Cape Verde

Cape Verde (Cabo Verde, officially the Republic of Cabo Verde) is an archipelago of ten larger islands and several islets in the central North Atlantic, roughly 450 to 570 km west of Senegal. Its islands are entirely volcanic in origin and form a horseshoe shape that is divided by the northeast trade winds into the windward Barlavento group and the leeward Sotavento group. Its territory is small, about 4,000 km², but its position on the Atlantic shipping routes, its mix of arid lowlands and humid volcanic peaks, and its position as a small island state facing sea-level rise and water scarcity make it a useful case in geology, climate studies and island development. It is one of the few sub-Saharan African states to have maintained competitive multiparty elections since 1991 and to have shifted power between parties several times.

The entry first sets out the physical setting: the archipelago's volcanic origin and the tectonic setting that produced it, its relief from the active stratovolcano on Fogo to the flat sandy islands of Sal and Boa Vista, and the arid, trade-wind climate that controls rainfall, water and vegetation. It then covers the environmental constraints (erosion, scarce surface water, biodiversity and endemism, and exposure to drought, tropical storms and sea-level rise) before turning to human history, from uninhabited islands settled by the Portuguese in the 15th century through the Atlantic slave trade, the port economy of Mindelo, and the path to independence in 1975. The later sections describe the constitutional system, the 2024–2026 electoral cycle and change of government, the population and Creole-speaking society, the tourism-led economy and high public debt, public finance and the euro-pegged currency, infrastructure and energy, education and health, culture and music, and the country's international relations.

Location and administrative divisions

Cape Verde occupies an archipelago in the tropical North Atlantic, off the western coast of Africa, broadly between 14° and 18° N and 22° and 26° W. Its nearest mainland region is the coast of Senegal; the national tourism authority gives a distance of approximately 455 km from West Africa. Mainland Portugal lies roughly 3,000 km to the northeast, with the precise distance depending on the island and mainland endpoint. The country’s combined land area is about 4,033 km², distributed among ten principal islands and five principal islets. The islands form a horseshoe-shaped arrangement open toward the west, extending approximately 300 km from north to south and 250 km from east to west. These dimensions describe the archipelago’s geographical spread, rather than a continuous landmass. (en.wikipedia.org)

The islands are conventionally divided into two geographical groups. The northern Barlavento, or windward, group comprises Santo Antão, São Vicente, Santa Luzia, São Nicolau, Sal and Boa Vista. The southern Sotavento, or leeward, group comprises Maio, Santiago, Fogo and Brava. Their names refer to their positions relative to the prevailing northeast trade winds: the Barlavento islands lie on the windward side of the archipelago, while the Sotavento islands lie farther downwind. Santo Antão marks the northern end of the island chain and Brava its southern end. The two groups are geographical designations, not separate administrative regions. (capeverde.com)

Nine of the ten principal islands are inhabited; Santa Luzia has no permanent resident population, and the smaller islets are also uninhabited. Population is concentrated particularly on Santiago, the largest island and the location of the national capital, Praia, and on São Vicente, where Mindelo is situated. Figures attributed to the 2021 census place approximately 55.7% of the population on Santiago and 15.4% on São Vicente. Santo Antão accounted for about 7.5%, while Fogo and Sal each accounted for approximately 6.8%. The remaining inhabited islands—Boa Vista, São Nicolau, Maio and Brava—each held a much smaller share of the national population. (capeverde.com)

Administratively, the territory is divided into 22 municipalities, called concelhos in Portuguese. Their distribution does not correspond to one municipality per island: Santiago contains nine, Santo Antão and Fogo three each, and São Nicolau two. São Vicente, Sal, Boa Vista, Maio and Brava each constitute a single municipality. Santiago’s municipalities include Praia, Santa Catarina, Santa Cruz, São Domingos, São Miguel, Tarrafal, São Salvador do Mundo, São Lourenço dos Órgãos and Ribeira Grande de Santiago. The qualifiers in names such as Ribeira Grande de Santiago and Tarrafal de São Nicolau distinguish municipalities bearing similar names on different islands. Municipal territories are further divided into freguesias, or parishes. (bluecatengenharias.com)

The official Portuguese name is República de Cabo Verde. On 24 October 2013, the country’s Permanent Mission notified the United Nations that its short name should be Cabo Verde in every official UN language and should not be translated. UN nomenclature consequently changed from “Republic of Cape Verde” to “Republic of Cabo Verde,” with “Cabo Verde” as the short form. This standardized international usage around the Portuguese name rather than introducing a new Portuguese designation. “Cape Verde” remains an established English-language name, but it is not the form requested for official UN usage. (bluecatengenharias.com)

Geological origin and volcanism

Cape Verde’s islands are entirely volcanic in origin, although their exposed rocks also include marine sediments and fragments of older oceanic basement. The volcanic edifices stand on the Cape Verde Rise, a broad, dome-shaped submarine swell whose seabed lies roughly 2,000 m above the depth expected for oceanic crust of its age. This regional elevation is distinct from the individual volcanoes built upon it. Offshore sedimentary records indicate substantial uplift around the Oligocene–Miocene transition or during the early Miocene, broadly coinciding with the onset of the archipelago’s younger volcanic development. (agupubs.onlinelibrary.wiley.com)

The principal explanation invokes a mantle plume: ascending hot mantle supplies magma and helps support the elevated seabed. Seismic studies have identified low-velocity mantle beneath Cape Verde, consistent with anomalously hot or compositionally distinct material, but disagree over its deeper structure. Proposed alternatives include shallower, edge-driven mantle circulation associated with the African continental root; the rise itself may also receive buoyant support from mantle residue left after melt extraction. Consequently, evidence for mantle upwelling does not uniquely establish a narrow plume extending continuously from the deepest mantle. Studies of the mantle transition zone have yielded both normal thicknesses and thinning of approximately 30 km, leaving the depth and geometry of the source debated. (frontiersin.org)

The islands’ ages must be distinguished from those of their foundations. Figures near 135 million years concern the Mesozoic oceanic basement, not the construction of the present island volcanoes: regional magnetic anomalies and drilling evidence place the underlying crust at approximately 140–120 million years old. The oldest dated rocks attributed to the younger volcanic province occur in the eastern islands. Published potassium–argon determinations include $25.6 \pm 1.0$ million years for Sal, $16.3 \pm 1.2$ million years for Boa Vista, and $19.3 \pm 1.3$ million years for Maio. These establish a late Oligocene–Miocene history for island-building magmatism, rather than a single Cretaceous age for the archipelago. (agupubs.onlinelibrary.wiley.com)

Development generally proceeded from submarine construction to extensive shield-building eruptions, interrupted by erosion and sometimes followed by renewed volcanism. Alkali-basalt-related rocks predominate, including basanites and nephelinites, while more evolved magmas produced phonolites and trachytes; carbonate-rich carbonatites are another distinctive component. Western edifices are generally younger than the eastern islands, but their eruptive histories overlap rather than forming a simple chronological chain. On Santo Antão, for example, an older basanite–phonolite series dated to 7.5–0.3 million years overlapped a younger nephelinite–phonolite series dated to 0.7–0.1 million years. Slow movement of the African plate relative to the magma source permits prolonged, intermittent activity in the same region. (beckassets.blob.core.windows.net)

Fogo is the only island with documented historical eruptions. Its active stratovolcano includes Pico do Fogo, approximately 2,829 m above sea level, rising within Chã das Caldeiras, a large depression associated with collapse of the earlier edifice. Twentieth-century eruptions occurred in 1951 and 1995. The next eruption began on 23 November 2014 from a fissure at Pico’s southwestern base and was declared over on 8 February 2015. Lava reached Portela on 2 December and Bangaeira on 6 December, destroying homes, farms and infrastructure and displacing more than 1,000 people. Satellite mapping calculated a final lava-covered area of approximately 5.42 km²; the flows remained within the summit depression rather than reaching the coast. (agupubs.onlinelibrary.wiley.com)

Relief and landforms

Cape Verde’s relief contrasts sharply between the rugged northern and western islands and the low-lying eastern islands of Sal, Boa Vista and Maio. Santo Antão and São Nicolau have steep ridges, deeply incised valleys and rocky coastal escarpments; Santiago, Fogo and Brava also possess substantial mountainous interiors. On the eastern islands, broad plains, low residual hills and sandy shorelines predominate. This contrast reflects not simply volcanic construction but differing degrees of erosion: Sal, Boa Vista and Maio have been extensively reduced by marine erosion and subsequently uplifted, leaving coastal platforms and sedimentary deposits alongside their volcanic rocks. (turismo.cv)

