{
  "id": "zambia",
  "title": "Zambia",
  "lang": "en",
  "source_lang": "en",
  "summary": "Zambia is a landlocked country in south-central Africa. It lies mostly on a high plateau and is drained chiefly by the Zambezi River.",
  "category": "geography",
  "subcategory": "",
  "type": "place",
  "aliases": [
    "Republic of Zambia",
    "Northern Rhodesia (colonial-era name)"
  ],
  "generated_at": "2026-10-09",
  "model": "pro/claude-haiku-5-5",
  "url": "https://aiwiki.page/en/zambia/",
  "translations": {
    "zh-Hans": {
      "url": "https://aiwiki.page/zh/zambia/",
      "json": "https://aiwiki.page/zh/zambia.json"
    }
  },
  "sections": [
    {
      "heading": "",
      "text": "Zambia is a landlocked country in south-central Africa, bordered by eight states and covering roughly 750,000 square kilometres. Its name comes from the Zambezi River, which forms much of the southern boundary and gives the country one of Africa's most recognisable landmarks at Victoria Falls. Most of the territory sits on a broad plateau, and the drainage of that plateau divides the country between the Zambezi basin and the Congo basin. The country was known as Northern Rhodesia under British administration before independence in 1964.\n\nGeography shapes nearly every part of national life in Zambia. The plateau climate, with a pronounced rainy season, governs agriculture and river flow, and the same rivers supply most of the country's hydroelectric power. The copper-bearing rocks of the northwest anchor the mining economy, while the floodplains, wetlands and miombo woodlands sustain a large share of the country's biodiversity and national parks. Settlement follows the transport corridors that link the Copperbelt and Lusaka, and the landlocked position makes external trade dependent on routes through neighbouring countries.\n\nThis entry proceeds from the physical foundations (geological basement, relief, rivers, lakes and climate) to the living and resource geography (vegetation, soils, protected areas, minerals, energy and population). It then covers transport, administrative and political geography, transboundary water management, climate-change exposure, and the history of geographical exploration and mapping."
    },
    {
      "heading": "Name, location and boundaries",
      "text": "Zambia takes its name from the Zambezi River, which gives the name \"Zambia\" its derivation, and \"Zambezi\" may mean \"the grand river\". The river's own name has no single accepted origin. One account links it to a Tonga term, in which 'nzambezi' referred to the great river that defined the landscape for the region's Bantu-speaking communities. Another credits the Bisa people with the naming of the river, and \"Zambezi\" seems to have survived because it is probably the oldest documented name. The explorer David Livingstone, who reached Victoria Falls in 1855, recorded the river as 'Zambesi' in his journals.\n\nThe territory took its present name only after the colonial period. British colonial administrators named the territory around the upper Zambezi 'Northern Rhodesia' in 1911, after Cecil Rhodes, and it became a Northern Rhodesia under British authority. Independence came on 24 October 1964, when Zambia became a republic within the Commonwealth, with Kenneth Kaunda as its first executive president. The new government replaced the colonial label with the river-based name, which some accounts describe as a compressed form of 'Zambezi'. The name change is part of the wider decolonization of the region, and the country's location in south-central Africa is what places it between the Congo and Zambezi drainage systems and the southern African states.\n\nZambia lies in the interior of the continent and has no sea outlet. Its coastline is 0 km, so all external trade must pass through neighbouring states, a point developed in the transport section. Its total area is 752,618 square kilometres, of which 9,220 km² is water. By area, the country ranks 38th in the world. Sources give slightly different rounded figures, usually about 752,000 km². Its extent in latitude and longitude is also reported differently: a national tourism source places the country between latitudes 10° and 18° South and longitudes 22° and 33° East, while another general reference gives latitudes 8° and 18° south of the equator and longitudes 22° and 34° east. The country's approximate centre lies near latitude -13.13 and longitude 27.85. Because the whole territory lies between the equator and the Tropic of Capricorn, Zambia is entirely within the tropics, and its climate is discussed in a later section.\n\nZambia has eight neighbours. Going around the compass, the Democratic Republic of the Congo lies to the north and north-west, Tanzania to the north-east, Malawi to the east, Mozambique to the south-east, Zimbabwe to the south, Botswana and Namibia to the south-west, and Angola to the west. The border with the Democratic Republic of the Congo is the longest, at 1930 km, while the frontier with Botswana is very short, less than 1 km. In total, the country has 5,664 km of land boundaries. The southern edge of Zambia is partly defined by the Zambezi, which rises in the north-west corner of the country and forms its southern boundary. The boundary lines that fixed these frontiers were drawn in the colonial era and are treated in the history section."
    },
    {
      "heading": "Geological basement and tectonic setting",
      "text": "Zambia's bedrock records a long Precambrian history. The oldest units, grouped as the Basement Supergroup, lie across the east, centre and south of the country. Their ages range from about 3,000 million years to less than 2,050 million years, and they consist mainly of granitic gneisses and migmatites, with marbles, quartzites and metapelites (the oldest being 3000Ma, but typically most are younger than 2050Ma), occur throughout eastern, central and southern Zambia. These consist mostly of granitic gneisses and migmatites, with marbles, quartzites and meta-pelites. These rocks form part of the cratonic interior of the continent, the old and stable cores that surround and separate older, Archean cratonic nuclei in the Proterozoic orogenic belts of Africa. Because heat and pressure have overprinted these basement rocks, much of their earliest history is no longer legible; they tend to be highly metamorphosed and may have formed earlier in the Archean, but heat and pressure has destroyed evidence of earlier conditions.\n\nAbove this crystalline floor lies a sedimentary cover of uneven age. Mid-Proterozoic sediments and metamorphic groups were followed by Neoproterozoic and Palaeozoic glaciations, which left glacial conglomerates and other deposits that became part of the Katanga and rift-related Karoo sequences (a series of glaciations in the Neoproterozoic and much of the Paleozoic which deposited glacial conglomerate as well as other sediments to form the Katanga Supergroup and rift-related Karoo Supergroup). The Karoo Supergroup is the most important younger sequence in the eastern and southern valleys. Its rocks, dated from the late Carboniferous to the Jurassic, occupy the rift troughs of the Zambezi, Luangwa, Luano-Lukusashi and Kafue valleys, and also outcrop in western Zambia. In the Luangwa Valley, the sequence is markedly thick. The basins there contain up to 8000m of Permo-Triassic, mainly clastic, sediments. The lower part includes glacial deposits at its base, overlain by coal-bearing shales and siltstones and a very thick lacustrine section, while the upper part consists of sandstones and siltstones that are thought to have been laid down by braided streams and floodplains (basal glacial deposits overlain by a sequence of interbedded coal, shale and siltstone, and capped by a very thick (up to 5000 m) lacustrine section of interbedded siltstone and mudstone). Volcanic rocks also appear in this sequence. The Batoka basalts occur in western Zambia and the Zambezi valley (forming Victoria Falls). Later Mesozoic basalt flows covered the Karoo beds across the region, and in western Zambia the Kalahari deposits of wind-blown sand overlie them (Aeolian sands of the Kalahari Group (Tertiary) cover much of western Zambia.)\n\nThe Copperbelt in the northwest lies within a different structural unit. The Lufilian Arc is a Neoproterozoic fold-and-thrust belt that is located between the Congo and Kalahari cratons and defines a structure which is convex to the north. Its rocks are the Katanga Supergroup, a thick sedimentary (clastic and carbonate strata, including evaporites) and volcanic sequence that was deposited in the early Neoproterozoic. The deformation that shaped the arc occurred in phases. The first, known as D1, produced northward-moving folds and thrust sheets (developed folds and thrust sheets with a northward transport direction. D1 deformation occurred in the Lufilian arc between ca. 800 and 710 Ma, with a peak in the range 790–750 Ma.) The second phase, D2, involved large left-lateral strike-slip faults. During this deformation phase, the eastern block of the belt rotated clockwise, giving the present day NWSE trend of D1 structures in this part of the Lufilian arc, and generating its convex geometry. This rotation is the reason the belt curves as it does, and it is separated from the Zambezi belt by the major transcurrent shear zone separating the Zambezi and Lufilian arc, mostly active during the D2 deformation phase.\n\nThe structure also controls where the ore lies. Copper and cobalt occur in sedimentary rocks that were folded and faulted during the orogeny. The Mine Series Group hosts most of the copper-cobalt mineralisation of the Copperbelt within mudstones, sandstones, conglomerates and carbonates. Within the folds, the cores of many anticlines are formed by megabreccias containing huge blocks of lower Roan dolomitic rocks of every size up to several kilometers. Many large clasts contain strata-bound Cu-Co sulfides and are actively mined. Salt movement during the orogeny also shaped the belt. Evaporite bodies were squeezed into diapirs, and the foreland shortened from 193 km to 85 km, which helps explain why the ore-bearing rocks are so tightly deformed.\n\nThe eastern and southern valleys reflect the East African Rift System, though to a much lesser degree than the rift in the north. The Luangwa Valley is an extension of the East Africa Rift System (EARS), and it is formed by a series of en echelon half-grabens that form a SW–NE-trending extension of the western branch of the EARS. The valley's basins were first formed in the Permo-Triassic and later reactivated. Inverted in the Mesozoic, it then experienced major Neogene extensional reactivation. The latter resulted in today's major border faults of varying polarity, with fault plane escarpments of up to 1000m, and associated rift flank uplifts that elevate the Central African plateau surface by 200 m. The border faults follow old structures. The two main border faults in the Luangwa Rift, the Chipola and Molaza faults, both follow Karoo–Basement contacts, and the most prominent Late Quaternary fault scarps occur along the 207 km long Chipola and 142 km long Molaza faults, which are the rift border faults and the longest faults in the region. Current activity is modest by regional standards. The Luangwa Valley is tectonically quiescent by comparison with the EARS to the north in Malawi and Tanzania. There is no active volcanism, there are no rift lake basins and large earthquakes are relatively rare. Nonetheless, historical earthquake data show Mw 6.7 and Mw 6.5 earthquake events occurring in 1919, which shows the rift can still produce significant seismic events."
