Fiji

Fiji, officially the Republic of Fiji, is an island country in the southwest Pacific Ocean, in the Melanesian subregion. It comprises more than 300 islands, roughly a hundred of which are inhabited, and most of its land area and population are concentrated on Viti Levu and Vanua Levu. Suva, on Viti Levu, is the capital and the main economic and academic centre. The islands are of volcanic and limestone origin, shaped by plate tectonics and fringed by extensive coral reefs and mangrove forests.

Fiji matters for several reasons. Its tropical environment supports rich biodiversity and endemic species, while its exposure to tropical cyclones, El Niño–Southern Oscillation variability and sea-level rise makes it a useful case of climate vulnerability in small island states. Its economy depends heavily on tourism and on remittances from citizens abroad. Its history, from Austronesian settlement and chiefly polities through British colonial rule, the arrival of Indian indentured labourers, independence in 1970 and a series of coups, produced a multiethnic society whose politics remain a central concern. This entry covers the country's physical geography, environment and natural hazards, people and culture, history, government, economy, infrastructure and foreign relations across seventeen sections, including the 2026–27 general election cycle.

Location, Territory and Administrative Divisions

Fiji is an archipelago in the South Pacific, east of Australia, northeast of New Zealand and southeast of Papua New Guinea. Counts of its islands depend on how small islets are classified. Sources give figures from more than 300 to more than 800, with roughly 100 to 110 permanently inhabited. Viti Levu and Vanua Levu hold more than four-fifths of the population, and Viti Levu alone contains the capital, Suva, on its southeast coast.

Fiji's national territory is defined in its deed of cession as lying between 15° and 22° south and between 177° west and 175° east. The 180th meridian therefore falls inside the country. The International Date Line bends eastward around the island group so that all of Fiji keeps one local time, while the meridian itself crosses land on Taveuni, where it is marked for visitors. The exclusive economic zone extends far beyond the islands, giving Fiji rights over the resources of a very large area of ocean, as is the general practice for exclusive economic zones under the law of the sea.

Viti Levu is the largest island and has a rugged interior, with its highest point, Mount Tomanivi, at 1,324 metres. Vanua Levu, the second largest, lies about 64 km north of Viti Levu, and its main towns are Labasa and Savusavu. Viti Levu and Vanua Levu together make up about 78 per cent of the land area. The smaller groups have distinct characters. The Lau Islands lie east of Viti Levu and differ from the volcanic islands because they are largely limestone with low relief. The Lomaiviti group includes Ovalau, where the former capital Levuka is located. The Yasawa and Mamanuca groups lie off the western side of Viti Levu and form part of the Western Division.

Rotuma is a small, formerly volcanic island about 500 km north of the main group, although sources give distances from roughly 465 to 500 km. It covers about 46 to 47 square kilometres. Its people are Polynesians who speak a distinct Polynesian language, and linguists describe Rotuma as a Polynesian outlier, a Polynesian island set apart from the Melanesian majority of Fiji. Rotuma's chiefs asked to be annexed by Britain, and the island was formally ceded in 1881 as part of the Colony of Fiji. Today it is a self-governing dependency, and it is administratively grouped with the Eastern Division.

Fiji is divided into four administrative divisions, which are subdivided into fourteen provinces. The divisions are mainly groupings of provinces that coordinate services and development, and they have few functions of their own. The Central Division, with its capital at Suva, includes eastern Viti Levu and the provinces of Naitasiri, Namosi, Rewa, Serua and Tailevu. The Northern Division, administered from Labasa, covers the whole of Vanua Levu through the provinces of Macuata, Cakaudrove and Bua. The Eastern Division, centred on Levuka, comprises Kadavu, Lau, Lomaiviti and Rotuma. The Western Division, whose largest city and capital is Lautoka, includes Ba, Nadroga-Navosa and Ra on Viti Levu, along with the Yasawa and Mamanuca islands. The 2017 census recorded about 378,000 people in the Central Division, about 337,000 in the Western Division, about 132,000 in the Northern Division and about 36,000 in the Eastern Division.

Nadi, on the western side of Viti Levu, is the country's principal gateway for international air travel because Nadi International Airport is located there. The Western Division is also Fiji's main tourism hub, which makes Nadi the first point of arrival for most visitors.

Geological Origin and Relief

Fiji sits in a tectonically complicated part of the southwest Pacific, where the boundary between the Indo-Australian and Pacific plates runs through a zone of plate interaction, microplate fragments and volcanic activity Fiji sits at one of the more geologically complex intersections on Earth. One common account holds that the islands largely formed as the Pacific Plate was pushed beneath the Australian Plate formed by the subduction of the Pacific Plate beneath the Australian Plate. The rocks themselves are mostly of island-arc origin, ranging from basalt to dacite The islands are mainly volcanic and of island-arc origin, of basaltic, basaltic andesite, andesitic, and dacitic composition. Younger lavas on some islands are more alkaline and were erupted within the plate rather than above a subduction zone The younger volcanic rocks are mostly more alkaline and mainly belong to the alkali–basalt suite, and are intraplate rather than subduction related.

The islands did not appear at once. The oldest exposed rocks, in western Viti Levu, are island-arc volcanics dated to the Late Eocene, roughly 56 to 34 million years ago The oldest rocks found in western Viti Levu are island-arc volcanics 56-34 million years old (Late Eocene).. Shallow-water limestones were later laid down around these arcs as uplift proceeded Subsequent uplift caused deposition of shallow-water limestones around these island arcs.. The main landmass of Viti Levu developed between about 16 and 5 million years ago, Vanua Levu around 7 million years ago, and Taveuni, the youngest of the three, less than 2.5 million years ago, as a basaltic island with more than 150 vents along its length The first significant land mass (Viti Levu) developed 16 to 5 million years ago (Middle to Late Miocene) from plutonic lava intrusions and uplift. Vanua Levu was formed about 7 million years ago while Taveuni formed less than 2.5 m million years ago as a basaltic volcanic island with over 150 vents along its 40 km length..

Limestone terraces and uplifted reef deposits

Limestone is a major component of the smaller islands rather than of the two largest. The Lau group, for example, includes many limestone islands surrounded by widespread reefs Lau, or eastern Fiji, the area most heavily influenced by the Tongan culture, includes numerous limestone islands and others of volcanic or composite structure, all set among widespread reefs., and Vanua Balavu is cited as a typical example A good example of a typical limestone island is Vanua Balavu in the Lau group.. Raised coral platforms are also characteristic of the remaining islands outside the two main ones the remaining islands range from raised limestone platforms to low-lying coral atolls.. Vanua Levu, by contrast, is built largely from volcanic rocks of Late Miocene to Pliocene age Vanua Levu comprises Late Miocene to Pliocene volcanic rocks (7–2.8 Ma)., so its limestone deposits are generally secondary to its volcanic core, and the uplifted reef and limestone surfaces there are less extensive than on the Lau islands.

Vertical movement of the land has also been measured. In one early survey, the southwestern coast of Viti Levu was found to have been uplifted while the Yasawa islands were depressed Recent differential movements have uplifted the southwestern shore of Viti Levu and at the same time depressed the Yasawa islands..

Mountain interior, highest peak and the drainage divide

Viti Levu, at about 10,389 square kilometres, is the largest island in the country It measures 146 kilometres (91 mi) long and 106 kilometres (66 mi) wide, and has an area of 10,389 square kilometres (4,011 sq mi).. Its interior is dominated by a range running roughly north to south, which divides the island into near-equal halves divided into roughly equal halves by a mountain range that runs north to south.. The highest point is Tomanivi, an extinct volcano in the northern highlands, reaching 1,324 metres Mount Tomanivi, previously named Mount Victoria and also known as Tomaniivi, is an extinct volcano located in the northern highlands of Viti Levu. At 1,324 metres (4,344 ft), Mount Tomanivi is the highest mountain in Fiji.. The main rivers, including the Rewa, Navua, Sigatoka and Ba, all rise in this central mountain area The main river systems, the Rewa, Navua, Sigatoka, and Ba, all have their headwaters in the central mountain area..

The steep relief strongly shapes climate on either side of the ridge. The windward southeastern slopes receive very heavy rainfall, while the western lowlands lie in the lee of the mountains and have a pronounced dry season Heavy rains (up to 304 cm or 120 inches annually) fall on the windward (southeastern) side, covering these sections of the islands with dense tropical forest. Lowlands on the western portions of each of the main islands are sheltered by the mountains and have a well-marked dry season favorable to crops such as sugarcane.. Vanua Levu shows a similar pattern, with a rugged range dividing the island and forming much of the boundary between two provinces A rugged mountain range divides the island horizontally, forming much of the boundary between the Provinces of Cakaudrove and Macuata..