Pico do Fogo, at approximately 2,829 m above sea level, is the archipelago’s highest summit. Its steep volcanic cone rises within the broad depression of Chã das Caldeiras, bordered by the Bordeira escarpment. The depression is about 8 km across and opens eastward; sections of its enclosing wall rise almost vertically for as much as 1,000 m above the floor. On Santo Antão, Tope de Coroa reaches about 1,979 m, making it the highest point in the Barlavento group. Santiago’s principal summit, Pico da Antónia, reaches approximately 1,394 m, while Serra Malagueta forms another prominent highland farther north, rising to about 1,064 m. (whc.unesco.org)

Santo Antão combines upland plateaus with abrupt descents into narrow valleys. Its eastern plateau lies mainly between 1,000 and 1,400 m, while western plateau surfaces extend roughly between 1,000 and 1,500 m around the higher volcanic summits. In the northeast, the Cova crater and Pico da Cruz overlook the deeply enclosed Paúl and Ribeira da Torre valleys, whose steep walls descend toward the sea. Cultivated terraces follow the contours of these slopes, their basalt retaining walls adapting to the gradient. São Nicolau likewise juxtaposes rugged ridges and valleys with plateau surfaces, including Campo Porto, reached from the valley near Belém. (documents1.worldbank.org)

The eastern islands are relatively flat rather than entirely featureless. Maio has low interior elevations surrounded by extensive coastal plains, including the saline landscapes of Terras Salgadas in the north and Porto Inglês in the southwest. Stony plains, dune fields and long sandy beaches form much of its coastal relief. Boa Vista and Sal share the broader pattern of subdued volcanic topography, with extensive sedimentary cover and low coastal platforms contrasting with the precipitous shorelines of the mountainous islands. (cplpmab.org)

Wind transport has reorganized coastal sand into mobile dunes, sand sheets and older cemented dune deposits. On Boa Vista, a major sand-transport corridor extends from the northwestern coast toward Praia do Curralinho in the southwest, connecting beaches and inland dune fields. Crescent-shaped dunes occur within this system and can merge into longer ridges. The sand is not simply material blown across from the Sahara: coastal sediment research identifies a substantial marine source, including fragments of calcareous red algae and mollusc shells. Wind carries these beach-derived grains inland and, along some corridors, back toward the ocean, producing a landscape in which beaches and dunes form interconnected sediment systems. (mdpi.com)

Climate

Most of Cape Verde has an arid or semi-arid tropical climate. Under the Köppen–Geiger classification, the principal types are hot desert (BWh) and hot semi-arid (BSh), with cooler semi-arid conditions (BSk) in some uplands. These categories conceal substantial differences between exposed coasts, mountain slopes and sheltered valleys. The national adaptation plan gives indicative annual rainfall averages below 100 mm for the arid coastal areas of Sal, Boa Vista and Maio, compared with approximately 600 mm in mountainous areas of Santiago, Fogo and Santo Antão. These figures describe contrasting climatic environments rather than uniform rainfall totals for entire islands. (documents1.worldbank.org)

The northeast trade winds dominate the atmospheric circulation because the archipelago lies on the southeastern periphery of the Azores subtropical high-pressure system. Cape Verde’s Third National Communication, prepared in December 2017, reports annual frequencies of 60–80% for these winds. The long dry season occupies most of November–June, while the principal rainy period extends from approximately mid-July to October. Rain becomes more likely as the intertropical convergence zone moves northward, bringing moist tropical air and disturbances associated with the West African monsoon. Southerly or southwesterly winds occur periodically during this period. In the dry season, continental easterly and northeasterly flows associated with the Harmattan can carry Saharan dust over the islands, producing the locally described “dry haze” and reducing visibility. (portaldoclima.gov.cv)

Relief modifies this regional climate sharply. Moist air rising over mountainous islands cools and condenses, increasing cloud thickness and producing orographic rainfall and persistent mist on exposed slopes. On Santo Antão, São Nicolau and Santiago, humid upland environments can therefore occur close to very dry lowlands. Air descending on the leeward side warms and becomes relatively drier, creating pronounced rain-shadow contrasts between northern and southern slopes. Cloud moisture is consequently important even outside episodes of measurable rainfall. A study published in the International Journal of Climatology examined Santiago’s rainfall using monthly records for 1981–2010 and daily records for 1997–2010, explicitly assessing elevation, slope and exposure as controls on its spatial variability. (mdpi.com)

Rainfall also varies greatly between years; the existence of a rainy season does not ensure dependable precipitation. Station records for 1960–2015 assessed in the Third National Communication show declining rainfall from the 1960s into the mid-1990s, followed by a modest recovery from about 1998. Ocean–atmosphere interactions contribute to this variability: research on the archipelago has identified associations between rainfall anomalies, Atlantic sea-surface temperatures and changes in low-level winds and tropical atmospheric circulation. These relationships do not reduce rainfall variability to a single ocean current or climatic index. (portaldoclima.gov.cv)

Temperatures have a smaller seasonal range than rainfall. The national adaptation plan places the annual mean near 25°C, with the coolest conditions from January to April and the warmest from August to October. Praia illustrates the seasonal combination relevant to agriculture and tourism: a 2014 meteorological study reports dry-season daily minima of approximately 21–23°C and maxima of 25–27°C, whereas August–October daily means remain above 25°C. The rainy months are also more humid and less windy; nighttime relative humidity can reach 80–90%. Thus, the short rainfall window coincides with the hottest, most humid conditions, while the prolonged dry season is generally cooler and more strongly ventilated by the trades. (unfccc.int)

Water resources and hydrology

Cape Verde has no large perennial rivers; most surface drainage follows seasonal watercourses, locally called ribeiras, whose channels may remain dry for much of the year. Intense rainfall produces short-lived flows through steep valleys, carrying water towards the coast rather than sustaining a dependable year-round supply. Aridity limits the volume available, while fractured volcanic rocks allow part of the rainfall to infiltrate before it can maintain surface flow. The absence of a substantial perennial river network does not mean that all watercourses are permanently dry: springs and groundwater seepage provide localized discharge, including in the Ribeira Paúl basin on Santo Antão. (sciencedirect.com)

Groundwater occurs in volcanic aquifers and in alluvial deposits within valleys. Its distribution depends on fractures, permeable lava layers and geological barriers: relatively impermeable volcanic dykes can obstruct underground flow and retain water at different elevations. Water is extracted through boreholes, wells, spring catchments and horizontal galleries excavated into basalt. Mountain rainfall is particularly important for recharge. A joint United States Geological Survey and Cape Verdean investigation conducted in 2005–2006 in Mosteiros on Fogo, Ribeira Paúl on Santo Antão and Ribeira Fajã on São Nicolau used dissolved gases to estimate recharge elevations ranging from about 700 metres to more than 2,000 metres. Groundwater dating indicated recharge within the preceding decade at some sites but more than 50 years before sampling at others, demonstrating that rainfall and abstraction can affect different parts of an aquifer on markedly different timescales. (sciencedirect.com)

Only part of precipitation becomes usable runoff or groundwater recharge. Evaporation from exposed surfaces and evapotranspiration through soils and vegetation return moisture to the atmosphere. The partition between these losses, surface runoff and infiltration varies with slope, surface permeability, soil-water storage and vegetation. Consequently, rainfall totals alone do not measure renewable water availability: highly permeable ground may favour recharge, whereas steep terrain can rapidly discharge storm water downstream. Cape Verde’s irregular rainfall also makes replenishment episodic, and prolonged drought reduces both groundwater levels and the reliability of springs. (sciencedirect.com)

The low-relief eastern islands have especially limited natural freshwater resources, but their dependence on manufactured supplies should not be confused with a complete absence of groundwater. On Sal and Boa Vista, available groundwater is insufficient in quantity or quality to meet demand, making seawater desalination the principal source for public supply. Water-sector figures for 2021, reproduced in a 2024 International Monetary Fund report, classified the supplied water on Sal, Boa Vista and Maio as entirely desalinated; nationally, desalination accounted for approximately 66 percent of freshwater supplied. These figures describe the supply system rather than every agricultural or private abstraction. Distribution networks carry the produced water to consumers, while some tourist resorts on Sal and Boa Vista operate their own desalination units. (documents1.worldbank.org)

