Malawi

Malawi is a landlocked republic in southeastern Africa, bordered by Zambia, Tanzania and Mozambique. Its landscape is shaped by the Great Rift Valley, a tectonic trough that runs the length of the country and holds Lake Malawi, one of the largest and deepest freshwater lakes in Africa. The physical setting, the climate and the country's water resources together define where and how its population of roughly 21 million lives and earns a living.

Malawi matters for several reasons that connect geography to wider scientific and economic questions. Lake Malawi is home to an exceptionally diverse assemblage of cichlid fishes, a classic case of speciation and endemism in a freshwater setting, and it supplies protein to many communities. The country's altitude-driven climate, with hot lowlands and cooler highlands, produces a sharp contrast between wet and dry seasons. Because the economy depends heavily on rain-fed farming, the country is highly exposed to drought and to the effects of El Niño events, while pressure on forests and soils compounds these vulnerabilities.

This entry covers the country's location and geological setting, its relief, lake, rivers and climate, the climate hazards it faces, its ecosystems, biodiversity and protected areas, and the human geography of settlement, agriculture, fisheries and urbanization. It then turns to the economy, society, the historical geography from prehistory through colonial rule and independence, and the political and administrative structure.

Location, size and borders

Malawi occupies a part of southeastern Africa and has no coastline of its own. It is a landlocked country located in southern central Africa along the western part of the Great Rift Valley of Africa. Overseas trade therefore has to pass through a neighbouring state, and the principal routes run through Mozambique, with Tanzania as a secondary option. The nearest sea access lies beyond the national border, which shapes transport costs and import prices, a theme the trade and infrastructure sections take up in more detail.

The national territory is elongated rather than compact. Its north–south extent approaches 900 km, while its east–west width ranges only from about 90 to 161 km. Covering a total area of 118,484 km², the country is comparable in size to a mid-sized European state, and its narrow profile means that most places lie within a short distance of a border. The Malawian portion of the East African Rift, which runs through the country from north to south, is discussed in the geology section.

Malawi's frontiers are unevenly distributed around its perimeter. Zambia forms the western edge, and Zambian official statistics record Malawi 837 km as the length of the shared land boundary. Tanzania occupies the north and northeast, while Mozambique encloses the eastern, southern and southwestern limits of the country. This arrangement gives Mozambique the greatest share of Malawi's land frontier and makes it the country's principal gateway to the Indian Ocean.

Lake Malawi, known as Lake Nyasa in Tanzania and Mozambique, is the defining feature of the eastern and northeastern boundary. It comprises about 25% of Malawi's area, and it is between 560 kilometres and 580 kilometres long, and about 75 kilometres wide at its widest point. Because the lake is shared, the frontier runs through water rather than over land. Its exact line between Malawi and Tanzania remains a matter of considerable contention that has boiled over into frequent diplomatic disputes. The three riparian states also each claim some shoreline rights and occasionally engage in disputes over fishing rights in different areas of the lake. The lake's water resources are treated in the rivers and biodiversity sections.

Malawi lies within the southern tropics, a latitudinal position that determines its warm temperatures and the seasonal rainfall pattern described in the climate section. Its position also governs the way water leaves the country. The Shire River flows from the south end of the lake and joins the Zambezi River 400 km (250 mi) south in Mozambique. This outflow links the national watershed to a major regional river system, which is why the lake's southern exit has long mattered for riverine transport and cross-border exchange.

Geological setting and the Great Rift Valley

Rift formation

Malawi occupies the southern end of the East African Rift System, and its section belongs to the western branch of that system. The Lake Malawi Rift, in the Western Branch of the East African Rift, is an archetype of a juvenile rift, which makes it a common reference point for studying young rifts. Extension is slow: when the Earth's crust pulls apart, the lithosphere extends, and in the case of Lake Malawi this amounts to less than an inch per year. Reconstructions of the faulted layers imply only about 7 km of total extension, and the southern basins are younger than the northern ones. Structural restorations indicate a weakly extended rift system (∼7 km), with diminishing values of extension and thinner rift fill from north to south, suggesting a progressively younger rift to the south.

Faults and basin structure

The trough is built from half-graben basins, each tilted away from a steep fault on one side. The lake basin is bounded on one side by steeply dipping normal faults (normal faults). Interpretations differ on how many units make up the rift. Seismic profiling resolves the Malawi Rift is composed of seven linked half-graben units, whereas another analysis treats the lake basin as a complex of intrabasins and intrabasin highs formed by three major fault segments, each about 100 km in length. Boundary faults are large: the border faults related to the current rift regime are up to120 km long and have throws of at least7-8 km. The polarity of each basin alternates along the axis. Half-graben alternate directions of asymmetry at intervals of 60 to 100 km along the axis of the rift, and the zones where the polarity changes, called accommodation zones, are typically basement highs between the sub-basins they divide.

Subsidence has deepened the trough for millions of years. The basin has been actively subsiding since the late Miocene, and has a maximum depth of about 3 km. Sediment fill varies sharply along the axis. Sediment sequences observed in the hanging walls of these border faults decrease in thickness from >5 km in the north of the lake to~1 km in the south, while south of Lake Malawi, shallow boreholes, electrical resistivity tomography, and depth-to-magnetic basement show rift sediment thickness of not more than 600 m. Because the lake water itself can reach about 700 m, subsidence has outpaced deposition; one study notes that present-day sediment totals will underestimate displacement by as much as 700 m. Thick fill in the north may also reflect loading. The volcanic load of the Rungwe magmatic system north of the lake and related subsidence may explain the presence of anomalously thick synrift fill in the northernmost part of the lake.

Rocks and minerals

Most of the bedrock is old. The oldest rocks in Malawi are crystalline metamorphic basement rocks in the south that formed nearly two billion years ago. These rocks were later reworked by successive mountain-building episodes, including the Ubendian, Irumide and Mozambican cycles. These rocks have been disturbed or reworked by orogenic episodes comprising Ubendian, Irumide and Mozambican cycles. Younger sedimentary cover includes rocks of the Karoo system, which in the north contain coal. Near Chilumba, outcropping Karoo rocks contain abundant coal beds, and beneath the lake the sediments are thought to be thicker still, since estimates from the western shore range from 1 km on the western shore in Malawi to ~3 km in the Ruhuhu Basin. Igneous intrusions are also significant: intrusive rocks of late Jurassic and early Cretaceous age occur within the catchment of the Lake Malawi Rift, and in southern Malawi include carbonatites and feldspathoid syenites of the Chilwa Alkaline Province.

Many economic minerals are tied to these rock groups. Genetic modelling has shown that Malawi's minerals are associated with either the basement complex or the intrusive carbonatites and syenites of the Chilwa Alkaline Province. Pegmatites are a notable source of gemstones, and the most important pegmatite belts containing gemstones are found in Chitipa, Mzimba, along with the Zomba–Malosa and Mulanje massifs. The country's broader resource base includes coal, vermiculite, rare earth elements and bauxite, many of which remain poorly understood or not exploited. Only a few have been mined so far: only phosphate, coal, limestone, and uranium have been exploited.

Long-term landscape change

The lake and its catchment have changed considerably over geological time. Since the late Pleistocene, the lake level has fallen by roughly 40 m, because tectonic lowering of the overflow sill, through subsidence of the rift floor, combined with erosional incision have lowered the water level by 40m since the late Pleistocene. Climate has also reorganized drainage. Model results indicate that the onset of arid climate conditions (140–95 kyr BP) causes extreme drainage adjustments downstream and the formation of mega‐catchments that flow axially into a shallow restricted paleo‐lake. Fault activity is similarly dynamic: "We now have conclusive evidence of fault migration away from the border fault of the half-graben," McCartney adds.

Relief, landforms and elevation zones

Malawi's surface is a mix of extensive plateaus, steep massifs and low-lying trough floors. One reference work states that about 75% of the land surface is plateau between 750 m and 1,350 m (2,460 and 4,430 ft) above sea level. Another source gives a narrower band for the plateaus west of the Rift, which rise generally 910 to 1,220 m (3,000 to 4,000 ft) above sea level. The two figures use different boundaries, so the typical plateau range should be read as approximate.

The southern plateaus are the most varied part of this surface. The Shire Highlands, a plateau in southern Malawi, located east of the Shire River, are reported at 600 to 1100 meters, with various hills and mountains rising higher. Other sources put the upper limit at 1,600 m. The highlands are bounded on the west and south by the valley of the Shire River, an extension of the African Rift Valley, and their highest point is Zomba Mountain at 2087 meters. In the north, the Nyika Plateau has a different profile. Most of it lies at elevations of between 2,100 and 2,200 m (6,900 and 7,200 ft), the highest point being 2,605 m (8,547 ft) at Nganda Peak. Its escarpments are steep: the south-east side rises about 1,000 m (3,300 ft) above the South Rukuru River valley.