Coastal lowlands and alluvial plains

Between the uplands and the sea lie lowlands formed from river sediment. Along parts of the southeastern and eastern coast of Viti Levu, low delta flats that are overgrown with mangroves pass into a narrow coastal plain The southeastern side of the island and a large portion of the eastern and northeastern sides are low delta flats overgrown with mangrove bushes.. On Vanua Levu, the larger rivers cross elevated plains before reaching flood plains along the northern coast The larger rivers run north and northwest across elevated plains 200 to 300 feet high before forming flood-plains along the northern coast.. These alluvial surfaces are the land most suited to agriculture and settlement, and they have long been the focus of cane cultivation and village life.

Mineral resources and the Vatukoula gold mine

Fiji's mineral wealth is linked to its volcanic history. Gold deposits are associated with hydrothermal activity: at Vatukoula, the ore occurs in quartz formations with disseminated gold, and the deposit is linked to hot springs near a volcanic caldera Jaspoid bluish to blackish gray quartz formations with disseminated gold. Ancient siliceous sludges from hydrothermal springs near a volcanic caldera.. The mine lies within the Tavua volcano and its basin in northern Viti Levu The Mine is located in the northern part of the island of Viti Levu within the Tavua Basin, situated within the Tavua volcano.. Gold was discovered in the late nineteenth century, but commercial mining began in the 1930s Gold was discovered in the late 19th century, and gold mining started in the 1930s.. Output expanded rapidly during this early boom, from 931.4 ounces in 1934 to 107,788.5 ounces in 1939 gold production rising more than a hundred-fold, from 931.4 oz in 1934 to 107,788.5 oz in 1939. The mine is estimated to hold 4.2 million ounces of gold, and it was closed in December 2006 before reopening in April 2008 The mine was closed in December 2006, and was subsequently reopened in April 2008 as the price of gold increased. The mine has an estimated 4.2 million ounces of gold.. Earlier colonial surveys also recorded manganese ore in western Viti Levu, associated with tuffs and limestones Manganese mineralisation appears to be associated in the majority of cases with tuffs and limestones of the Ndakandaka Succession..

Climate and Weather Systems

Seasonal pattern and temperature

The climate in Fiji is tropical marine and warm year-round with minimal extremes. Seasonal temperature differences are small. Mean daily temperatures in the summer months are about 27°C, and in the winter months about 22°C. The main seasonal difference lies in rainfall. The wet season is usually counted from November to April, while the drier months run from May to October. The wet season is also the period when humidity is highest, and the air feels hotter despite similar thermometer readings.

Rain falls in a particular pattern. Much of Fiji's rain however falls in heavy brief local showers. Thunderstorms and sharp downpours are therefore common, while prolonged all-day rain is less typical. Wet-season rainfall is driven largely by the South Pacific Convergence Zone, a band of cloud and rain whose north–south shifts determine much of the year-to-year rainfall variation across the region.

Trade winds and windward–leeward contrasts

At all seasons the predominant winds are the Trade Winds from the east to south-east. These winds give the country its basic climate structure. Because the air is moisture-laden, any high land mass lying in their path receives much of the precipitation. On Viti Levu, the central mountain range forces moisture-laden trade winds upward on the eastern (windward) side, wringing out rain before the air descends on the western (leeward) side. This produces a rain shadow on the western and northwestern coasts.

The contrast is large. Suva and the east coast receive roughly twice to three times the rainfall of Nadi and the western coast, and the gap is widest in the wet season. Nadi is one of the driest places in the country, and averages only about 104 wet days per year. Rainfall on the windward mountains is far higher. The windward mountains receive 5000–10,000 mm of rainfall per year. Annual rainfall in the dry zones is commonly given as around 1500-2000mm, whereas in the wet zones, it ranges from 3000mm around the coast to 6000mm on the mountainous sites.

Regional variation

The two largest islands show the strongest climatic differentiation. The mountains of Viti Levu and Vanua Levu create wet climatic zones on their windward sides and dry climatic zones on their leeward sides. The drier northwestern portions of both islands experience less rain overall with a winter dry season. By contrast, little climatic differentiation occurs on the smaller islands having low relief. Temperatures vary less across the archipelago than rainfall does. Rainfall, not temperature, is therefore the main factor that distinguishes one region from another.

El Niño–Southern Oscillation and rainfall

Interannual variability is strongly shaped by the El Niño–Southern Oscillation (ENSO). El Niño or La Niña events are a natural part of the global climate system and usually recur after every 2 to 7 years. El Niño tends to bring drier and cooler conditions than normal, while La Niña events usually bring wetter than normal conditions over most parts of Fiji. Most of the meteorological drought in Fiji is associated with strong El Niño events, which result in severe rainfall reductions. The 1997/98 event is a notable case: it was described as a 1-in-100 year event, with rainfall failure occurring across two consecutive dry seasons.

ENSO also affects cyclone activity. Tropical cyclones occur more often in Fiji during negative values of the Southern Oscillation Index, and all TCs that occurred during El Niño conditions caused floods. The current event is a relevant example. The Fiji Meteorological Service's September 2026 outlook states that this El Niño event is likely to reach strong to very strong intensity and continue through the remainder 2026 and into early 2027. The same outlook notes that El Niño usually brings below normal rainfall to Fiji.

Cyclone season and forecasting

Fiji lies within the area affected by tropical cyclones. They are mostly confined to the period November to April, with greatest frequency around January and February. On average, some ten to fifteen cyclones per decade affect some part of Fiji, and two to four will do severe damage. The dominant tracks run from north-west to south-east, which gives some increased risk of damage in the outlying north-west island groups and the north and west coasts of the main islands. Long-term projections are more nuanced: tropical cyclones are projected to be less frequent but more intense in the long-term.

Monitoring and forecasting are carried out by the national meteorological service, which has kept long-term records of storms; for example, the Republic of Fiji has experienced 37 TCs during the period 1970-1998. The service's seasonal outlooks link ENSO phases to expected rainfall and warn of drought. In 2026, the service's director noted that some remote islands have started requesting water supplies as water sources begin drying up amid a lack of rainfall. Such warnings allow water, drought and cyclone preparedness to be planned together, as the same ENSO phase can simultaneously reduce rainfall and raise the risk of storms.

Rivers, Lakes and Freshwater Resources

Most of Fiji's significant surface water is found on the larger high islands, and the larger islands are well-watered, with many permanent rivers and streams. However, only Viti Levu has rivers of any considerable size. Over 70% of this island is drained by three large river systems, the Rewa, Navua and Sigatoka, which enter the sea along the south coast. The Rewa is the largest of these, and its catchment covers nearly one third of the island. It rises on the Nadrau Plateau, is fed by the Wainibuka and Wainimala, and reaches the sea by a delta of many mouths. It is navigable by small crafts up 80 kilometers from its mouth and its basin is enriched by a deep deposit of alluvial soil. The Navua and Sigatoka serve the same south-coast function on a smaller scale. The Sigatoka has its source on the west side of Mount Victoria and flows for 120 kilometers to the coast between the central and western ranges. In its headwaters, the Nadarivatu Dam was completed in 2012, and historically the river was the only means of transport from the Fijian coast to the island's lush interior, providing fisheries, as well as water for agriculture and drinking.

The Ba, on the northwest coast, behaves differently. Its catchment drains an area of about 930 km² on the northwest side of Viti Levu, and the Ba River catchment is steep and mostly unforested, features that tend to promote rapid-rising floods during intense rains. A long flood record kept at a sugar mill on the river shows that flood waters reached the mill floor every four years on average, while the same study found no increase in the frequency of major floods across the twentieth century. Cyclones passing east of the Ba basin tend to spare the Ba valley because of the rain shadow effect, yet can cause severe flooding on the Rewa. Where these rivers meet the sea, their mouths form estuaries and mangrove-fringed deltas. The Rewa, Ba and Labasa deltas alone support a combined total of 10,683 ha of mangrove, or 28% of the national resource.

Fiji's lakes are few and small, and most are formed in volcanic depressions. Lake Tagimaucia, on Taveuni, is in an old volcanic crater in the mountains above Somosomo. Its water surface sits at roughly 820 to 830 metres, and rainfall exceeds evaporation in all seasons and residence time for water in the shallow lake (2.5–5.5 m deep) is only 4 days. The water is chemically dilute and acidic: dissolved ion concentrations are low and the water is slightly acidic (pH 5.0–6.5 at 25°C). Around the margins, the swamp vegetation is dominated by Lepironia articulata and algae, which form floating sedge peat islands, along with Pandanus taveuniensis and other small trees. The aquatic fauna is sparse. The only aquatic vertebrates observed were Anguilla eels and cane toads, and the study noted that several recently introduced plants and animals had been recorded there. The lake is also the habitat of the endemic tagimaucia flower, which grows only at high altitude near water and, apart from at a few isolated locations on Vanua Levu, Lake Tagimaucia on Taveuni is the only place in the world you can see it.