    },
    {
      "heading": "Plateau relief and elevation zones",
      "text": "Most of Zambia sits on a broad upland. Its terrain is mostly high plateau, with some hills and mountains, and its surface is shaped by uplifted planation surfaces. Ground falls from the upper Congo basin in the north toward the Zambezi depression in the south, and that slope is what forms the plateau itself (the level of land falls from the upper Congo towards the Zambezi depression in the South forming a plateau). Sources disagree on the typical height. One general reference gives between 1,000 to 1,400 meters, a geological study places the plateau at 1100 to 1600 m above sea level, and national statistics give a mean elevation of 1,138 m. The 1,000–1,500 m range commonly cited therefore reflects this spread rather than a single measured value.\n\nThe plateau's gentle relief results from a long and comparatively quiet geological history. Its rocks are largely gneisses and schists of Precambrian age, which belong to the basement complex of the African craton (craton). Repeated uplift separated by long periods of planation produced the present surface. One study links this to intermittent continental uplift since Karroo times with intervals long enough for peneplanation. The result is a landscape of gently undulating surface, punctuated by occasional inselbergs and deep soil profiles that have developed over millions of years of stability. Residual hills of harder rock, such as quartzite ridges, stand proud of the plateau surface, and the rock beneath the soil is deeply weathered to at least 10 m. Because weathering has run for a very long time, the soils are devoid any further weatherable minerals and poor in cations and other plant nutrients. These erosional features are explained in more detail in the geology and erosion sections.\n\nSouthern African usage divides the veld, the open country of the region, into zones by elevation: high veld, middle veld, low veld and others, with the main regions distinguished by height. Applied to Zambia, the same three terms are the Highveld, sitting above 1,200 meters, the Middleveld, ranging between 600 and 1,200 meters, and the Lowveld, which covers the regions below 600 meters, primarily found in deep river valleys. These thresholds come from a single informal source, and other definitions differ. Zimbabwean usage, for instance, places the Highveld at 1200 and 1500 meters above sea level and the Middleveld at 900- 1200 meters above sea level, so the boundaries should be treated as conventions rather than fixed limits. Across the zones, the highveld occupies higher elevations with cooler temperatures, while the lowveld is at lower altitudes with warmer conditions. The Middleveld tends toward savanna and miombo woodland, while the lowest valleys show significantly higher temperatures and different vegetation patterns.\n\nThe extremes of Zambian elevation are clearly separated. The highest point is Mafinga Central in the Mafinga Hills, at 2,339 m (7,674 ft) above sea level. Its nearby rival, Mafinga South, is only slightly lower, and a 2014 climb by an international team measured Central as marginally higher, though a more accurate survey is needed to establish for certain which peak is taller. The Mafinga Hills form a plateau covered by hills on the border with Malawi, and their rock is composed of quartzites, phyllites and feldspathic sandstones of sedimentary origin. The lowest point is the Zambezi river, at 329 m (1,079 ft) above sea level. The gap of roughly 2,000 metres between these two points gives Zambia a wide relief range, even though Zambia lacks the extensive, high-altitude mountain ranges found in other nearby African nations."
    },
    {
      "heading": "Rift valleys, escarpments and highlands",
      "text": "Zambia's relief is framed by two large valleys, the Luangwa Valley in the east and the middle Zambezi Valley in the south, which lie against the central plateau. Adjacent to the central plateau, Zambia features two major valleys: the Zambezi Valley in the south and the Luangwa Valley to the east. Both are bounded by steep escarpments, and the highlands in the northeast rise above the plateau surface.\n\nLuangwa Valley\n\nGeologists describe the Luangwa trough as a rift valley or graben. It extends the East African Rift toward the south-west, branching from the Lake Rukwa–Lake Malawi section and stretching nearly as far as Lusaka. The junction with the main rift is not obvious because the valley has been filled with material from an ancient, extinct volcano. Near Mfuwe, the valley floor is about 100 km wide, the floodplain about 10 km wide, and the river lies at roughly 520 metres. A north-west escarpment about 700 metres high, the Muchinga Escarpment, lies on one side, and a south-western escarpment about 450 metres high lies on the other. There are at least 20 hot springs, characteristic of a rift valley, in the valley or on its escarpments.\n\nMiddle Zambezi valley\n\nThe escarpments along the middle Zambezi are fault scarps. They rise 500 to 600 m above the lake or river, run roughly 800 km toward the lower Zambezi, and face each other across a gap of about 50 to 100 km, closer in the west and opening up in the east. The northern escarpment is the steeper of the two. It is especially well formed from a point north of Siavonga, running east through Lower Zambezi National Park to the Luangwa confluence, where the valley floor stays comparatively flat. The Zambezi channel is the country's lowest point, at 329 metres above sea level.\n\nMuchinga escarpment\n\nThe Muchinga escarpment is better understood as a geological edge than as a mountain range. It is characterized by a steep, dramatic descent from the central plateau down into the Luangwa River valley. Its highland crest reaches about 1,800 metres, and the region sees more rainfall than the rest of the country, resulting in the growth of lush forests and several endemic species. The escarpment also forms a divide: it separates the drainage basins of the Zambezi River, which flows to the Indian Ocean, from the Congo River basin, which flows to the Atlantic. Vegetation changes down the slope as well. Starting in miombo woodland, the escarpment slopes down through mopane woodland to the valley floor.\n\nNortheastern highlands\n\nThe highest ground lies in the Mafinga Hills on the Zambia–Malawi border, which form a plateau covered by hills. The summit, Mafinga Central, reaches 2,339 m (7,674 ft). The hills are composed of quartzites, phyllites and feldspathic sandstones of sedimentary origin. Other peaks exceed 2,000 metres, including Kangampande at 2,221 m and Kongera at 2,205 m. The Mafinga Hills form an important part of the watershed dividing the Zambezi River basin via its tributary, the Luangwa, from the Lake Malawi basin. The Mafinga Hills are part of the wider Kipengere Range, which runs across Zambia, Malawi and Tanzania. Only very able 4-wheel drive vehicles are able to cross this area, especially during the rainy season.\n\nMbala, on the Tanzanian border, is lower than the 2,000-metre threshold. Its elevation is about 1,570 metres, and Mbala Airport lies at 1,662 m. The high ground that exceeds 2,000 metres in the northeast is therefore concentrated in the Mafinga massif rather than around Mbala itself.\n\nEscarpment effects on drainage, climate and forest\n\nEscarpments shape the country's hydrology and ecology. The escarpment profoundly influences regional drainage patterns, directing rivers into the Luangwa, and impacts local climate conditions. The Luangwa itself has its source in the Mafinga Hills, so the highlands feed the valley below. Because the escarpment tops receive more rain than the plateau and the valley floor, the rainfall contrast across each escarpment helps explain the distribution of forest patches, with moist woodland on the upper slopes and drier savanna below. The lower valley floors, by contrast, support a wide range of wildlife and flora because of their lower altitudes and higher temperatures."
    },
    {
      "heading": "River systems and drainage divide",
      "text": "Zambia sits on the Congo–Zambezi watershed, a broad band of higher ground that runs roughly east to west and separates the Zambezi system from the upper Congo. The high ground falls abruptly to the north and south and cuts off the Lualaba, the main branch of the upper Congo, from the Zambezi. Near the head of the river the divide is less distinct, but the two systems still do not connect. The traditional source of the Zambezi is a small spring on the Congo-Zambezi watershed in northwest Zambia. A 2025 study that measured the river from the Lungwebungu tributary, in Angola, found the Zambezi to be about 342 km longer than the traditional figure, which shows that the exact source is still debated. Basin area figures also vary between sources, with one giving about 1,359,000 km² and another 1,390,000 km².\n\nThe upper Zambezi is the most natural stretch of the river. Its gradient is very slight, and long stretches of low-gradient river with associated floodplains and swamps alternate with extensive rapids. Its first large tributaries, the Kabompo and the Lungwebungu, join in the northwest, and these confluences mark the beginning of the floodplains. The best-known of these is the Barotse floodplain, which extends from Lukulu in the north to Nangweshi in the south, and is approximately 240 km long and up to 35 km wide. The floodplain acts as a natural sponge, slowing floodwaters and trapping sediments, and it supports large numbers of birds, fish and hippos. Flood peaks usually arrive in April and recede slowly over several months. Downstream, the river reaches a hard rock barrier at the Ngonye Falls, where harder rock resists the river's tendency to cut a channel down, and the floodplain has formed behind it.\n\nVictoria Falls, roughly 98 m high, marks the boundary between the upper and middle Zambezi. Its mean discharge is about 1237 m³/s. Below the falls the river runs through deep basalt gorges and forms the Zambia–Zimbabwe border for about 500 km. Two of the largest tributaries of the middle course enter from the Zambian side. The Kafue and Luangwa are the two largest left-hand tributaries of the Zambezi. The rainfall pattern gives the northern tributaries more influence than the southern ones. One tabulation estimates that the Northern Highlands catchment of the upper Zambezi contributes 25%, Kafue 8%, Luangwa and Shire Rivers 16% each.\n\nThe Kafue is the longest river lying wholly within Zambia, at 1,576 km (979 mi), although tourism sources give a shorter route length of about 960 km. It rises at an elevation of 1350 meters on the relatively flat plateau just south of the border with the Democratic Republic of the Congo. It starts as a trickle from marshy dambos and, with little slope, meanders sluggishly before taking on the character of a mature river. The Kafue later drops 550 meters over 60 kilometers through the Kafue Gorge, and it joins the Zambezi near Chirundu. The Luangwa flows in a generally level valley, bounded by steep plateau escarpments, and is generally shallow and rapid, though fairly wide. It generally floods in the rainy season, from December to March, and then falls considerably in the dry season.\n\nThe Bangweulu basin lies on the plateau to the north. The Chambeshi, which now feeds the Bangweulu swamps, was \"captured\" by aggressive southern tributaries of the Congo. The Luapula drains Lake Bangweulu northward through Lake Mweru into the Congo system, so this part of the country belongs to the Congo rather than the Zambezi.\n\nRapids and waterfalls limit navigation on several plateau rivers. Rapids occur in several areas between Nangweshi and Katima Mulilo, and from Mombova to the Victoria Falls. Dry-season flows also make the river fairly shallow in many places. The same drops that impede boats make hydroelectric development practical. The Kafue Gorge has a second dam that generates electricity, with a smaller reservoir. Further downstream, the Kariba Dam, completed in 1959 (created in 1959 following completion of the Kariba Dam), created one of the largest man-made lakes in the world."
    },
    {
      "heading": "Lakes, swamps and wetlands",
      "text": "Zambia's water bodies are dominated by a deep rift lake in the north, a shallow floodplain basin in the northeast, and a large reservoir on the Zambezi in the south. Their ecological and economic roles depend on rainfall, flood timing and the operation of dams.\n\nIn the far north, the country shares Lake Tanganyika with Tanzania, the Democratic Republic of the Congo and Burundi. The lake is located in the Albertine Rift, which is the western section of the East African Rift. Zambia's share of the lake is small: Zambia and Burundi each have 7% of the lake. Its depth is nonetheless striking. Only Siberia's Lake Baikal sinks deeper, and Tanganyika's maximum depth is about 1,470 metres, while Tanganyika reaches 1,470 m. Estimates of its volume vary: one database gives a volume of 17,800 km³, while other sources give about 18,900 km³. Most residents around the lake depend on its fish, and Mpulungu is one of the Zambian settlements on its shore.\n\nLake Mweru lies on the border with the Democratic Republic of the Congo and is linked to the Luapula system, which carries water from the south toward the Congo basin. Further south, the Bangweulu wetlands form a very different water body. The Great Bangweulu Basin, incorporating the vast Bangweulu Lake and a massive wetland area, lies in a shallow depression on the North Zambian Plateau. The wetland is not simply a lake. It is spread across 6,000 km² of a 9,850 km² ecological region comprised of open water, seasonal floodplains, miombo woodlands, permanent swamps and seasonally flooded grasslands, and it is fed by several rivers, including the Chambeshi and the Luapula.\n\nThe wetland's rhythm is set by the rains. The area floods in the wet season between November and March, and although annual rainfall is high, 90% of the water entering the system is lost to evapo-transpiration. The flood extent changes greatly from year to year. One source reports that permanent open water of about 3,000 square kilometers expands to over 15,000 square kilometers during floods, although this figure comes from a secondary source and should be treated as approximate. Water depth also varies across the plain, sometimes one and two meters.\n\nThe seasonal pulse supports fisheries and wildlife. Estimates of the annual catch differ widely: one study puts it at approximately 15,000 tons of fish each year, while another reports about 57 000 metric tons of fish harvested from the lake each year. The fish community is diverse, with eighty-three species representing 13 taxonomic families recorded from the area. Fisheries here are typically small-scale and multi-gear. Floodplain fisheries of this kind yield higher production rates than static water bodies, enhancing fishery resilience. Because stocks came under heavy pressure, a nationally-mandated three-month fish breeding ban has been implemented to allow fish stocks to recover. Seasonal grazing is equally important: as the plains dry, the area of the floodplain becomes dry soon the lechwe and other animals move near towards the fixed swamp, concentrating antelope on the permanent swamps.\n\nLake Kariba, on the Zambezi along the border with Zimbabwe, is the largest artificial water body in the country. It was formed by damming the river, and it was formed by damming the Zambezi River in the Kariba Gorge approximately 400 km downstream of Victoria Falls. Construction of the dam took place between 1956 and 1960, and Lake Kariba was filled between 1958 and 1963 following the completion of the Kariba Dam at its northeastern end, flooding a former gorge on the Zambezi River and displacing large numbers of the local Tonga people. The reservoir is the world's largest man-made reservoir by volume, four times as large as that created by the Three Gorges Dam. Figures for its storage capacity differ slightly between sources, from about 180 to 185 cubic kilometres. Its surface covers 5,580 km2 (2,150 sq mi), and its basin is shared with Zimbabwe, which is discussed elsewhere in this article.\n\nThe lake's economic roles are substantial. Its functions include hydroelectric power production and fishery. The reservoir also supports a commercial fishery for small sardine-like fish known as kapenta, which were introduced from Lake Tanganyika. Its shoreline has a deeply indented shore and contains many islands, which supports fishing and tourism. Its environmental record is less settled. The filling of the reservoir is linked to induced seismicity in the seismically active region, including over 20 earthquakes of greater than 5 magnitude on the Richter scale. Water quality and riparian ecosystems are also under pressure, and Lake Kariba is facing gradual deterioration of its water quality and its riparian ecosystems, potentially affecting its fishery and tourism industries.\n\nTaken together, these water bodies combine fish production, seasonal pasture and power generation, but their value depends on how they are managed, since the same seasonal and hydrological processes that sustain fisheries also make them vulnerable to drought, flood and dam operation."
