africa and the longest African river flowing into the Indian Ocean.
Countries through which the river flows: Angola, Namibia, Botswana, Zambia, Zimbabwe, Mozambique.
Feeding: rain, in the upper reaches - groundwater.

Source: A spring on the Lunda Plateau in northern Zambia, near the NDRK border.

Main tributaries: Lungwebungd, Kwando, Luangwinga, Kabombo, Kafue, Luangwa and Shire.

Largest rapids: Katima, Kebrabasa.

The largest waterfalls: Victoria, Chavuma, Ngonye.

Population of the Zambezi Basin: about 32 million people.

Large settlements along the banks: Mongu (Zambia), Katima Mulilo (Namibia), Seshek (Zambia), Livingstone (Zambia), Victoria Fole (Zimbabwe), Kariba (Zimbabwe), Chemba (Mozambique).
Largest reservoirs: Kariba, Cahora Bassa.
The largest lake in the Zambezi basin: Nyasa (Malawi).
Port: Xinde (Mozambique).

Bridges: in the towns of Chingwingi, Katima Mulilo, Victoria Falls, Chirundu and Tete.

Most important airport: in Livingston, connected by daily flights to O.R. International Airport. Tambo in Johannesburg (South Africa).

Numbers

Length: 2,574 km.

Pool area: 1,570,000 km2.

Maximum width: 1380 m (dry season) - in front of Victoria Falls.

Average water flow at the mouth: 7000 m 3 /s.
Average annual flow: 220 km 3

Climate and weather

Equatorial, mild Three seasons: cold and dry - from May to August (winter), hot and dry - from September to November (spring), warm and humid - from November to April (summer).

The national average temperature ranges: in cold months from +16°С to +27°С, in hot months - from +27°С to +38°С.

Average annual precipitation: from 1100 to 1400 mm.
Average annual evaporation rate: 1600-2300 mm.
Floods during the rainy season: November-April.

Most high level water: november.

Economy

Hydropower: Hydroelectric power stations Kariba and Cahora Bassa.
Agriculture: growing sorghum, maize, vegetables; cattle breeding.

Shipping.
Fishing and fish farming.

Services: tourism (to Victoria Falls, rafting and kayaking on the Zambezi and its tributaries).

Attractions

■ Waterfalls: Victoria, one of the world's greatest waterfalls (listed as a World Heritage Site) natural heritage UNESCO), Chavuma on the Zambia-Angolan border and Ngonye in Zambia.
■ Zambezi Delta.
■ Lake Kariba(Caribbean Reservoir) - as a recreation area.
■ Ruins ancient city Great Zimbabwe (object World Heritage UNESCO).
■ National parks in the Zambezi basin: Mana Pools (UNESCO World Natural Heritage Site), Zambezi, Mosioatunya, Victoria Rolle, Cameo, Liuwa Plains, Liuwa Sioma Nguezi, Chobe, Hwange, Lower Zambezi.
■ Crocodile Farm (Livingston).

Curious facts

■ The Zambezi has its own god. His name is Nyaminyami, he has the body of a snake and the head of a fish. The tribes who have long lived on the banks of the river pray to him so that it does not rage too much when the time of floods comes. In 1957, the elders of the Batonka tribe living on the lower Zambezi, dissatisfied with the construction of the Kariba dam, turned to Nyaminyami for help, whom they believed the dam would separate from his wife. And that same year, a severe flood on the Zambezi, caused by an earthquake, poured streams of water onto the dam. Oma survived, but many of its outbuildings were destroyed.
■ When David Livingstone found himself in the Victoria Falls area, he was accompanied by a detachment of local warriors of 300 people. But only two of them dared to approach the waterfall together with the “mad Englishman”.
■ In the Zambezi River valley, in the jungles of Zambia and Zimbabwe, in the Vadomo tribe, most people have only... two toes on their feet, and both are big. The owners of such feet are also called “ostrich people” (“sapadi”). There are two scientific opinions about this anatomical anomaly. The first is some kind of virus. The second is a consequence of consanguineous marriages. But in all other respects, these people are completely normal, and they move very deftly through trees and run quickly.
■ Kariba hydroelectric power station provides electricity most Zambia and Zimbabwe, Kahora Bassa hydroelectric power station - the rest of Zimbabwe and South Africa. There is also a small power station in the town of Victoria Falls.
■ In 1975, negotiations were held on the Victoria Bridge in a railway carriage between the two sides at war in Southern Rhodesia (now Zimbabwe). For nine hours they argued, proving something to each other, but were distracted too often to admire the waterfall, and never agreed on anything.
■ The women of the Batonka tribe look, in the eyes of Europeans, very strange, but in the eyes of their fellow tribesmen, they are perfect: in the name of beauty, their six front teeth have been removed, this procedure is carried out by a special dentist of the tribe. In addition, to protect against mosquitoes, they smear red ocher on their faces and exposed parts of the body.