The highest massif is Mount Mulanje. Sapitwa Peak, the highest point on the massif at 3,002 m, is the highest point in Malawi. The massif consists of rolling grassland at elevations of 1,800–2,200 m, intersected by deep forested ravines. Its form results from differential erosion: the surrounding rock eroded away over time, leaving behind the erosion-resistant igneous rock of the Mulanje Massif. The mountain rises steeply and suddenly from the undulating plain to the highlands, and the plains around it have an average altitude of just 650m, a contrast that gives the massif its local name of "island in the sky".

These massifs function as water sources for the surrounding lowlands. The Mulanje forests are vital for watershed protection and are the catchment of headwaters for nine strong rivers in the two districts. Its upper slopes also feed nine perennial rivers. The Kirk Range, on the south-western side of the Shire valley, plays a similar role. It forms the Malawi-Mozambique border, and the divide between the watersheds of Mozambique's Revúboé River to the west and Malawi's Shire River to the east. Streams in the Shire Highlands likewise drain west, south, and southeast towards the Shire River, or northeast into the closed basin of Lake Chilwa.

The lowest ground lies along the Shire River and at the lake margins. Malawi's lowest point sits at the junction of the Shire River and the border of Mozambique at 37 m. Within the valley, the river changes character. Between Matope and Chikwawa, the middle river drops approximately 400 m (1,300 ft) through a series of falls and gorges, including Kapachira Falls. Beyond Chikwawa, the lower river turns southeast and enters the low-lying Mozambique plain. The lake itself is a low-lying trough feature. Its surface is located at 460 m (1,500 ft) above sea level, with a maximum depth of 700 m (2,300 ft), which means the lake bottom is over 210 m (700 ft) below sea level at some points.

Altitude is the main control on temperature and rainfall over short distances. Temperatures are greatly influenced by the topography and decrease with increasing altitude. The lakeshore illustrates the lowland end of this gradient. Although the water body has a cooling effect, because of the low elevation, the margins of the lake have long hot seasons and high humidity. The highlands are different. The highlands have a cooler climate and more rainfall than the surrounding lowlands, and the highest rainfall is experienced in the high altitude and mountainous areas of Mulanje, Zomba, Dedza and the plateaus. Lilongwe, on the central plateau at an elevation of 1,041 m (3,415 ft), has a moderately warm climate with adequate rainfall. Because the relief rises so sharply, a traveller can pass from hot, humid lowland to cool, wet upland within a short distance, which is why the same country contains both extremes.

Lake Malawi: physical characteristics

Lake Malawi extends roughly 560 to 580 kilometres from north to south, and its broadest point measures about 75 kilometres across. Because the lake narrows toward its ends, its mean width is considerably smaller, at about 40 kilometres. Its surface sits at about 468 metres above sea level, although a hydrological study gives 474 metres, so the exact figure depends on the source and the measurement date. The lake covers about 29,600 square kilometres, which makes it Africa's third-largest lake by surface area and the ninth-largest in the world. Its total area is comparable to roughly a quarter of Malawi's entire land and water territory, although the lake is shared with two other states.

Estimates of volume range from about 8,400 to 8,640 cubic kilometres. Rankings by volume also vary: one NASA summary places the lake fourth among the world's freshwater lakes by volume, while a geochemical study ranks it fifth in the world by volume and second-deepest in Africa. The lake's depth is its most distinctive feature. The average depth is about 292 metres, and the deepest point, 706 metres, lies in a major depression in the north-central part of the lake. A smaller depression in the far north reaches 528 metres, while the southern half is much shallower, with depths under 400 metres in the south-central area and under 200 metres at the far southern end. The steep, asymmetric northern and central basins are bordered by faults, whereas the south is a broad, gently sloping shelf.

The lake's water is alkaline and relatively hard. Its pH ranges from 7.8 to 8.5, and carbonate hardness exceeds general hardness. Surface temperatures generally fall between 24 and 29 °C, while deeper water averages about 22 °C throughout the year. The water column is permanently stratified, which makes Lake Malawi a meromictic lake: a clear chemocline at roughly 200 metres separates the oxygenated upper layer from the anoxic deep water. The upper boundary of the stratified zone, the thermocline, lies between about 40 and 100 metres, and oxygen is limited to depths of about 250 metres. In tropical lakes like this one, the stability comes mainly from temperature: small temperature differences between top and bottom produce strong density contrasts at high water temperatures. Although the surface layer is well mixed, the deeper water is isolated, and the seasonal mixing that does occur is largely confined to the shallow southern end during the dry season.

These mixing processes strongly influence the lake's biological productivity. Lake Malawi is oligotrophic, and phytoplankton, the base of the food web, is limited because nutrients are sequestered in the stratified layer below about 250 metres. Biogenic material from surface production sinks and accumulates in the anoxic deep water. The main exception is the southeastern arm, where strong southerly winds drive upwelling of nutrient-rich water and support a much richer fishery. Productivity is controlled by the strength of stratification, the rate of mixing, and climatic variability. Sediment records indicate that stratification has intensified since the end of the Little Ice Age, with primary productivity declining after about 1950 as thermal stratification strengthened. Monitoring of surface waters also points to a summer warming trend of roughly 0.25 °C per decade, a change with possible consequences for the lake's productivity.

Lake Malawi lies within the territory of three states. The basin is shared by Malawi, Mozambique and Tanzania, and the lake is known as Nyasa in Tanzania and as Lago Niassa in Mozambique. The shoreline is approximately 1,600 kilometres long, and Malawi occupies the western shore, with the lake forming the eastern part of its frontier. The lake's Mozambican and Tanzanian shores lie across the water from Malawi, so its waters and boundaries are a matter of joint management. The southern lake and its coastal zone were designated a Ramsar wetland in 2011 under the name "Lake Niassa and its Coastal Zone".

Rivers, drainage and freshwater resources

Malawi's surface drainage is organised around Lake Malawi, and the lake's water balance is unusual. The largest inflow is the river Ruhuhu, which rises in the Kapengere Range in Tanzania's Ruvuma Region and flows for about 160 km before draining into eastern Lake Malawi. Rainfall on the lake surface adds roughly 1.3 m of water a year, and inflows add about 0.9 m, but evaporation removes about 1.8 m and outflow about 0.4 m. Evaporation accounts for more than 80% of the water loss from the lake, considerably more than the outflowing Shire River. Because of this, the lake's level is highly sensitive to the drainage basin inputs and to climate. The Ruhuhu's variable flow alone can produce level changes of up to 7 m.

The Shire is the lake's sole outlet. It flows into the Zambezi River in Mozambique and runs for about 402 km. The upper Shire leaves the lake and runs approximately 19 km (12 mi) before entering the shallow Lake Malombe. Lake Malombe is itself a shallow impoundment, with an average depth of about 2 m, and the river leaves it to flow south through Liwonde National Park. Further downstream, the river enters the Ruo, whose inflow joins below the upper valley, before the Shire turns southeast and enters the low-lying Mozambique plain.

Discharge from the lake is not constant. Outflow measured at Mangochi varies from 50 m3/s to 1000 m3/s, averaging 480 m3/s in the upper valley. The outflow depends primarily on lake levels, and secondarily on basin inflow and evaporation. Discharge therefore tends to follow the wet-season rise in lake level, which is one reason the Shire's flow can swing sharply from year to year. The Shire's average flow, given as about 486 m³/s, makes it the largest river in Malawi.

Groundwater is the main source of drinking water for most Malawians, even though the country has abundant surface water. Most rural Malawians rely on groundwater for their domestic supply, and groundwater is increasingly used for irrigation by smallholder farmers. In rural areas, most supply comes from hand-dug wells, springs and hand-pumped boreholes, while in the urban areas, most public supply is derived from surface-water sources. An estimate cited by the British Geological Survey puts dependence on groundwater for domestic supply at 65% of the population, rising to 82% in rural areas, while in urban areas it is closer to 20%. The most widely used aquifers are the weathered crystalline basement rocks, which cover most of the country, and the alluvial deposits of the river valleys. In the alluvial aquifers, the average borehole yields about 15 litres per second and is around 60 m deep. Groundwater quality is uneven: fluoride concentrations of more than 1.5 mg/l are common in groundwater in alluvial aquifers in the Salima/Nkhotakota and Karonga lakeshore areas. Borehole water is generally microbiologically safer than water from open dug wells, which are more vulnerable to contamination.

The Shire's gradient gives the river its hydroelectric value. Between Matope and Chikwawa, the middle river drops approximately 400 m (1,300 ft) through a series of falls and gorges, including Kapachira Falls. The first development on the river was the Nkula Falls scheme, with 3x8MW units which came into operation in 1966. The Tedzani plants followed from 1973 onward, and the Kapichira station at the falls opened in 2000. Its second phase, switched on in January 2014, doubled the previous 64 megawatts to the maximum capacity of 128 megawatts. The three Shire plants together have a combined capacity of 346 MW, together accounting for 88 percent of Malawi's energy production. Other assessments give a higher hydropower share, reporting that 95% of electricity generation comes from hydropower.