    },
    {
      "heading": "Climate regime and seasonal cycle",
      "text": "Zambia lies within the tropics, but altitude softens that baseline. The climate is usually described as tropical in origin and modified by elevation, so for much of the year conditions feel more subtropical than equatorial. The modifying influence of altitude gives the country pleasant subtropical weather rather than tropical conditions for most of the year.\n\nThe annual cycle is best understood as one wet season and one dry season, with the dry season divided in two. The rainy season runs from November to April, starting a little earlier and ending a little later in the north, while the dry season runs from May to October or November. The dry season is subdivided into the cool dry season (May to August), and the hot dry season (September to October/November). The boundaries are not fixed in every source. Some sources place the start of the cool phase in April or May, and others use May to September for it, so the exact dates vary with the locality and the authority consulted.\n\nTemperature patterns across the plateau\n\nMost of the population lives on the central plateau, where the cool season is marked by a wide gap between day and night. The cool dry season experiences a mean daytime range of between 15°C and 27°C (6°C – 10°C in the evenings). In the capital, July is typically the coldest month in Lusaka, with night temperatures dropping as low as 9°C (48°F). Frost is possible in sheltered places: during the cool season, night frosts may occur in places sheltered from the wind. Clear skies allow heat to escape at night, and in depressions, radiation occurs on cloudless nights.\n\nThe hottest conditions occur late in the dry season rather than during the rains. Daytime temperatures are around 31°C/88°F in October, which is the hottest month. Extreme heat is concentrated in the low-lying river valleys. The Zambezi and Luangwe valleys occasionally reach into the early forties. By contrast, the high plateau stays much cooler, and the difference between plateau and valley temperatures is one of the clearest expressions of the altitude effect.\n\nThe ITCZ and the rainy season\n\nThe rains are driven by the Intertropical Convergence Zone (ITCZ), a belt where the trade winds of the two hemispheres meet. The climate is affected by the movement of the intertropical convergence zone (ITCZ), which is the meeting place of the sub-tropical high-pressure areas of the northern and southern hemispheres. The belt follows the apparent path of the sun. In January the ITCZ is in its southernmost position, and the rainy season is at its peak; by June it has moved north, and the weather is dry. The onset of rain is staggered. The movement into Zambia of the moist Congo air mass from the northwest heralds the start of the rains, in the north usually in early November and toward the end of the month around Lusaka. The retreat is equally gradual, and precipitation declines rapidly in April with the northward movement of the ITCZ. Because the zone lies north of the country during the dry months and drifts south in the second half of the year, the rains reach the north earlier and leave it later than the south. December and January are the wettest months.\n\nRainfall is also linked to large-scale climate variability. Research on Malawi and Zambia suggests that the ITCZ, alongside ENSO, shapes the wet and dry season characteristics in the region. Year-to-year differences in the timing and strength of the rains therefore affect how long the wet season lasts and how intense it is.\n\nKöppen classification\n\nUnder the Köppen system, most of Zambia falls into humid subtropical or tropical wet-and-dry categories. In the Köppen climate classification, most of the country is classified as humid subtropical or tropical wet and dry, with small patches of semi-arid steppe climate in the south-west. A regional survey of municipal climate types lists the humid subtropical type (Cwa) as dominant, with examples including Lusaka, Kitwe, Ndola, Chingola, Kabwe. The tropical savanna type (Aw) is found in other areas, with examples including Chipata, Mongu, Nakonde, Mwenzo. The Cwa category describes a warm, humid year with a marked dry winter, which matches the pattern of plateau rainfall described above. Annual totals vary widely, with most areas fall into the range of 700 to 1,200 mm, and the lowest values occur in the drier valleys."
    },
    {
      "heading": "Rainfall gradient and hydrological variability",
      "text": "Rainfall falls steadily from north to south, and this gradient shapes both the seasonal rhythm of rivers and the country's agricultural and energy systems. Typical figures place the northern provinces near 1,250 mm a year, against roughly 750 mm in the south. Rainfall is generally highest in the northern provinces of Zambia, decreasing from north to south. The climate-profile analysis treats the north and west as the wettest agro-ecological zone, with totals of 1,000 to 1,500 mm. Station data show the same contrast: Kasama in the north averages about 1,343 mm a year, while Choma has an average rainfall of 800 mm of which 369 mm falls in January and February. The driest areas lie in the Luangwa and middle Zambezi valleys, where totals are near 500 mm, and parts of these valleys are sometimes called semi-arid, though the country as a whole is not arid.\n\nThe wet season begins in the north and advances southward. The rains generally start in the north around the first week of November, and propagates towards the capital of Lusaka, reaching the central plateau over a period of weeks. Rain peaks in December and January, when the heaviest monthly totals are recorded. Much of this rain falls as intense showers rather than steady drizzle, with the rains occur mainly in the form of downpours or thunderstorms. Storms can arrive early: periodic thunderstorms lead to heavy rainfall and potential flash flooding in October, before the main season sets in. These brief, intense events produce rapid runoff, so river levels can rise sharply within a single season. The timing of this sequence follows the southward movement of the intertropical convergence zone.\n\nThe flood pulse that results is a recurring feature of the landscape rather than an exception. Inundation of floodplains happens every year, and people and wildlife are adapted to it. Seasonal water spreading across the lowlands supports fishing, grazing and wildlife movements, and the height and timing of each year's flood determine how productive these cycles will be. Because flows in the upper and middle rivers carry the wet-season pulse downstream, the size of a flood in one part of the basin affects communities many hundreds of kilometres away.\n\nYear-to-year variation is large. In the south, normal annual rainfall in southern Zambia is 600-900 mm per year but can be as little as 300-450 mm during El Niño periods and as high as 1,200 mm during flooding events. The El Niño–Southern Oscillation is the most consequential driver of this swing. The 2023–24 El Niño phenomenon intensified drought conditions across Southern Africa, reducing rainfall and Zambezi River inflows into Lake Kariba. Sources differ on the naming and timing of the worst phase. One account describes the 2024-2025 El Niño event as one of the region's worst droughts in decades, and reports that by the end of 2024 Lake Kariba held less than 2% of its usable capacity. Some climate scientists also warn that another strong El Niño could develop during the 2026–27 rainy season.\n\nThe effects of low flows appear most clearly in reservoir storage during the dry season. Most rivers, lakes and swamps are permanent, with the hotter, drier south as the principal exception. Even so, a weak rainy season can leave a reservoir with little reserve for the following months. At Lake Kariba, the level in one poor season moved less than 30 centimetres after the last rainy season, which barely materialized. In previous years, the water level would rise by six meters or more after the rains. Live storage available for generation fell to 7.7% of its usable storage. On the same date last year, this stood at 25%. Because more than 80% of Zambia's power supply came from hydropower in 2024, falling reservoir levels translated directly into outages, and severe shortages forced industries to scale back production and increased operating costs. The same low-flow conditions constrain pumping for irrigation and domestic supply, and downstream communities receive less water when reservoir releases are reduced."
    },
    {
      "heading": "Vegetation and ecoregions",
      "text": "Woodland dominated by miombo is the main plant cover in Zambia. One regional assessment places it at about 65% of the country, and it is the most extensive of the six ecoregions recognised there. Ecologists call this vegetation miombo, a term for the open woodland that is classed among the largest ecoregions on the African continent. Its canopy is built mainly by legume trees of the genera Brachystegia and Julbernardia, with Uapaca kirkiana and Combretum molle also common. Most of these trees lose their leaves in the long dry season, a period that lasts around seven months in the region.\n\nThe wetter central variant covers much of the north and centre of the country. It has the highest plant richness of any African miombo ecoregion, and its species peak lies in Zambia. It occupies the Central African Plateau between roughly 1,000 and 1,600 metres. Termite mounds concentrate nutrients in otherwise poor soils, creating patches of richer ground within the woodland.\n\nIn the drier south, woodland gives way to other types. The Zambezian and mopane woodlands occupy the lowlands along the Zambezi and its major tributaries. The dry miombo of southern Zambia includes stands of Baikiaea plurijuga, and much of its Zambian portion is rugged country where granite hills and inselbergs rise above the trees. Acacia and mopane woodlands are typical of the Luangwa valley in the east, where miombo grows on the Muchinga escarpment and thickets, grasslands and riparian forests occur on the valley floor. Baobab trees, which are typical of the drier lowland savanna, are a general feature of these southern and valley landscapes rather than a dominant element everywhere.\n\nThe high ground forms a separate pattern. On the Mafinga Mountains in the northeast, the highest parts are covered by montane grassland, while hill miombo covers most slopes, sometimes up to the crests. Montane forest patches occur within the reserved forest on these hills, and the massif hosts dozens of endemic plant and bird species. Intact miombo on the Muchinga escarpment supports a rich flora: the Mutinondo Wilderness alone has recorded 1,769 plant species. Fire in the montane grasslands and clearing for cultivation are the main threats to these forests.\n\nAlong the rivers and in the seasonally flooded plains, the vegetation changes with the water. The Barotse floodplain is predominantly grassland, with patches of semi-evergreen, evergreen and deciduous forest and shrubland. Its edges are bordered by dry grassland on sandy ground, woodland savanna to the east and south, and evergreen forest patches in the north and east. The flooded area grows from roughly 2,595 km² in the dry season to about 10,750 km² in the rainy season. The flooded grasslands of the Zambezi basin, the Bangweulu swamps and the Luapula delta are grouped as one ecoregion, although their grass and swamp communities differ from site to site. Adjacent sandy plains are classed separately as Western Zambezian grasslands, which have deep, nutrient-poor soils that are waterlogged in the rainy season and very dry in the dry season.\n\nMany of these vegetation zones have been reduced or altered by people. Around Lusaka, forest has been largely cleared for planting, firewood and charcoal, and on the Copperbelt, woodland has been extensively cleared while mining has polluted waterways. Protected areas such as Kafue National Park and Kasanka National Park cover parts of these ecoregions."