Coastal aquifers are vulnerable to saltwater intrusion. Fresh groundwater commonly forms a lens above brackish or saline water; increased pumping can draw saline water into freshwater-producing zones. Rising demand from settlements, agriculture and tourism therefore places pressure on both groundwater quantity and quality, especially when drought restricts recharge. A 2010 USGS assessment of Mosteiros identified increased abstraction as a potential cause of contamination and depletion. The IMF’s subsequent diagnostic likewise documented groundwater stress associated with increasing water use and climatic aridity, alongside substantial losses in water-distribution systems. (pubs.usgs.gov)

Soils, vegetation and erosion

Cape Verde’s soils are predominantly derived from volcanic material, but their agricultural value varies markedly with slope, depth and moisture availability. Many hillsides have shallow, medium- to coarse-textured soils with little organic matter; erosion and repeated cultivation have reduced their fertility despite the mineral nutrients supplied by basaltic parent rock. In Santiago’s Ribeira Seca watershed, Regosols and Cambisols predominate on slopes, whereas deeper Vertisols and Kastanozems occur on some plateaus, and alluvial Fluvisols support irrigated cultivation in valley bottoms. A 2015 assessment placed the national arable area at approximately 41,000 hectares, with more than 90% devoted to rain-fed farming. Maize intercropped with beans is the characteristic dryland system, constrained by irregular rainfall and rapid loss of water from sloping fields. (mdpi.com)

The flora has affinities with Macaronesia, the Atlantic island region that also includes the Canary Islands, Madeira and the Azores, but incorporates substantial continental African and Mediterranean elements. Shared evolutionary lineages include Aeonium, Echium, Sonchus and Tolpis. Vegetation ranges from sparse drought-adapted communities in dry lowlands to more developed shrublands on humid mountain slopes. The endemic tree-like spurge Euphorbia tuckeyana is a characteristic component of native scrub. These affinities do not imply that Cape Verde formerly supported the same laurel forests as Madeira or the Canaries: a 2020 vegetation study found no evidence for such Lauraceae-dominated forests in the archipelago. (mdpi.com)

Native vegetation was extensively altered after settlement through agricultural clearance, cutting for fuel and construction, and livestock grazing, especially by goats. These pressures affected both accessible coastal lowlands and upland vegetation, exposing soils to wind and rainfall. Palaeoecological research at Monte Gordo on São Nicolau reconstructs a pre-settlement upland landscape containing Euphorbia, figs, dragon trees and tamarisks, providing evidence that the present vegetation is not simply a product of natural aridity. Introduced trees and plantation species subsequently replaced portions of the native cover. (reflor.maa.gov.cv)

Erosion operates through different processes across the islands. In dry, sparsely vegetated areas, wind removes loose surface particles and transports sand; research on São Vicente identifies wind erosion as particularly important in arid terrain. On cultivated mountain slopes, intense rain produces surface runoff, rills and gullies. The contrast is important: a Ribeira Seca assessment estimated that water erosion affected 26–50% of the watershed, whereas wind erosion and biological degradation affected a much smaller proportion. Measurements from maize-and-bean plots during 2011–2012 reported mean annual soil losses of 0.30 tonnes per hectare at a site with slopes of no more than 8%, compared with 9.10 tonnes per hectare at another site with slopes reaching 37%. (researchgate.net)

Soil protection has combined tree planting with terraces, contour stone walls, vegetative barriers and small check dams. Walls slow runoff and trap sediment; barriers of plants such as Aloe vera interrupt overland flow, while check dams retain material in drainage channels. After independence in 1975, conservation works and afforestation expanded through public employment schemes. Drought-tolerant Prosopis juliflora was widely planted for erosion control, fuelwood and fodder. Its spread into cultivated land and watercourses has also created management problems, and more recent restoration designs include native shrubs such as Artemisia gorgonum and Globularia amygdalifolia. (sciencedirect.com)

Forest statistics distinguish qualifying forest from broader planted or wooded land. FAO’s Global Forest Resources Assessment 2025 reports approximately 51,000 hectares of forest in Cape Verde, about 13% of its land area, including approximately 37,000 hectares of planted forest. This is below the frequently repeated estimate of around 21%. Earlier publications used broader afforestation totals: the 2015 conservation assessment, for example, reported 92,000 hectares afforested by 2012. Such totals are not interchangeable with FAO forest area, which excludes predominantly agricultural land and applies specific tree-height and canopy-cover criteria. (scribd.com)

Biodiversity, endemism and coastal environments

Cape Verde’s endemism is unevenly distributed among islands and habitats. The national biodiversity report submitted in 2015 recorded approximately 891 plant species, about 10% endemic to the archipelago; Santo Antão, São Nicolau and Fogo had the greatest numbers of endemic plants. Examples include the Cape Verde dragon tree, Dracaena draco subsp. caboverdeana, and endemic bellflowers such as Campanula feijoana. Introduced plants, habitat fragmentation and grazing threaten these restricted populations. On Boa Vista, the report identified the spread of Prosopis juliflora through dunes at the expense of native date palms, Phoenix atlantica, illustrating how invasive species can alter coastal vegetation as well as inland habitats. (cbd.int)

Island-specific reptiles and birds provide further examples of restricted distributions. Maio supports endemic lizards including Tarentola mayensis and Chioninia spinalis mayensis. The Raso lark, Alauda razae, had survived only on the small islet of Raso before conservationists reintroduced it to Santa Luzia in 2018. The operation involved the Cape Verdean organisation Biosfera, Portugal’s Sociedade Portuguesa para o Estudo das Aves, the national environmental directorate and University of Cambridge researchers. Breeding was subsequently confirmed, establishing a second population and reducing dependence on a single island. Coastal islets also support endemic seabirds: the Curral Velho wetland complex includes habitat for the Cape Verde shearwater, Calonectris edwardsii, and Cape Verde storm petrel, Hydrobates jabejabe. (unesco.org)

The archipelago is a major breeding area for loggerhead turtles, Caretta caretta. A 2024 study reported that Sal, Boa Vista and Maio hosted more than 90% of loggerhead nesting activity nationally. It also documented sporadic nesting by green, olive ridley and hawksbill turtles between 2013 and 2022, recording respectively 20, 25 and three nesting events. Protection encompasses beaches and adjacent waters rather than terrestrial sites alone. Maio became a UNESCO biosphere reserve in 2020, covering 73,972 hectares, including 47,072 hectares of marine area. Its constituent protected areas include lagoon and beach reserves, protected landscapes and the Porto Inglês salt pans. The surrounding waters support turtles, cetaceans, sharks and locally endemic marine gastropods. (doi.org)

Coastal ecosystems include sandy beaches, dunes, rocky shores, saline lagoons and salt pans. Lagoa de Rabil on Boa Vista, designated a Ramsar site in 2005, combines a permanent coastal lagoon with dunes and associated shrubs and trees. Curral Velho, designated the same year, encompasses permanent and temporary lagoons, beaches, dunes and an offshore islet; its salt-tolerant vegetation and lagoons provide habitat and feeding grounds for migratory birds. Marine diversity extends below these coastal environments. Research published in 2025 described structurally complex black-coral and gorgonian assemblages at depths of 30–40 metres off Santo Antão, while surveys around Cadamosto Seamount and the slopes of Fogo and Brava identified cold-water coral gardens and sponge aggregations. (rsis.ramsar.org)

Management of offshore resources operates within the exclusive economic zone. The United Nations Convention on the Law of the Sea permits an EEZ extending up to 200 nautical miles from the relevant baselines, subject to delimitation with neighbouring states. It gives the coastal state sovereign rights over resource exploration, exploitation, conservation and management, together with jurisdiction over marine environmental protection and scientific research. These rights are accompanied by obligations to conserve living resources; other states retain navigation and overflight freedoms. (un.org)