The dams have a practical problem: they fill with sediment. Because of heavy sediment inflow from the tributaries feeding into the Shire River, the reservoirs of all three Shire plants have lost much of their usable storage. A 2013 survey found that the Kapichira reservoir had lost over 40 percent of its initial live storage after 13 years in operation. The loss of active storage shortens the period when the station can generate at peak demand, and sediment at the upstream Nkula dam has been linked to a 10-12 percent reduction in power generation. The plants feed the national grid, which supplies households, agriculture, businesses, manufacturing and mining. Hydropower is therefore central to national electricity supply, although actual energy production from the hydropower plants has been well below installed capacity because of frequent equipment failures.

Climate regimes

Seasonal cycle

Malawi has a subtropical or tropical climate, depending on altitude. The year divides into a rainy season and a dry season. About 95% of precipitation falls during the summer rainy season, which runs from November to April. The dry season that follows is generally dry, with occasional rains, particularly in high-lying areas. Within the dry season, June and July are the coolest months. Daytime temperatures in those months hover around 21°C, and nights can be very cold. The hottest part of the year comes before the rains, when temperatures climb to the year's highest levels from September to November.

Rainfall in the core months is intense and concentrated in short episodes. Equatorial cloudbursts and violent thunderstorms are typical during the rainy season, peaking in March and easing in April. In the dry season, damp mists form in the highlands from May to September and drift down onto the plateaus.

Temperature by zone

Altitude controls temperature more than latitude does. The large water surface of Lake Malawi has a cooling effect, but because of the low elevation the lands around the lake remain tropical. Along the lake and in the lower Shire Valley, it is hot and humid from September to April, with average daytime maxima around 27 to 29 °C. The southern end of the Shire Valley is the hottest part of the country. Near the river's mouth, the altitude falls to sea level, and daytime temperatures regularly exceed 32 to 33 °C for many months, sometimes passing 40 °C.

The central plateau is milder. Lilongwe, at about 1,041 m, has a mean daily maximum of roughly 25 °C in most months, dropping to about 21 °C in July. In June through August, the lake areas and the south stay comfortably warm, while the rest of the country can be chilly at night. High-altitude areas such as Mulanje and Nyika often fall to 6–8 °C at night in June and July. Mean annual temperature on the highland plateaus is about 20 °C, compared with about 24 °C in the lowlands. Frosts are recorded on the highest northern mountains.

Karonga, on the northern lakeshore, is an exception. Its daytime maxima stay near 25 to 26 °C all year, and April and May are its wettest months because of strengthening southerly winds along the lake.

Rainfall gradient

Annual totals vary strongly with elevation and exposure. Sources differ on the exact range. One national-level summary gives annual precipitation between 700 and 2,500 mm, while another puts the low end of the range at approximately 600 mm on rift valley floors and around 1,600 mm in mountainous regions. The driest zones are the Shire Valley and the lakeshore plain, which are semi-arid. Totals on the high ground are much greater. The southern slopes of Mount Mulanje exceed 2,000 mm a year, and rainfall is heaviest along the northern coast of Lake Malawi, where the yearly average is more than 1,600 millimeters.

Most of the country lies in the middle of this range. About 70 percent of the country averages roughly 750 to 1,000 millimeters a year. The gradient also runs from south to north. Patches in rain-shadow zones receive 600 to 750 mm, while much of the coastal lake plains, the north and the highlands get between 1,000 and 2,500 mm. Rainfall variability within the wet season is also high, and there is a high degree of inter- and intra-seasonal variability in precipitation amounts and patterns.

Winds and moisture sources

The rainy season is controlled mainly by the migration of the Intertropical Convergence Zone, whose oscillations interact with the zonal Congo air mass, the meridional south-eastern trade winds, and monsoonal north-eastern winds. The national summary notes that rainfall is largely influenced by the Intertropical Convergence Zone, the Congo Air Mass, tropical cyclones, and easterly waves. The convergence zone reaches the country in late October and then moves south through November. In the dry season, the winds blow from the south-east and are strongest in August. Tropical cyclones form in the Mozambique Channel and occasionally cross the southern lowlands; in March 2023, Tropical Cyclone Freddy struck Malawi.

Because the country lies between two different climatic response regions, prediction is difficult. Its position between eastern equatorial Africa and southern Africa produces apparent climate anomalies that make predicting weather and future rainfall challenging.

Climate variability and climate hazards

Drought has the largest effect on national output, because farming is almost entirely rain-fed. Maize, which supplies around two-thirds of the country's calorie intake, is the crop most exposed. The 2023/24 season was the clearest recent case. National maize output fell by about 23%, from 3.5 million to 2.7 million metric tons, leaving production below the country's annual needs. Reported declines differ by season and by source. A UN flash appeal for 2024 gives a 17 per cent decrease in maize production compared to last year. The human cost was large. Roughly 4.4 million people, more than one in five residents, were in crisis-level food insecurity between June 2023 and March 2024. Malawi and Zambia declared a state of national disaster because of the drought.

The main driver of these shocks is the El Niño–Southern Oscillation. In El Niño years, the probability of drought rises markedly in southern Malawi, along with parts of Zimbabwe, Zambia, Mozambique and South Africa. Because Malawi lies at the northern fringe of the regional maize belt, the degree to which it is affected by drought during strong El Niño years has varied widely. Meteorologists describe the country as sitting between two signals: El Niño usually brings below-normal rain to South Africa and above-normal rain to eastern Africa, so Malawi's outcome changes from season to season. The strong events in the record are 1982/83, 1997/98, 2015/16 and 2023/24. Their typical effects include late or erratic onset of the rains, false starts, and longer runs of dry days. El Niño conditions are also frequently linked to warmer than usual temperatures, which worsen the impact of dry spells. Since the 1980s, two out of three El Niño events have negatively affected food production, reducing maize harvests by an average of 22.5% in the affected years. The threat is current. A strong El Niño has developed in the Pacific Ocean, raising the risk of below-normal rainfall and prolonged dry spells during the November 2026 to March 2027 season, especially in the south.

The opposite phase brings different hazards. Forecasts for the 2024/25 season projected above-average rainfall, with floods predicted in many of the drought-affected districts. Rapid swings from drought to flood therefore strain the same communities, and the tropical cyclone season adds a further source of extreme rain.

Flooding is most concentrated in the low-lying Shire Valley. The area is frequently hit by floods during the rainy season because of its low-lying terrain along the Shire River. Floods along the Shire and Ruo rivers in Nsanje District have occurred about once every two years, and the 1989 event was the worst on record. Earlier floods in the Lower Shire came in January 2015 and March 2019, and more recently with Cyclone Freddy in 2023. Mud flooding after prolonged heavy rain killed more than 1,000 people in 1991. Infrastructure is also exposed: floods have left the Mankhanga–Bangula road and rail link unserviceable since 1989 because of damage.

Lake levels create a second flood pathway. When Lake Malawi reached about 495 metres above sea level, the highest level in twelve years, the law's 477-metre contour, below which activity is prohibited, was breached and buildings and crop fields below it were affected. High water levels linked to the lake flooded farmland along the Shire River, the lake's sole outlet, particularly on the East Bank. Managing the outflow is difficult. Releases through the Kamuzu Barrage at Liwonde cannot rise indefinitely, because larger releases would significantly increase flood risk in the Lower Shire. Between February and April 2026, heavy rain left around 10,000 people homeless, mainly along the East Bank, and floodwaters destroyed homes and swept away crops ready for harvest.

Long-term change is harder to separate from natural variability. A study of the Shire basin in Chikwawa District covering 1980 to 2019 found that mean temperature, average rainfall and baseflow index all increased, which suggests that flood intensity and frequency were also rising. Projections of how these trends will evolve are most developed for near-term seasonal forecasts. An IFPRI economic model of a strong El Niño that significantly cut crop production found that GDP would fall, domestic food prices would rise, and hundreds of thousands would be pushed into poverty, with millions more undernourished. The modelled average scenario puts nearly 500,000 more people into poverty and about 4.6 million more undernourished, and these estimates also include fuel and fertilizer price shocks. Because rainfed maize is the country's dominant staple crop, each shift in rainfall or temperature passes directly to productivity, food security and household incomes.

Vegetation and land cover

Miombo woodland

Most of Malawi's drier land is covered by miombo woodland, a formation that extends across southern Africa and is stretching over seven countries, Malawi among them. Its dominant trees belong to the legume family, mainly the genera Brachystegia, Julbernardia and Isoberlinia. One land-cover study describes Malawi as predominantly covered by Miombo woodland (94%), a figure that other assessments do not directly match. The woodland is comparatively open. Its trees grow to 10-20 meters in height and lose their leaves in the long dry season, sprouting new growth with the rains, so the canopy is usually semi-deciduous rather than dense and evergreen. Fire is a fundamental part of the ecosystem, and it keeps a balance between trees, shrubs and grassy patches. Miombo in Malawi falls between a drier type and a moister type, with mean annual rainfall ranging from about 650 mm for dry miombo to 1400 mm for moist miombo. Grassy, seasonally wet hollows called dambos are interspersed through the woodland, and they may constitute up to thirty percent of the region in the wider Zambezian miombo belt. Along watercourses, narrower riparian belts with acacia species occur, differing in composition from the surrounding miombo.