Groundwater is more important to supply than the surface lakes. On the two largest islands, groundwater is found in superficial and medium-depth strata on the larger islands of Viti Levu and Vanua Levu, in either fractured rock or sedimentary formations. One of the most significant deposits is the Nadi Valley coastal aquifer, which is available and under pressure for development. Groundwater use is heavier than the surface supply in many places: not everyone can access reticulated water sources, which poses heavy dependence on groundwater sources. The picture is different on the small, low-lying islands, where there are cases in Fiji of islands with superficial groundwater lenses in sandbeds or coral formations, which lie on marine water and can be readily exhausted. Surface water is the main source for all major towns on the high islands, but on some low islands supplies depend entirely on groundwater and rainwater collection.

Freshwater in Fiji faces several pressures. Groundwater has been left vulnerable to contamination and depletion over the years, and rivers are affected by both extremes of the climate. River floods and hydrological droughts (low stream water resources) are a recurrent problem in different parts of Fiji, causing disruption and hardship for many rural communities. Sediment is a further concern, particularly where forest cover is removed. On Taveuni, for example, local environmentalists and dive operators feared that without proper ground cover the soil will be washed into the lagoon after logging was approved. Water supply and sanitation work in rural and peri-urban settlements has therefore focused on extending reticulated systems to villages. In Coqeloa, a village on Vanua Levu, the water supply system in Coqeloa Central and Coqeloa Number Three settlements was improved and expanded in 2017, ensuring the access to clean and safe drinking water for the residents.

Coastlines, Reefs and Marine Environment

Fiji's coasts combine fringing reefs around the larger islands with barrier reef systems and lagoons further offshore. Large sections of the southern coast of Kadavu are enclosed by a barrier reef system that encompasses Kadavu Island, Ono Island and other small islands within a natural protective lagoon. The Great Astrolabe Reef is among the most studied of these systems. Its lagoon floor holds unusual structures: a mound-shaped formation of mushroom corals about 10 m high, with core samples giving radiocarbon dates that suggest it began building roughly 4,500 years ago, at a mean accretion rate of 2.2 mm per year. Gaps in the barrier, or passes, funnel tidal current through the reef, and with it the life that current carries. Reefs around Kadavu and Ono also suffered from coral bleaching in 2000 and 2002, and observers reported that these reef areas had not yet recovered when they were surveyed in 2005.

Mangroves line many of Fiji's estuaries, river mouths and sheltered coasts. They shield villages, roads and industrial sites from swells, storm waves and floodwater, and their roots act as natural sieves that keep rubbish from washing out to sea, and they absorb pollutants, including heavy metals. Mangrove forests also serve as nurseries: they provide nurseries for fish and other marine species, and juvenile reef fish use them for food and cover. Their protective value is clear where they have been removed. A study by Nunn in 2000 at Ovalau and Moturiki compared villages, and settlements that kept their mangrove fringe reported no landward movement of the shoreline in living memory, while those where mangroves were cleared experienced abrupt shoreline erosion. The benefit of replanting is less certain. One review found no records of planting mangroves having halted coastal erosion in Fiji, and planting in unsuitable places such as seagrass beds has replaced one valuable habitat with another.

Seagrass beds occupy shallow nearshore waters and link mangroves and reefs. In a study of low-canopy seagrass in two shallow Fijian settings, seagrass beds reduced wave height by 30% and wave energy by 47% on average, which suggests that they contribute to shoreline stability as well as to fish habitat. Seagrass health depends on mangroves: if mangroves are deforested or absent, the consequences for seagrass are severe, through lower water quality, more pollution, higher nutrient loads and increased freshwater input.

Fiji's fisheries are both offshore and inshore. Oceanic fisheries, including tuna, operate across the wide exclusive economic zone, while coastal fishing supports subsistence and local markets across many villages. Inshore waters are governed largely by customary arrangements. The Fisheries Act recognises the customary fishing rights of mataqali (traditional clans) in their traditional fishing grounds, known as qoliqoli. Within these grounds, communities have established locally managed marine areas (LMMAs), a system described as the way Fiji seeks sustainable use and management of coastal fisheries. The first LMMA was set up at Ucunivanua on Viti Levu in 1997, where scientists and villagers agreed a three-year harvest ban on a shellfish stock. After seven years of local management, clam populations had recovered and village incomes had risen substantially. Estimates of the network's scale vary: one source reports some 250 LMMAs by 2009, covering about 10,745 square kilometres, or more than 25% of Fiji's inshore area, while another says the network represents 400 communities and over 22% of all inshore fishing areas. Within these areas, tabu areas often cover up to 15 percent of a village's fishing waters.

Coastal erosion is common on exposed coasts, especially those facing the trade winds and tropical cyclones. Sea-level rise has intensified the problem, and there are now cases of erosion of village shorelines where it has never previously been experienced. Sediment is a further concern. Clearing inland forest, road building and mining can increase the load of soil and sediment that rivers carry to lagoons and reefs, where it can smother corals and reduce water clarity, although the scale of this effect varies from catchment to catchment.

Biodiversity, Endemism and Conservation

Fiji lies within the Micronesia-Polynesia biodiversity hotspot, one of the world's most threatened such regions, and a large share of its plant and animal species are found nowhere else. Its forest ecosystems include lowland rainforest, upland rainforest, cloud forest, tropical dry forest, talasiga shrub grassland, mangroves, coastal strand forest and man-made agroforests. Published counts of plant species differ considerably. One estimate gives more than 3,000 plant species, of which approximately 1,500 are endemic, while a vegetation review refers to most of the 1769 native species that make up the forests. Many of these figures come from popular or tourism sources and should be read as approximate.

Forest types and plant endemism

Fiji's forests are commonly divided into moist and dry types. The wet-zone forests of the uplands feature two gymnosperms, Agathis vitiensis and Nageia vitiensis, along with many species also found in lowland rainforest. Dry forest develops where mountains create a long dry seasons created by rain shadows of mountains on the larger islands lie. A study of Fiji's dry zone identified tropical dry forest as a distinct type, with a pronounced dry season (5 consecutive months with <100 mm rainfall each) and several deciduous canopy species. Dry forest occupies roughly a third of the land along the northwest lowlands of Viti Levu and Vanua Levu, and dry forests have 310 plant species recorded with 96% endemic to the archipelago and 36% endemic to dry forests. Its canopy is typically led by the conifer Dacrydium nidulum and Fagraea gracilepes. These forests are among the most threatened in the Pacific, and the typical dry forest now survives mainly as remnant stands.

Endemic animals

Fiji's isolation has produced a distinctive fauna, especially among birds and reptiles. Estimates of the bird fauna vary by source: one tourism guide counts 76 native land and sea bird species, 27 of which are endemic, whereas a Wikipedia-based summary cites 177 species of birds, including 31 endemic species. The critically endangered red-throated lorikeet is a notable example, and its greatest threat is habitat loss. Fiji has only two endemic frog species, the Fijian Tree Frog and the Fijian Ground Frog, and the ground frog is threatened. The ground frog is confined to a few islands; it is extant on only four mongoose-free islands, Taveuni, Ovalau, Gau and Viwa. Reptile endemism is high among iguanas: the Fiji crested iguana inhabits the northwestern islands of Fiji, while the Fiji banded iguana is an arboreal species of lizard endemic to some of Fiji's southeastern islands. The crested iguana is the flagship species of the dry forest ecoregion. Fiji's only endemic mammal, the Fijian monkey-faced bat, is also known as the Fijian flying fox.

Invasive species

Introduced animals have been a major cause of native decline. The small Indian mongoose was introduced to Fiji in 1883 to control pests in sugar cane fields. It has since spread widely, and one source notes that it is now established on 13 of Fiji's approximately 332 islands. Its diet depends on habitat: a study of 4,404 mongoose droppings on Viti Levu found that crabs were the main food item in mangrove forests, rats were most common in cane-field scats. The species is among the 100 worst invasive species in the world according to the IUCN. The extinction of the barred-winged rail coincided with introduction of the small Indian mongoose there. Rats have also been damaging. Rats, cane toads, feral cats and big-headed ants all prey on ground frogs, and no recruitment of young into the population due to the destruction of breeding sites (deforestation) has been observed. The Pacific rat may have contributed to earlier declines of the ground frog as well. On Viwa, the smallest island with a ground frog population, the frogs face further threat from another invasive species, the cane toad. Research on managing mongooses has found that the monetized benefits of kill trapping exceed the benefits of live trapping and hunting.

Habitat loss, overharvesting and deforestation

Clearance of forest for agriculture and settlement has reduced habitat for many endemic species, and it removes the breeding sites that some frogs depend on. Overharvesting also has a long history. The sandalwood trade of the early nineteenth century heavily depleted these forests and the species survives only as small relict populations. The endemic yasi sandalwood (Santalum yasi) remains restricted to the driest habitats.