Just like the northern part of this continent, it has its own unique, luxurious and very full-flowing attraction - the Zambezi. The river originates in Zambia and flows through countries such as Angola, Namibia, Botswana, Zimbabwe and Zambia. In Mozambique, the Zambezi estuary flows into the Indian Ocean. Along the course of this river is located the greatest attraction of Africa - Victoria Falls.

River flow. Top part

The source of the Zambezi River is in the northwestern part of Zambia, surrounded by black swamps. here it is equal to one and a half meters. A little above the source there is a mountain slope along which there is a clear watershed between the basins of two water streams - the Congo and the Zambezi. The river flows to the southwest, and at about the 240th kilometer, tributaries begin to flow into it. On one of the slopes the river turns into a small Chavama waterfall. This makes it unsuitable for shipping. During its first 350 km, approximately to Victoria Falls, the height above sea level along which the waters flow is approximately the same. It changes its direction a couple of times from south to east, but these changes are insignificant. In the place where the waterfall is located, the upper Zambezi ends. River in central Africa brings most of its waters to Victoria Falls, forming a stunning phenomenon in this place, which billions of tourists come to admire.

Middle part of the river

It is considered the dividing boundary between the sources of the river and its middle course. Starting from there, the channel heads strictly east, where it runs between the hills. The approximate length of this part of the reservoir is 300 meters. We also note that the source of the Zambezi River, which we talked about above, is surrounded by bushes, savanna and sandy-clayey rocks. Here the water flows along the basalts, which form hills and small rocks that enclose the waters of the river. An important point in the middle part is the Caribbean Reservoir (also called Lake Kariba). This is one of the largest artificial lakes in the world. It was formed here in the mid-20th century, after a dam of the same name was built in the middle reaches of the Zambezi. From then until today, the Kariba hydroelectric power station has provided all residents of the surrounding area with the opportunity to use electricity. Also along the middle course we encounter two more large tributaries - Kafue and Luangwa, which flow into the Zambezi. Thanks to them, the river becomes wider and fuller. Therefore, a little further downstream, another dam was built on it - Cabora Bassa. At this point the middle part of the Zambezi ends.

Lower channel of the water artery

The Zambezi, crossing the Cabora Bassa reservoir, redirects its waters to the west. The length of its final part is the largest compared to the previous ones, namely 650 km. This area is already suitable for navigation, but there are often shoals here. The fact is that the area through which the water flows is a wide valley, and they simply spread along it, forming wide river, but not very deep. The channel narrows only when it passes through the Lupata Canyon. Here its width is only 200 meters, while in all other places the river literally spreads out to 5-8 kilometers. At a distance of 160 km from the ocean, the Zambezi intersects with the river. Wider. Thanks to this, it is fed by its waters, as well as by waters from Lake Malawi. After this, our beauty breaks up into many small channels, forming a delta. Near the shores of the Indian Ocean, the Zambezi River on the map looks like a triangular branch that connects to large waters.