Highland grasslands and evergreen forests

Above roughly 1,800 m, the woodland gives way to a different vegetation mix. On the Nyika Plateau, the 1800m contour usually marks the transition zone from woodland to montane grassland and forest. Most of it lies at elevations of between 2,100 and 2,200 m, and the highest point, Nganda Peak, reaches 2,605 m. The plateau is dominated by undulating montane grasslands with perennial streams in the hollow. Evergreen forest occurs as patches of tropical montane evergreen forest in sheltered hollows, while on the wetter eastern escarpment are large areas of sub-montane evergreen forest. Juniper stands survive in only a few places, including a few remaining Juniper forest patches on the south eastern escarpment of the park at 2130m - 2220m. In the south, the highlands around Mount Mulanje form a separate mosaic: the ecoregion covers a region of highlands and plateaus that includes Mount Mulanje (3,002 m) in the southeast, and its forest patches include the Mulanje cypress, Widdringtonia whytei. The ecoregion is listed with a conservation status: critical/endangered.

Forest cover and its loss

Estimates of how much of Malawi is forested vary with the definition and the data source. One study reports that forest cover of the country reduced from 47% in 1975 to 36% in 2005. World Bank data compiled from FAO sources put the share at about 37% of the country's land area in 1990 to roughly 22% in 2023. Global Forest Watch satellite data record a more modest decline in tree cover, with the country losing almost quarter of a million hectares of its 1.5 million hectares of tree cover between 2001 and 2023. The pace is uneven: in 2023 alone, the data show, the country had nearly 23,000 hectares cleared of tree cover, the highest forest loss in a single year since 2001. Official estimates are in a similar range, with the Ministry of Forestry and Natural Resources estimating yearly loss at around 30,000 hectares. Losses are concentrated in some areas. In a protected-area study, grassland, shrubland and woodland were the major LULC types throughout 1975-2015, and woodland cover fell from 20.9% to 8.9% of the area over that period. The causes identified there include increasing human population size, agriculture, settlements and policy changes fires and elephant browsing. Nationally, the main drivers are agriculture expansion and excessive use of biomass, such as wood, charcoal, and agricultural residues mostly used for cooking. The loss of forest cover is therefore closely tied to the deforestation pressures discussed in the land use section.

Biodiversity, endemism and conservation

The cichlid radiation

The lake's biodiversity is dominated by cichlid fishes that have diversified into a very large number of species. Published estimates differ: one genomic study describes over 500 species in the radiation, while a later review states that more than 800 cichlid species have originated within the last 800 thousand years from a common ancestral population. The difference largely reflects how species are counted and which groups are included.

The radiation is a central case study in adaptive radiation and speciation. Genomic work suggests that the founding population was itself a mixture of two lineages that had separated 3–4 Ma, and that hybrid-derived genetic variants later sorted into different ecological groups. Sediment cores from the lake extend the record: the lake is described as an iconic "laboratory" for testing questions about rates, modes, and drivers of evolution, and its long, undisturbed sediments allow changes in lake conditions to be compared with episodes of species formation. The lake's age and stratification are central to this role. The lake is deep (706 m), old (>5 My), and permanently stratified, which has helped preserve a long sedimentary record.

Endemism

Endemism is the defining feature of the lake's fauna. Estimates vary somewhat: one source puts it at more than 98% of cichlid fish known only from Lake Malawi, while a World Heritage assessment gives a figure of 99% endemism. The rock-dwelling mbuna group illustrates the pattern. Of more than 350 mbuna species, nearly all are found only in Lake Malawi, and all but five of over 350 species of mbuna are endemic to Lake Malawi and represented in the park. Some species are confined to a single island or rocky promontory, which makes their populations especially vulnerable to local disturbance.

Threats to these fish come mainly from the surrounding catchment and the lakeshore. Rapid population growth has driven deforestation and soil erosion in the lake's catchment areas, and ever-more intensive exploitation of fisheries. Sedimentation from eroded soils reduces water clarity, and the sources list additional pressures such as proposed oil exploration and the introduction of non-native species.

Lake Malawi National Park and World Heritage status

Lake Malawi National Park occupies the southern end of the lake. It was designated as a World Heritage site in 1984 for its natural beauty, its value as an example of biological evolution, and the diversity of its freshwater fishes. It is the country's only natural World Heritage property. The park is small: it covers 94km2, of which only 7 km2 covers aquatic habitats, which is a very small fraction of the lake's surface. Because of this limited coverage, a 2017 UNESCO assessment called for boundaries to be extended to include other high-biodiversity areas around the lake. The same assessment concluded that the values that resulted in the establishment of Lake Malawi National Park as a World Heritage Site are still intact.

Other protected areas protect the land-based fauna. Nyika National Park in the north is described as one of Malawi's jewels and offers unique wildlife viewing on its rolling grassland plateau. Liwonde National Park in the south is the country's longest-established park, and its riverine habitat supports elephants, hippos and buffalo. Majete Wildlife Reserve, in the Lower Shire Valley, covers more than 70,000 hectares. The area was decimated by decades of poaching before a management change in 2003 and large translocations of game restored its populations. Liwonde was also a source: during June–August 2016 and 2017, African Parks relocated approximately 500 elephants from Liwonde and Majete to Nkhotakota Wildlife Reserve.

Community-based conservation and enforcement

Wildlife management is the responsibility of the Malawi Department of National Parks and Wildlife (DNPW), the statutory organisation in charge of national parks, wildlife reserves and sanctuaries as well as wildlife management on communal lands. Public-private partnerships have supplemented this work. At Majete, the restoration programme is linked to local livelihoods: providing hundreds of jobs and supporting thousands of community members with education, health and socio-economic opportunities.

Enforcement remains the main constraint. Poaching is an ongoing threat, as is the grazing of livestock, tree cutting for building poles, timber and firewood, extraction of sand, gravel and rock for building. Settlement inside the park has also grown: the enclave villages supported about 5,400 people in 1977, but have expanded considerably in subsequent years. The UNESCO assessment identified weaknesses in monitoring and enforcement and weak environmental education as problems, while also noting that the difficulties are considerable but not insurmountable.

Fisheries and the lake economy

Lake Malawi is the core of the country's fishery. One recent analysis attributes over 93 % of the 2019 national fish output to the lake, and more than 98.5 % of national production came from small-scale fisheries rather than industrial operators. Fish is a major source of animal protein for households across the country. One widely cited estimate puts the fishery's share of national animal protein consumption at about 40 %. The most prized species is chambo, a group of indigenous tilapiine cichlids (mainly Oreochromis lidole, O. squamipinnis and O. karongae). Chambo was traditionally sold fresh in lakeshore towns, and it has long been regarded as the lake's premium food fish. Its value is matched in nutritional terms by usipa (Engraulicypris sardella), a small pelagic species that is caught in large numbers and dried for storage. Dried usipa and other small fish are transported inland, and they are an important source of protein for rural households far from the shore. Usipa is at its most abundant in the September to November season in districts such as Nkhata Bay.

Fishing supports a large workforce. Estimates of the number of small-scale fishers vary between about 64,000 and 75,000, and the number of people who depend on the sector across the value chain is put at around 2.8 million. Processing, fish trading, net making and boat building provide additional work, and the commercial sector employs crews and creates demand for buyers, processors and firewood sellers. Fishing on the lake is largely a male occupation, while fish trade is an important income source for women and for small-scale traders with limited capital. Many fishers live with their families in fishing camps and make day trips onto the water. Surveys of these camps have found that access to safe water and sanitation is not universal, and that many fishers drink from the lake and use it as a toilet while working.

The chambo fishery collapsed in the 1990s. Estimated chambo landings across the lakes reportedly peaked at about 15,000 tonnes a year in the late 1980s and fell to about 3,000 tonnes by the end of the 1990s. Catches of large species were replaced by smaller ones, a pattern that fisheries scientists describe as fishing down the food web, moving from chambo to utaka and then to usipa. Several factors drove this change. Fishers adopted light-attraction methods, first using Tilley lamps and later brighter LED bulbs, and motorised boats and monofilament nets increased the reach of fishing effort. Fishers also took immature fish and used very fine mesh that catches the smallest individuals, while spawning closures were often ignored. The ornamental fish trade, which collects cichlids from the lake, has added pressure on edible species. Habitat loss, pollution and the dumping of waste into the water have further degraded breeding grounds, a process that is closely tied to the lake's ecosystem and its biodiversity.