Protection and conservation programmes

Some native species have legal protection. The Fiji parrotfinch, for instance, is classified as Least Concern on the IUCN Red List, and it is protected under Fijian law. Botanical institutions also contribute to conservation. Botanical Gardens Fiji, for example, is dedicated to conserving endangered lowland tropical rainforest plants especially endangered palms, and planned gardens will conserve Fiji's highly threatened tropical dry forest trees. Much of Fiji's land is held under customary tenure, so the design and enforcement of protected areas depend heavily on the consent and cooperation of landowning communities, a balance that is discussed further in the population section.

Natural Hazards and Climate Risk

Fiji's exposure to natural hazards reflects three features: its position in the South Pacific cyclone belt, its steep interior terrain, and a coastline where many villages sit close to sea level. Hazards tend to combine, so a single cyclone can bring wind damage, storm surge, river flooding and landslides within a few days.

Tropical cyclones

Tropical cyclones are the most damaging recurring hazard. The most severe recent event was Cyclone Winston, which struck on 20 February 2016. The World Health Organization described it as the most powerful cyclone recorded in the Southern Hemisphere, and it killed 44 people. It made landfall on Koro Island, and the worst damage occurred on the outer islands and in northern and western Viti Levu, including Rakiraki and Ra Province. Estimates of economic loss exceeded US$1.4 billion, roughly one-fifth of GDP at the time. Losses to sugarcane and root crops contributed to food insecurity. Figures for housing damage differ between sources: UNICEF cited 28,000 damaged or destroyed homes, while a figure attributed to the prime minister at the time was about 40,000. The WHO reported that at least 88 of 214 health facilities were damaged, which disrupted medical services, water, power and transport.

Flooding, storm surge, landslides and drought

Storm surge is the hazard most closely tied to coastal settlement. Winston's surge drowned residents in Ra Province at the height of the storm, and low-lying villages on the outer islands, including those in the Lau group and the Yasawas, were especially exposed. River flooding affects the alluvial plains and deltas of Viti Levu, particularly where intense rainfall from cyclones and monsoon troughs fills rivers draining the central highlands. Landslides occur on steep hillsides, and the risk is higher where forest cover has been cleared. Drought is concentrated on the drier western and leeward coasts, where the rain shadow of the central ranges limits rainfall, and its severity increases during El Niño phases.

Seismic and volcanic hazards

Fiji lies in a complex plate-boundary zone where the Pacific and Indo-Australian plates interact, and the Tonga–Kermadec subduction system to the east is seismically active. Earthquakes can therefore occur, and offshore quakes can generate tsunamis. Most of Fiji's islands are volcanic in origin, but their volcanism is now largely extinct, so volcanic risk on land is low compared with seismic risk. Submarine volcanism in the wider region remains a potential source of hazard for shipping and coastal communities.

Sea-level rise and relocation

Sea-level rise, together with erosion and saltwater intrusion, is changing where people can live. Vunidogoloa, a village of 26 houses on the northern coast of Vanua Levu, was built on stilts but was still repeatedly flooded when heavy rain coincided with high tides. Villagers asked the government for help in 2006, and the community moved about two kilometres inland in January 2014, making it the first village in Fiji relocated because of climate change. Reports from 2023 counted six Fijian villages moved for climate reasons, with dozens more under assessment. Relocation depends heavily on customary land and on traditional leaders, and it is costly: in 2026, Vunidogoloa residents reported spending nearly US$600,000 on the move while still lacking basic infrastructure and access to their traditional fishing grounds. Government planning now includes vulnerability assessments and national relocation guidelines.

Climate diplomacy and national adaptation planning

Fiji held the presidency of the 23rd Conference of the Parties to the UN Framework Convention on Climate Change (COP23) in Bonn in November 2017, with Prime Minister Frank Bainimarama serving as president. Fiji's presidency gave priority to managing climate risk and building resilience, including through loss and damage mechanisms, and to access to climate finance. At the conference, Fiji launched its National Adaptation Plan framework, which sets out institutional arrangements and the principles guiding the adaptation process, and presented its five-year and twenty-year National Development Plan. The National Climate Change Policy 2018–2030 drew on the post-disaster needs assessment for Cyclone Winston and a national climate vulnerability assessment, and it links adaptation to Fiji's Nationally Determined Contribution under the Paris Agreement.

Population, Settlement and Demography

Size and growth

Fiji's population is small by world standards but has grown steadily. The demographic picture is shaped by natural increase and by sustained emigration. The UN Population Fund gives a rounded 2025 total of 900,000. Estimates based on the UN's World Population Prospects 2024 put the 2025 mid-year population at 933,154, and the 1950 figure of about 309,500 means the population has tripled since then. Figures for 2026 are higher still in some online counters, so the exact total depends on the source and date.

In 2025, births exceeded deaths by about 12,900, but external migration reduced the population by roughly 6,100. Growth is therefore modest, and the balance of migration now matters as much as the birth rate. The median age is about 28 years.

Urban concentration and internal movement

About 61 per cent of the population lives in urban areas. The largest urban centres are Nadi, Suva and Lautoka, which together form the country's main population corridor on Viti Levu. Growth in these centres reflects the concentration of wage employment, government services, schooling, health care and tourism-related work there. Movement from villages and outer islands toward these towns has been a steady feature of the post-independence period, and it has placed pressure on housing, water and transport in peri-urban areas.

Settlement patterns also differ by community. The iTaukei live throughout the country, whereas Indo-Fijians reside primarily near urban centres and in the cane-producing areas of the two main islands.

Village settlement and customary land

Most iTaukei families belong to villages organised around kin groups, with leadership and land rights linked to those groups. Much of the land is held under customary tenure rather than freehold, and access to it is administered through the Native Land Trust Board, which leases land to farmers, businesses and developers. This system protects indigenous land ownership but can complicate long-term leases, collateral for loans and large-scale development, and it shapes where new housing, plantations and tourism projects can be built.

Ethnic composition

The 2017 census is the most recent full national count used in most sources, but its figures are presented in different ways. The indigenous Melanesian or mixed Melanesian-Polynesian population, referred to as iTaukei, formed a majority of 555,499 people, or 62.8 per cent. A government ministry citing the same census gives a lower share of 56.8 per cent for the iTaukei and 37.5 per cent for Fijians of Indian descent, with 5.7 per cent in other categories. The term iTaukei was formally adopted in a 2010 law that replaced "Fijian" when referring to the original and native settlers of Fiji.

The Indo-Fijian community is the country's second-largest group. Its ancestors arrived as indentured labourers, with about 60,000 brought in by 1916. After forming roughly half of the national population in the late twentieth century, the community had fallen to about a third by 2017. The census recorded 289,237 Indo-Fijians, or 32.7 per cent.

Rotumans form a smaller group with a distinct identity. The 2017 census counted 1,583 people on Rotuma itself, although many more Rotumans live on the main islands, with a total of around 10,000. The census did not provide an updated ethnic breakdown for the "other" category that includes Rotumans, so their share is usually given as an estimate. Under Fiji's citizenship and electoral laws, Rotumans are regarded as indigenous.

Emigration and diaspora

Emigration has been a major feature of Fiji's population history since independence in 1970, and it has peaked during times of political crisis, such as national elections. The 1987 coups prompted large-scale emigration, driven by political instability and concern over increasingly hostile ethnic nationalism. An earlier analysis found that about 90 per cent of emigrants were Indo-Fijians, although educated and skilled iTaukei and other minority members of the middle class have increasingly left.

The most recent surge followed the COVID-19 pandemic. Before 2018 there were on average about 9,000 more departures than arrivals each year, while the number rose above 40,000 in each of 2022 and 2023. In 2023 net out-migration reached about 5 per cent of the population.

Australia and New Zealand are the main destinations, and the diaspora in these two countries makes up more than 60 per cent of the total Fijian diaspora according to UN data. Census counts show 61,748 Indo-Fijians in Australia in 2016 and 38,310 in New Zealand in 2022. Many current migrants hold temporary visas, including workers under the Pacific Australia Labour Mobility and Recognised Seasonal Employer schemes, and these workers are expected to return home. Ties between migrants and home communities remain strong, and the government is working on a Diaspora Policy to make Fijians abroad part of national economic development.

Languages, Religion and Social Customs

Fiji is multilingual. Fijian, the language of the iTaukei, is an Austronesian language of the Malayo-Polynesian family with verb-object-subject word order. Its standard form is based on the Bau dialect, an East Fijian variety, and sub-regional dialects remain strongest on Vanua Levu and in the eastern Lau islands. The 2013 Constitution recognises Fijian (referred to as iTaukei), English and Hindi as national languages, and Rotuman as a regional language. English dominates government, the courts, business and most secondary and tertiary education, while Fijian and Fiji Hindi are common in everyday village, market and family life. Fiji Hindi, the vernacular of most Indo-Fijians, is a distinct contact variety that is spoken alongside standard Hindi, which is used in religious and formal settings.