Coastal pressures include tourist development, urban wastewater, sand extraction and disturbance of nesting beaches. Lagoon recreation also includes vehicle excursions and water sports, bringing human activity into sensitive dune and wetland habitats. Climate-related pressures operate alongside these local impacts: ocean warming and ocean acidification pose risks to coral communities and fisheries, although their effects vary among species and habitats. An OECD assessment identified both processes as threats to Cape Verde’s marine resources, while the 2025 Santo Antão coral study emphasised the need for local thermal-tolerance research rather than assuming uniform responses across the archipelago. (cbd.int)

Natural hazards and climate risks

Drought is Cape Verde’s most recurrent natural hazard, affecting food production, freshwater availability and rural livelihoods. Rainfall shortages reduce crop yields and pasture growth while limiting replenishment of water supplies; their effects extend beyond farming through higher food costs and pressure on household incomes. The January 2015 maize harvest was reported by the Food and Agriculture Organization as the lowest then recorded in the country, and another severe drought occurred in 2017. The emergency response to the latter included a drought-mitigation programme supported by US$8 million from the European Union, alongside assistance from other international partners. (documents1.worldbank.org)

The archipelago gives its name to “Cape Verde-type hurricanes”: Atlantic tropical cyclones that become tropical storms within approximately 1,000 km of the islands and reach hurricane strength before arriving in the Caribbean. Their long passage over warm ocean water can allow substantial intensification; the designation describes their development region, not necessarily a direct strike on Cape Verde. Direct hurricane passages are uncommon, but Hurricane Fred crossed the islands on 31 August 2015—the first such passage documented since 1892. Its storm surge, high waves and rainfall caused coastal damage and flooding, while the rain also replenished reservoirs depleted by drought. Two Cape Verdean fishermen were reported missing and presumed dead after their boat failed to return to Boa Vista. (aoml.noaa.gov)

Volcanic disasters constitute a separate, non-climatic risk, concentrated on Fogo. Its 2014–2015 eruption lasted 88 days, displaced 964 residents of the caldera and caused damage and losses estimated at US$28 million, approximately 2% of national gross domestic product. Elsewhere, intense rainfall can generate flash floods and slope failures despite the generally dry climate. Heavy runoff threatens water-distribution systems, carries contamination into water supplies and damages agricultural plots in low-lying areas. Rapid urbanization and land degradation increase exposure to these hazards, making settlement location and infrastructure design important components of disaster-risk management. (documents1.worldbank.org)

Sea-level rise adds a long-term pressure to storm-driven coastal flooding and beach erosion. Low-lying coastal areas, including those on Sal, Boa Vista and Maio, face risks to settlements, infrastructure and tourism assets. Coastal inundation and saltwater intrusion also threaten freshwater quality and irrigated land. The National Adaptation Plan identifies the loss of coastal infrastructure, livelihoods and ecosystem services among the country’s principal climate risks; these pressures intersect with the economic dependence on beaches and coastal development. (unfccc.int)

The government’s National Adaptation Plan for 2022–2030 integrates climate risk into planning and budgeting. Proposed measures include water harvesting and drainage, drip irrigation, treated-wastewater reuse and reducing distribution-network losses from approximately 30% to 10% by 2030. Disaster-management reforms implemented with World Bank support during 2018–2022 incorporated hazard assessments into territorial planning, operationalized the National Emergency Fund and established a risk-management service within the Ministry of Finance. A US$10 million contingent-financing facility provided access to liquidity following qualifying emergencies. (unfccc.int)

In international climate policy, Cape Verde’s nationally determined contribution submitted on 1 November 2025 combines adaptation priorities with differentiated mitigation commitments. It pledges greenhouse-gas emissions reductions of 18% below a business-as-usual projection by both 2030 and 2035 without additional international support; conditional targets rise to 28% by 2030 and 39% by 2035. Its submission links stronger action to finance, technology transfer and capacity-building, emphasizing the constraints faced by a small island developing state. It also recognizes that insufficient global mitigation can exceed national adaptation capacity and produce residual loss and damage. (unfccc.int)

Settlement and the Portuguese colonial era

The islands had no indigenous population when Portuguese navigators reached them in the mid-fifteenth century. Permanent Portuguese settlement began in 1462 on Santiago, where Ribeira Grande—now Cidade Velha—became the principal settlement and the archipelago’s first colonial capital. Colonization combined European settlement with the forced transportation of Africans from the nearby mainland; enslaved labour was integral to the colony’s development rather than a later addition. Ribeira Grande’s surviving street layout, churches, royal fortress and sixteenth-century pillory reflect its administrative, religious and commercial functions. UNESCO identifies it as the first European colonial town established in the tropics. (cambridge.org)

The islands’ position off West Africa connected coastal commerce with longer voyages through the Atlantic. During the sixteenth and seventeenth centuries, Ribeira Grande served ships travelling between Africa, the Cape route, Brazil and the Caribbean, supplying provisions and acting as a centre for merchants and colonial administration. Vasco da Gama’s expedition called at the islands during its 1497–1498 voyage to India. Livestock supplied meat and hides, while the Ribeira Grande valley also became a site for acclimatizing and circulating cultivated plants between continents. Maritime commerce nevertheless exposed the settlement to attack: the French force commanded by Jacques Cassard devastated Ribeira Grande in 1712. (whc.unesco.org)

Cotton cultivation and textile manufacture linked plantation production directly to the Atlantic slave trade. A royal concession in 1466 opened mainland trading opportunities to island residents, while subsequent restrictions tied permitted commerce to locally produced goods. Cotton cloth known as panos di terra became an important exchange commodity on the Upper Guinea coast, alongside horses bred on the islands. Enslaved Africans cultivated and processed cotton and worked as skilled weavers; cloth and livestock were exchanged for additional captives, some retained locally and others transported onward. Cotton plantations developed on Santiago and Fogo, whereas attempts to establish sugar production were constrained by aridity. The islands thus functioned both as a slave-labour economy and as an entrepôt for the forced movement of people toward the Americas. (bpb-us-e1.wpmucdn.com)

A different maritime economy developed around Mindelo on São Vicente in the nineteenth century. Porto Grande’s broad, deep natural harbour offered a suitable refuelling point for Atlantic steamships, particularly those connecting Britain with South America. The settlement received the name Mindelo in 1838, commemorating the Portuguese liberal forces’ landing at the mainland beach of that name in 1832. British coal depots and shipping services subsequently made it a major coaling port. Mindelo attained city status in 1879; a public-works map from 1888 recorded 5,377 inhabitants and an urban centre organized around the church, municipal buildings and customs house. Its commercial and working life consequently developed around fuel handling, shipping and waterfront services rather than plantation agriculture. (hpip.org)

Creole society developed through sustained interaction among Africans, Europeans and their descendants, under the unequal conditions of colonial slavery. Cultural exchange affected social customs, religious beliefs, food preparation and artistic practices; it was not simply a matter of mixed ancestry. Archaeological finds at Alcatrazes, Santiago’s second captaincy settlement, place West African pottery alongside Iberian ceramics and locally made vessels, while spindle whorls indicate textile production. Enslaved people also shaped society through resistance: documentary evidence records fugitives finding refuge in Santiago’s mountains by 1512 and forming independent communities in the interior. Colonial Cape Verde therefore contained both port-based societies tied to Atlantic commerce and inland communities whose development challenged slaveholders’ control. (whc.unesco.org)

Independence and transition to multiparty democracy

The African Party for the Independence of Guinea and Cape Verde (PAIGC), founded in 1956 under Amílcar Cabral’s leadership, connected Cape Verdean nationalism with the wider struggle for decolonization in Portuguese Africa. Its programme sought independence for both Portuguese Guinea and Cape Verde, followed by political unity between them. The party launched an armed struggle in Portuguese Guinea in 1963; Cape Verdean members participated in its military organization and diplomacy. Abílio Duarte, for example, served in the party’s command structures in Guinea and argued for Cape Verdean self-determination before United Nations bodies in 1974. Cabral was assassinated on 20 January 1973, before either territory secured internationally recognized independence. (paigc.gw)

Following the overthrow of Portugal’s dictatorship in April 1974, negotiations between the Portuguese government and the PAIGC established a route to independence through an elected constituent assembly. The election of 30 June 1975 returned 56 representatives, and the assembly first convened on 4 July. Independence was proclaimed on 5 July 1975 at the Várzea stadium in Praia, where Duarte read the declaration. Aristides Pereira became president and Pedro Pires prime minister. The PAIGC governed as the sole legal party, while the first constitution, approved on 5 September 1980, formalized the new state’s institutions. The military coup in Guinea-Bissau on 14 November 1980 ended the project of political unity; in January 1981, the Cape Verdean party organization became the African Party for the Independence of Cape Verde (PAICV). (parlamento.cv)