    },
    {
      "heading": "Soils and agricultural land suitability",
      "text": "Zambia's soils follow its geology and rainfall, and they determine where crops can be grown without heavy inputs. The largest constraint lies in the west. Across the Western Sandy Plains of the Kalahari Basin, the soils are very deep and drain freely, but they contain almost no clay or silt. Because clay is the main store of nutrients, these soils retain nutrients only where organic matter is present, and bare, sun-exposed surfaces lose that organic matter quickly. Soils of the Kalahari Sands therefore have little agricultural potential and remain largely under woodland. Some low-lying parts of the sand country are exceptions. Clay-rich old river beds that sit beneath the sand, which can be identified by termite mounds, are more productive, and the dambos and seasonal pans of the plains provide grazing and cropland. The floodplain of the Zambezi in Western Province is more fertile still.\n\nMost of the plateau is covered by weathered soils that are typically acidic and low in nutrients. A government-linked study of Zambian agro-ecological zones describes the dominant soils of the southern and western sandy zones as sandy, acidic and poor in nutrient reserves, with poor water retention. Heavy rain leaches nutrients out of such soils, and dry spells cause water stress. Soil acidity is therefore a dominant constraint on crop production in much of the country, and the valley soils, which are slightly acidic to alkaline, are generally more fertile than those of the plateau. Long-term cultivation makes the problem worse. A 2025 study of two rainfall zones found that soil organic carbon fell on average by 1.2 g per kg after five years of cultivation on Arenosols in the high-rainfall zone, and by 0.8 g per kg after ten years on Acrisols in the medium-rainfall zone, which indicates the vulnerability of the sandy soils to disturbance.\n\nAgricultural planning is organised around three agro-ecological regions, which are defined by rainfall, altitude, soil type and temperature. Region I, in the south, is the hottest, driest and poorest zone, with rainfall of roughly 600 to 800 mm and sandy, poorly fertile soils. Its farming relies on maize as well as sorghum, millet, groundnuts and cattle, with cassava also important. Region II, the central band with 800 to 1,000 mm of rainfall, is the main farming zone. Its sub-region IIa is the most productive area for maize, wheat, soybean, groundnut and tobacco, and it supports most of the commercial maize output. Region III, in the north and northwest, receives more than 1,000 mm of rain and has moderately fertile acidic soils that suit cereals, legumes, tubers and cassava. Crop choice therefore follows the rainfall gradient: maize dominates the south and east, while cassava forms the staple in the north and northwest. Sources differ on the altitude limits of the zones, so the exact boundaries should be read as approximate.\n\nCoffee is grown mainly in the cooler, wetter northern highlands. Kasama, Mungwi and Mbala districts are identified as the most suitable areas, and according to provincial government material, Northern Province contributes about half of national coffee exports. Coffee is part of a wider group of cash crops that includes cotton, tobacco, tea and sugarcane, which together form the main agricultural exports. Within the overall land use, more than 2.4 million hectares are planted with annual crops, most of them rain-fed. Maize accounts for about 42% of this area, followed by wheat at about 12.8% and cassava at about 11.8%. Because rain-fed farming is sensitive to variable rainfall, the sandy and acidic soils of much of the country are a persistent limit on yields, and they are one reason that fertiliser use and irrigation feature so prominently in agricultural policy."
    },
    {
      "heading": "Protected areas and wildlife geography",
      "text": "Zambia's protected estate is organised largely around its river systems and seasonal floodplains, which concentrate water and grazing for wildlife. The main parks are described below, followed by the wetlands and the transboundary framework.\n\nRiver-valley and floodplain parks\n\nSouth Luangwa covers 9,050 km² in the valley of the Luangwa River, which forms the park's eastern boundary. A steep escarpment, the Muchinga Escarpment, bounds it to the west. The area was first protected as a game reserve in 1938 and became a national park in 1972. Its vegetation is a patchwork that includes miombo forests and open dambos, mopane forests, and lush riverine vegetation along the Luangwa River.\n\nLower Zambezi lies on the opposite side of the country's southern border. A floodplain runs alongside the river, dotted with curved lagoons and sandbanks. The park lies opposite Zimbabwe's Mana Pools Reserve, so the area on both sides of the Zambezi forms one large wildlife sanctuary. Its wildlife is concentrated along the river, where elephants and buffalo are especially easy to see.\n\nKafue, the largest park in the country by most accounts, is roughly split by the Kafue River. The river runs across rapids and calm stretches before reaching the Itezhi Tezhi Dam. The area was founded as a reserve in the 1920s and formally established as a national park in the 1950s. Its size is commonly given as about 22,000 km², and it hosts large carnivores. Lochinvar, a much smaller park, lies on the southern edge of the Kafue Flats, a wide Kafue River floodplain between the Itezhi Tezhi dam and the Kafue Gorge.\n\nLiuwa Plain, in the west, is set in a floodplain of the upper Zambezi and covers about 3,660 km². Large herds of wildebeest gather there in November. Predators such as wild dog, lion and hyena also occur there. The park was remote for a long time, and it had no roads until recently.\n\nWetlands and seasonal water\n\nBangweulu is the country's principal wetland system. It is adjacent to Lake Bangweulu in the north-east of the country. Its landscape consists of floodplains, seasonally flooded grasslands, woodlands and permanent swamps, fed by the Chambeshi, Luapula, Lukulu and Lulimala rivers. The water cycle sets the wildlife calendar. During the rainy season, from November to April, the lake floods and the grasslands are covered in water. As the dry season sets in, the wetlands recede quickly over May, June and July.\n\nThe system supports unusually specialised species. The area holds several hundred shoebills and is the only place in the world where black lechwe are found. Black lechwe are endemic and gather in herds of up to 10,000 animals. Over 400 bird species have been recorded, and the wetlands are home to about 80 fish species.\n\nThe Kavango–Zambezi transboundary area\n\nZambia's wildlife geography extends beyond its borders through the Kavango–Zambezi Transfrontier Conservation Area (KAZA). It spans parts of five southern African countries: Angola, Botswana, Namibia, Zambia and Zimbabwe. The area was formally established in 2011 by the five partner countries. Sources differ on its ranking. WWF calls it the world's largest land-based transboundary conservation area, while another reference describes it as the second-largest nature and landscape conservation area in the world. The Zambian portion lies in the south-west, and includes Kafue National Park, Sioma Ngwezi National Park and Mosi-oa-Tunya National Park, together with adjoining game management areas and forest reserves.\n\nThe framework is designed to reconnect habitats fragmented by borders and development. Its stated objectives include the creation of a linked network of protected areas that restores dispersal corridors and migratory routes. Historically, migratory pathways were blocked for decades by political borders, fences and human settlements. KAZA's land uses include national parks, forest reserves and community-managed areas.\n\nPressures and management responses\n\nWildlife losses in Zambian protected areas have been severe in places. Before management changed at Bangweulu, heavy poaching decimated the park's large mammals, and lion, cheetah and black rhino were completely wiped out. Other pressures are documented across the wetlands: the area is under pressure from poaching, fishing, livestock grazing and chitemene cultivation on its margins. Gillnet use has also reduced fish stocks, as the increased use of mosquito nets for fishing has decreased fish populations in Bangweulu and throughout Zambia.\n\nManagement has taken a co-management form. In 2008 African Parks began managing Bangweulu in partnership with the Department of National Parks and Wildlife, through the Bangweulu Wetland Management Board. That board includes representatives of African Parks, the Zambia Wildlife Authority and six community members. Community programmes, including beekeeping and sustainable fisheries management, were developed, and poaching and other illegal activity have been largely contained, with fish stocks recovering. Restocking has also been used. In 2017, 250 animals including impala and zebra were released into the wetlands, and in 2019, 95 buffalo were moved from another Zambian park to increase genetic diversity.\n\nAcross the KAZA landscape, restoration programmes include efforts to promote forest cover restoration, restocking of wildlife, nature-positive livelihoods, and the stabilisation of headwater, riverine and lagoon wetlands. These measures respond to the same pressures that shape the parks: competing land use along their edges, and seasonal water that determines where wildlife can live."
    },
    {
      "heading": "Mineral resources and mining geography",
      "text": "Zambia's mineral wealth is concentrated in the northwest, where the geological setting of the Copperbelt has produced some of the largest sediment-hosted copper and cobalt deposits in the world. The Zambian Copperbelt forms the southeastern part of the Neoproterozoic Lufilian Arc, a belt of folded and thrust-faulted rock about 900 km long that crosses the border with the Democratic Republic of the Congo. Its ore output is exceptional: in excess of 1 × 10^9 t of ore at about 2.7% copper has been extracted to date, and major cobalt accumulations are also present. The copper-cobalt ores of the region contain more than 200 Mt of copper, equivalent to 15% of known global copper resources, and the region holds the world's largest cobalt reserve.\n\nThe ores sit in Neoproterozoic sedimentary rocks. The copper and cobalt mineralization is hosted by the Lower Roan sedimentary rocks of the late Precambrian Katangan Supergroup. Mining in the Lower Roan Formation targets ore dominated by pyrite, chalcopyrite, bornite and chalcocite, and the primary sulphides are predominantly chalcopyrite, bornite and chalcocite. Structure controls where the metal concentrates. Two distinct structural regimes are recognized in the Nchanga area, and faulting and folding are considered to be synchronous, as folding predominantly occurred at the tips of propagating thrust faults. At Luswishi, higher copper grades are linked to the Kirilabombwe anticline and fault zones along the axial plane. Near-surface weathering has also reworked the ores, with deep supergene enrichment and leaching occurring up to a km in depth.\n\nGemstone mining is dominated by the Kagem emerald operation in the Kafubu area. The 41 square kilometre licence area is located in the Ndola Rural Emerald Restricted Area and lies south of Kitwe and west of Ndola, in Zambia's Copperbelt Province. It is 75% owned by Gemfields and 25% owned by the Government of the Republic of Zambia. The mine is the largest emerald mine in the world and supplies roughly a quarter of global production, sold through auctions. Yields are low: at Kagem, a mere 50 grams of \"emerald and beryl mix\" is recovered for every 100 tonnes of earth excavated, and within that mix only 0.3g is considered premium emerald. Earlier bulk-mining methods were also costly to the stones themselves, since ore below the weathered zone was blasted, crushed, washed, and sorted, at the expense of some loss of emerald crystals.\n\nCoal is much less geographically concentrated. Maamba in Southern Province is the country's only large coal operation, majority held by India's Nava, and it is linked to a 300 MW thermal power station, with a second 300 MW unit under construction. The mine's output has been unstable; after the 1997 flooding of the mine, production returned to a range of 150,000 to 180,000 tonnes per year. Coal supply therefore links the mineral sector to the power system rather than to export markets.\n\nMining has shaped the country's towns and infrastructure more than any other sector. Copperbelt towns such as Kitwe and Ndola grew around the mines, and their demand for water and rail and road transport follows mine output. Water is a particular pressure point: in February 2025, nearly 500,000 households in Kitwe were cut off from water supply after a spill, which shows how dependent urban supply is on the surrounding river systems. Export of copper and cobalt also relies on ports reached through neighbouring countries, which connects the mining economy to the logistics networks described elsewhere in this entry.\n\nMining has also caused serious environmental damage. On 18 February 2025, a tailings dam at a Sino Metals operation at Chambishi released more than 50 million litres of acidic effluent into the Mwambashi River, and the spill flowed through the Kafue River and farmland, poisoning fish, livestock and damaging aquatic and terrestrial ecosystems. Much of the chronic pollution comes from acid mine drainage, which forms when mining activities expose sulfide minerals to the near-surface environment and oxygen, and it pollutes surface water and groundwater resources and destroys aquatic ecosystems. Other sources include dust fall out from tailing facilities and emissions from smelters, which contaminate soil and crops. In Kitwe, heavy metal pollution originates from the Uchi mine tailings, Nkana smelter, and slag dump sites in the town's industrial area. Local soils near Nkana show copper concentrations far above the global terrestrial average of 23 ppm. The Kafue River has some natural buffering, since the contamination of the Kafue River water is relatively limited due to its high neutralization capacity. Responses to these incidents have been limited, although the Zambia government announced an independent investigation into the ongoing pollution of the nation's waterways, particularly in the Copperbelt region."
