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[[File:Vitilevu topo.jpg|250px|right|Viti levu]]
[[File:Vitilevu topo.jpg|250px|right|Viti levu]]
E dua na [[yanuyanu]] mai [[Viti]].


E dua '''Viti Levu''' (pronounced {{IPA-fj|ˈβitʃi ˈleβu|}}) sai koya na [[yanuyanu]] levu duadua ena loma ni vanua o [[Viti]], na vanua e tiko kina na mata ni matanitu, e [[Suva]], kei na itikotiko vei ira e vuqa sara na lewe levu ni iwiliwili nei Viti.

== Geology ==
Fiji lies in a [[plate tectonics|tectonically complex area]] between the [[Australian Plate]] and the [[Pacific Plate]]. The Fiji Platform lies in a zone bordered with active extension fault lines around which most of the shallow earthquakes were centered. These fault lines are the Fiji Fracture Zone (FFZ) to the north, the [[Spreading ridge|176° Extension Zone]] (176°E EZ) to the west, and the Hunter Fracture Zone (HFZ) and Lau Ridge to the east.<ref name="Greenbaum">{{cite web|url=http://eird.org/deslizamientos/pdf/eng/doc8455/doc8455-2a.pdf|title=Landslide hazards in Fiji|last=Greenbaum|first=D.|author2=Bowker, M. R|author3=Dau, I|author4=Drospy, H|author5=Greally, K. B|author6=McDonald A. J. W|author7=Marsh, S. H|author8=Northmore, K. J|author9=O'Connor, E. A|author10=Prasad, R. S|author11=Tragheim, D. G.|last-author-amp=yes|year=1995|work=Technical Report WC/95/28 Rapid methods of landslide hazard mapping : Fiji case study|publisher=British Geological Survey|accessdate=23 March 2011}}</ref>

The oldest rocks on the island consist of the [[Eocene]] to [[Lower Miocene]] Wainimala [[Group (geology)|Group]]. The Lower portion of the Group are composed of [[volcanic]] flows and volcanoclastics, which grade from [[basalt]] to [[trachyte]] and [[rhyolite]]. Geographically, this group is found south of [[Nadi]], including the peaks of Koromba (3528’) and Natambumgguto (1242’), down to [[Sigatoka]]. From Sigatoka, the Group extends almost all the way to Lodoni, and includes the peaks of Tuvutau (3060’) and Tikituru (3071’), while along the southern coast it extends almost to [[Nausori]]. The Group is [[intruded]] by the Tholo [[pluton|Plutonics]] consisting of similar age [[stock (geology)|stocks]] of [[tonalite]], [[granodiorite]], [[gabbro]] and [[diorite]]. [[Miocene|Mio]]-[[Pliocene]] [[sandstone]]s and [[marl]], grading into epiclastics and [[andesite|andesitic]] volcanics of the Suva Group are found mainly in the river valleys such as those formed by the [[Nadi River]] and [[Navua River]]. The Plio-[[Pleistocene]] Mba Grouop is found on the northern portion of the island and consists of [[porphyritic]] basalt flows and volcanoclastics grading into [[greywacke]]. Geographically it includes the peaks of Koroyanitu (3921’), Malua (3294’), Monavatu (3708’), [[Mount Tomanivi]] (4341’), and Ndelamendamu (2540’), and extends along the eastern coast almost to Nausori. It also includes the Emperor Mine near [[Vatukoula]].<ref>{{cite book |title=Provisional Geologic Map of Fiji |date=1965 |publisher=Fiji Geological Survey |location=Suva}}</ref><ref>{{cite journal |last1=Rodda |first1=P. |title=Outline of the geology of Viti Levu |journal=New Zealand Journal of Geology and Geophysics |date=1967 |volume=10 |issue=5 |pages=1260–1273 |doi=10.1080/00288306.1967.10420217|doi-access=free }}</ref>

== Geography and economy ==
[[File:Vitilevu topo.jpg|thumb|left|300px|Topography of Viti Levu island.]]
Viti Levu is the largest island in the nation, home to 70% of the population (about 600,000), and is the hub of the entire Fijian archipelago. It measures {{convert|146|km}} long and {{convert|106|km}} wide, and has an area of {{convert|10389|km²}}. [[1953 Suva earthquake|Earthquakes]] and volcanic eruptions account for the somewhat rugged terrain of the island, which is divided into roughly equal halves by a north-south mountain range. The centre of the island is forested and includes the nation's highest peak [[Mount Tomanivi]] (otherwise Mount Victoria) rising to {{convert|1324|m}}.