The PAICV announced a political opening on 19 February 1990. The Movement for Democracy (MpD), led by Carlos Veiga, emerged as its principal electoral opponent. The decisive legal change came on 28 September 1990, when constitutional revision removed Article 4’s provision establishing the ruling party as the directing force of society and the state. This permitted competitive party politics and direct presidential elections. In the first multiparty parliamentary election, on 13 January 1991, the MpD won 56 of 79 seats, against the PAICV’s 23. The PAICV accepted defeat, and Veiga succeeded Pires through a peaceful transfer of power. António Mascarenhas Monteiro defeated Pereira in the presidential election of 17 February and was inaugurated on 22 March 1991. A new constitution, approved on 5 August 1992, subsequently entrenched pluralist democracy and the separation of powers. (expressodasilhas.cv)

The MpD and PAICV thereafter alternated as governing parties, each winning parliamentary majorities rather than depending on coalition governments. The MpD retained office in 1995; the PAICV returned in 2001 and won again in 2006 and 2011. The MpD regained its majority in 2016 and retained it in 2021, before the PAICV won the 2026 election. The table records parliamentary seats, distinguishing these contests from the separately held presidential elections. The assembly contained 79 seats in 1991 and 72 in every subsequent election listed. (cndhc.org.cv)

The historical seat totals appear in the national electoral guide and parliamentary records; the National Electoral Commission publishes the official election-result series and confirmed the 2026 allocation on 29 May 2026. PCD denotes the Democratic Convergence Party; ADM was the Democratic Alliance coalition; UCID denotes the Independent and Democratic Cape Verdean Union. (cndhc.org.cv)

Political system and government

Cape Verde is a unitary republic with a semi-presidential system: the directly elected president is head of state, while the prime minister directs the government and depends on parliamentary confidence. Its Constitution, which entered into force on 25 September 1992, establishes political pluralism, separation of powers and autonomous local government. The president serves a five-year term and appoints the prime minister after consulting the parties represented in the National Assembly and considering election results and possible governing alliances. Ministers are appointed on the prime minister’s proposal. The president may veto legislation and dissolve parliament under constitutionally specified conditions, but ordinary policymaking is principally the government’s responsibility. (congress.gov)

The unicameral National Assembly (Assembleia Nacional) has 72 members elected for five-year terms through closed-list proportional representation. Voters choose party lists, and successful candidates take seats in the order established on each list. Of the 72 seats, 66 represent domestic constituencies; the remaining six represent citizens abroad, with two seats each for the Americas, Africa, and Europe and the rest of the world. Domestic seat allocations reflect registered voter numbers, subject to a minimum of two deputies per constituency. Parliament passes legislation, approves the national budget and scrutinizes the executive. The Constitution provides for confidence and censure motions: rejection of a confidence motion or approval of a censure motion by an absolute majority of serving deputies entails the government’s resignation. (parl.ca)

Local government operates through 22 municipalities, each with a deliberative municipal assembly (Assembleia Municipal) and an executive municipal chamber (Câmara Municipal). Voters cast separate ballots for these bodies, whose members serve four-year terms; the first candidate on the most-voted chamber list becomes its president, equivalent to mayor. Municipal responsibilities include development planning, waste collection, street cleaning, sanitation, social housing and local transport regulation. The municipal assembly supervises the executive and approves budgets, development plans and municipal accounts. Law No. 48/X/2025, published on 4 April 2025, adopted a new municipal statute specifying these institutions’ powers and procedures. (parl.ca)

The judiciary is constitutionally independent, with judges subject to the Constitution and law rather than executive instructions. The judicial structure includes the Supreme Court of Justice, appellate and first-instance courts, while the Court of Accounts reviews the legality of public expenditure. The Constitutional Court exercises constitutional review and jurisdiction over electoral and political-party matters. Its judges are elected by the National Assembly for non-renewable nine-year terms. Established as a separate institution in 2015, it was formally installed on 15 October that year; previously, the Supreme Court performed constitutional-court functions. These arrangements give institutional expression to the constitutional principle of the rule of law. (parlamento.cv)

Separate presidential and parliamentary mandates have allowed periods of cohabitation, in which the president and prime minister come from opposing political camps. From 2011 to 2016, President Jorge Carlos Fonseca, supported by the Movement for Democracy (MpD), served alongside Prime Minister José Maria Neves of the African Party for the Independence of Cape Verde (PAICV). A reverse configuration began in 2021, when Neves won the presidency while MpD leader Ulisses Correia e Silva remained prime minister. These periods occurred within a system of competitive elections and peaceful transfers of governing power between the principal parties, without requiring the presidency and parliamentary majority to change together. (cidob.org)

Recent elections and change of government (2024–2026)

The municipal elections of 1 December 2024 gave the African Party for the Independence of Cape Verde (PAICV) control of 15 of the country’s 22 municipal executives, against seven for the Movement for Democracy (MpD). These figures were reported by the national news agency, Inforpress, from the National Electoral Commission’s (CNE) definitive results published on 13 December. The PAICV won Maio for the first time and secured São Lourenço dos Órgãos by a single vote. Nationally, it received 87,030 votes, or 50.80%, in the municipal-executive ballot, electing 98 of 142 executive members; the MpD received 72,312 votes, or 42.21%, and elected 41. The separate municipal-assembly ballot returned 183 PAICV representatives out of 350. (inforpress.cv)

In Praia, Francisco Carvalho secured re-election as mayor, having first won the office in 2020. His strengthened municipal mandate preceded his election as PAICV leader in May 2025 and his subsequent parliamentary-election campaign. Participation was already a significant feature of the municipal results: 176,756 of 351,935 registered electors voted, while abstention reached 49.78%. The CNE recorded particularly high abstention in Sal, at 57%, and Praia, at 55.31%. (rtp.pt)

The legislative election took place on 17 May 2026. Definitive results proclaimed by the CNE on 29 May gave the PAICV 90,660 votes, or 48.04% of valid votes, and 37 of the National Assembly’s 72 seats—the minimum required for an absolute majority. The MpD obtained 84,458 votes, or 44.75%, and 33 seats; the Independent and Democratic Cape Verdean Union (UCID) received 9,812 votes, or 5.20%, and two seats, both in São Vicente. Neither of the other participating parties secured representation. The PAICV won ten seats against the MpD’s nine in Santiago South and both seats in the Americas constituency. The incoming legislature included 34 women, representing 47.22% of its membership. (cne.cv)

Turnout fell to 46.5%: 193,335 people voted from a register of 416,096, leaving 222,761 electors, or 53.5%, abstaining. Contemporary reporting described abstention as a record for legislative elections; this should not be confused with a record across all election types, since presidential contests had previously recorded higher abstention. The official figures established that parliamentary representation had been decided by fewer than half of registered electors, but did not establish a single explanation for non-participation. Ahead of the presidential election, the CNE made participation and voter registration explicit priorities of its public-information campaign. (cne.cv)

President José Maria Neves appointed Carvalho prime minister through Presidential Decree No. 14/2026 of 19 June, following consultations with the parties represented in the National Assembly. Carvalho and the new government were sworn in that day at the Presidential Palace in Praia, succeeding Ulisses Correia e Silva, who had headed the government since 2016. The executive comprised 15 ministers and three secretaries of state. Carvalho also assumed the finance portfolio; Clóvis Silva took responsibility for justice, the presidency of the Council of Ministers, parliamentary affairs and social communication, while Manuel Amante da Rosa received foreign affairs, communities and national defence. (boe.incv.cv)

The presidential election was scheduled for 15 November 2026, with a possible second round on 29 November if no candidate obtained an absolute majority of valid votes. These remained forthcoming elections as of 10 October 2026. Neves announced his candidacy for a second term at a press conference in Praia on 14 September, having first been elected president in 2021. The presidential contest therefore followed, rather than coincided with, the parliamentary election and June transfer of executive power. (presidenciais2026.cne.cv)