    },
    {
      "heading": "Hydroelectric power and energy geography",
      "text": "Hydropower dependence and the main stations\n\nZambia's electricity system rests on a small number of large dams on the Zambezi and Kafue rivers. It brought the Kariba Dam online in 1960, four years before it gained independence, and completed the Kafue Gorge Dam in 1973. Estimates of the hydro share differ by source and year: one recent figure puts it at 84% of electricity supply, while another gives 83%. Installed capacity figures also vary. One breakdown lists Kafue Gorge (990 megawatts) and Kafue Gorge Lower (750 megawatts) as the country's two largest stations, followed by Kariba North Bank (720 megawatts) and its extension (360 megawatts) and Victoria Falls (108 megawatts), whereas other sources give the Kariba North Bank station a larger rating of about 1,080 MW.\n\nKafue Gorge Lower, built with Chinese finance, is the most recent major addition. By March 2023, all five units of the hydropower station were successfully connected to the grid and in operation. The station also plays a role in regulating the grid, providing peak and frequency regulation.\n\nThe siting of these plants follows the terrain. The Kafue system is central to the country's economic geography, since most of the country's mining, agriculture, and population is concentrated in the Kafue Basin. Across the wider Zambezi basin, more than half of the potential is in Mozambique, about one-quarter in Zambia and one-sixth in Zimbabwe, which means Zambia's hydro resource is significant but not the largest in the basin.\n\nDrought, seasonal variation and supply shortfalls\n\nBecause hydro output depends on inflow, rainfall deficits translate directly into lost generation. In the 2015 drought, because of decreased water levels, Zambia had to cut its generation from 500MW to 305MW in late August. Earlier, the 2014 drought had already forced it to implement rolling blackouts – often lasting for 8 hours a day – in residential areas.\n\nThe most severe episode came in 2024. The Kariba North Bank Power Station has closed 5 of its 6 generating units due to decreased lake levels. This shutdown has drastically reduced electricity generation capacity from the initial 1,080 megawatts to only 214 MW. The shortfall reached 1,600 megawatts in February 2024, and ZESCO has implemented load shedding for up to 21 hours per day. Output at Kafue Gorge also fell: Kafue Gorge generated 3,187.35 gigawatt hours in 2024, down from 3,805.87 gigawatt hours in 2023.\n\nDemand concentration amplifies these effects. Approximately 70 percent of national electricity output is consumed by the country's mines in the Copperbelt Province. When supply falls, cuts reach industry first, and the 2015 drought forced it to extend these blackouts to copper mines, cutting their electricity supply by 30 percent. Shortages also affected the regional trade position. Zambia had once produced an electricity surplus and exported it to Mozambique, Tanzania and South Africa, and in the 2024 crisis the withdrawal of 400 MW from exports cut revenue for the utility.\n\nTransmission, imports and shared water\n\nThe Kariba complex sits on a shared river. Each country has its a power plant on different sides of the dam wall but they share the water source. Zambia has also relied on imports from its southern neighbour: power imports from neighboring Zimbabwe have doubled, rising from about 200 megawatts to around 400 megawatts.\n\nOfficials have identified grid infrastructure as a bottleneck. Recent government statements note that seven transmission line projects are currently under construction to ensure reliable evacuation of power and improved grid stability once new capacity is commissioned. President Hichilema has also urged energy sector players to prioritise investment in transmission and distribution infrastructure so that new generation capacity can be delivered reliably to consumers. Zambia's involvement in regional power trading is expected to grow, with new battery-storage projects cited as a way to improve grid flexibility.\n\nDiversification and its geographic constraints\n\nSince 2021 the government has pushed diversification, mainly toward solar. Zambia's installed solar PV capacity has surged from 88 MW in 2021 to approximately 841 MW in 2026, including around 584 MW of identified utility-scale projects and 30 MW under net metering. A later government announcement put installed solar at 1027MW, surpassing the 1000MW target by 27MW, so figures from different dates and definitions should be read with care. Solar plants are concentrated in the Copperbelt and central regions; the largest operating facility is the 136 MW Itimpi II PV plant in Kitwe.\n\nSolar and hydro complement each other seasonally, since stronger solar potential often coinciding with drier conditions and weaker hydro output. However, the solar resource is not the binding constraint. One analysis notes that bankable projects are constrained by wheeling tariffs and PPA bankability, not by sun resource. Thermal generation fills part of the gap. Coal contributes 9%, solar 3%, and heavy fuel oil 5% in one breakdown, with coal-fired projects such as those linked to Maamba Collieries in the south under development. The long-term goal is ambitious: Zambia remained committed to reaching 10000MW of generation capacity by 2031, which would require a large expansion of both generation and grid capacity."
    },
    {
      "heading": "Population distribution and urbanisation",
      "text": "Zambia's population is distributed very unevenly across its territory. The 2022 census recorded a total of 19,693,423 people, and the national split between countryside and towns was close to even, with 55.3 percent of the total population in rural areas and 44.7 percent in urban areas. Settlement density, however, is highest in a few provinces. Lusaka Province was the most densely populated, at 140.1 persons per square kilometre, and Copperbelt Province was second, with a density of 88.0 persons per square kilometre. Most of the dense settlement lies along the transport axis: estimates describe the urban population as concentrated along the line of rail. By contrast, Muchinga Province had the lowest share of the population at 4.7 percent in 2022.\n\nThe major urban centres are the product of mining and administration. Lusaka, the capital, is the largest city, with a city population of 2,212,301 in the 2022 census, while the Copperbelt cities of Kitwe and Ndola recorded 665,961 and 627,503 respectively. The Copperbelt's early urban growth is rooted in the colonial period: Zambia was already one of the most urbanised colonial territories in Africa mainly because of the industrialisation of the Copperbelt, which created large towns in that region. Since then, Lusaka has become the fastest-growing centre. The province has the highest growth rate, with an average of 4.6%, compared to the national growth rate of 2.8%. Lusaka Province also surpassed the Copperbelt as the most populated province by the 2010 census. Nationally, the urban population rose from 5,173,450 in 2010 to 8,793,369 in 2022, a faster pace than the rural increase over the same period. Figures for Lusaka Province vary between publications: the preliminary census report gave a slightly lower total than the final analytical report, so the final figures are used here.\n\nRural settlement is more dispersed and less uniform in character. Rural residents still outnumber urban residents in absolute terms, with the rural population (10.9 million) outnumbering the urban population (8.8 million). Eastern Province had the largest rural population at 2,018,497, which makes it the most important region for smallholder settlement. Zambia's ethnic composition follows a similar regional logic. Nine main ethnolinguistic groups are commonly identified, including the Nyanja-Chewa, Bemba, Tonga and Lozi, and in the rural areas, each ethnic group is concentrated in a particular geographic region of the country. Urban areas, especially Lusaka, mix these groups far more, and Lusaka is often described as a place where every Zambian ethnic group is represented.\n\nRapid urban growth has outpaced formal service provision, and much of the new housing in Lusaka is informal. An estimated 60-70% of Lusaka's residents live in low-income informal settlements known as Peri-Urban Areas (PUAs). These areas are unplanned and have poor access to primary services including water, trash collection, electricity, and sewage. Water supply is patchy: water supply is through a combination of stand points, kiosks, hand pumps, and unprotected wells, and 57 percent of Lusaka's water supply is derived from fairly shallow groundwater abstracted within the city, which is prone to contamination. Sanitation is weaker still, since sanitation facilities are mostly pit latrines; septic tank systems are rare. To partly close the gap, Water Trusts were created: public/private partnerships designed to provide clean water to peri‐urban community residents. The consequences are serious; sanitation problems have caused regular cholera outbreaks in the capital. Urban planning in these areas is therefore a continuing challenge, as population growth and urban influx have strained the ability of the Lusaka City Council and service providers to provide adequate water and basic sanitation facilities."
    },
    {
      "heading": "Transport corridors and landlocked access",
      "text": "Zambia has no seaport of its own, so nearly all of its external trade moves through the territories of its neighbours. It uses ports in South Africa, Mozambique, Tanzania, and Namibia. The main gateways are Dar es Salaam, Beira, Durban, Walvis Bay, and the Angolan and Mozambican ports of Lobito and Nacala. Durban is reached through the North–South Corridor, and Beira is a close and frequently used port. Zambia's government has described its corridors as giving access to all Southern African Development Community seaports, yet with those routes largely unexploited. Because the country's copper exports dominate the cargo mix, the choice of outlet has large effects on mining costs and export revenue.\n\nRail links\n\nThe Tanzania–Zambia Railway (TAZARA) is the most important rail link to the Indian Ocean. The Tanzania-Zambia Railway runs approximately 1,860 km between Dar es Salaam and New Kapiri Mposhi in Zambia. It was constructed in the 1970s with Chinese assistance, and it was intended to provide Zambia with a reliable export route to the Indian Ocean. Its traffic was small for decades; by one account the Dar es Salaam port now handles 15 million tonnes a year as opposed to five million in the 1970s, which reflects the rise in regional freight rather than a single railway's performance. A 30-year concession signed in 2025 provides for rehabilitation, and it is intended for rehabilitation of track and railway infrastructure, along with new locomotives and wagons.\n\nThe Lobito Corridor is the western alternative. It is a rail and logistics project that aims to connect the Port of Lobito on the Atlantic coast of Angola to the Central African Copperbelt, and it is about 1,300 km long. The Benguela Railway behind it was completed in 1931, but decades of civil conflict in Angola reduced operations to just 34 km, which pushed Zambian copper towards the eastern and southern routes. The Angolan section has since been rebuilt, but reports disagree on the Zambian section. A 2025 agreement between the EU and Zambia covers feasibility studies for a new rail line through the Northwestern Province to the Copperbelt, while a 2026 report states that the Zambian extension has not yet broken ground.\n\nRoad routes\n\nTwo highways carry most of the road freight. The Great North Road, designated T2, runs north from Lusaka through Kabwe, Kapiri Mposhi, Serenje, Mpika, Isoka and Nakonde to the border with Tanzania. It is about 1,019 km long and forms the Zambian section of the Tanzam Highway, which links the country with Dar es Salaam. Kapiri Mposhi, where the TAZARA line meets the road network, has been developed as a logistics site, with a planned logistical hub at Kapiri Mposhi that will combine customs and warehousing for Zambia and the Democratic Republic of the Congo.\n\nThe Great East Road, about 595 km long, runs east from Lusaka and is also the major link between Zambia and Malawi and between Zambia and northern Mozambique. Its position is also a weakness. Because the Luangwa valley blocks direct routes, a narrow neck of land in the west became the only way in from or out to the rest of Zambia, and as the only highway to cross it, the Great East road is strategically vulnerable. A project to upgrade about 360 km of the road links the country to the Nacala Development Corridor, and that route will offer a significantly shorter route to/from the sea for Zambian imports and exports than other existing routes through South Africa and Tanzania once it is fully upgraded.\n\nAir links and border crossings\n\nKenneth Kaunda International Airport in Lusaka is the country's principal air gateway and is the only airport that handles air cargo. The airport was expanded in a project that began in 2015 with funds borrowed from the Exim Bank of China, and its international terminal, Terminal Two, opened in August 2021, has six gates and handles all international flights. Air freight is expensive for a country whose exports are mainly bulk minerals, so air transport serves mainly high-value goods and urgent shipments.\n\nBorder crossings add time and cost to road freight. A 2009 United States International Trade Commission study described the Chirundu crossing with Zimbabwe, which was then one of the busiest inland crossings in the region, where queues of trucks which have to wait an average of 4 days to clear Customs. More recently, Zambia moved to full 24-hour operations at the One Stop Border Post, matching Tanzania's existing schedule, aimed at the Tunduma–Nakonde crossing. Delays of this kind raise the cost of every tonne of copper or fuel that crosses a border, and they encourage fewer opportunities for informal payments that quietly inflate transport costs."