Management has moved from top-down control toward shared responsibility, but enforcement has lagged behind. Licensing dates back to the colonial period, and the regulatory framework was centralised for several decades after independence. In the 1990s policy shifted toward participatory management, yet the results have been uneven, partly because the new structures were designed at government level and paid too little attention to customary institutions. The commercial sector is mechanised and mainly uses trawls and ring nets, concentrated in the southern lake. Under current rules, the lake is divided into fishing zones, each allocated a fixed number of licensed units based on stock status, and commercial fishing is barred from areas near the shore. Closed seasons apply to both sectors, and gillnet size limits and rules on beach seines are in place. Fish under 15 centimetres are supposed to be returned to the water. Enforcement remains the central weakness: penalties include fines, refusal of licence renewal and the confiscation of illegal gear, but breeding-season closures are still breached. Scientists have recommended combining input controls on gear with output controls such as individual catch quotas. Malawi's National Plan of Action for small-scale fisheries (2023–2030), prepared with the Food and Agriculture Organization, is the current framework for these reforms. Fisheries management is therefore a central concern of sustainable development policy.

The lakeshore economy links fishing with trade, food supply and tourism. Fish is a major commodity in the markets of towns such as Mangochi and Nkhata Bay, and the lake connects shoreline communities with interior markets. Mangochi district, which includes parts of Lake Malombe and the Shire River, is one of the sector's principal hubs, and more than 40,000 people there depend on fishing. Fish trade also has a broader economic effect: a government-linked study estimated that each unit of value in fish production generates about four units of activity along the chain from production to consumption. Because fishing communities depend on the lake's productivity, declines in catches reduce incomes for fishers and traders, and they affect the poverty and nutrition outcomes of lakeshore households, as well as the appeal of the shoreline for visitors.

Population distribution and settlement

Malawi's population has grown quickly for several decades. Since 2000, Malawi has maintained a high population growth rate, averaging 2.3% per year. The population has significantly increased from 3.6 million people in 1960 to an estimated 21.1 million in 2023. Growth in recent years has come mainly from natural increase rather than migration. In 2025 the natural increase was positive, as the number of births exceeded the number of deaths by 679,560. Due to external migration, the population declined by 8,341. Projections that extend the current trend suggest that Malawi's population will reach 33 million by 2043.

The country remains predominantly rural. Malawi is a predominantly rural country and one of the least urbanised in the world. In 2023, still only 18% of the population resided in urban areas, accounting for 3.8 million people. The urban share has risen only slowly. Around 2008, the urban population growth rate was high at 7 per cent per year, but urban residents still made up only 15.3 percent of the population at that time. Urban growth is expected to accelerate, and urbanization is projected to shift the national balance considerably over the coming decades. The largest towns are the capital, Lilongwe, with a population of 1 115 815, followed by Blantyre with 902,588 and Mzuzu with 249,564 in the same estimates.

Population density has risen sharply because the land area has stayed the same. Malawi's population density continues to grow while the land area remains static. During the 2018 PHC Malawi population density stood at 186 persons per square kilometer up from 138 in the 2008 census. By 2023 the figure had reached 223 persons per square kilometre, and population densities are projected to more than double over the next four decades, reaching 458 persons per square kilometre by 2063.

Population is unevenly spread across the three regions. The southern region has the highest number of people with 7,750,629 or 44 percent. The central region is the second most populous with 7,526,160 people representing 43 percent of the total population while 2,286,960 people (13 percent) live in the northern region, according to the 2018 census. Densities differ even more than totals, because the Southern Region is smaller than the Central Region. Southern 31,780 km2 density 244 per km2 in 2018; Central 211; Northern 84. The concentration in the central and southern regions is also visible in geospatial estimates, which show the north as comparatively sparsely settled. Lakeside and lowland settlement is shaped by terrain and access to water: the FAO country profile states that distribution is mostly influenced by the topography and proximity to Lake Malawi.

Land scarcity shapes settlement and livelihoods. Malawi is a densely populated country with an estimated 15 million people, whereby 85% of the population lives in rural areas and derives its livelihood from agriculture. Because most rural households depend on small plots, rising density places significant pressure on land use planning and resource management. Internal migration intensifies this pressure in some places. In the Southern Region, migration into the region, as well as the region's relatively small cropland are per capita has been linked to a higher poverty rate than in the other two regions, as recorded in 2003.

Urbanization, infrastructure and transport

Major urban centres

Malawi is still a predominantly rural country, but its towns have grown quickly. Lilongwe is the capital and largest city of Malawi, with a population of 989,318 as of the 2018 census, up from 674,448 in 2008. The city's status dates from the decision made in 1965 to move the capital from Zomba to Lilongwe, and it sits at about 1,050 m above sea level. Blantyre is Malawi's centre of finance and commerce, and its second largest city, with a population of 800,264 as of 2018. It is sometimes referred to as the commercial and industrial capital of Malawi as opposed to the political capital, Lilongwe. Mzuzu City is the third largest with 221,272 people, followed by Zomba. These four cities together hold a small share of the national population, so the urban transition is best understood as rapid growth from a low base rather than a majority urban society.

Informal settlements and urban services

Growth in the main cities has tended to outpace the supply of planned housing, serviced plots and municipal infrastructure. Many residents of peri-urban areas live in unplanned or partly planned settlements where piped water, drainage and sanitation are unevenly available. Water shortages, the spread of pit latrines and crowded housing in these areas create public-health risks, which are discussed in the health section. Municipal councils face constraints in land registration, revenue collection and maintenance, which limits their ability to extend services to new neighbourhoods at the pace of settlement growth.

Road network

Roads carry most of the country's passenger and freight traffic. Rural feeder roads are often impassable in the wet season, and non-motorised road users such as pedestrians and cyclists account for a very high share of traffic fatalities, estimated at 70 percent of fatal accidents. Malawi's transport sector depends on regional transport corridors to reach international markets.

Rail links

The rail network is small and fragmented. The railway network in Malawi consists of 933 km of mainline single cape gauge track, part of which is currently non-operational due to flood damage. The historic link to Beira was cut when the link south from Makhanga to Mozambique's Beira corridor has been closed since the Mozambique Civil War. The Nacala line is therefore the principal route: Malawi's second rail link to the Mozambique port of Nacala is its principal route for imports and exports today. Recent investment in infrastructure and rolling stock has raised speeds on the Nacala Corridor from as low as 20 km/h on some sections to 70 km/h. There is no direct link with neighbouring Tanzania because of a break of gauge.

Lake transport

Inland water transport on Lake Malawi extends from the northern to the southern region, passing through the centre. Main ports include Monkey Bay in the south, Chipoka and Nkhota-kota in the central region, and Nkhata Bay and Chilumba in the northern region. The service provides both passenger and freight transport on the lake, including links to Tanzania and Mozambique. Its development is slow due to a lack of adequate funding, and operation relies heavily on private concessions.

Electricity supply

Electricity is generated mainly by hydropower on the Shire River and is distributed by the national utility ESCOM. Demand has outgrown supply for some time. With peak demand of 350 megawatts and growing at about 6 percent annually, the grid has very little flexibility. According to ESCOM, the main challenge has been electricity demand outpacing supply, which has led to frequent power outages across the country. Dependence on a few large hydro units makes the system vulnerable. In May 2026, available generation capacity from the country's major hydropower suppliers fell from 348.15 MW to 306.75 MW after two units tripped, which forced emergency load shedding. In August 2026, solar generation from independent power producers fell to about 10 MW from 111 MW due to weather conditions, and a fault at a hydro unit compounded the shortfall.

Power shortages constrain industry, commerce and public services. ESCOM has urged households and businesses to reduce electricity use during specific evening and early-morning periods to ease the load. Longer-term plans centre on the 358.5 MW Mpatamanga hydroelectric project on the Shire River, with a commissioning date expected in 2032, alongside transmission links to neighbouring countries, including the Malawi-Mozambique Interconnector.

Agriculture and land use

Agriculture underpins Malawi's economy, and it runs on two distinct systems: a large base of smallholder households and a smaller set of commercial estates. The smallholder sub-sector, which is based on customary land tenure and is primarily subsistence, contributes more than 70% to agricultural GDP, with the remaining 30% ascribed to large estates growing tobacco, sugar, tea, coffee and tree-nuts. The weight of the sector in national life is large: farmers account for 80 percent of the total population, among them around 75 percent are small family farms.

Smallholder systems and maize

Maize is the core of smallholder production. Maize is the main staple in Malawi and grown on two-thirds of the country's arable land, largely on smallholdings of 0.5 – 0.8 ha. Other sources put the share higher, at over 75% of the arable land area, and note that maize supplies more than 50% of the caloric intake, so the exact figure depends on how the arable base is defined. Production is almost entirely dependent on the weather. More than 90% of agri-production is rain-fed, and irrigation is marginal: current small-scale irrigation schemes benefit only 3.3% of rural farming households. Women farmers have even less access to irrigation than men.