The eastern side of the island experiences heavy rainfall, while the western side (colloquially called the "burning west") is noticeably drier in the range's [[rain shadow]]. Accordingly, [[sugar cane]] production thrives in the west, while a [[dairy]] industry is being built in the east. {{Citation needed|date=September 2016}} Fiji's biggest cattle ranch is at Yaqara, with 7000 head of cattle on its {{convert|70|km²|acre}}, located halfway between [[Tavua, Fiji|Tavua]] and [[Rakiraki District, Fiji|Rakiraki]]. The island is the only known home of one of the world's largest insects, the [[Giant Fijian long-horned beetle]].

== Localities ==
[[File:Korotogo.jpg|thumb|Korotogo beach, Coral Coast.]]
[[File:Navala.jpg|thumb|The highland village of [[Navala]].]]
Viti Levu hosts the capital city of [[Suva]], and is home to nearly three quarters of the population of the Republic (about 580,000). Other important towns, all around the coast, include [[Ba (town)|Ba]], [[Lautoka]], [[Nadi, Fiji|Nadi]], [[Nausori]], Rakiraki, and [[Sigatoka]]. One major road has been built around the perimeter of Viti Levu. Well-known localities include [[Natadola Beach]], [[Pacific Harbour]] (a resort center about 50 kilometers from Suva).

== Politics ==
Eight of Fiji's fourteen [[Local government in Fiji|Provinces]] are in Viti Levu. The Provinces of [[Ba Province|Ba]], [[Nadroga-Navosa Province|Nadroga-Navosa]], and [[Ra Province|Ra]] comprise the [[Western Division, Fiji|Western Division]], while [[Naitasiri Province|Naitasiri]], [[Namosi Province|Namosi]], [[Rewa Province|Rewa]], [[Serua Province|Serua]], and [[Tailevu Province|Tailevu]] form the [[Central Division, Fiji|Central Division]]. In part because of its high concentration of [[Indians in Fiji|Indo-Fijians]], whose ancestors came mostly as indentured workers from [[India]] between 1879 and 1916, the political dynamics of western Viti Levu are somewhat different from those of eastern Viti Levu, where, apart from the multi-racial urban areas, [[Fijians|indigenous Fijians]] are more heavily concentrated.

== History ==
Viti Levu is believed to have been inhabited longer than the northern island of [[Vanua Levu]]. According to oral traditions, the first [[Melanesia]]n settlers landed at [[Vuda Point]] and established [[Viseisei]], believed to be Fiji's oldest settlement, although archaeologists refute this claim.

==Other==
The Canadian entrepreneur [[Peter Munk]] named his [[Klosters]] house after the island, as Viti Levu was where he and [[David Gilmour (businessman)|David Gilmour]] started the [[Southern Pacific Hotel]] chain in the 1960s.<ref>"Peter Munk: A mining magnate nears the end of his golden reign" ERIC REGULY. [[The Globe and Mail]] 15 March 2014</ref>

==Veitikina==
{{reflist}}

{{commons|Viti Levu}}
{{Viti Levu}}
{{Viti Levu}}
{{Islands of Fiji}}
{{Islands of Fiji}}


[[Category:Viti Levu]]
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[[Category:Viti Levu| ]]
[[Category:{{SIL|Islands of Fiji}}]]
[[Category:{{SIL|Islands of Fiji}}]]

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Latest revision as of 23:15, 4 Okosita 2021

Viti levu
Viti levu

E dua Viti Levu (pronounced [ˈβitʃi ˈleβu]) sai koya na yanuyanu levu duadua ena loma ni vanua o Viti, na vanua e tiko kina na mata ni matanitu, e Suva, kei na itikotiko vei ira e vuqa sara na lewe levu ni iwiliwili nei Viti.