    },
    {
      "heading": "Administrative divisions and political geography",
      "text": "Provinces, districts and the capital\n\nZambia's first-level divisions are its ten provinces. The Electoral Commission's district sittings in February 2026 covered all 116 districts of the country (the ECZ conducted district delimitation sittings across all 116 districts of Zambia). Lusaka Province, which contains the national capital, is the smallest province by land area at 21,896 km², yet it is the most populous and densely settled, with 3,079,964 residents in 2022 (It is the smallest in terms of land area, covering 21,896 km2. However, it is the most populated and densely populated province in Zambia, with a population of 3,079,964 as of 2022). The city of Lusaka is the provincial capital and also the national capital (The provincial capital is Lusaka, which is also the national capital of Zambia.). The province has six districts, and Lusaka District, the most urbanised of them, is governed through a mayor-council structure (Type: Mayor-council government).\n\nLegislature and presidential elections\n\nThe National Assembly is the unicameral legislature of Zambia, and the head of state is elected directly. A presidential candidate must secure more than 50% of the valid votes cast to be elected in the first round. General elections follow a five-year cycle. The previous poll before 2026 was held on 12 August 2021, and the 2026 general elections took place on 13 August 2026 (General elections were held in Zambia on 13 August 2026 to elect a president, members of the National Assembly, councillors and council chairs.). Both dates fall on the second Thursday of August.\n\nConstitutional reform and electoral geography\n\nThe electoral map was redrawn by the amendments to the constitution in 2025, which were enacted as the Constitution of Zambia (Amendment) Act No. 13 of 2025. The constituency count had stood at 156 since a 2016 amendment (There was an amendment to the constitution whereby the number of constituencies was increased to 156.). The 2025 amendment expanded the number of constituency seats to 226, and the Electoral Commission of Zambia announced the 70 new constituencies on 16 April 2026 (The amendment increased the number of constituency-based seats from 156 to 226 through the creation of 70 new constituencies, which the Electoral Commission of Zambia announced on 16 April 2026.). The reform also created a second tier: 40 members elected by proportional representation based on the presidential vote (of which 20 are seats reserved for women, 15 for youth and five for persons with disabilities), up to 11 members appointed by the president. The reform was contested before it took effect; a legal challenge over its constitutionality reached the Constitutional Court, but the amendment was revised and passed by parliament.\n\nThe new constituencies are distributed unevenly among provinces. The Copperbelt, Eastern and Southern provinces each have 29 constituencies, while Muchinga has 14 and Lusaka has 18 (Central Province now has 23 constituencies, Copperbelt 29, Eastern 29, Luapula 20, Lusaka 18, Muchinga 14, Northern 19, North-Western 19, Southern 29, and Western 26.). Lusaka Province's constituency count is therefore modest relative to its population, and the Lusaka District alone is divided into ten constituencies.\n\nResults and local government\n\nThe 2026 presidential result was declared on 18 August, when the Electoral Commission chairperson named the incumbent Hakainde Hichilema as president-elect (\"I therefore declare Hichilema Hakainde S to be president-elect of the Republic of Zambia this 18th day of August, 2026\"). Official figures gave him roughly 61% of the vote against about 38% for Brian Mundubile (Official results show the incumbent receiving roughly 61 percent of votes, compared with 38 percent for his main challenger, Brian Mundubile.). The United Party for National Development won 136 of the constituency seats (UPND | Hakainde Hichilema | 136). Mundubile had claimed victory on 14 August, before the commission had named a winner (At the time, the ECZ had not announced a winner and was still verifying and tabulating results from the 226 constituencies.). Observers differed in their assessments: one regional mission described the environment as peaceful in most areas, while another summary notes that observers cite violence and a tilted campaign field.\n\nBelow the national level, the same election cycle chose local bodies. Zambia has 116 city, municipal and town councils, each led by a mayor or council chairperson, and 1,858 wards with councillors. These councils are the institutions that deliver municipal services such as roads, markets and drainage, and they operate within the national framework set by the central government."
    },
    {
      "heading": "Transboundary waters and regional cooperation",
      "text": "The most prominent shared water asset is the Zambezi system, where the Kariba Dam sits on the border with Zimbabwe. The project was a joint venture between the former self-governing protectorates of Northern and Southern Rhodesia (now Zambia and Zimbabwe) and Nyasaland (now Malawi). The arch dam was constructed between 1956 and 1959 and supplies water to two underground hydropower plants located on the north bank in Zambia and on the south bank in Zimbabwe. Building the dam and its reservoir displaced around 57,000 Tongan people living along the Zambezi in Northern and Southern Rhodesia. Sources give differing capacity totals: one puts the output at 1,626MW of electricity, while another lists a combined installed capacity of 2,010 MW.\n\nOperation of the dam rests on an institution rather than on either government alone. The predecessor body, the Central African Power Corporation, was established in 1963 to control power generation and transmission in both Northern and Southern Rhodesia. It was later reconstituted as the Zambezi River Authority (ZRA) through parallel legislation passed in 1987. The ZRA is a bi-lateral organisation jointly and equally owned by the Governments of Zambia and Zimbabwe. Its remit covers the operation, maintenance, and management of the Kariba Dam Complex and the sustainable management of the shared water resources of the Zambezi River. The authority also handles the water allocation to the Kariba North and Kariba South power plants. The dam's early decades were marked by serious flood management problems: in the first 20 years after the dam was constructed there were sustained heavy spillage episodes, which led to a later rehabilitation. That project cost US$294 million and was financed by the European Union, the World Bank, the African Development Bank, the government of Sweden and the ZRA itself.\n\nAt the basin scale, cooperation is organised through the Zambezi Watercourse Commission (ZAMCOM). It is an intergovernmental organization currently set up by eight (8) Riparian States that share the Zambezi Watercourse through the ZAMCOM Agreement of 2004. The member states are Angola, Botswana, Malawi, Mozambique, Namibia, United Republic of Tanzania, Zambia and Zimbabwe. The basin drains about 1.4 million sq km. The agreement entered into force in 2011, and the commission's headquarters are in Harare. Its stated objective is the equitable and reasonable use of the basin's water resources and their sustainable development. The diagnostic phase identified five major issues affecting the basin including persistent poverty, the management of competing uses, an infrastructure deficit, environmental degradation, and a lack of climate-resilient development. Member states have chosen to focus on the infrastructure deficit and on deeper basin-wide collaboration as guiding principles for future planning. The work is anchored in a Strategic Plan for the Zambezi (2018 – 2040), which provides a framework for investment and management of shared water resources.\n\nThe northern boundary includes Lake Tanganyika, which lies within the western branch of the East African Rift Valley. The lake is the longest, and second deepest, freshwater lake in the world and is shared by four riparian countries: Burundi (8%), the Democratic Republic of the Congo (45%), Tanzania (41%) and Zambia (6%). Zambia's share of the shoreline is therefore small, but its fisheries depend on the lake. The Convention on the Sustainable Management of Lake Tanganyika was adopted in Dar es Salaam, Tanzania on 12 June 2003, and entered into force in 2005, with Zambia among the contracting states. The Lake Tanganyika Authority, launched in December 2008, has the mandate to safeguard the lake and its resources. Management remains uneven: while there is cross-border cooperation to gather fisheries data to inform lake-wide management, the ban's unbalanced implementation shows that cross-border resource governance is fragmented.\n\nFurther east and south of the lakes, the Luapula system links Lake Bangweulu with Lake Mweru on the border with the Democratic Republic of the Congo, so that flows and fisheries in the Congo basin are shared across the same boundary. Across all these basins, the same pattern recurs: dams and hydropower depend on water allocation agreed between states, fisheries and navigation depend on joint rules, and trade and transport routes run across river and lake crossings. Cooperation over shared watercourses therefore shapes the reliability of electricity supply and the cost of regional commerce as much as it does environmental management."
    },
    {
      "heading": "Climate change exposure and adaptation",
      "text": "Observed and projected change\n\nZambia's climate has already warmed. Mean annual temperature has risen by about 1.3 °C since 1960, and rainfall has declined, with the south-west hit hardest and its rainy seasons shortening (climate change trends recorded in the UNEP and national data). Annual rainfall has fallen by roughly 1.9 mm per month per decade since 1960, a drop of about 2.3% per decade, concentrated in December to February (ITCZ and ENSO shifts are the main drivers of variability). Droughts, dry spells and floods have all become more frequent and more intense.\n\nProjections for the mid-century point to continued warming of about 1.5 to 3 °C by 2050, depending on emissions pathways. Hot days are expected to increase by 15 to 29% and hot nights by 26 to 54%. Under a high-emissions scenario, late-century warming could reach 3 to 5 °C. Rainfall projections are less certain. Model ensembles generally show drier conditions in September to November and somewhat wetter conditions in December to February. Rainfall in the south-west could fall by up to 8%, while the north-east could receive up to 7% more. Drought hazard is projected to rise markedly in the Western, Southern, North-Western and Lusaka provinces, and a larger share of rain is expected to fall in heavy events.\n\nWater resources and hydropower\n\nBecause most of the country's water comes from rainfall, changes in precipitation feed directly into river flows. One basin-level study projects that national water availability could drop by about 13% by 2100. The Zambezi, Kafue and Luangwa basins are among those expected to lose the most, while northern basins may hold steady or gain slightly. The same pressures weigh on the energy system. Hydropower supplies more than 80% of electricity generation, mainly from Kariba and Itezhi-Tezhi, so any reduction in inflow to these reservoirs translates quickly into lost generation.\n\nThe 2023–2024 drought showed how exposed this system is. Lake Kariba's live storage, the water actually available for turbines, fell to about 7.7% of usable capacity in September 2024, and the Zambian station at the lake was shut down. Rolling outages of up to 21 hours per day followed. Analysts attributed the low levels to a combination of drought, high evaporation under extreme heat and water abstraction for growing energy demand. Planned expansion adds further uncertainty: the Batoka Gorge scheme, a 2,400 MW project on the Zambezi that Zambia and Zimbabwe are advancing, has drawn criticism because its projected output depends on river flows that climate change may reduce.\n\nAgriculture and rural livelihoods\n\nAgriculture employs a large share of the rural population, so changes in rainfall and temperature affect food security and household income directly. Economy-wide modelling projects that crop yields will fall over time, with maize expected to be the hardest hit. Adaptation planning has warned that shorter rainy seasons and higher seasonal temperatures could make large areas unsuitable for maize, which is the staple crop. Southern and western districts face the greatest risk. Under these conditions, cassava is often cited as a more resilient option than annual cereals, and sorghum, beans, cowpeas, groundnuts and pigeon peas are promoted as alternatives. Crop trials have also shown that some crops, such as cowpea and pigeon pea, can sustain yields under water stress because of their ability to fix nitrogen.\n\nAdaptation measures\n\nZambia's National Adaptation Plan identifies agriculture, food security, fisheries, water, forestry, wildlife, health, mining, tourism, human settlements and infrastructure as priority sectors. Its agricultural measures include promoting drought-tolerant seed and climate-smart practices, such as conservation farming, agroforestry, crop rotation and integrated soil-fertility management. Water measures include water harvesting, weirs and small-scale irrigation, along with better catchment management and community-based water governance. The government is also strengthening early-warning systems, including a drought management system, to give farmers and utilities earlier notice of dry spells.\n\nIn the energy sector, policy aims to diversify generation toward solar, wind and other renewables, so that hydropower is no longer the dominant source. Reducing reliance on charcoal and firewood is also seen as a way to cut deforestation and the emissions that accompany it. Because these alternatives depend on different geographies and infrastructure, their effectiveness varies by region and by the timing of investment."