The same crop is often grown repeatedly on the same plots. In the subsistence system, continuous cultivation of maize on the same land without adding organic or inorganic fertilizers is common, which keeps yields low. Researchers have described a "maize poverty trap", in which farmers keep planting maize even on land that does not suit it, so that in the event of prolonged drought, maize fails thus leaving farmers food insecure.

Export crops and the estate economy

Tobacco is the most important commercial crop and the largest source of foreign exchange. It is "green gold" as it is popularly known in Malawi, is the country's primary export and an important cash crop for both smallholder farmers and large estates. Smallholders dominate its cultivation: almost 20 per cent of the farming households in Malawi grow tobacco, and almost 93 per cent of these grow burley tobacco. Estimates of its weight in exports vary by source and year. One series reports that tobacco accounts for about 60 percent of Malawi's total merchandise export earnings and 13 percent of its GDP, while Reserve Bank data show tobacco proceeds as a share of total exports increased from 49 percent in 2019 to 66 percent in 2023. Sales in the 2025 season were reported at approximately $540 million, up from $394 million the previous year.

Tea and sugar are the other main export estate crops. Tea is grown on large highland estates; Malawi's Thyolo and Mulanje highlands produce world-class tea sold at the Limbe Tea Auction. Tea production is concentrated in estates: one industry account states that over 93% of all Malawian tea is produced by private companies on 44 large estates. Sugar has been less stable, with export revenue dropping from $62.6 million (K109 billion) in 2019 to $51.7 million (about K90 billion) in 2023. The dependence on a few crops creates risk, and the revenue has not always been reinvested productively; one analysis finds that its tobacco export revenues have not been invested in yield-increasing technologies and inputs to improve productivity.

Land pressure, soil degradation and erosion

Land scarcity is a central constraint. Land degradation, characterized by declining soil fertility and erosion, is a major constraint of maize productivity in Malawi, where more than half of the arable land is degraded. Official estimates place the degraded area even higher, at over eight million hectares of land in Malawi. Soil loss is often cited as the main cause. Estimates of erosion rates differ: one study recorded average national soil loss rates in 2014 were 29 ton per hectare per year. Losses are uneven across the country, and erosion is especially severe in the north, where the soil erosion problems in the north of the country arise from the fragile and shallow soil types, lack of good soil management practices, steep slopes, and high erosive rainfall. Between 2010 and 2016, the soil erosion level increased in most districts (22 districts among 31). Economic estimates indicate that production loss equivalent to 1 to 3% of Malawi's GDP under different increasing soil erosion scenarios is possible.

Input programmes, irrigation and diversification

Since 2005 the government has used subsidies to support maize growers. In Malawi, the Government has been providing a subsidy on fertilizer targeted at smallholder maize producers since 2005. Critics argue that a narrow focus on fertilizer has not solved underlying problems: narrow fertilizer-led intensification has contributed to stagnant or declining land productivity because of persistent soil degradation and inadequate rehabilitation investments. Other interventions are smaller in scale. Conservation-based practices have been tested on farms; one multi-season trial in central and southern Malawi compared hybrid and open-pollinated maize under different Conservation Agriculture (CA) and conventional practices (CP). Watershed projects have also built erosion barriers, and one such effort applied close to 2,000 km of soil erosion control measures including water absorption trenches, check dams, marker ridges and tree planting over an area covering 2,883 hectares.

Diversification is a long-standing policy goal, but progress has been slow. Maize-heavy and tobacco-heavy cropping has negative impacts on biodiversity, and increases the risk of diseases and pests. Legumes and other crops are promoted as alternatives; farmers in some districts grow soybeans, pigeon peas, orange-fleshed sweet potatoes and groundnuts, and mixed cropping has been reported to improve soil fertility. Agroforestry is also promoted, with species such as Faidherbia albida, Sesbania sesban, Gliricidia sepium, Cajanus cajan and Tephrosia vogeli commonly planted. The government has itself acknowledged the constraints, citing heavy reliance on rain-fed farming, adverse impacts of climate change, land degradation, declining soil fertility, and poor access to and application of fertilizers by smallholder farmers.

Economy and resource dependence

Malawi is a small, donor-dependent economy in southern Africa. Inflation has been above 20% on an annual basis for the past four years, and public debt exceeds 90% of GDP. Agriculture is the base of the economy, both for employment and for export earnings, so output tracks the weather and the markets for a few crops. The IMF has described the economy as facing a "challenging environment" because of climate shocks and falling demand for tobacco, the country's main export. The government's own projections show the same vulnerability. The central bank cut its 2026 growth forecast to 2.8%, lower than its previous forecast of 3.8%, reflecting weaker performance in non-agricultural sectors, which suggests that high borrowing costs and weak demand are weighing on businesses outside farming.

The exchange rate is the most contested part of the economy. The official kwacha rate has been stable for months: it has held near 1,734 to the US dollar, although the rate was about 1,749 at the start of October 2026. The gap between the official and parallel market rates is wide. The World Bank says the premium "remains very high", and the central bank has responded with controls. On 18 September 2026 it barred any individual from holding more than US$1,000 in foreign cash without permission. Reserves are thin: total reserves covered only 2.4 months of imports in July. The IMF argues that an overvalued official rate discourages exports, subsidises some imports and drives foreign exchange towards informal channels. The World Bank has called for the exchange rates to be unified, while the government has said that devaluation of the Malawi Kwacha is not under discussion with the IMF. Devaluation has historical precedent in Malawi: currency adjustments preceded the 2012 and 2023 ECF approvals. The price effects are direct, because a weaker kwacha would raise the kwacha cost of imported fuel, fertiliser, medicines and machinery.

Inflation has fallen from its peak, but the decline remains fragile. Prices rose by an average of 28.4 percent in 2025. By August 2026 the annual rate had dropped to 20.01 percent, the seventh monthly fall in a row. Analysts attribute most of this to food prices after a better maize harvest, while non-food prices have stayed high because of electricity tariff increases and the rising cost of imported goods. The Reserve Bank of Malawi has used the policy rate to manage these pressures. It cut its policy rate from 26 to 24 percent on 5 March 2026, the first move since February 2024, and it has kept the rate unchanged since then. The bank expects inflation to be 22.0% in 2026, which remains far above its medium-term objective of 5%. The bank has also warned that a possible El Niño episode could push food prices up again, since it could reduce food supplies.

Relations with international financial institutions shape the room for policy. The previous IMF programme, under an Extended Credit Facility worth about US$175 million, expired in May 2025 after no review was completed during an 18-month period, and the country received only the initial disbursement, amounting to approximately US$35 million. The latest IMF mission, which met in Lilongwe from 22 September to 6 October 2026, reported considerable progress on a policy package, but talks will continue before any agreement is finalised. The proposed package is meant to align with the government's National Economic Recovery Plan, and it emphasises stronger domestic revenue collection and spending controls consistent with the 2026/27 budget. Any arrangement must pass through the IMF's formal internal approval process, including a decision by the Executive Board, so the timing of any disbursement remains uncertain. Until a programme is in place, Malawi finances its gap from domestic borrowing and grants, and this keeps pressure on interest rates and the budget.

Society, language and religion

Ethnic groups and language families

Malawi's population includes a number of distinct communities. The national summary lists the Chewa, Tumbuka, Lomwe, Yao, Ngoni, Sena, Mang'anja, Tonga, Ngonde, Lambya and Sukwa as the main groups. The Chewa are the largest and dominate the Central Region, while the Tumbuka are concentrated in the north. The Sukwa live mainly in the northern districts of Chitipa and Karonga. Yao communities are especially visible in the Muslim-majority southern districts of Mangochi and Machinga. Almost all of the country's indigenous languages belong to the Bantu family, a legacy of migrations into the region that began centuries ago.

Official languages and linguistic practice

English is the sole official language, and the constitution treats it as the statutory national language. It has an outsized role relative to its number of first-language speakers: parliamentary debate, laws, most newspapers and commerce operate largely in English, and entry to secondary and higher education requires demonstrated competence in it. Chichewa, also called Chinyanja or Chewa, is the most widely spoken language and is spoken by roughly half the population. Chitumbuka is the other major language. Both Chichewa and Chitumbuka held official status for a period. Chitumbuka became official in 1934, but President Hastings Kamuzu Banda removed official status from both languages in 1968, leaving English as the only official language. The name Chinyanja was changed to Chichewa in the same year. In government schools, lessons are generally given in Chichewa, and English is taught as a second language from about age ten. Chichewa remains the dominant vernacular in everyday life, particularly in the centre and south, and it is the language of many local administrative and educational functions.