Geology[veisau | edit source]

Fiji lies in a tectonically complex area between the Australian Plate and the Pacific Plate. The Fiji Platform lies in a zone bordered with active extension fault lines around which most of the shallow earthquakes were centered. These fault lines are the Fiji Fracture Zone (FFZ) to the north, the 176° Extension Zone (176°E EZ) to the west, and the Hunter Fracture Zone (HFZ) and Lau Ridge to the east.[1]

The oldest rocks on the island consist of the Eocene to Lower Miocene Wainimala Group. The Lower portion of the Group are composed of volcanic flows and volcanoclastics, which grade from basalt to trachyte and rhyolite. Geographically, this group is found south of Nadi, including the peaks of Koromba (3528’) and Natambumgguto (1242’), down to Sigatoka. From Sigatoka, the Group extends almost all the way to Lodoni, and includes the peaks of Tuvutau (3060’) and Tikituru (3071’), while along the southern coast it extends almost to Nausori. The Group is intruded by the Tholo Plutonics consisting of similar age stocks of tonalite, granodiorite, gabbro and diorite. Mio-Pliocene sandstones and marl, grading into epiclastics and andesitic volcanics of the Suva Group are found mainly in the river valleys such as those formed by the Nadi River and Navua River. The Plio-Pleistocene Mba Grouop is found on the northern portion of the island and consists of porphyritic basalt flows and volcanoclastics grading into greywacke. Geographically it includes the peaks of Koroyanitu (3921’), Malua (3294’), Monavatu (3708’), Mount Tomanivi (4341’), and Ndelamendamu (2540’), and extends along the eastern coast almost to Nausori. It also includes the Emperor Mine near Vatukoula.[2][3]

Geography and economy[veisau | edit source]

Topography of Viti Levu island.

Viti Levu is the largest island in the nation, home to 70% of the population (about 600,000), and is the hub of the entire Fijian archipelago. 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). Earthquakes and volcanic eruptions account for the somewhat rugged terrain of the island, which is divided into roughly equal halves by a north-south mountain range. The centre of the island is forested and includes the nation's highest peak Mount Tomanivi (otherwise Mount Victoria) rising to 1,324 metres (4,344 ft).

The eastern side of the island experiences heavy rainfall, while the western side (colloquially called the "burning west") is noticeably drier in the range's rain shadow. Accordingly, sugar cane production thrives in the west, while a dairy industry is being built in the east. [citation needed] Fiji's biggest cattle ranch is at Yaqara, with 7000 head of cattle on its 70 square kilometres (17,000 acres), located halfway between Tavua and Rakiraki. The island is the only known home of one of the world's largest insects, the Giant Fijian long-horned beetle.

Localities[veisau | edit source]

Korotogo beach, Coral Coast.
The highland village of Navala.

Viti Levu hosts the capital city of Suva, and is home to nearly three quarters of the population of the Republic (about 580,000). Other important towns, all around the coast, include Ba, Lautoka, Nadi, Nausori, Rakiraki, and Sigatoka. One major road has been built around the perimeter of Viti Levu. Well-known localities include Natadola Beach, Pacific Harbour (a resort center about 50 kilometers from Suva).

Politics[veisau | edit source]

Eight of Fiji's fourteen Provinces are in Viti Levu. The Provinces of Ba, Nadroga-Navosa, and Ra comprise the Western Division, while Naitasiri, Namosi, Rewa, Serua, and Tailevu form the Central Division. In part because of its high concentration of Indo-Fijians, whose ancestors came mostly as indentured workers from India between 1879 and 1916, the political dynamics of western Viti Levu are somewhat different from those of eastern Viti Levu, where, apart from the multi-racial urban areas, indigenous Fijians are more heavily concentrated.

History[veisau | edit source]

Viti Levu is believed to have been inhabited longer than the northern island of Vanua Levu. According to oral traditions, the first Melanesian settlers landed at Vuda Point and established Viseisei, believed to be Fiji's oldest settlement, although archaeologists refute this claim.

Other[veisau | edit source]

The Canadian entrepreneur Peter Munk named his Klosters house after the island, as Viti Levu was where he and David Gilmour started the Southern Pacific Hotel chain in the 1960s.[4]

Veitikina[veisau | edit source]

  1. Greenbaum, D.; Bowker, M. R; Dau, I; Drospy, H; Greally, K. B; McDonald A. J. W; Marsh, S. H; Northmore, K. J; O'Connor, E. A; Prasad, R. S & Tragheim, D. G. (1995). "Landslide hazards in Fiji" (PDF). Technical Report WC/95/28 Rapid methods of landslide hazard mapping : Fiji case study. British Geological Survey. Retrieved 23 March 2011.
  2. Provisional Geologic Map of Fiji. Suva: Fiji Geological Survey. 1965.
  3. Rodda, P. (1967). "Outline of the geology of Viti Levu". New Zealand Journal of Geology and Geophysics. 10 (5): 1260–1273. doi:10.1080/00288306.1967.10420217.
  4. "Peter Munk: A mining magnate nears the end of his golden reign" ERIC REGULY. The Globe and Mail 15 March 2014