    },
    {
      "heading": "Exploration, mapping and geographical knowledge",
      "text": "Human activity in the territory is documented far earlier than any written record, and some of the clearest evidence lies at Kalambo Falls. The falls, a 235-metre (772 ft) single-drop waterfall on the Kalambo River, sit on the Zambia–Tanzania border near the southeastern end of Lake Tanganyika. The site is considered one of the most important archaeological sites in Africa, with occupation spanning over 447,000 years. Its waterlogged sands were excavated in the 1960s, but the wooden finds could not be dated at that time. Later luminescence dating showed that the deposits are far older than had been assumed, and in 2023 researchers described two interlocking logs about 476,000 years old that may represent the earliest use of wood in construction. The find challenged the assumption that Stone Age people were wholly nomadic, since the site offered both water and forest resources for a more settled life.\n\nWritten knowledge of the interior grew through nineteenth-century exploration. Before European travellers arrived, the plateau was home to states such as those among the Chewa, Bemba, Lunda and Luyana (later Lozi), whose networks of exchange and political ties shaped the regional geography. Kalambo Falls illustrates how measurements improved over time: early estimates of its height exceeded 300 metres, while 1920s measurements gave a figure above 200 metres, and a 1956 measurement gave 221 metres. A 1928 expedition led by Enid Gordon-Gallien mapped the falls and the surrounding area.\n\nThe most famous explorer associated with the region is the Scottish missionary and explorer David Livingstone. On 16 November 1855 he viewed the falls from an island now known as Livingstone Island, immediately upstream from the falls near the Zambian shore. He named the sighting in honour of Queen Victoria, although the Lozi name Mosi-oa-Tunya, meaning \"the smoke that thunders\", remained in common use. At the falls he also measured the depth of the gorge with a weighted string and estimated the width of the cataract, which made his account unusually quantitative for its time. Livingstone's later journeys took him to the Bangweulu region: he pressed on through swampland and, the following year, became the first European to see Lake Bangweulu. He died in 1873 at Chief Chitambo's village near Lake Bangweulu, which was then part of what became Northern Rhodesia.\n\nThe modern borders were not drawn by surveys of the land itself but by diplomacy in the 1890s. The British South Africa Company, chartered in 1889 under Cecil Rhodes, administered the region, and the boundaries came from treaties between Rhodes's agents and African chiefs, along with agreements between Britain, Germany, Portugal, and Belgium. In 1890 Lewanika, the Lozi ruler, consented to an exclusive mineral concession that the company treated as a basis for its authority. The northern frontier was legally signed in the Anglo-Belgian Treaty of 1894. The eastern boundary followed from the Anglo-German agreement of 1890, which fixed the limits of the two territories between Lake Tanganyika and the Malawi tripoint, and a joint demarcation commission made decisions on the exact alignment in 1898, and an agreement approving its work was signed in 1901. Agreements with Portugal and the Congo Free State in 1891 fixed the western and northwestern limits. The result is the elongated outline that Zambia still has, which resulted from agreements in the 1890s between Britain and Germany, Portugal, and the Belgian king Leopold II. The territory was later known as Northern Rhodesia, after the North-Western and North-Eastern Rhodesia areas merged in 1911, and it became a British protectorate in 1924 before gaining independence in 1964.\n\nModern cartography rests on different foundations. Early maps relied on route surveys, sketches and astronomical fixes made by explorers and missionaries, and the accuracy of many features, such as the height of the falls, was revised repeatedly as instruments improved. Aerial photography and satellite imagery later allowed the country's rivers, wetlands and forest margins to be mapped at much finer detail, and geographic information systems now combine these layers with census, land-use and boundary data. These tools have changed the geographical knowledge of the country, making it possible to track floodplain extent, deforestation and urban growth over time, and to assess how precisely the colonial-era boundaries correspond to the ground. Mapping of this kind relies on maps, remote sensing and geographic information systems."
    }
  ],
  "links": [
    "africa",
    "electricity",
    "biodiversity",
    "erosion",
    "floodplain",
    "river",
    "el-nino-southern-oscillation",
    "maize",
    "fertilizer",
    "irrigation",
    "geology",
    "railway",
    "logistics",
    "climate-change",
    "map",
    "remote-sensing",
    "geographic-information-system"
  ],
  "sources": [
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    },
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    },
    {
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    },
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    },
    {
      "title": "Lake Tanganyika - Shadows Of Africa",
      "url": "https://www.shadowsofafrica.com/lake-tanganyika"
    },
    {
      "title": "Lake Kariba Recreational Park",
      "url": "https://www.zimparks.org.zw/lake-kariba-recreational-park/"
    },
    {
      "title": "Climate of Zambia",
      "url": "https://en.wikipedia.org/wiki/Climate_of_Zambia"
    },
    {
      "title": "When Is The Best Time To Visit Zambia: Zambian Climate",
      "url": "https://journeysbydesign.com/destinations/zambia/when-to-go"
    },
    {
      "title": "Understanding the Weather of Zambia: Weather Patterns and Best Travel Times",
      "url": "https://www.explorelusaka.com/post/the-climate-of-zambia"
    },
    {
      "title": "Zambia Climate & Weather - AfricanMecca Safaris",
      "url": "https://www.victoriafalls-zambiatravel-safaris.com/country-info/climate-weather"
    },
    {
      "title": "Zambia Weather & Climate (+ Climate Chart)",
      "url": "https://www.safaribookings.com/zambia/climate"
    },
    {
      "title": "Climate of Zambia",
      "url": "https://www.zambiatourism.com/about-zambia/climate/"
    },
    {
      "title": "Zambia - Tropical, Monsoonal, Humid",
      "url": "https://www.britannica.com/place/Zambia/Climate"
    },
    {
      "title": "Intertropical Convergence Zone (ITCZ): Significance and symbolism",
      "url": "https://www.wisdomlib.org/concept/intertropical-convergence-zone-itcz"
    },
    {
      "title": "Zambia Climate: Weather Zambia & Temperature By Month",
      "url": "https://en.climate-data.org/africa/zambia-192/"
    },
    {
      "title": "Ecoregions of Zambia",
      "url": "https://en.wikipedia.org/wiki/Ecoregions_of_Zambia"
    },
    {
      "title": "Zambia - reNature",
      "url": "https://www.renature.co/countries/zambia/"
    },
    {
      "title": "Blue Green Atlas - The Climate of Zambia",
      "url": "https://bluegreenatlas.com/climate/zambia_climate.html"
    },
    {
      "title": "Choma, Zambia",
      "url": "https://en.wikipedia.org/wiki/Choma,_Zambia"
    },
    {
      "title": "Climate Profiles of Countries in Southern Africa: Zambia",
      "url": "https://www.climatecentre.org/wp-content/uploads/Climate-Profiles-of-Countries-in-Southern-Africa-Zambia.pdf"
    },
    {
      "title": "Zambia climate: temperature, rain, when to go - Climates to Travel",
      "url": "https://www.climatestotravel.com/climate/zambia"
    },
    {
      "title": "displays the average seasonal rainfall over figure, it can be seen that...",
      "url": "https://www.researchgate.net/figure/displays-the-average-seasonal-rainfall-over-figure-it-can-be-seen-that-the-north-and_fig2_277621684"
    },
    {
      "title": "Climate shocks hit hydropower in Southern Africa, reviving interest in coal",
      "url": "https://news.mongabay.com/2026/07/climate-shocks-hit-hydropower-in-southern-africa-reviving-interest-in-coal/"
    },
    {
      "title": "El Niño Droughts Threaten Hydropower; Zimbabwe And Zambia Turn To Solar - The Energy Pioneer",
      "url": "https://theenergypioneer.com/el-nino-droughts-threaten-hydropower-zimbabwe-and-zambia-turn-to-solar/"
    },
    {
      "title": "As drought cripples Kariba Dam water levels, Zambia faces power crisis",
      "url": "https://www.philippinetimes.com/news/274713621/as-drought-cripples-kariba-dam-water-levels-zambia-faces-power-crisis"
    },
    {
      "title": "Zambia faces 21-hour power cuts as Lake Kariba dries up",
      "url": "https://africanarguments.org/2024/09/zambia-faces-21-hour-power-cuts-as-lake-kariba-dries-up/"
    },
    {
      "title": "(PDF) Rainfall Variability over Northern Zambia",
      "url": "https://www.researchgate.net/publication/277621684_Rainfall_Variability_over_Northern_Zambia"
    },
    {
      "title": "The major ecoregions of Zambia.",
      "url": "https://www.researchgate.net/figure/The-major-ecoregions-of-Zambia_fig1_228714681"
    },
    {
      "title": "Central Zambezian miombo woodlands",
      "url": "https://en.wikipedia.org/wiki/Central_Zambezian_Miombo_woodlands"
    },
    {
      "title": "Dry Miombo Woodlands",
      "url": "https://www.oneearth.org/ecoregions/dry-miombo-woodlands/"
    },
    {
      "title": "Central Zambezian Miombo Woodlands",
      "url": "https://zm.chm-cbd.net/ecosystems/central-zambezian-miombo-woodlands"
    },
    {
      "title": "Central Zambezian Wet Miombo Woodlands",
      "url": "https://www.oneearth.org/ecoregions/central-zambezian-wet-miombo-woodlands/"
    },
    {
      "title": "Southern miombo woodlands",
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    },
    {
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    },
    {
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    },
    {
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      "url": "https://conservationzambia.org/programs/mafinga-afromontane/"
    },
    {
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    },
    {
      "title": "Land Use change and its Drivers in the Wetlands of Barotse Floodplain of Zambezi River Sub-Basin, Zambia",
      "url": "https://www.researchsquare.com/article/rs-501786/v1"
    },
    {
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      "url": "https://movingrivers.org/locations/barotse-floodplains-zambia-2/"
    },
    {
      "title": "Zambezian flooded grasslands",
      "url": "https://en.wikipedia.org/wiki/Zambezian_flooded_grasslands"
    },
    {
      "title": "Western Zambezian grasslands",
      "url": "https://en.wikipedia.org/wiki/Western_Zambezian_grasslands"
    },
    {
      "title": "Central Zambezian miombo woodlands",
      "url": "https://en.wikipedia.org/wiki/Central_Zambezian_miombo_woodlands"
    },
    {
      "title": "Kalahari Sands",
      "url": "https://www.zambiatourism.com/about-zambia/vegetation/kalahari-sands/"
    },
    {
      "title": "Zambian Kalahari Sands and Zambezian - Miombo Loamy Sands Respond Differently to Agricultural Expansion",
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    },
    {
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    },
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    {
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    },
    {
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    },
    {
      "title": "(PDF) Commercial dynamics in Zambia’s cassava value chain. Food Security Research Project Working Paper No",
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    },
    {