Religious landscape

Christianity is the largest religious tradition. The 2017 census recorded Christians at about 69 per cent of the population, Hindus at 24 per cent, Muslims at 5.8 per cent, and other groups at around 1 per cent. Within Christianity, the Methodist Church is the largest denomination; at the 2007 census it accounted for about 35 per cent of the total population, followed by Catholic, Assemblies of God and Seventh-day Adventist congregations. Religious affiliation broadly follows ethnic lines, with most iTaukei being Christian and most Indo-Fijians Hindu, alongside a substantial Muslim minority. Before the nineteenth century, iTaukei religion involved forms of animism and divination, with traditional priests known as bete. Methodist missionaries, who arrived in the early nineteenth century, converted leading chiefs and their followers, and after the 1874 cession to Britain Christianity became dominant. Hinduism, Islam and Sikhism arrived with South Asian workers in the late nineteenth and early twentieth centuries. The Methodist Church has remained influential among the chiefs, particularly in rural areas.

Vanua, kinship and chiefly structures

Social life among the iTaukei is organised around the vanua, a concept that combines land, people and the relationships between them. A vanua is the largest collective group associated with a particular territory, divided into yavusa (tribes), which are made up of mataqali (clans), which in turn comprise tokatoka (family units). The vanua is traditionally headed by a turaga i taukei, usually the most prominent chief from the most prominent family. Land is understood as an extension of the self, and people as an extension of the land. Chiefly authority was reinforced under British rule through indirect administration, and the Great Council of Chiefs (Bose Levu Vakaturaga) once made laws and regulations for the iTaukei. Since independence, the chiefly system has adapted to modern government and the market economy, but it retains a strong role in land matters, precedence and ceremony. Membership of a vanua has also been extended in specific cases; a Fiji Times report describes a Noco ceremony in which people of Indian descent were formally incorporated into a vanua kinship network with the same obligations as other members.

Kava (yaqona) and ceremonial life

Yaqona, known as kava in English, is Fiji's national drink. It is prepared from the dried roots of the pepper plant Piper methysticum, traditionally pounded in a wooden mortar and mixed with water in a large carved bowl, the tanoa. Its most formal expression is the chiefly yaqona ceremony, in which the servers come from the chiefly clan and the first cup goes to the highest-ranking person present. Guests traditionally arrive with a bundle of roots, a presentation called sevusevu, accompanied by a speech explaining their visit, and the hosts respond with a speech of acceptance. Participants clap before drinking and clap again several times after, typically with a cheer of "Bula!" The ceremony marks births, marriages, deaths, official visits and the installation of a chief. Tongan influence introduced the practice of chewing the roots before mixing, a custom that later gave way in most places to pounding.

Communal labour, known as solesolevaki, is another core social custom. Households or groups within a village pool their labour for tasks such as building, gardening and community projects, on the understanding of reciprocity. It sustains village cohesion and is closely tied to the obligations of the vanua.

Public holidays and festivals

Fiji's calendar reflects its religious and cultural diversity. The Cabinet endorsed eleven public holidays for 2026. Christian observances include New Year's Day, Good Friday, Easter Saturday, Easter Monday, Christmas Day and Boxing Day. Diwali, the Hindu Festival of Lights, falls on 9 November 2026, and Prophet Mohammed's Birthday is observed on 24 August. National commemorations include Girmit Day on 15 May, which marks the arrival of the first Indian indentured labourers, and Ratu Sir Lala Sukuna Day on 29 May, honouring a leading statesman of the twentieth century. Fiji Day on 10 October marks both the 1874 cession to Britain and independence in 1970, and the week before it features seven days of religious and cultural ceremonies. Regional festivals, such as the Bula Festival in Nadi, the Hibiscus Festival in Suva and the Sugar Festival in Lautoka, add to the year's cultural calendar.

Early Settlement and Pre-colonial Societies

Lapita settlement and the first inhabitants

The earliest well-documented settlers of Fiji are usually associated with the Lapita cultural complex, a decorated pottery tradition that takes its name from a New Caledonian site where comparable wares were first identified. Lapita takes its name from an archaeological site in New Caledonia where similar pottery was first discovered. Fiji's first Lapita finds came from the Sigatoka Sand Dunes on Viti Levu, where Ratu Rabici and Lindsay Verrier identified the first Lapita pottery in Fiji, a discovery that later helped researchers map how the style spread. Large-scale excavations in the mid-1960s recovered a late Lapita ceramic horizon that included many nearly complete vessels. Radiocarbon and geoarchaeological work indicates that these ceramics were deposited within a short span around 2,500 years before present, and the shoreline setting suggests the spot served as a canoe landing rather than a permanent village.

Chronology is still debated. One analysis places the start of Lapita settlement in Fiji at roughly 2,900 to 2,700 calibrated years before present, and it notes that disturbance at many sites complicates dating. Older claims exist: a researcher working at Bourewa in Nadroga has argued that occupation there began around 1200 BC, a date far earlier than most others. Oral traditions of Fijian ancestors arriving about 2,500 years ago also circulate, and popular accounts often round the arrival to roughly three millennia.

Subsistence, canoes and voyaging

Pre-colonial communities depended on gardens of root crops, especially taro and yam, supplemented by reef and lagoon fishing and the cultivation of coastal and inland plots. Navigation was central to daily life and to contact between islands. Voyagers crossed open water in wooden canoes, using stars, ocean swells and bird flight as guides. Fijian and Tongan builders also relied on large ocean-going craft; Tongan visitors, for instance, sought sandalwood and suitable timber for double canoes, which were hard to produce on their own islands. The Tongan double-hulled canoes known as kalia were large enough to carry provisions for a substantial crew, and they supported regular trading voyages between Fiji and Samoa.

Chiefdoms, alliances and external ties

Before the mid-nineteenth century, Fiji's political balance rested on a number of powerful chiefdoms rather than a single state. Fiji didn't have a single empire but rather a patchwork of competing chiefdoms. Chiefs jockeyed for power across more than 300 islands. Authority was typically layered, with paramount chiefs governing large regions, high chiefs managing individual islands or districts, and village chiefs handling local affairs. The strongest chiefdoms were Bau, Rewa, and Cakaudrove. Alliances were fluid, and rival polities frequently shifted their loyalties. Smaller states such as Nadroga were also significant; in pre-colonial times Nadroga was one of the larger polities in the country. Scholars studying chiefdoms such as Bua, Bau, Lau and Somosomo have shown that outsiders, goods and newcomers were absorbed according to local rules and existing Fijian categories.

Contact with Tonga and Samoa was significant. Tongan authority reached its height in the thirteenth century, when its realm extended over part of the Lau group. Historians continue to debate whether this relationship was one of domination or reciprocal exchange, and the Tavuni Hillfort in the Sigatoka Valley is cited as a Tongan fortified settlement. Pre-contact interaction between Samoa, Tonga and Fiji was intense, and marriage exchanges between high-ranking families linked the three archipelagos.

Material culture

Pre-colonial material culture included pottery, stone and shell tools, and bark cloth (tapa), along with wooden bowls and carved implements. Early ceramics, such as the Lapita wares, were decorated with incised and stamped motifs, while later plainware assemblages show decoration that had largely disappeared. Shell jewellery and hunting tools have also been recovered from coastal sites, indicating a long tradition of craft and personal adornment.

European sightings

The first recorded European sighting of Fiji came in 1643. On February 6, 1643, European eyes sighted the islands of Fiji for the first time. Abel Tasman passed the northeastern fringe of the group, and he did not land or make contact with the indigenous population, fearing for his ships among the reefs. The reef-strewn passage became known as Heemskerck's Shoals. James Cook's visit came more than a century later: Cook sighted, charted, and landed on Vatoa, the most southern and easterly island of the southern Lau islands in 1774, where islanders retreated into the forest as the crew came ashore. Fiji's government notes that the first significant European exploration is credited to William Bligh rather than to Cook, and that the islands' contact with Europeans remained sporadic until the late eighteenth century.

European Contact and Colonial Rule

European contact began with commercial rather than settler interests. In 1804, two ships bought sandalwood in Fiji for the first time, and the find on the southwest coast of Vanua Levu drew a rush of Western vessels. The sandalwood stands were depleted within little more than a decade. Traders then turned to bêche-de-mer (sea cucumber), which was prized in China, and by the 1820s they were again working the Fijian islands. Unlike sandalwood cutting, which foreigners largely carried out themselves, bêche-de-mer collection drew in large numbers of Fijians, who gathered, cleaned and dried the animals and supplied food and firewood. Beachcombers and shipwrecked sailors who settled among chiefly communities served as interpreters and armourers, and Methodist missionaries arrived at Lakeba in 1835. Levuka, on Ovalau, became the first modern town in Fiji in the early 1820s and grew into the commercial centre of the European community.