Religious composition

Christians form the majority of the population. The 2018 census recorded 17.2 percent as Roman Catholic, 14.2 percent as members of the Church of Central African Presbyterian, and 9.4 percent as Seventh-day Adventist, Baptist or Apostolic, with a further large group of other Christian denominations. Muslims were counted at 13.8 percent, or about 2.4 million people, and 2.1 percent reported no religion. Published totals for Christians vary by source: a U.S. government report gives 77.3 percent, while a country summary gives 82.3 percent for Christianity as a whole. Most Malawian Muslims of African descent are Sunni and follow the Shafi'i school, while Muslims of Asian descent generally follow the Hanafi school. The Muslim population is geographically concentrated; in Mangochi district, Muslims made up 72.6 percent of residents in the 2018 census.

Cultural expression

Cultural life combines local languages, oral traditions, music and dance. The Mwinoghe dance of the Sukwa people is an instrumental dance performed in three ethnic communities in northern Malawi. Dancers form two lines, men and women facing each other, and move to drums, a whistle and the leader's calls. The dance is performed at social gatherings and on national occasions, and attracts spectators from all social backgrounds.

Education and literacy

Primary education is free and is provided by the government. Access has expanded considerably: nearly 90 percent of school-age children attend primary school, and the primary net enrollment rate stood at about 96 percent. The gross enrollment rate exceeds 100 percent, because many pupils are over-age or under-age for their grade. Participation drops sharply after primary school. The lower secondary gross enrollment rate is about 46 percent, and only about 38 percent of primary graduates find places in existing secondary schools.

Completion rates reveal further inequality. In 2019, primary completion was 76 percent for boys and 85 percent for girls, but only 11 percent of children from the poorest wealth quintile finished primary school, compared with 67 percent from the richest. Adult literacy was 62 percent in 2015, down from 64 percent in 1998, and the male rate exceeded the female rate. Geography is a constraint: in rural areas, students often walk long distances to reach school, and the scarcity of secondary schools means many must travel far each day. Out-of-pocket costs for secondary school are also more than ten times those for primary school, which further limits access for families in remote areas.

Prehistory and pre-colonial history

The oldest hominin evidence from the Malawi region is a jawbone dated to about 2.4 million years ago. The specimen is one of the oldest occurrences of the genus Homo and is assumed to be of the species Homo rudolfensis. Its discovery is seen as a link between archaeological sites in East and South Africa. Later periods are represented by stone tools and animal remains. At Mwanganda's Village in Karonga, a Middle Stone Age site was first known for the findings of an elephant butchery site. Chaminade I, a late Middle Stone Age site in the same district, dates to 43,400 - 21,000 years ago. Most Later Stone Age occurrences, dated between 17,000 and 10,000 years ago, are in rock shelters, which is a broader African pattern.

Hunter-gatherers and the Hora 1 cremation

The most distinctive prehistoric find is at Hora 1, a rock shelter at the foot of Mount Hora in the Mzimba District of northern Malawi. The shelter lies beneath a granite-gneiss inselberg that rises about 110 metres above the Kasitu River valley. Research led by Thompson since 2016 has established that human occupation of the site began around 21,000 years ago, with its use as a burial ground spanning from approximately 16,000 to 8,000 years ago, during which all individuals were interred intact. A pyre at the site, dated to ~9500 years ago, departs from that pattern. Analysis of the remains indicates that the cremated person was an adult woman between 18 and 60 years old, with a stature under 1.52 meters. According to the study published in Science Advances, the pyre is the earliest evidence for intentional cremation in Africa, the oldest in situ adult pyre in the world, and one of only a few associated with hunter-gatherers. The remains show evidence for perimortem defleshing and postcremation manipulation.

Iron Age farming and rock art

Ironworking and farming reached the region later. In the southern lake area, the earliest Iron Age communities arrived early in the third century, according to archaeologists working there. Sources differ on the timing of wider arrivals: a national diplomatic website states that by the 4th century AD, Bantu people arrived in the area and introduced iron tools and weapons. Local ceramic chronology has been tested with radiocarbon dating; several archaeologists carried out various research projects in the area where they discovered and described five different Iron Age pottery types. This enabled archaeologists to establish a pottery sequence which C-14 dates have confirmed.

The Chongoni Rock Art Area in the central plateau contains 127 rock art and painting sites. Red paintings there are considered much older than the white ones, dating to as early as the Iron age. The white tradition corresponds closely to the territory of the modern Chewa, and the symbols used in the paintings are still used in their rituals today. The red traditions are linked to hunter-gatherers, who worked in unison with the farming community until the 19th century. Excavations at Mankhamba, a Late Iron Age Maravi settlement in central Malawi, show that hunting was the predominant source of animal protein, but that a reasonable portion of the meat was derived also from herded animals. The site also was an important link in the ivory trade.

The Maravi Confederacy and long-distance trade

Migrating clans from the Luba region are traditionally recorded as having entered the lake region. Beginning perhaps as early as the thirteenth century, the first elements of a large-scale migration of related clans entered the region of Lake Malawi. Dating for the confederacy itself varies; one encyclopedia states that they established the Maravi Confederacy about 1480. During the 16th century the confederacy encompassed the greater part of what is now central and southern Malawi, and, at the height of its influence, in the 17th century, its system of government affected peoples in the adjacent areas of present-day Zambia and Mozambique. Authority rested with a paramount ruler: it was ruled by a karonga (king), whose authority was passed down through the leaders of each clan within the confederacy.

Trade with the Indian Ocean coast reshaped the confederacy. Its decline began when clan leaders, who traded with the Portuguese and Arabs in ivory, slaves, and iron, became increasingly independent of the central authority of the Karonga. By 1720, the confederacy had broken into several autonomous factions. Among the intermediaries that followed, the Yao, living south and east of the lake, became rivals of the Maravi as middlemen between the interior and coastal markets. By the nineteenth century the commerce linking the interior to the coast was dominated by the traffic in enslaved people.

Colonial rule, independence and boundary formation

European knowledge of the lake expanded through David Livingstone's Zambezi expedition. On a third journey up the Shire they left the boat, walked 3 weeks overland, and discovered Lake Nyasa on Sept. 17, 1859. The expedition was recalled before completion by the British government, and its practical results came later. A German explorer, Roscher, had already discovered the lake's eastern shore, so Livingstone was not the first European to reach the area, though his accounts drew wider attention. In the 1860s, missionary work began under the Universities' Mission to Central Africa, the Church of Scotland and the Free Church of Scotland, followed by a small number of settlers. The Church of Scotland mission near the lake was named Livingstonia.

Colonial control was shaped by rivalry with Portugal. The British sent Harry Johnston as a British Consul to agree treaties with local rulers and to keep the Portuguese out of the established areas. A protectorate was declared over the Shire Highlands in 1889, and by 1891 it covered the whole territory of present-day Malawi as the British Central Africa Protectorate. The frontiers with Portuguese Mozambique to the east and German East Africa to the north were fixed through agreements between European powers during the 1890s. Control of the territory passed from the British South Africa Company to direct British rule in 1907, when the name was changed to Nyasaland. Cecil Rhodes's British South Africa Company was actually in charge of the protectorate when their authority was withdrawn in 1907, and direct British rule was instituted.

Colonial land policy had lasting effects. Nyasaland's history was marked by the massive loss of African communal lands in the early colonial period. Valuable land went to white settlers, while many Africans were pushed onto Crown Lands or became migrant workers. The 1915 rising led by the Reverend John Chilembwe, which was in protest at discrimination against Africans, was one of the early expressions of resistance to these conditions.

From 1953 the territory was part of the Federation of Rhodesia and Nyasaland, which joined Southern Rhodesia and Northern Rhodesia under one government. Britain agreed to this federation rather than full amalgamation, and the federation was pushed through in 1953 against very strong African opposition. The Nyasaland African Congress, which had been formed from earlier local associations, received financial and political support from Hastings Banda, then living in Britain. Banda returned from a thirty-year exile in London in July, 1958, to lead the antifederation movement in Nyasaland. The unrest that followed led to a state of emergency in 1959, which was declared on 3 March 1959 – 16 June 1960 and in which 51 killed, 79 injured, 3,300 arrested were recorded. A constitutional commission under Walter Monckton later canvassed the Federation, and found widespread opposition to the political structure. Britain then accepted that Nyasaland could secede from the union. The federation was formally dissolved on 31 December 1963.

Nyasaland became independent from Britain on 6 July 1964, and was renamed Malawi. Banda, who had led the independence movement, became prime minister and then, when the country became a republic in 1966, its first president. The transition from a monarchy-based protectorate to a republic under a single dominant leader set the framework for the political system described in the government section.

Government, administration and political geography

Constitutional framework and the presidency

Malawi is a presidential representative democratic republic with a multi-party system, and the president is both head of state and head of government. The politics of Malawi takes place in a framework of a presidential representative democratic republic, whereby the President of Malawi is both head of state and head of government, and of a multi-party system. The current framework rests on the 1994 constitution. Voters approved a move to multiparty politics by a wide margin in a 1993 referendum, and the new constitution was adopted on 16 May 1994, with elections held the following month. The president appoints cabinet members, and members need not necessarily be MPs. The president is elected directly and serves a term set by the constitution, a structure that places the executive at the center of national decision-making.