Tributaries of the river

This flow is considered the fourth largest among its “brothers” on the continent. The Zambezi River in Africa would not be so full of water if it were not for its numerous tributaries, lakes and canals crossing its bed. Well, let's look at them in more detail. The first and most important feeding artery of the water flow is the Capombo River. It originates in the hills where the sources of the Congo and Zambezi are located not far from each other. In the first knee of our subject of study, where the direction changes from western to eastern, it is crossed by Kwando, a very deep river. In the middle reaches of the Zambezi, the waters of Kafue and Langi feed. Below we meet another extremely important tributary - the Luangwa. It not only supplies its waters to the Zambezi, but also comes into contact with Lake Malawi, making it very wide and deep. In the lower part of the flow, the river is fed by the waters of the Sanyati, Shangani and Khanyani tributaries.

History and research of the reservoir

People had knowledge about this geographical object back in the era early Middle Ages. Historians believe that this knowledge was based on Arabic chronicles and documents. Thus, the Zambezi River appeared on the map of Africa back in the 1300s, but, as you understand, only high-ranking persons could know about it. Major exploration of these African waters began only in the 19th century. The first person to pay attention to the river was scientific point sight, it turned out He swam upstream, starting from Lake Malawi and ending with Victoria Falls. Along the way, he discovered many of the now famous tributaries and gave them their names. Until the end of the century, the river and all adjacent elements were fully studied by Europeans, and all the data was firmly established on world maps.

Fish world

Most of the fish that are found in the waters of the Zambezi are endemic. All their species are found exclusively in this area. And even if many of the names that we list below seem familiar to you, rest assured that in reality this aquatic inhabitant will not look the way we are used to contemplating it. There is a special microflora here, which allows all living organisms to develop differently than in Europe or America. So, this is where cichlids are found various types, catfish, terapons and catfish. A very popular inhabitant of the lower one is the blunt-nosed shark, or bull shark. It is found both in the coastal waters of the Indian Ocean and in the tributaries of the Zambezi.

Fauna

Based on the previous material, you can imagine where the Zambezi River is located from a geographical point of view. This central part African continent, tropical zone, a zone of eternal heat, sand and savannah. It is through such a landscape that the Zambezi flows, which creates the corresponding fauna around it. There are countless crocodiles here various types. According to this characteristic, the river can be easily compared with the Nile. Along with them, smaller lizards live, as well as snakes (especially in the area of ​​the source, where there are many swamps). On land there are elephants, zebras, bulls, lions, buffalos - in a word, a typical African safari. Unfortunately, there are not so many birds in the skies over the Zambezi. Monitor lizards, pelicans, African eagles fly here, and white herons stroll along the banks of the river.

"Fish" economy

You can understand just by looking at the photo: the Zambezi River is very deep, wide, rich in fauna and flora, and therefore is a significant economic link in the development of all the countries through whose territory it flows. In addition to the fact that two giant hydroelectric power stations have been built here, which supply electricity to all surrounding countries and cities, fishing is also thriving here. Residents of cities that grew up on the banks of the Zambezi can use the gifts of its waters free of charge to feed their families. Visitors from more distant settlements pay a tax for fishing here. Many of the banks of the Zambezi are reserved for sport fishing. People come here for pleasure and rare species Pisces people from different parts of the planet. Also, the same endemics that serve as decoration for any aquarium are caught from the river basin.

Ecological situation

Perhaps we will begin our description of the ecology of the Zambezi River with its problems, since they are truly large-scale. All the misfortune lies in the fact that the discharge is made here Wastewater, and not through special treatment facilities, but directly. Sewage from populated areas, ports, single houses and other objects simply drains into the river. This not only causes water pollution, but also gives rise to diseases such as typhoid, cholera, dysentery, and a host of other, more or less serious infections. Big problems also arose after the construction of the Cabora Bassa hydroelectric station. It was filled thanks to rains literally in one season, while the authorities planned that it would be filled gradually over several years. As a result, the flow decreased sharply, which led to a reduction in the area mangrove forests around the water. This also scared away the animals that previously lived on the banks of the river. Many useful microelements also disappeared from the waters, and the number of fish species that lived here decreased.