      "title": "COUNTRY REPORT ON THE STATE OF PLANT GENETIC RESOURCES FOR FOOD AND AGRICULTURE",
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    },
    {
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    },
    {
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    },
    {
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      "url": "https://en.wikipedia.org/wiki/South_Luangwa_National_Park"
    },
    {
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      "url": "https://www.naturalworldsafaris.com/africa/zambia/safaris-and-planning/parks"
    },
    {
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    },
    {
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    },
    {
      "title": "Zambia's National Parks • South Luangwa, Lower Zambezi & Kafue",
      "url": "https://freedomdestinations.co.uk/africa/zambia/national-parks"
    },
    {
      "title": "Zambia National Parks - Gorilla Trekking Uganda",
      "url": "https://www.gorillaugandasafaris.com/zambia/zambia-national-parks/"
    },
    {
      "title": "Bangweulu Wetlands",
      "url": "https://en.wikipedia.org/wiki/Bangweulu_Wetlands"
    },
    {
      "title": "Place - Bangweulu Wetlands",
      "url": "https://ukuri.travel/places/bangweulu-wetlands"
    },
    {
      "title": "Bangweulu Wetlands",
      "url": "https://www.safari-online.com/bangweulu-wetlands/"
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    {
      "title": "Bangweulu Swamps wildlife location in Zambia, Africa",
      "url": "https://www.wildlifeworldwide.com/locations/bangweulu-wetlands"
    },
    {
      "title": "The Bangweulu wetlands in northern Zambia",
      "url": "https://www.earth.com/animals/the-bangweulu-wetlands-in-northern-zambia/"
    },
    {
      "title": "Kavango Zambezi Transfrontier Conservation Area (KAZA)",
      "url": "https://www.worldwildlife.org/places/kavango-zambezi-transfrontier-conservation-area-kaza/"
    },
    {
      "title": "Kavango%E2%80%93Zambezi Transfrontier Conservation Area",
      "url": "https://en.wikipedia.org/wiki/Kavango%E2%80%93Zambezi_Transfrontier_Conservation_Area"
    },
    {
      "title": "Kavango-Zambezi Transfrontier Conservation Area - Whole Earth Education",
      "url": "https://wholeeartheducation.com/kavango-zambezi-transfrontier-conservation-area/"
    },
    {
      "title": "TFCA Network - Kavango-Zambezi Transfrontier Conservation Area",
      "url": "https://tfcaportal.org/tfcas/kavango-zambezi-transfrontier-conservation-area"
    },
    {
      "title": "Kavango–Zambezi Transfrontier Conservation Area - African Travel Book",
      "url": "https://africantravelbook.com/kavango-zambezi-transfrontier-conservation-area/"
    },
    {
      "title": "Bengweulu Wetlands Safaris & Tours",
      "url": "https://absolutezambiasafaris.com/destinations/zambia/bengweulu-wetlands/"
    },
    {
      "title": "Wildlife of Zambia",
      "url": "https://en.wikipedia.org/wiki/Wildlife_of_Zambia"
    },
    {
      "title": "The Kavango-Zambezi Landscape",
      "url": "https://www.iisd.org/capa/kaza"
    },
    {
      "title": "Zambia National Parks and Game Reserves. South Luangwa",
      "url": "https://www.africaguide.com/country/zambia/parks.htm"
    },
    {
      "title": "Bangweulu Wetlands",
      "url": "https://www.discoverzambia.co.zm/bangweulu-wetlands"
    },
    {
      "title": "(PDF) Origin of the copper-cobalt deposits of the Zambian Copperbelt: An epigenetic view from Nchanga",
      "url": "https://www.researchgate.net/publication/29813166_Origin_of_the_copper-cobalt_deposits_of_the_Zambian_Copperbelt_An_epigenetic_view_from_Nchanga"
    },
    {
      "title": "Zambia's Copperbelt Area and Copper Mining: A Review",
      "url": "https://www.scirp.org/pdf/gep_2022031110033039.pdf"
    },
    {
      "title": "Comparative geology and metamorphic evolution of the Luswishi Dome, Copperbelt, Zambia: Implications for exploration targeting",
      "url": "https://www.researchgate.net/publication/353734893_Comparative_geology_and_metamorphic_evolution_of_the_Luswishi_Dome_Copperbelt_Zambia_Implications_for_exploration_targeting"
    },
    {
      "title": "Origin of the Nchanga copper–cobalt deposits of the Zambian Copperbelt",
      "url": "https://link.springer.com/article/10.1007/s00126-005-0032-8"
    },
    {
      "title": "Kagem Mining Limited (Emerald)",
      "url": "https://www.gemfieldsgroup.com/assets/kagem-mining-limited-emerald-mines/"
    },
    {
      "title": "The top 10 mines in Zambia",
      "url": "https://projectsiq.co.za/insights/top-10-mines-in-zambia/"
    },
    {
      "title": "Green light: A look behind the scenes at Zambia's Kagem, the world's largest emerald mine",
      "url": "https://www.thenationalnews.com/lifestyle/luxury/green-light-a-look-behind-the-scenes-at-zambia-s-kagem-the-world-s-largest-emerald-mine-1.968543"
    },
    {
      "title": "THE MINERAL INDUSTRY OF ZAMBIA—2001 30.1 THE MINERAL INDUSTRY OF ZAMBIA",
      "url": "https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/mineral-pubs/country/2001/zamyb01.pdf"
    },
    {
      "title": "The Environmental Toll of Mining on Zambia’s Copperbelt",
      "url": "https://diggers.news/guest-diggers/2025/03/10/the-environmental-toll-of-mining-on-zambias-copperbelt-part-i/"
    },
    {
      "title": "Impact of Mining and Ore Processing on Soil, Drainage and Vegetation in the Zambian Copperbelt Mining Districts: A Review",
      "url": "https://www.mdpi.com/2075-163X/13/3/384"
    },
    {
      "title": "Mining-related contamination of surface water and sediments of the Kafue River drainage system in the Copperbelt district, Zambia: An example of a high neutralization capacity system",
      "url": "https://www.researchgate.net/publication/251582430_Mining-related_contamination_of_surface_water_and_sediments_of_the_Kafue_River_drainage_system_in_the_Copperbelt_district_Zambia_An_example_of_a_high_neutralization_capacity_system"
    },
    {
      "title": "Evaluation of heavy metal contamination in copper mine tailing soils of Kitwe and Mufulira, Zambia, for reclamation prospects",
      "url": "https://www.nature.com/articles/s41598-022-15458-2"
    },
    {
      "title": "Environmental disaster unfolds in Zambia - BirdLife International",
      "url": "https://www.birdlife.org/news/2025/03/07/environmental-disaster-unfolds-in-zambia/"
    },
    {
      "title": "An acid spill in Zambia tests the country's plans to boost production",
      "url": "https://www.climatechangenews.com/2025/03/28/catastrophic-acid-spills-at-copper-mines-test-zambia-plans-to-boost-production/"
    },
    {
      "title": "Zambia Electricity Shortage Highlights Africa's Hydropower Shortfalls - Circle of Blue",
      "url": "https://www.circleofblue.org/2015/water-energy/zambia-electricity-shortage-highlights-africas-hydropower-shortfalls/"
    },
    {
      "title": "Copyright ©Afrobarometer 2026 1 Dispatch No. 1178",
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    },
    {
      "title": "Zambia’s Power Shortages Worsen As Drought Deepens",
      "url": "https://pulitzercenter.org/stories/zambias-power-shortages-worsen-drought-deepens"
    },
    {
      "title": "Zambia Energy Sector 2026",
      "url": "https://www.zambiainvest.com/energy/page/3/"
    },
    {
      "title": "Kafue Gorge Lower Hydropower Project Lights Up Thousands of Households in Zambia",
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    {
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    {
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      "url": "https://www.pressreader.com/south-africa/the-star-south-africa-early-edition/20151112/281822872687230"
    },
    {
      "title": "Kafue Gorge Lower Power Station",
      "url": "https://en.wikipedia.org/wiki/Kafue_Gorge_Lower_Power_Station"
    },
    {
      "title": "\"Not by chance\": Zambian president attributes improved power supply to sector diversification-Xinhua",
      "url": "https://english.news.cn/africa/20260120/7b683f55c7b2458dbe6f1f007392eda9/c.html"
    },
    {
      "title": "Government Says Load Shedding to Ease in 2026 -",
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    },
    {
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      "url": "https://www.greenbuildingafrica.co.za/zambia-reaches-1000mw-solar-generation-target/"
    },
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      "url": "https://www.industrialinfo.com/news/article/zambias-solar-expansion-builds-resilience-against-hydropower-risk--363223"
    },
    {
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    },
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    },
    {
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      "url": "https://africanminingmarket.com/zambia-electricity-industry-challenges-and-solutions/24808/"
    },
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    },
    {
      "title": "2022 CENSUS NATIONAL ANALYTICAL REPORT",
      "url": "https://www.zamstats.gov.zm/wp-content/uploads/2025/08/2022-Census-National-Analytical-Report.pdf"
    },
    {
      "title": "2022 CENSUS OF POPULATION AND HOUSING PRELIMINARY REPORT O F F I C I A L S T A",
      "url": "http://www.zamstats.gov.zm/wp-content/uploads/2023/12/2022-Census-of-Population-and-Housing-Preliminary.pdf"
    },
    {
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    },
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    },
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    },
    {
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      "url": "https://en.wikipedia.org/wiki/Lusaka_Province"
    },
    {
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    },
    {
      "title": "Demography",
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    },
    {
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    },
    {
      "title": "Drinking Water Quality and Provision in Six Low‐Income, Peri‐Urban Communities of Lusaka, Zambia - PMC",
      "url": "https://pmc.ncbi.nlm.nih.gov/articles/PMC7770328/"
    },
    {
      "title": "PROJECT: LUSAKA SANITATION PROGRAM",
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    },
    {
      "title": "Field Diary: From Sewerage to Sanitation For All in Lusaka",
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    },
    {
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    },
    {
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    },
    {
      "title": "1 Republic of Zambia ZAMBIA’S NATIONAL EXPERIENCE ON TRANSPORT CORRIDORS BY",
      "url": "https://www.un.org/ohrlls/sites/www.un.org.ohrlls/files/session-3-experience-on-national-corridors-zambia-tembo.pdf"
    },
    {
      "title": "From Lobito to Lagos: 10 Infrastructure Projects to Watch Across Africa From Lobito to Lagos: 10 Infrastructure Projects to Watch Across Africa",
      "url": "https://highways.today/2026/10/05/10-projects-across-africa/"
    },
    {
      "title": "TAZARA modernisation boosts Southern Africa trade - Railway Supply",
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    },
    {
      "title": "Lobito Corridor",
      "url": "https://en.wikipedia.org/wiki/Lobito_Corridor"
    },
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    },
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    {
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    {
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    {
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      "title": "David Livingstone",
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    {
      "title": "Central Africa 1914 CE",
      "url": "https://timemaps.com/history/central-africa-1914ad/"
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  ],
  "license": "https://creativecommons.org/licenses/by/4.0/"
}