Parliament and the National Assembly

Under the constitution, all legislative powers of the Republic shall be vested in Parliament, and "Parliament" consists of the National Assembly and the President as Head of State. In practice the National Assembly holds the decisive role. The National Assembly alone possesses legislative supremacy and thereby ultimate power over all other political bodies in Malawi. Members are elected from single-seat constituencies for five-year terms. The constitution also originally provided for a second house, a Senate of 80 seats, but to date no action has been taken to create the Senate, and the provisions allowing for its creation were deleted in 2001. The country therefore has a unicameral legislature in practice.

The size of the chamber has grown over time. The 1994 election filled all 177 seats in the National Assembly, while the 2025 general election covered all 229 seats in the National Assembly. Some reference material still gives a 193-member figure, which reflects an earlier configuration. The 2025 contest was held on 16 September 2025 to elect the president, the 229 members of the National Assembly and 509 local government councillors.

The 2025 presidential and parliamentary elections

Peter Mutharika of the Democratic Progressive Party won the presidency with 56.8 percent of the valid votes cast, surpassing the 50-percent-plus-one threshold required for an outright victory, while incumbent Lazarus Chakwera of the Malawi Congress Party took about 33 percent. Mutharika, who served as president from 2014 to 2020, will return to office with former MEC Chairperson Jane Ansah as his vice president. Chakwera conceded before the final tally was announced. Mutharika's victory was a return to power by a former head of state, and the result was shaped by public dissatisfaction with the economy.

The legislative outcome was fragmented. DPP won 78 seats, MCP 52 seats, UTM 8 seats, and UDF 4 seats, while independents took 73 seats. With 115 seats needed for a majority, no single party controlled the chamber on its own. The large share of independent members points to weak party discipline and to strong local, personal bases of support. A president from a party that lacks a majority must therefore build alliances or negotiate case by case to pass legislation.

Administrative divisions

Malawi is divided into 3 regions which comprise a combined total of 28 districts. The regions are the Northern, Central and Southern regions, with Mzuzu as the northern capital, Lilongwe as the central capital and Blantyre as the southern capital. In the 2018 census, the Southern Region was the most populous of the three, with 7,750,629 residents, while the Northern Region had 2,289,780. Sources differ on the administrative role of the regions. One describes them as having no administrative function; they serve merely to group districts. Another states that local government is carried out in 28 districts within three regions administered by regional administrators and district commissioners who are appointed by the central government. Counts of districts also vary because some lists separate urban and rural units. A recent listing gives 32 districts forming the second and final level of subnational government, which counts the city and rural parts of Blantyre and Lilongwe separately.

Local government

Local government is covered in Chapter XIV of the constitution, and the local government system has 35 single-tier authorities: 28 district councils, four city councils, two municipal councils and one town council. Councils have overlapping responsibilities. All councils have the same responsibilities including primary education, primary health, forestry, natural resources and community services. Their financial autonomy is limited, since the majority of their revenue comes from national government grants. Each district is led by a district commissioner, who is appointed by the President of Malawi and acts as the chief executive of the district. The office dates to the colonial period, and Banda used them to have access to rural areas. The arrangement combines elected councils with central appointees, so national authority remains strong at the district level.

Political geography and regional identity

Electoral results are mapped by region and district, and Malawian voting is commonly analysed through the three-region division, since party support has tended to cluster in particular areas. Regional and ethnolinguistic identity has been a factor in this clustering. The early multiparty contests illustrate the pattern. In 1994, Bakili Muluzi of the UDF won 47.15 percent of the presidential vote, and the party's parliamentary strength came from its ability to build support beyond a single base. Regional distribution of votes is therefore an important guide to the country's political divisions, alongside the constitutional and administrative structure described above.

Health and environmental risk

Malaria is the most widespread disease tied to climate and water. Malaria is endemic in more than 95% of Malawi. Estimates of its burden vary by source: one malaria profile puts it at approximately 7 million cases and 36% of outpatient visits across all ages, while another estimate gives 6.2 million cases each year and 30% of outpatient visits. Transmission peaks during the rainy season from November to April. It is most intense along the lake and in the lowlands of the lower Shire Valley, which are warmer, wetter, and more humid. Plasmodium falciparum accounts for 95% of malaria infections and all severe diseases and deaths. Children carry a heavy share of the load: the Ministry of Health has said that malaria remains the leading cause of death in the country, claiming three lives a day. A malaria vaccine introduced in 2019 as part of a three-country pilot has been linked by health workers to fewer and milder episodes in children, though malaria remains a major cause of illness.

Waterborne disease is the second major concern, and flooding has made it worse. In Malawi, one of its worst cholera outbreaks killed nearly 2,000 people in 2022. During the 2025–2026 rainy season, devastating flooding displaced thousands, damaged critical sanitation infrastructure, and disrupted access to health services. By mid-February 2026, the flooding had affected over 160,000 people, resulting in 40 deaths and displacing thousands into emergency camps. Contaminated water sources had led to 828 suspected cholera cases, with emergency interventions focused on the hardest-hit districts of Blantyre and Chikwawa. In January 2026 health officials began a vaccination rollout in Blantyre, starting with 24,000 of the oral vaccines, and they identified unsafe water sources as the likely cause of cases in one township. WHO figures for the first weeks of 2026 show that Malawi, Mozambique, Namibia, Zambia and Zimbabwe were all reporting cases, a sharp increase over the same period in 2025. Storm damage has had similar effects before: in 2022, Tropical Storm Ana flooded more than 54,000 latrines and 340 wells in Malawi.

Poliomyelitis has returned as a public health issue twice in recent years. Health authorities declared an outbreak of wild poliovirus type 1 on 17 February 2022, after a 30-year polio-free period. Laboratory analysis showed that the strain detected in Malawi was linked to that which had been circulating in Sindh Province of Pakistan. By May 2024, thanks to multiple vaccination campaigns, vigilant surveillance and strengthened immunization systems, Malawi was declared polio-free once again. In early February 2026 the Ministry of Health and Sanitation declared a new outbreak after poliovirus was found in fecal samples from a public toilet in Blantyre, a finding the ministry said signals active circulation of the virus and poses a serious threat to public health, especially to children. Officials stressed vaccination as the main defense and hygiene as a key measure, since the virus is transmitted from person-to-person mainly through the faecal-oral route or, less frequently, through contaminated water or food. A four-day campaign in February 2026 vaccinated around 1.3 million children against polio.

Access to safe water and sanitation varies sharply between towns and villages. One local report noted that treated water in Malawi costs 86 Malawian Kwacha per five gallons, and impoverished communities often turn to local streams instead. CARE has also pointed to limited access to sanitation facilities among the country's poor, which compounds outbreak risk when water sources are contaminated. Drought is the other major environmental hazard. In October 2025 the government declared a state of disaster in response to worsening food insecurity driven by prolonged dry spells, high commodity prices. Since over 80% of the country depends on agriculture with most being subsistence farmers who depend on rainfed agriculture, both drought and flooding quickly affect nutrition and household resilience, and through them the capacity of health services to respond.

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251. MUTHARIKA DECLARED WINNER OF MALAWI’S 2025 PRESIDENTIAL ELECTION - The Zambian Observerzambianobserver.com
252. TRT Afrika - Malawi Electoral Commission declares Peter Mutharika winner of September 16 presidential electiontrtafrika.com
253. Malaria in Malawi: Statistics & Factsseveremalaria.org
254. Malawiimpactmalaria.org
255. Malawi health workers report drop in malaria cases following vaccine introgavi.org
256. Malawi rolls out cholera vaccines as rains and floods raise threat of deadly outbreaks in Africa - KIRO 7 News Seattlekiro7.com
257. Combatting Flooding and Cholera Outbreak in Malawiprojecthope.org
258. Floods trigger humanitarian crisis in Southern Africa: the battle against Cholera and Malariawaterdiplomat.org
259. Malawi rolls out cholera vaccines as rains and floods raise the threat of deadly outbreaks - ABC Newsabcnews.go.com
260. Southern Africa faces acute surge in cholera due to floods, displacementafro.who.int
261. WASH your Water: Cholera Re-emerges in Malawi — The Caravelthecaravelgu.com
262. Malawi polio outbreak: What next? - PMC - NIHpmc.ncbi.nlm.nih.gov
263. pmc.ncbi.nlm.nih.govpmc.ncbi.nlm.nih.gov
264. Malawi — Newsafro.who.int
265. Malawi: Govt Declares Polio Outbreak, Virus Detected in Blantyre Toilet Samplesallafrica.com
266. Malawi declares polio outbreakextranet.who.int
267. Cholera Outbreak Worsens in Malawi as Hunger Increases - CAREcare.org
268. Public Health Situation Analysis (PHSA)cdn.who.int
269. Malawi declares polio outbreak, reviving fears of another resurgenceafricanews.com