Transport situation

In total, the length of the Zambezi River is 2574 kilometers, taking into account all its bends and turns. This makes it one of the largest water flows in Africa, but this is not at all a sign that it is an ideal transport artery for its region. We have already said above that the river bed often changes its direction, and radically, the same applies to its width, depth and other indicators. The main obstacles to navigation are the artificial lakes, dams and waterfalls that cross its course. However, often many transport operations are carried out precisely thanks to individual sections of this reservoir. For example, steamships often pass through the lower part of the Zambezi, carrying both passengers and cargo. Middle and top are used predominantly local residents. The surrounding roads are always washed out due to the instability of the local soils, and the easiest way to get from one settlement to another is by boat.

Bridges over the Zambezi

Africa's fourth largest watercourse is crossed by just five bridges. Their construction began at the dawn of the 20th century, and is still ongoing, despite the fact that many projects have already been completed. The first was built in 1905 in Victoria Falls. It rises 125 meters above the water surface, its width is 150 meters, and its length is 250 meters. Since then it has been reconstructed, but not radically rebuilt. It was originally planned as part railway, which would run from Cape Town to Cairo. Further, in 1939, a bridge was built in the city of Chirundu (Zambia), which was rebuilt in 2003, and in the 60s bridges appeared in the cities of Tete and Chingwingi. In later years, namely in 2004, construction of the last, fifth bridge across the Zambezi was completed. It runs between the cities of Sesheke (Zambia) and Katimo Mulilo (Namibia).

Cities and towns surrounding the river

We looked at where the Zambezi River originates, where it flows, and what other bodies of water cross it as it flows. Now the subject of consideration is the settlements surrounding its shores. Firstly, the river passes through more or less six countries. Among them are Angola, Namibia, Zambia, Mozambique, Zimbabwe and Botswana. But there are more cities located on its banks. Let's list them briefly: Lakalu, Kariba, Mongu, Tete, Songo, Lilui, Livingstone, Sesheke and Katimo Mulilo. All settlements are very small geopolitical objects. In total, only 32 million people live in the river valley. Most of them lead rural image life, being content with local floating soils and practically complete absence livestock. Local cities make money mainly from tourism, but this industry is not properly developed here either. Many of them work as fishermen, and poaching is also rampant.

And the indigenous people of Africa call her Kasambo Wayze. Coastline extends across the territory of six states of the African continent. Where does the Zambezi River flow? Straight into the Indian Ocean, forming the widest delta. Its length is about 2600 km. Formed on this river beautiful waterfall- Victoria. It is unique in its kind and known throughout the world. A dam was built on it, which formed the Kariba Reservoir, a large reservoir on a global scale. The Zambezi River basin is striking in its size, its area is 1.57 million square meters. km.

From source to delta

The Zambezi originates in Zambia, in the northwest, where the terrain is marshy and hilly. The source is located at an altitude of 1.5 km above sea level; dense, almost impenetrable forests grow here. The river heads southwest, then turns south (240 km from the source) to let in the first small tributaries and recharge with groundwater.

The vegetation also changes here - this is the territory of savannah: sparse dry forest and shrubs. After the small Chavuma Falls, crossing the Angolan border, the river returns to Zambia.

After the Ngonye Falls, the Zambezi expands due to a large tributary - the Kwando River - and turns east, slowing down before the “main” waterfall (Victoria). Passing the Cabora Bassa reservoir, the Zambezi rushes into the valley, where the channel becomes shallow and branches. Downstream, the water flow communicates with (the Shire tributary) and rushes towards Indian Ocean. See the map for more details.

The Zambezi Delta has a large extent from north to south with an area of ​​5 thousand square meters. km. However, navigation here is difficult due to natural sand deposits and shallowing of the branches. This is due to the construction of dams. The only branch passable for ships is Shinde.