Inter-chiefly rivalry shaped the colonial path. Seru Epenisa Cakobau, a chief from Bau, proclaimed himself Tui Viti (King of Fiji) in 1871 and created a unified state across most of the group, excluding Rotuma. His authority, however, was not universally accepted by other chiefs, and his claim to the title was questioned even by Europeans. Facing debts owed to American creditors and pressure from Ma'afu of Tonga on the south coast of Viti Levu, Cakobau first offered to cede the islands to Britain in exchange for assumption of his debts, but London declined in 1862 after investigating his standing. He later renewed the offer through the British consul. The kingdom's government was run largely by European advisers, and in 1874 Cakobau made a final offer that Britain accepted. On 10 October 1874 he and twelve other high chiefs signed the Deed of Cession at Levuka, and Sir Hercules Robinson arrived as the first governor. Britain established the Colony of Fiji, with the British monarch as head of state from 1874 until 1970.

Colonial administration rested on a partnership with Fijian chiefs and on the protection of customary land. Governor Sir Arthur Gordon, who held office in the late 1870s and early 1880s, promoted a policy of preserving the traditional village structure and the authority of chiefs rather than integrating Fijians into the wage economy. The Great Council of Chiefs became the principal channel for indirect rule over Fijians, while Fijian land remained held under communal customary tenure and was administered through chiefly and government mechanisms, not sold freely to settlers. This arrangement limited Europeans' access to land and shaped the later institutions responsible for Fijian land. Racial hierarchy nevertheless defined the colonial state: the Legislative Council was reformed in 1904 into a partly elected body in which European male settlers gained the vote, while Fijian chiefs were given only indirect input and most seats remained nominated.

The colonial economy was built around sugar, which was established in the 1870s under Australian capital and dominated for nearly a century by the Colonial Sugar Refining Company (CSR). Because Indigenous Fijians were largely reluctant to work the cane fields on the company's terms, and because the colonial government was unwilling to coerce them, planters looked to India for labour. Between 1879 and 1916 the indenture system, known as girmit, brought approximately 60,000 Indian labourers to Fiji. The first ship, the Leonidas, reached Levuka on 14 May 1879. Workers signed five-year contracts, after which they could return to India at government expense or remain as free settlers. Conditions were harsh, with low wages, a skewed sex ratio, and frequent violence, and agitation within India, including the visit of C. F. Andrews, helped end importation in 1916; the last agreements lapsed by about 1920. Many former labourers stayed, leased land and built farms, and their descendants became the Indo-Fijian community, which by the mid-twentieth century came close to matching the Indigenous population in size.

Beyond sugar, the colonial economy relied on copra and gold, and Suva replaced Levuka as the capital in 1882, reflecting the shift of administrative and commercial life toward the Viti Levu coast. Rotuma was annexed to Fiji in 1881. The colonial period therefore established the ethnic, legal and economic divisions that would later shape the independence era.

Independence and Early Post-colonial Politics

Fiji became a sovereign state on 10th October 1970 when its colonial status was abrogated. Ratu Sir Kamisese Mara was appointed Fiji's first prime minister on 10 October 1970, when Fiji attained its independence from Britain. Mara had already led the territory's government as chief minister since 1967, and his British predecessors had prepared the transfer through a constitutional conference in London. His Alliance Party drew its strongest support from ethnic Fijian and European voters, while the opposition National Federation Party spoke for many Indo-Fijians. The 1970 constitution contained negotiated provisions meant to protect the political position of the indigenous Fijian population, a compromise that shaped every later dispute over the country's constitutional order.

The 1987 coups and the republic

The first major rupture came in 1987. Timoci Bavadra's Labour Party government took office on 13 April 1987 and lasted until 14 May 1987. Lieutenant Colonel Sitiveni Rabuka led a military takeover on 14 May, and a second coup followed on 25 September. Rabuka's stated aim was to secure indigenous Fijian control of government. The coups ended the monarchy: the Dominion's status was replaced by a republic proclaimed on 6 October 1987. Mara returned as prime minister in December 1987, and the 1970 constitution was abrogated. A 1990 constitution reserved the office of Prime Minister and a built-in majority in the House of Representatives for indigenous Fijians, which proved very unpopular with the Indo-Fijian community. The Commonwealth suspended Fiji for a decade, from 1987 to 1997.

The 1997 constitution and readmission

Under pressure over the 1990 document, the government agreed to rewrite it in the mid-1990s. In 1995, President Ratu Sir Kamisese Mara appointed a three-member Constitutional Review Commission. The resulting 1997 text ethnic Fijians agreed to give up their guaranteed majority in the House of Representatives and their monopoly on the Prime Minister's office, but in return, their ownership of most of the land was written into the constitution. The Great Council of Chiefs retained influence over the presidency and the Senate. Many of the commission's proposals on non-racial electoral rolls were later reversed by a parliamentary select committee, and Fiji was readmitted into the Commonwealth in 1997.

The 2000 and 2006 coups

The 1999 election was won by a coalition of Indo-Fijian-led parties, which made Mahendra Chaudhry Fiji's first Indo-Fijian prime minister. In May 2000, armed men led by the ethnic Fijian nationalist George Speight seized Parliament and held Chaudhry and most other MPs for 56 days. Mara resigned after meeting the coup leaders, and Commodore Frank Bainimarama then declared martial law and set aside the 1997 constitution. Speight was later convicted of treason, and he received a presidential pardon in September 2024. The Commonwealth suspended Fiji again in 2000 and 2001.

Tensions returned after the Qarase government introduced bills on land, qoliqoli fishing rights and reconciliation that critics saw as favouring ethnic Fijians. Bainimarama presented the government with a list of demands that included withdrawing the bills, and attempts at negotiation failed before the military launched a coup in early December. Qarase and his cabinet were removed, and Bainimarama reached an understanding with President Ratu Josefa Iloilo and reinstated him as president on 4 January 2007. Bainimarama justified the takeover as a means to "lead us into peace and prosperity and mend the ever widening racial divide". In 2009 the Court of Appeal ruled the military government illegal, and Iloilo then abrogated the 1997 constitution in April 2009. Fiji remained suspended from the Commonwealth until 2014.

Foreign responses and the return to parliamentary government

Regional and international reactions to the coups were consistently critical. Australia and New Zealand condemned the coup, and several international organizations imposed penalties on Fiji. Diplomatic isolation lasted for several years. Electoral rules were reformed in the 2010s, and the country's supporters of the military government argued that a new constitution would end ethnic voting. The restoration of parliamentary government came through a 2013 constitution and a 2014 election, after which Fiji was readmitted to the Commonwealth following the democratic election of Bainimarama.

Across these episodes, ethnic politics remained central. Analysts have observed that the 1987 and 2000 coups came after parties largely representing Indo-Fijians made electoral progress, gaining a role in government. Bainimarama's 2006 action was presented by its leader as a defence of multiculturalism against proposed changes that would have increased Indigenous Fijian privileges, and his government later abolished communal voting rolls. Assessments of these events differ, and the debate over power sharing, electoral design and the role of the chiefly system remains active in Fijian politics.

Constitutional System and the 2026 Election Cycle

Fiji is a parliamentary republic whose framework rests on the 2013 Constitution. Parliament has 55 seats, and 28 seats are needed for a majority. The next legislature will be the eighth Parliament elected under this constitution. The head of state is the President, and the process of calling an election begins with a writ. The writ of elections, a formal document issued by the President, signifies the dissolution of Parliament and the initiation of a general election. Once issued, the writ also opens candidate nominations, the campaign period and polling day (it sets in motion key events, including candidate nominations, campaign periods, and polling day.).

The 2022 election and the coalition government

The previous general election was held on 14 December 2022. Of the nine parties that contested the election, four passed the 5% threshold needed to enter parliament, but no party won a majority. FijiFirst won the largest number of seats, securing 26 seats, while the People's Alliance took 21 seats and its coalition partner, the National Federation Party, won five. SODELPA kept three seats. After several days of negotiation, SODELPA's management board voted to form a coalition government with the People's Alliance and the NFP. The resulting government was led by Prime Minister Sitiveni Rabuka, who remained in office at the time of the latest sources.

Timetable and the writ window

The constitutional deadline sets the outer limit for polling. Under the Constitution, polling must take place no later than 6 February 2027. Within that limit, the writ may be issued between late June and late December 2026. The Electoral Commission gave 24 June, 2026 as the earliest writ date, which would allow a first polling day on 7 August 2026, and 24 December, 2026 as the latest writ date, which would place polling on 6 February 2027. One report gives 26 June as the earliest writ date, so the exact start of the window should be checked against official notices. Prime Minister Rabuka has reportedly expected polling between late December 2026 and early February 2027, which would mean the writ would likely be issued between 10 November and 24 December. In practice, the window narrows to a six-week window between November and Christmas.

Parties and the campaign

The 2026 contest is expected to have the largest field of parties under the 2013 Constitution. Fiji's next general election will feature a record ten political parties — the highest number since the introduction of the 2013 Constitution. The tenth party, One Nation, was registered on 29 June 2026 after its application was resubmitted, bringing the number of political parties eligible to contest the next General Election to 10. For comparison, seven parties contested the 2014 election, six in 2018, and nine in 2022, alongside two independent candidates. Registration is governed by the Political Parties (Registration, Conduct, Funding and Disclosures) Act 2013, and new parties must gather a substantial number of signatures (5,000 valid signatures). The Electoral Commission has since officially declared the campaign period open.