Population, language and society

Cape Verde’s population was estimated at approximately 527,000 in 2025, with settlement concentrated on Santiago and São Vicente. The 2021 census recorded 269,370 inhabitants on Santiago, which contains the capital, Praia, and 74,016 on São Vicente, where most residents live in Mindelo. The next-largest island populations were Santo Antão, with 36,632 inhabitants, Fogo with 33,519, and Sal with 33,347. These island totals should be distinguished from city populations: Praia had 137,868 residents and Mindelo 69,013 in the same census. The two cities form the principal concentrations of administration, commerce and urban services, while the smaller islands retain much more dispersed settlement patterns. (populationpyramid.net)

Portuguese is the official language under Article 9 of the constitution, which also requires the state to promote conditions for giving the Cape Verdean mother tongue official status on an equal footing with Portuguese. Cape Verdean Creole, commonly called Kriolu, is the first language of virtually the entire population and the usual language of everyday conversation; Portuguese predominates in formal writing and schooling. This division makes literacy a question of language as well as access to education: children generally enter Portuguese-medium classrooms speaking Kriolu. Efforts to develop written Kriolu and bilingual teaching have included the experimental adult bilingual-literacy project begun in 1987 and the language-harmonization group chaired by linguist Manuel Veiga in 1993. That group developed ALUPEC, the unified alphabet for written Cape Verdean, in 1994; the government approved it experimentally in 1998. Educator Ana Josefa Cardoso subsequently coordinated a bilingual school experiment in Cape Verde between 2013 and 2019. These initiatives connect the recognition of a Creole language with literacy, classroom practice and national identity. (parlamento.cv)

Emigration has produced substantial communities in the United States, Portugal, France and other countries, linking resident families to relatives abroad through money transfers, visits and investment. The International Organization for Migration describes the wider diaspora as larger than the resident population, although its size depends on whether descendants as well as emigrants are included. Remittances support household consumption and investment in housing, small businesses and tourism-related activities. Its 2024 Diaspora Investor’s Guide, using central-bank figures, reported transfers of approximately 28.7 billion Cape Verdean escudos in 2023, equivalent to €260 million and 11.6 percent of gross domestic product. Such transfers make migration an important component of family livelihoods as well as national economic activity. (iom.int)

Household arrangements are varied rather than organized around a single family model. The National Statistics Institute’s 2022 household survey estimated 150,643 households, averaging 3.3 members; rural households averaged 3.7 members and urban households 3.2. Women were recorded as the household representative in 55.1 percent of cases. Couple-with-children nuclear households accounted for 22.0 percent of households, while one-person households represented 21.2 percent. Christianity, particularly the Catholic Church, remains the largest religious affiliation: a United States State Department report drawing on the 2021 census placed Catholics at approximately 73 percent of the population, with Seventh-day Adventists and Nazarenes each accounting for about 2 percent. Approximately 16 percent reported no religious affiliation. The constitutional framework separates religion and the state and protects freedom of conscience and worship. (ine.cv)

Urbanization has substantially changed the distribution of the population: about 74 percent lived in urban areas in 2021, compared with 62 percent in 2010. Expansion is concentrated not only in Praia and Mindelo but also in settlements serving the tourism economies of Sal and Boa Vista. Urban growth increases demand for serviced land, housing, water, sanitation and transport; these pressures are especially consequential where peripheral development extends beyond established infrastructure networks. World Bank urban-development programming has consequently targeted Praia and Mindelo alongside Espargos on Sal and Sal Rei on Boa Vista, combining the upgrading of urban infrastructure with measures to improve resilience. (documents1.worldbank.org)

Economy, tourism and growth

Cape Verde’s economy is dominated by services, particularly tourism, commerce and transport, rather than by agricultural or industrial production. A 2024 World Bank diagnostic described services as accounting for roughly three-quarters of gross domestic product (GDP) over the preceding decade and estimated tourism’s direct contribution at approximately 25%, rather than one-fifth; estimates including indirect effects are larger and are not directly comparable with the sector’s own value added. In 2025, GDP at current prices reached approximately US$3.06 billion, with GDP per capita of about US$5,796. These nominal dollar measures describe the economy’s size and average output per resident, rather than household disposable income. (documents1.worldbank.org)

Tourism is geographically concentrated and predominantly serves overseas markets. The National Statistics Institute (INE) recorded 1,248,052 guests in hotel establishments in 2025, up 6.0% from 2024, and 6,120,204 overnight stays, up 8.3%. These are accommodation-survey counts, not a count of unique international visitors: non-residents represented 95.5% of recorded guests. Sal received 57.7% of guests and Boa Vista 24.4%, compared with 8.1% for Santiago and 4.4% for São Vicente. The United Kingdom supplied 29.3% of non-resident guests, followed by Portugal, Germany, France, and the combined Belgian–Dutch market. Bed occupancy rose from 60% to 72%. The predominance of resort accommodation on two islands limits the geographical distribution of tourism earnings, while weak links between resorts and local suppliers restrict opportunities for domestic businesses. (ine.cv)

INE’s April 2026 national-accounts release reported real economic growth of 6.3% in 2025, following a revised 7.0% in 2024; fourth-quarter growth was 7.1% year-on-year. The release revised earlier quarterly estimates using updated agriculture and accommodation-and-food-service indicators, explaining why older publications contain different figures. The World Bank’s 2026 Economic Update likewise reported annual growth of 6.3%, with services contributing 4.1 percentage points. Its country overview reported a further 6.4% year-on-year expansion in the first quarter of 2026, driven by tourism and investment. Forecasts must be distinguished from these observed rates: the July 2026 Economic Update projected 4.8% growth for the full year, whereas the Bank’s country overview incorporating July inflation data projected 5.3%. Both anticipated slower annual growth than in 2025. (ine.cv)

The domestic production base remains narrow. Limited water availability and recurrent drought constrain farming, while the World Bank’s climate-and-development assessment estimated that imports supplied approximately 80% of domestic food consumption. Manufacturing has a much smaller economic weight than services. Dependence on imported food and energy exposes households and firms to international commodity prices, and distribution across separate island markets adds further costs. The 2026 Economic Update identified irregular ferry services, expensive freight and high passenger fares relative to incomes as constraints on fisheries, agribusiness and market integration. These costs reduce producers’ margins and make it harder for local suppliers to compete with imports or supply hotels consistently. (worldbank.org)

Diversification policy has sought to expand the private sector and connect tourism more closely with domestic production. The Strategic Plan for Sustainable Development, PEDS II for 2022–2026, operationalized the government’s Ambition 2030 framework, emphasizing digitalization and diversification. Identified investment areas include sustainable tourism, marine-based activities, renewable energy, digital services and transport. World Bank-supported tourism and blue-economy projects combine institutional reforms with improvements to coastal facilities, maritime passenger terminals, heritage sites and public spaces. Their economic purpose is to attract private investment beyond the established resort islands and strengthen links with local enterprises; the accompanying reform agenda includes clearer transport-service contracts, transparent subsidies and greater scope for private operators. (mf.gov.cv)

Public finance, currency and monetary policy

The Cape Verdean escudo (CVE) has been fixed to the euro since 1 January 1999 at $1\text{ EUR}=110.265\text{ CVE}$. This arrangement succeeded the peg to the Portuguese escudo established under the 1998 exchange cooperation agreement with Portugal. The fixed exchange rate anchors monetary policy: domestic interest-rate decisions must take account of foreign-exchange availability and interest rates in the euro area, rather than domestic credit conditions alone. In February 2025, for example, Banco de Cabo Verde (BCV) explicitly identified the interest-rate differential with foreign markets, particularly the euro area, as a potential source of currency outflows and a risk to the peg, and raised its policy rate by 0.25 percentage points to 2.5%. (bcv.cv)

BCV, the country’s central bank, uses its policy rate, standing lending and deposit facilities, and minimum reserve requirements to manage banking-system liquidity. On 17 September 2026, its board maintained the policy rate at 2.5%, the standing lending rate at 2.75%, the liquidity-absorption rate at 2.25%, and the minimum cash-reserve ratio at 12%. Foreign-exchange reserves provide a buffer for maintaining convertibility at the fixed parity. The World Bank’s July 2026 economic update reported reserves of €975 million at the end of 2025, equivalent to 7.1 months of prospective imports; its subsequent country overview continued to report import coverage above seven months. (bcv.cv)

