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Geography of Fiji

Continent	Pacific Ocean
Region	Oceania
Coordinates	18°00′S 179°00′E / 18.000°S 179.000°E / -18.000; 179.000
Area	Ranked 151st
• Total	18,272 km (7,055 sq mi)
• Land	100%
• Water	0%
Coastline	1,129 km (702 mi)
Borders	None
Highest point	Mount Tomanivi 1,324 metres (4,344 ft)
Lowest point	Pacific Ocean 0 m
Exclusive economic zone	1,282,978 km (495,361 sq mi)

Fiji is a group of volcanic islands in the South Pacific, lying about 4,450 kilometres (2,765 mi) southwest of Honolulu and 1,770 km (1,100 mi) north of New Zealand. Of the 332 islands and 522 smaller islets making up the archipelago, about 106 are permanently inhabited. The total land size is 18,272 km (7,055 sq mi). It has the 26th largest Exclusive Economic Zone of 1,282,978 km (495,361 sq mi).

Viti Levu, the largest island, covers about 57% of the nation's land area, hosts the two official cities (the capital Suva, and Lautoka) and most other major towns, such as Nausori, Vaileka, Ba, Tavua, Kororvou, Nasinu, and Nadi (the site of the international airport), and contains some 69% of the population. Vanua Levu, 64 km (40 mi) to the northeast of Viti Levu, covers just over 30% of the land area though is home to only some 15% of the population. Its main towns are Labasa and Savusavu. In the northeast it features Natewa Bay, carving out the Loa peninsula.

Both islands are mountainous, with peaks up to 1,300 m (4,300 ft) rising abruptly from the shore, and covered with tropical forests. 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.

Other islands and island groups, which cover just 12.5% of the land area and house some 16% of the population, include Taveuni southeast off Vanua Levu and Kadavu Island, south off Viti Levu (the third and fourth largest islands respectively), the Mamanuca Group (just off Nadi) and Yasawa Group (to the north of the Mamanucas), which are popular tourist destinations, the Lomaiviti Group (just off Suva) with Levuka, the former capital and the only major town on any of the smaller islands, located on the island of Ovalau, and the remote Lau Group over the Koro Sea to the east near Tonga, from which it is separated by the Lakeba Passage.

Two outlying regions are Rotuma, 400 km (250 mi) to the north, and the uninhabited coral atoll and cay Ceva-i-Ra or Conway Reef, 450 km (280 mi) to the southwest of main Fiji. Culturally conservative Rotuma with its 2,000 people on 44 km (17 sq mi) geographically belongs to Polynesia, and enjoys relative autonomy as a Fijian dependency.

Fiji Television reported on 21 September 2006 that the Fiji Islands Maritime and Safety Administration (FIMSA), while reviewing its outdated maritime charts, had discovered the possibility that more islands could lie within Fiji's Exclusive Economic Zone.

More than half of Fiji's population lives on the island coasts, either in Suva or in smaller urban centers. The interior is sparsely populated because of its rough terrain.

Statistics

Location

Oceania, island group in the South Pacific Ocean; geographic coordinates:

18°00′S 179°00′E / 18.000°S 179.000°E / -18.000; 179.000

Map references

Oceania

Area

• Total: 18,274 km (7,056 sq mi)
• Land: 18,274 km (7,056 sq mi)
• Water: 0 km (0 sq mi)

Area – comparative

Slightly smaller than New Jersey; slightly less than one third Nova Scotia's size; slightly smaller than Wales

Land boundaries

0 km (0 mi)

Coastline

1,120 km (700 mi)

Maritime claims

• Measured from claimed archipelagic baselines
• Territorial sea: 12 nautical miles (22 km; 14 mi)
• Exclusive economic zone: 1,282,978 km (495,361 sq mi). 200 nmi (370 km; 230 mi)
• Continental shelf: 200 m (660 ft) depth or to the depth of exploitation; rectilinear shelf claim added

Terrain

• Mostly mountains of volcanic origin, beaches
• A recent global remote sensing analysis suggested that there were 438 km of tidal flats in Fiji, making it the 49th ranked country in terms of tidal flat area.

Elevation extremes

• Lowest point: Pacific Ocean 0 km (0 mi)
• Highest point: Mount Tomanivi 1,324 metres (4,344 ft)

Natural resources

Timber, fish, gold, copper, offshore oil potential, hydropower

Land use

• Arable land: 9.03%
• Permanent crops: 4.65%
• Other: 86.32% (2011)

Irrigated land

30 km (12 sq mi) (2003)

Total renewable water resources

28.55 km (6.85 cu mi) (2011)

Freshwater withdrawal (domestic/industrial/agricultural)

• total: 0.08 km/a (0.019 cu mi/a) (30%/11%/59%)
• per capita: 100.1 m/a (130.9 cu yd/a) (2005)

Natural hazards

Cyclonic storms can occur from November to January

Environment – current issues

Deforestation; soil erosion

Environment – international agreements

• Party to: biodiversity, climate change-Kyoto Protocol, desertification, endangered species, law of the sea, marine life conservation, ozone layer protection, Tropical Timber 83, Tropical Timber 94, wetlands
• Signed, but not ratified: None of the selected agreements

Geography – note

Includes 322 islands and islets of which approximately 110 are inhabited

Climate

Fiji has a tropical rainforest climate and a tropical monsoon climate (Af and Am according to the Köppen climate classification). Suva, the capital city, receives more rainfall than Nadi or the other side of Viti Levu. El Niño and La Niña events have significant impacts on rainfall. Tropical cyclones can impact Fiji and in some cases they can cause severe damage and many deaths. In 2016, Cyclone Winston caused widespread destruction and affected hundreds of thousands of people after striking Fiji. A few years later, Cyclone Harold also caused widespread damage.