Campaign finance reform

The campaign finance bill that had been awaiting passage has now become law. The Political Parties (Registration, Conduct, Funding and Disclosures) Amendment Bill 2026 was passed by Parliament on Thursday as part of a package of electoral reforms. Under the amended law, political parties will face a $4 million campaign spending cap, while candidates will be limited to $100,000 in campaign expenditure. The annual donation limit for Fijian citizens and former citizens is $20,000. The original draft had proposed a $3 million spending limit for political parties and $300,000 for individual candidates, so the caps were raised during parliamentary debate. Reports differ on donations from non-citizens. One account says the ban on donations from non-Fiji citizens and former Fiji citizens has been removed, with donations required to be declared, while another says that following committee consideration, that proposal was removed. Candidates must also disclose their campaign funding, and the law requires this within 60 days after polling day.

Local government elections

Municipal elections were scheduled separately from the national poll. Municipal elections will be held in September 2026 in Fiji to elect members of various town councils. They will be the first local elections in the country since 2005, and an earlier plan for 2023 was never carried out. 141 total councillors will be elected under the first past the post system, where the candidate with the most votes wins. Reports in mid-2026 raised the possibility of a delay to the municipal polls. Because the September date has now passed relative to the current date, the current status of these elections should be confirmed with the Fijian Elections Office and other official sources.

Economy and Key Sectors

Size and growth

Measured by output and industrial development, Fiji is regarded as the second-largest economy in the Pacific islands, and it also handles much of the region's re-exports. The World Bank describes Fiji as an upper-middle-income South Pacific island nation. Nominal GDP for 2025 is about US$6.2 billion, with GDP per capita near US$6,600 according to the World Bank's latest indicators. Other compilers give somewhat lower totals, with one estimate near US$5.7 billion for the same year (FocusEconomics), which reflects differences in revisions and currency conversion. Real output grew by an estimated 3.2 percent in 2025, a pace the IMF attributed to tourism inflows, remittances and fiscal stimulus (IMF Executive Board).

Tourism

Tourism is the economy's most visible engine. Fiji received 986,367 international visitors in 2025 (Travel And Tour World). The 2026 figures have been stronger still: March recorded 71,765 arrivals, up 12 percent year on year (Travel Weekly), and July became the first month to exceed 100,000 visitors, with 105,791 arrivals (Fiji Bureau of Statistics). August then recorded 99,963 arrivals, a monthly record for that month but only 0.2 percent above the previous year (Fiji Bureau of Statistics). Australia and New Zealand supply most visitors; in March they accounted for 43 and 17 percent of arrivals respectively (Travel Weekly). These numbers are provisional, and the IMF has warned that softer tourism demand, linked to higher oil prices, will weigh on 2026 growth (IMF Executive Board).

Remittances and external income

Money sent home by migrants is a second major source of foreign currency and household income. The World Bank's latest series puts personal remittances received at about 7.1 percent of GDP (World Bank). The IMF points to continued remittances as one of the main supports for activity, and it notes that diaspora transfers include earnings from Pacific labour mobility schemes (World Bank Macro Poverty Outlook).

Key sectors

The main industries listed for Fiji are tourism, sugar processing, clothing, copra, gold, silver and lumber (Economy of Fiji). Garment manufacturing and agriculture are considered core strengths, while bottled water and refined petroleum feature among the exports (GFMag). Sugar, long the colonial-era staple, remains an important agricultural product, though it no longer dominates export earnings as it once did. Agriculture is also the largest source of employment in the older official estimates: in 2011 it accounted for 44.2 percent of the labour force, against 41.6 percent in services and 14.3 percent in industry (Economy of Fiji). Fisheries and forestry contribute further income, and the fisheries sector is discussed in the marine section of this entry.

Macroeconomic outlook

The 2026 outlook has deteriorated since the start of the year. In March, IMF staff expected growth to moderate to about 2.5 percent and inflation to rise above 2 percent (IMF staff mission). In May, the IMF Executive Board projected real growth of 2.4 percent for 2026 and 3.0 percent by 2028 (IMF Executive Board). A later revision by Fiji's Macroeconomic Committee cut the 2026 forecast to 1.5 percent, down from 3.0 percent, as fuel and food costs rose (Fiji Times). Inflation rose to 3.9 percent in May after negative readings in 2025, and year-end inflation is now expected to exceed 6 percent (Islands Business).

Fiscal space is limited. The IMF stated that the budget passed the previous year leaves the government with very little room to handle unexpected needs for extra spending. Public debt has remained high, at around 79 percent of GDP in World Bank assessments (World Bank Macro Poverty Outlook). Downside risks include fiscal financing pressures, higher global fuel prices and the country's exposure to natural disasters.

Infrastructure, Transport and Energy

Air links centred on Nadi

Air travel is the main external link for an island state whose territory is spread across a very large sea area. Nadi International Airport lies at Namaka, about 10 km from Nadi town and 20 km from Lautoka, on the western side of Viti Levu. In 2019 the airport handled 2,485,319 passengers, of whom 2,166,584 were on international services. It handles about 97% of international visitors to Fiji.

Nadi is also the operating base of the national carrier. Fiji Airways, the flag carrier formerly known as Air Pacific, uses Nadi as its main hub, with Nausori International as a secondary hub. Its domestic and regional subsidiary, Fiji Link, is also based at Nadi. Nausori International serves the capital, Suva, and the Nadi–Suva route is one of the busiest Fiji Airways services from the western airport. Several foreign carriers, including Air New Zealand, Virgin Australia and Korean Air, also operate services into Nadi.

Ports, shipping and roads

Suva, on the south-eastern coast of Viti Levu, hosts the country's principal port and handles most cargo and passenger movements between the main islands and abroad. Inter-island vessels carry goods and people to outlying groups such as Lau, Lomaiviti and the Yasawa islands, and to Rotuma, where regular air and sea links are limited and weather-dependent. On Viti Levu, the coastal highway known as Queens Road links Suva with Nadi and Lautoka, while Vanua Levu has a smaller network that mainly connects its principal towns. Many rural communities depend on unsealed tracks, which become impassable after heavy rain. Tropical cyclones, such as Winston in 2016, have repeatedly damaged bridges, culverts and road surfaces, so maintenance costs are high and repairs can take a long time to complete.

Electricity generation and renewable targets

Electricity in Fiji is largely generated from renewable sources, but the mix is narrow. Of roughly 226 megawatts of renewable capacity, hydropower accounts for about 61 percent, bioenergy 29 percent, and solar and wind about five percent each. Earlier government figures give different shares: hydropower was described as the dominant renewable source at 54–55%, with bioenergy at about 16%. The discrepancy reflects differing reference years and methods. Because hydro output varies with seasonal rainfall, the country still depends heavily on imported fossil fuels, particularly when renewable generation falls.

Official goals aim for the entire power supply to come from renewable sources by 2036, with net-zero emissions by 2050. These goals are reflected in the national legal framework, which includes the Climate Change Act 2021. Solar development is still at an early stage. A prominent example is the Mua Solar Farm on Taveuni, which began operating in January 2025. The government has also launched pilot projects to convert organic waste into biogas and biofuels, aimed mainly at resorts and rural areas.

Several constraints slow the transition. Ageing infrastructure restricts how much new renewable generation the grid can absorb. Local technical expertise for large-scale deployment and grid modernisation is in short supply. According to an IRENA assessment prepared with the Department of Energy, outdated laws, slow approvals and weak institutional arrangements could delay projects and deter the private investors needed to reach national targets. Access figures also show a gap: the headline electricity access rate is about 98%, but the grid-connected population is roughly 90%, with the rest served by off-grid and mini-grid solutions.

Telecommunications and submarine cables

Fiji's international internet and telephone traffic depends mainly on undersea fibre-optic cables. The Southern Cross Cable Network is the major international submarine cable landing in Fiji, and it comes ashore at the Suva Cable Landing Station on Viti Levu. Fiji hosts one of the nine landing stations in this protected ring network, which also reaches Australia, New Zealand, Hawaii and the US mainland. A newer system, Southern Cross NEXT, has branching units that link Fiji with Tokelau and Kiribati. Fintel, Fiji's international gateway and wholesale telecommunications provider, has committed capacity to that cable.

Regional cables also terminate in Suva. The Tonga-Fiji cable connects Nuku'alofa with Suva and links to the Southern Cross system there. The Tui-Samoa cable connects Samoa with Fiji through a landing in Suva. Under a partnership with Google, the Fiji government has supported the Tabua cable, which is intended to connect Fiji directly with the United States and Australia. Fiji's history with international cables is long: its connection to international submarine cables across the Pacific dates back to 1902.