Zambezi and nutritional features

The Zambezi originates in a mountainous area with a subtropical climate. In this area in summer season heavy rainfall occurs in the form of prolonged downpours. These rains, in fact, form the river, and they are also the main source of nutrition. And to a lesser extent, the watercourse is fed by groundwater from the marshy area. This type nutrition is characteristic mainly in upper reaches.

The regime of the Zambezi River is accompanied by constant changes. From March to November (South African winter and drought), the flow becomes very shallow, and in November it is replenished again, increasing its level by 1.5 m. During the rainy season, this river can be called turbulent; it moves a huge amount water masses With high speed currents.

Usage

The population living in the Zambezi Basin region is mainly occupied agriculture. However, the regime of the Zambezi River is so variable that it is not always possible to use its water for irrigation. But fishing is well developed here. The watercourse abounds in both small and big fish, many of the species are endemic. Fishing is the main income of the local population. The fish is used not only for food, but also for breeding in aquariums: Zambezi - habitat habitats of everyone's favorite barbs and cichlids.

Structures on the river

This water flow provides energy to several states in the south of the continent at once, through the Kariba and Cabora Bassa hydroelectric power stations. However, the special regime of the Zambezi River was the reason for the construction of canals that ensure the stable operation of hydroelectric power stations. But this leads to another problem: the dams shred the delta branches. However, in other places (below Cabora Bassa), on the contrary, the river became navigable.

The Zambezi Path runs through several states and many regions, so an important fact is the presence of five full-fledged bridges providing interregional and interstate communication.

Natural diversity

The waters of the Zambezi not only abound in diverse small fish. Also here you can find large predators: bull shark, crocodiles and monitor lizards. The coastal area is home to many animals and birds: hippos, elephants, giraffes, zebras, herons, eagles and pelicans. Tourists can observe them either by traveling by boat or by visiting one of the many nature reserves or safari parks.

Tourism

The Zambezi River attracts fishing tourists. You can rent gear here. Due to the many rapids, rafting along this stream is quite popular among fans of extreme rafting.

The “Thundering Smoke” waterfall (Victoria) is known throughout the world. It has a unique ratio of width and height (1800 x). Entire families of large animals live in the reserves adjacent to the waterfall, and there are also rare white rhinoceroses. A little further downstream, lovers are offered kayaking.

In order to have the most interesting time and visit the Zambezi water stream and other rivers of Africa, you can see the exact routes of organized excursions on the map.

The Zambezi is the fourth longest river in Africa. Geographically, the river is located in South Africa, it originates in the territory of Zambia, then, flowing through the territory of five more states (Angola, Botswana, Namibia, Zimbabwe and Mozambique), it flows into the Indian Ocean.

The area of ​​the territory from which the Zambezi River collects its waters is 1390 thousand square meters. km., and the length of the watercourse itself is 2574 kilometers. It is on this river that one of the most famous waterfalls in the world, Victoria, is located. But it is not the only one - the rocky rocks along which the river basin passes contribute to the formation of waterfalls, among which Chavuma and Ngambwe can also be noted.

Hydrological and morphological characteristics

The source from which the Zambezi River begins is located among a swamp area located at an altitude of about 1500 m above sea level. The watershed separating the river basin from the neighboring Congo River basin is not clearly defined, but two river systems don't connect. In its upper reaches the river is shallow and wide, subject to frequent floods. The river is fed predominantly by rain and underground, with pronounced periods of rain floods. After the Victoria Falls, the middle course of the river begins, which is characterized by the intersection of basalt rocks, overcoming which, the watercourse forms numerous riffles, rapids and rapids. In the lower reaches, which is located in a wide valley, the Zambezi becomes navigable.

Human use of the river

The Zambezi River underwent its first serious research in the middle of the 19th century, thanks to the famous expeditions of Livingstone, although it was known to medieval geographers. Today, about 32 million people live directly in the river valley alone, mainly engaged in agriculture and fishing. Despite its considerable length, this river is crossed by only five bridges. Significant Negative influence The condition of the river was affected by the construction of two large dams, and in our time there continues to be pressure on the ecosystem due to regular discharges of untreated wastewater.