Public debt remained close to annual gross domestic product despite its decline following the pandemic. The World Bank’s July 2026 update estimated the 2025 debt ratio at 100.7%; its subsequent country overview put it at 99.9% and projected declines to 93.9% in 2026 and approximately 86% by 2028. These are successive estimates and forecasts, not completed debt reductions. The later overview recorded a 2025 fiscal surplus of 1.1% of GDP, supported by strong revenue collection and final airport-concession receipts, but projected a deficit of 1.5% in 2026. Identified spending pressures included election expenditure, investment projects, wage-bill reforms, education and health commitments, and compensation to fuel and electricity distributors. It projected the deficit narrowing to 0.7% by 2028. (worldbank.org)

Fiscal consolidation combines revenue measures with expenditure controls and management of state-owned-enterprise risks. The IMF’s February 2026 assessment envisaged reducing tax exemptions, strengthening tax administration and digital compliance, improving investment execution, and reducing untargeted subsidies. Its medium-term projections assumed that the public wage bill would grow more slowly than nominal GDP, eventually converging to 10.1% of GDP. Enterprise capitalization, government on-lending and guarantees remain important potential claims on the budget. The World Bank’s July update reported debt service absorbing 34.2% of government revenue, rising to 46.3% when state-owned-enterprise obligations were included. (imf.org)

External financing relies substantially on concessional borrowing. The IMF’s early-2026 borrowing framework envisaged US$102 million in new public or publicly guaranteed external borrowing during 2026, entirely concessional, including US$70.9 million from multilateral lenders. The International Monetary Fund supports fiscal and balance-of-payments adjustment through the Extended Credit Facility, approved in June 2022, and climate-related reforms through the Resilience and Sustainability Facility, approved in December 2023. Reviews completed on 6 February 2026 authorized approximately US$3.25 million and up to US$7.23 million respectively. World Bank budget support included a US$15 million International Development Association credit for the Third Fiscal Space and Sustainable Growth Development Policy Financing operation, approved on 11 December 2025. (imf.org)

Infrastructure, energy and water supply

Praia’s port on Santiago and Porto Grande at Mindelo on São Vicente are the principal hubs of the national port system, which includes a port on each of the nine inhabited islands. These facilities connect international cargo services with inter-island shipping, allowing imported goods and domestic produce to circulate through the archipelago. Air transport complements maritime services: the country has seven airports, including international airports on Santiago, São Vicente, Sal and Boa Vista. Nevertheless, the World Bank’s 2026 economic update described domestic flights as expensive and unpredictable, and maritime services as constrained by ageing vessels and weak performance incentives. Unreliable connections limit access to employment and public services, and complicate the supply of agricultural and fishery products to tourist markets. (enapor.cv)

Electricity production remains dependent on imported diesel and other petroleum fuels. An International Monetary Fund diagnostic published in 2024, drawing on the generation series through 2021, reported a mix of approximately 83% thermal generation and 17% renewable energy, principally wind. Cabeólica’s four wind farms on Santiago, São Vicente, Sal and Boa Vista began commercial production in 2012, with a combined capacity of 25.5 MW. Expansion requires not only additional turbines and solar installations but also storage and improvements to island electricity grids. In June 2025, the African Development Bank approved €19.6 million for Cabeólica Phase II, designed to add 13.5 MW of wind capacity on Santiago and 26 MWh of battery storage across the four islands. The batteries are intended to regulate frequency and voltage and reduce the curtailment of wind generation; the announced financing and design do not, by themselves, indicate completed commissioning. (elibrary.imf.org)

Water production is closely linked to electricity costs. Desalination supplied approximately 66% of the country’s freshwater supply in 2021, although its contribution varied considerably between islands. Sal and Boa Vista, together with São Vicente, depend heavily on seawater treatment because local groundwater is insufficient in quantity or quality. Treatment plants must be complemented by storage, pumping and distribution networks: the IMF diagnostic estimated that technical and commercial losses together represented about half the water entering supply systems. Utility consolidation and network rehabilitation were central to the US$41 million Water, Sanitation, and Hygiene Project financed under the Millennium Challenge Corporation’s 2012–2017 compact. Its 2023 evaluation reported 43% more households with piped water than before the compact and twice as many sewer connections, while identifying drought-related interruptions to service. (elibrary.imf.org)

Regulated energy prices can shift part of imported-fuel costs from consumers to public finances. Resolution No. 95/2026, adopted on 30 June 2026, assigned the government 70% of the deficit created by incomplete adjustment of fuel prices that June; the remaining 30% was to be recovered progressively within twelve months. For electricity, it established state-financed compensation for distributors’ foregone revenue: social-tariff beneficiaries received a discount covering the entire tariff increase, while other categories received a discount covering 70% of the increase. These arrangements distinguish the regulator’s cost-based tariff from the amount charged to consumers, preserving distributor revenue through public compensation rather than eliminating the underlying supply cost. (boe.incv.cv)

Telecommunications access is predominantly mobile. At the end of 2024, the multisector regulator ARME recorded 587,026 active SIM cards and 542,912 internet subscriptions, 88% of the latter using small-screen mobile broadband. CVTelecom and Unitel T+ accounted respectively for 73% and 27% of internet subscriptions. Subscription counts are not counts of individual users, and national penetration figures conceal differences in household access and equipment. In the 2024 household survey, internet access at home reached 71.8% in urban areas and 58.9% in rural areas; computer ownership was 34.3% and 15.1%, respectively. Among households without home internet, 51.3% cited equipment costs and 43.6% service costs. These affordability and equipment gaps are important dimensions of the digital divide, alongside geographical coverage. (arme.cv)

Education, health and human development

The school system comprises eight years of free, compulsory basic education, followed by secondary schooling through grade 12, with general and technical pathways. Curriculum frameworks adopted in July 2022 reorganized both levels, emphasizing languages, mathematics, science and technology and aligning secondary-school qualifications with university entrance requirements. The 2021 census recorded substantial generational and geographical differences in literacy: 99.1% of people aged 15–19 could read and write, compared with 39.1% of those aged 70 or over; literacy among residents aged 15 and above was 91.2% in urban areas and 82.4% in rural areas. (boe.incv.cv) In presenting the 2025 budget, Education Minister Amadeu Cruz announced an allocation of approximately 12.4 billion Cape Verdean escudos for education, higher education, science and educational social assistance—11.9% above the corresponding 2024 allocation and 13.27% of the state budget. Priorities included teachers’ remuneration, technical education, school rehabilitation, digital learning and scholarships. (governo.cv)

Domestic higher education expanded through the establishment of the public University of Cabo Verde, or Uni-CV, on 20 November 2006. It brought together existing institutions specializing in teacher education, engineering and marine sciences, and administration and management, providing a local base for professional training previously undertaken through separate institutes or overseas study. Brazilian universities supported its early development through staff training and exchanges of administrative experience. A particularly direct connection between higher education and national workforce needs was the integrated master’s programme in medicine, introduced in 2015 in partnership with the University of Coimbra in Portugal. Uni-CV moved to its new Palmarejo Grande campus in Praia in 2021; cooperation with foreign universities remained part of its teaching and research development. (unicv.edu.cv)

The health system combines publicly financed services with contributory social insurance administered through the National Institute of Social Welfare, INPS. The Ministry of Health and INPS pool resources, with INPS purchasing services from the ministry for its contributors. Childhood immunization, antenatal care and family planning are provided without charge; children under five receive free health services, while people formally assessed as unable to pay are exempt from primary-care charges. Nevertheless, household payments at the point of service accounted for 23% of health expenditure in 2020. (afro.who.int) The 2025 budget allocated approximately 8.5 billion escudos to health, an increase of 10.7% over 2024, for personnel, primary and hospital care, facilities and medical equipment. (governo.cv)

Communicable-disease control coexists with a growing burden of chronic illness and nutrition-related risks. WHO’s 2024–2028 country strategy reported 208 tuberculosis cases in 2020 and a 23% decline in incidence between 2015 and 2020. It also cited an overall HIV prevalence of 0.6%. The 2020 noncommunicable-disease risk-factor survey found 44% of the surveyed population overweight and average daily salt consumption of 9.2 grams. (afro.who.int) On 12 January 2024, WHO announced Cabo Verde’s certification as malaria-free, following evidence that indigenous transmission had been interrupted nationwide for at least three consecutive years. (who.int)