External Relations and Regional Cooperation

Multilateral memberships and the 2009 rupture

Fiji's multilateral portfolio includes the United Nations, the Commonwealth, the Forum Fisheries Agency, the Melanesian Spearhead Group and the World Health Organisation, and Fiji maintains diplomatic relations with more than 170 countries. Fiji is a member of many regional and international groups including Pacific Islands Forum, the Forum Fisheries Agency, The Commonwealth of Nations, the Melanesian Spearhead Group, the World Health Organisation and the United Nations. Fiji is a founding member of the Pacific Islands Forum, which was established in 1971.

That regional standing was disrupted in 2009. Regional isolation intensified in 2009 after Bainimarama failed to hold the elections he had promised, and the Forum and the Commonwealth responded by suspending Fiji. Excluded from the Forum, Fiji redirected its diplomacy. It expelled Australia's high commissioner in November 2009 and New Zealand's in 2010. It used its 2011-2013 chairmanship of the Melanesian Spearhead Group, a sub-regional organization which excludes Australia and New Zealand, to promote Fiji's particular policy priorities. Fiji also established the Pacific Islands Development Forum as a means of reclaiming its lost leadership on regional policies. In 2013 it became the first Pacific nation to hold the 12-month chairmanship of the Group of 77 plus China.

The isolation ended after the September 2014 elections, which were widely viewed as a step back toward democracy. In October 2014 Australia and New Zealand removed the final sanctions put in place against Fiji following the coup. Sanctions were also lifted by the United States, and the Commonwealth Ministerial Action Group and the Pacific Islands Forum Secretariat fully lifted Fiji's suspension from the Commonwealth and the Forum, respectively.

Bilateral relations with major partners

Australia and New Zealand remain Fiji's traditional partners, but Fiji sought to lessen its dependence on them after 2009. Fiji also sought out new international partners, such as China, to reduce its historical reliance on Australian aid. China became an important aid donor, and Fiji's earlier "Look North" orientation had broadened its diplomatic network. Since the early 2000s, Fiji has expanded its diplomatic relations to over 170 countries from the initial 'Look North' foreign policy. Defence ties with Australia were restored in 2014, when the Australian Government lifted all remaining restrictions and resumed its Defence Cooperation Program with Fiji. Fiji also has long-standing bilateral ties with India and Japan. With the United States, Fiji is an eligible beneficiary developing country under the Generalized System of Preferences (GSP), the largest and oldest U.S. trade preference program. Fiji became the 14th country to join the Indo-Pacific Economic Framework (IPEF) and the first Pacific Island country to do so.

Pacific climate diplomacy

Fiji's approach to climate change has given it a leading regional voice. Its stance on climate change has positioned it as a regional leader on a critical policy matter. Pacific states also pursued collective action at the United Nations. At the UN in New York they organised the Pacific Small Island Developing States Group, which owed nothing to Australia and New Zealand, and that grouping became, to a point where it replaced the PIF as the main representative of the Pacific voice at the UN. Fiji's presidency of the 2017 UN climate conference and the national adaptation work are discussed in the climate and natural hazards sections, while the shared Pacific position on sea-level rise and emissions is a central theme of that diplomacy.

Labour mobility

Labour mobility is one of the most economically significant external ties. The Australian Pacific Australia Labour Mobility scheme was formed when Australia consolidated the Seasonal Worker Programme (SWP) and the Pacific Labour Scheme (PLS) into a single program called the Pacific Australia Labour Mobility (PALM) scheme in July 2023. Under it, workers from Fiji and other Pacific Islands can work in Australia for periods of up to four years. There were 5,165 Fijians employed in Australia under the PALM scheme in November 2025, and remittances by Fijian PALM scheme workers were estimated at FJ$145.5 million in the period July 2024 to June 2025. Remittances are large relative to the economy: in 2021 they totalled nearly US$394 million or around 9.2% of GDP, and more than 60% of the funds originated from Australia, New Zealand and the United States. Critics have raised concerns about worker welfare and the loss of skilled workers, with the scheme having faced criticism for alleged worker exploitation and for its rate of deaths and injuries. Compared with its neighbours, Fiji's share of working-age people abroad is modest: temporary labour mobility accounts for 15 per cent of the working-age population in Tonga being overseas, 11 per cent in Vanuatu and 2 per cent in Fiji.

Trade relations

Fiji became a member of the World Trade Organization in January 1996 and accords at least m.f.n. tariff treatment to all its trading partners. Its regional arrangements include the Melanesian Spearhead Group, which grants market access to MSG member countries including Papua New Guinea, Solomon Islands, and Vanuatu. Fiji is also a party to the Pacific Island Countries Trade Agreement, a free trade agreement between the 14 Pacific Island Forum Countries. Access to Australian and New Zealand markets was historically organised under SPARTECA, and this scheme has since been replaced by the Developing Country Preference Scheme (DCPS) in 2015 in the case of Australia.

Trade with the European Union has been shaped by a long preference history. Sugar, which once accounted for roughly close to 40 per cent of exports, was largely sold into preferential markets, mainly in the EU. Fiji ratified the Economic Partnership Agreement (EPA) with the EU on trade in goods in 2014. Negotiations continue for a Comprehensive EPA to secure preferential access to the EU market for some Fiji exports (with a notable exception being sugar) and implementation of the EPA. Finally, Fiji has not ratified the PACER Plus agreement, a comprehensive regional development-centered free trade agreement between Australia, New Zealand, and nine Pacific Island countries.

Culture, Arts and Sport

Visual arts and crafts

Fijian visual arts are closely tied to ceremony and to the material life of villages. Masi, the bark cloth that is also called tapa, serves as ceremonial dress, wall decorations and table mats. Its production is shared with several other Pacific societies, and it has remained a living practice. The Ba-born artist Joana Monolagi, whose work is in the collection of Auckland Art Gallery, belongs to the Veiqia Project collective, and she received the Pacific Heritage Art Award in 2015 for work that also included supporting cultural events such as the Pasifika Festival. Woven mats, carved wooden objects and other handicrafts are sold at open-air markets, such as the one in Nadi, where visitors can buy handmade soaps and oils made from coconut and hibiscus alongside artworks.

Music and dance

The meke is the most visible form of performance. In Fijian the word covers all traditional song and dance, from graceful fan performances to athletic war dances. Dancers are normally accompanied by a seated group that sings, chants and plays percussion instruments [14-6]. Meke are typically performed during celebrations and festivals. Traditionally, men and women performed in separate groups, though outside influences, including the Tongan ma'ulu'ulu, have produced mixed-gender forms [17-4]. Meke also carried historical memory: in a society without writing, meke was the primary means by which Fijian communities preserved and transmitted their oral history.

Vocal string bands form another strand of musical life. Groups of three or more performers playing guitar, ukulele or mandolin and singing in multi-part harmony are popular across the islands. Their repertoire includes the sere ni cumu, social songs that accompanied beer- or kava-drinking gatherings from the 1920s onward, and that combined pre-European music styles with European melodies and harmonies [23-5].

Indo-Fijian music developed in parallel. Its most common devotional form, the bhajan, uses instruments such as the harmonium and the dholak [22-5], and qawwali has partly merged with it in Fiji because trained tabla players were scarce [22-6]. The most notable cross-community style is vude, which was pioneered by Laisa Vulakoro, using modern electronic instruments, as a relaxed fusion of country-and-western, reggae and rock 'n roll. Vude has also drawn on meke [20-15]. Scholars describe fusion between Indo-Fijian and indigenous Fijian music as extremely rare, yet in many ways a metaphor for attempts at racial reconciliation in Fiji.

Literature

Literature in English has become an important medium for reflecting on Fiji's multicultural society. Indo-Fijian writers such as Satendra Nandan have explored the history of the Indo-Fijian community and its place in the nation's identity, while writing in Fijian has developed alongside it, both shaping national discussions about history, belonging and identity.

Cuisine and feasting

Feasting is central to communal life, and the lovo is the most distinctive form. Indigenous Fijian feasts are cooked in a 'lovo', an underground earth oven heated by hot stones. The slow cook technique usually takes a couple of hours and gives food a light smokiness. Typical foods include yam, taro, kumala (sweet potato) and cassava (tapioca), as well as pork, chicken, fish or lamb. Coconut is equally important; in many dishes, meat and fish are marinated in coconut milk and spices before cooking. The national dish Kokoda is also widely served as a taste of Fijian heritage.

Rugby sevens and Olympic success

Rugby is the dominant sport. The Pacific island is obsessed with rugby, and particularly sevens, with official sources estimating that 10 percent of the population plays. Sevens has produced Fiji's greatest sporting achievements. At the Rio 2016 Olympics, Fiji defeated Great Britain 43-7 in the final of the first men's rugby sevens tournament, winning the nation's first-ever Olympic medal and becoming the first men's rugby Olympic gold medallists in 92 years. The victory prompted celebrations across the country, and the government announced a further day of public holiday. Fiji went on to retain the title at the Tokyo Games in 2021, beating New Zealand 27-12 in the final.

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