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Vanua Levu has a number of rivers, including the Labasa, the Wailevu, and the Qawa. These three form a delta on which the town of Labasa stands. None of the island's rivers are navigable by large vessels. There are also many well known rivers on Vanua levu. The first is the most dangerous, the Wainikoro river, known for its shark attacks.
The Vanua Levu Group is an archipelago in northern Fiji. It takes its name from its predominant island, Vanua Levu. Among the other island in the group, the most important is Taveuni. Other islands in the group include Laucala, Matagi, Namena Lala, Qamea, Rabi, Vorovoro and Yadua Tabu.
Levuka, 1842 Fijian ship, 1842 Fijian house, 1842. Dutch explorer Abel Tasman was the first known European visitor to Fiji, sighting the northern island of Vanua Levu and the North Taveuni archipelago in 1643 while looking for Terra Australis incognita, or the Great Southern Continent. [15]
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Qelelevu may have been first inhabited by people from Futuna.Later in time, people from Laucala arrived and soon dominated the population. [6] Qelelevu has been in the Laucala sphere of influence, as well as other islands like Naitauba, Namalata, Yacata and villages of Vutuna, Daliconi and Mavana on Vanua Balavu.
Cakaudrove (Fijian pronunciation: [ðaˈkɔuɳɖʳove]) is one of fourteen provinces of Fiji, and one of three based principally on the northern island of Vanua Levu, occupying the south-eastern third of the island and including the nearby islands of Taveuni, Rabi, Kioa, and numerous other islands in the Vanua Levu Group.
In 1804, the discovery of sandalwood on the southwestern coast of Vanua Levu led to an increase in the number and frequency of Western trading ships visiting Fiji. A sandalwood rush began in the first few years but it dried up when supplies dropped between 1810 and 1814.
Fiji has more than 300 islands. Viti Levu and Vanua Levu are the largest, and together comprise 78% of Fiji's land area. The highest peak in Fiji is Mount Tomanivi (1,324 m) on Viti Levu. The islands are volcanic in origin, formed by the subduction of the Pacific Plate under the Australian Plate. The islands emerged from the sea 5 to 20 million ...