The United Nations Development Programme’s 2025 Human Development Report, using 2023 data, placed Cabo Verde 135th among 193 countries and territories, with a Human Development Index of 0.668, within the medium-human-development category. Its component indicators included life expectancy at birth of 76.1 years, expected schooling of 11.4 years and mean adult schooling of 6.1 years. Adjustment for inequalities in health, education and income reduced the index to 0.478, a loss of 28.4%. (hdr.undp.org) Universal health coverage remains a policy objective rather than a declaration that all needs are met. The draft National Health Policy 2025–2035, discussed at the First National Health Conference and reported by WHO in February 2026, prioritized equitable integrated care, sustainable resources, emergency resilience and digital transformation. The associated WHO partnership programme includes work on health-financing assessment and financial protection, alongside primary-care governance and access to essential medicines. (afro.who.int)

Culture and arts

Morna combines song, instrumental music, poetry and dance, with lyrics addressing love, departure, separation, reunion, the ocean and attachment to the islands. Now predominantly sung in Cape Verdean Creole, it commonly uses guitar, violin and cavaquinho, with piano, bass and percussion also incorporated into ensembles. It accompanies weddings, christenings and family gatherings; transmission occurs through performances, workshops, radio and festivals. In 2019, UNESCO inscribed “Morna, musical practice of Cabo Verde” on the Representative List of the Intangible Cultural Heritage of Humanity. (ich.unesco.org) Cesária Évora brought this repertoire to international audiences: her recordings included “Sodade” on Miss Perfumado (1992), while Voz d’Amor won the 2004 Grammy Award for Best Contemporary World Music Album. (cesaria-evora.com)

Coladeira is a livelier dance-song tradition whose lyrics frequently employ social satire; its circulation across the islands and diaspora expanded during the 1960s, and later forms absorbed Caribbean influences, including zouk. (caboverde-info.com) Funaná, associated particularly with rural Santiago, is distinguished by the interaction between the gaita, a diatonic accordion, and the ferrinho, an iron bar scraped with another metal implement to maintain the rhythm. Bulimundo, led by Carlos Alberto Martins, known as Katchás, helped popularize amplified arrangements in the 1970s and 1980s. Ferro Gaita subsequently restored the accordion and ferrinho to prominent roles while retaining bass, guitar and drums. (caboverde-info.com)

Modern Cape Verdean literature developed through writing in Portuguese and Cape Verdean Creole. The journal Claridade, founded on São Vicente in March 1936 by Jorge Barbosa, Baltasar Lopes da Silva and Manuel Lopes, shifted literary attention toward the archipelago’s social realities. Its poems, fiction and essays treated drought, hunger, emigration and the conflicting obligations of departure and remaining at home. Nine issues appeared irregularly between 1936 and 1960, with a long interruption between the initial three issues and the resumption of publication in 1947. (expoimprensacolonial.fcsh.unl.pt) Later writing broadened this thematic range: Dina Salústio’s Mornas eram as noites (1994), a collection of 35 short narratives, examines women’s everyday experiences and unequal social relationships. Germano Almeida, whose fiction draws on island history and daily life, received the Camões Prize in 2018. (letras.ufmg.br)

Mindelo’s Carnival is sustained by neighborhood groups whose preparations involve months of rehearsals, costume-making and workshop activity. Its street processions combine music, dance and elaborate visual displays, attracting visitors alongside local participants. (elpais.com) The Baía das Gatas music festival, first held on 18 August 1984, established a major beach-based performance venue on São Vicente. (uccla.pt) Food traditions similarly connect household routines with communal celebrations. Cachupa, the characteristic national dish, is a slow-cooked preparation based on maize and beans, with vegetables and, according to the version, meat or fish. Cachupa rica incorporates a more extensive selection of ingredients, while cachupa guisada is commonly served at breakfast with a fried egg and sausage. Recipes vary between islands and are passed down within families; other staples include maize-based xerém, fish dishes and locally produced goat cheese. (visit-caboverde.com)

Visual and material arts include weaving, pottery, embroidery, basketry and woodcarving. Panu di terra is a traditional woven cloth associated with geometric patterns; Fogo artisans also carve decorative objects from porous volcanic stone. (visit-caboverde.com) Mindelo’s National Centre for Art, Crafts and Design supports certified craft production and opened its dedicated shop in January 2023. (governo.cv) Architectural heritage is particularly visible at Cidade Velha, whose historic centre entered UNESCO’s World Heritage List in 2009. Its surviving street layout, churches, royal fortress and sixteenth-century marble pillory preserve material evidence of the early colonial town and its Atlantic connections. (whc.unesco.org)

International relations and regional integration

Cape Verde joined the United Nations on 16 September 1975 and the Organization of African Unity, predecessor of the African Union, on 18 July 1975. Its multilateral engagement includes cooperation among small island developing states on development financing, ocean governance and the implementation of the Sustainable Development Goals. Praia hosted the interregional preparatory meeting for the fourth UN International Conference on Small Island Developing States from 30 August to 1 September 2023. At the conference itself, held in May 2024, the Cape Verdean government organized a session on adapting development goals to island conditions and local institutions. (treaties.un.org)

The country joined the Economic Community of West African States in 1977. Membership places it within regional frameworks for trade liberalization, free movement, residence and business establishment. The ECOWAS Trade Liberalization Scheme provides duty-free treatment for qualifying regional products, with rules of origin determining eligibility rather than simply the country from which goods are shipped. The 1979 free-movement protocol established a phased approach to entry, residence and establishment; implementation remains distinct from the rights envisaged in regional agreements. In June 2024, ECOWAS launched a national platform in Praia for its 2023–2027 cross-border cooperation programme, explicitly including the archipelago despite its lack of land borders. (ecowas.int)

Relations with Portugal combine bilateral development cooperation with Portuguese-speaking multilateral institutions. Cape Verde was one of the seven founding members of the Community of Portuguese Language Countries, established in Lisbon on 17 July 1996. At the bilateral summit in Praia on 7 March 2022, Prime Ministers António Costa and Ulisses Correia e Silva signed a Strategic Cooperation Programme for 2022–2026 with an indicative financial envelope of approximately €95 million, alongside five bilateral agreements. Mobility cooperation also extends beyond Portugal: the EU–Cape Verde Mobility Partnership, signed in 2008, provides a framework for migration dialogue, visa facilitation and readmission. The original EU visa-facilitation and readmission agreements entered into force on 1 December 2014. (cplp.org)

The European Union relationship is organized through a Special Partnership established in 2007, covering governance, security, regional integration, regulatory convergence, knowledge and development; investment, ocean governance and public-administration reform were added in 2017. Trade cooperation includes the GSP+ preferential-access regime, which Cape Verde entered in January 2014 and which links tariff preferences to international conventions on labour, human rights, environmental protection and governance. Fisheries cooperation has a separate contractual mechanism: the 2024–2029 protocol permits 56 EU vessels to fish for tuna and related species in Cape Verdean waters. It provides an EU contribution of €780,000 annually, including €430,000 for fisheries-sector support, in addition to vessel operators’ payments. (eeas.europa.eu)

Maritime security cooperation connects national surveillance with the regional Yaoundé maritime-security architecture. On 26 October 2022, Cape Verde and ECOWAS signed the headquarters agreement for the Zone G Multinational Maritime Coordination Centre in Praia; the centre was launched in January 2024. EU assistance through the Support to West Africa Integrated Maritime Security programme supported coordination structures, equipment and enforcement capacity. Cooperation also includes joint maritime-surveillance operations with European partners. In March 2024, Portugal deployed a P-3C maritime-patrol aircraft for missions operating from Praia and São Tomé, providing a concrete example of external support for maritime monitoring. (un.org)

The United States established diplomatic relations with Cape Verde in 1975. Development cooperation included a $110 million Millennium Challenge Corporation compact signed in 2005 and a second, $66.2 million compact completed in November 2017, focused on water, sanitation and land-management reforms. A bilateral status-of-forces agreement entered into force in November 2018, while a partnership with the New Hampshire National Guard began in 2021. China established diplomatic relations on 25 April 1976; the relationship became a strategic partnership in September 2024. Chinese assistance has financed public buildings and the Poilão dam, alongside scholarships and medical-team exchanges. According to China’s foreign ministry, bilateral trade reached $103 million in 2023. (2021-2025.state.gov)

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