Climate change in Fiji is an exceptionally pressing issue for the country – as an island nation, Fiji is particularly vulnerable to rising sea levels, coastal erosion and extreme weather. These changes, along with temperature rise, will displace Fijian communities and will prove disruptive to the national economy – tourism, agriculture and fisheries, the largest contributors to the nation's GDP, will be severely impacted by climate change causing increases in poverty and food insecurity. As a party to both the Kyoto Protocol and the Paris Climate Agreement, Fiji hopes to achieve net-zero emissions by 2050 which, along with national policies, will help to mitigate the impacts of climate change.

Tectonics

Fiji is located on the northeast corner of the Indo-Australian plate near where it subducts under the Pacific plate on the North Fiji Basin microplate between the North Fiji Fracture Zone on the north and the Hunter fracture zone on the south. It is part of the Ring of Fire, the string of volcanoes around the boundary of the Pacific Ocean.

Extreme points

This is a list of the extreme points of Fiji, the points that are farther north, south, east or west than any other location.

• Northernmost point – Uea Island, Rotuma, Eastern Division
• Easternmost point – Vatoa Island, Eastern Division
• Southernmost point – Ceva-i-Ra island, Western Division
• Westernmost point – Viwa Island, Western Division

Ecology

Fiji has more than three hundred islands, four of which are of a significant size. From largest to smallest, these four islands are Viti Levu, Vanua Levu, Kadavu Island, and Taveuni Island. The Fiji islands are home to numerous indigenous flora and fauna. These include:

• Fiji banded iguana
• Fiji crested iguana

Fiji once hosted several now-extinct Pleistocene and Holocene species, including a large crocodilian of the genus Volia, which was likely the apex predator of its environment. Other notable extinct species include Lapitiguana impensa, a giant iguana, as well as the flightless Viti Levu giant pigeon.

References

1. "Fiji". CIA World Factbook. CIA. Retrieved 28 December 2014.
2. Fiji. SOPAC – Applied Geoscience and Technology Division
3. Murray, N.J.; Phinn, S.R.; DeWitt, M.; Ferrari, R.; Johnston, R.; Lyons, M.B.; Clinton, N.; Thau, D.; Fuller, R.A. (2019). "The global distribution and trajectory of tidal flats". Nature. 565 (7738): 222–225. doi:10.1038/s41586-018-0805-8. PMID 30568300. S2CID 56481043.
4. Fiji Sugarcane Climate Outlook from May 2021 Planting & Harvesting Season (PDF) (Report). Fiji Meteorological Service. p. 5. Retrieved 18 August 2022.
5. Republic of Fiji: Third National Communication Report to the United Nations Framework Convention on Climate Change (PDF) (Report). United Nations Framework Convention on Climate Change. 27 April 2020. p. 62. Retrieved 18 August 2022.
6. Yeo, Stephen W; Blong, Russell J (2010). "Fiji's worst natural disaster: the 1931 hurricane and flood". Disasters. 34 (3): 657–683. doi:10.1111/j.1467-7717.2010.01163.x. PMID 20298265.
7. Nadia Khomami (21 February 2016). "Cyclone Winston: Fiji counts deaths and damage from giant storm". The Guardian. Retrieved 21 February 2016.
8. Fiji: Severe Tropical Cyclone Winston Situation Report No. 8 (as of 28 February 2016) (PDF). United Nations Office for the Coordination of Humanitarian Affairs (Report). ReliefWeb. 28 February 2016. Retrieved 28 February 2016.
9. "Pacific Humanitarian Team - Tropical Cyclone Harold Situation Report #9, 21 April 2020" (PDF). 22 April 2020. Retrieved 22 April 2020.
10. ^ COP23. "How Fiji is Affected by Climate Change". Cop23. Archived from the original on 28 August 2022. Retrieved 5 September 2022.{{cite web}}: CS1 maint: numeric names: authors list (link)
11. UN Climate Change News (5 March 2019). "Fiji Submits Long-Term National Climate Plan". unfccc.int. United Nations Framework Convention on Climate Change. Retrieved 17 July 2021.
12. "Nandi Climate Normals 1961–1990". National Oceanic and Atmospheric Administration. Retrieved 24 March 2015.
13. "Klimatafel von Nandi (Int. Flugh.) / Viti Levu / Fidschi" (PDF). Baseline climate means (1961–1990) from stations all over the world (in German). Deutscher Wetterdienst. Retrieved 22 November 2016.
14. Patrick Maillet, Etienne Ruellan, Martine Gérard, Alain Person, Hervé Bellon, Joseph Cotten, Jean-Louis Joron, Setsuya Nakada, and Richard C.Price (9 October 1995). Tectonics, Magmatism, and Evolution of the New Hebrides Backarc Troughs (Southwest Pacific). Plenum Press. CiteSeerX 10.1.1.604.4184.{{cite book}}: CS1 maint: multiple names: authors list (link)

 This article incorporates public domain material from The World Factbook. CIA.

• Geography of Fiji