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Mofmanu Beach In Motusa, Rotuma
Motusa is a group of close villages in the district of Itu'tiu, on the island of Rotuma, one of the islands of Fiji. Rotuma is made up of two volcanic landmasses connected by a sandy isthmus, on which Motusa is located. For this reason it has one of the islands longest white sandy beach. Motusa also sits between the Islands two largest bay; Maka Bay to the North and Hapmafau Bay to the South. Motusa consists of the following places: * Ạilala *Agai Maftoa *Atapisi *Elsee *Elsio *Fagmạn *Farsạu *Fonmạn *Hamatua *Haroa *Islepi *Jumjumi *Leitunoa *Lum'ava *Malniu *Mofmanu *Tạnmohini *Tia *Tuifiriga *Salagvaka *Samoa *Uanheta *Upu Motusa also has a primary school known as Motusa District School, that consist of Year 1 to Year 8. Motusa is about one kilometer southwest of Ahau, the government station, which is also the location of the island's post office, and a small hospital. Ahau is now the administrative center of Rotuma, although for a long time Motusa, being the ...
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Mofmanu Beach In Motusa, Rotuma
Motusa is a group of close villages in the district of Itu'tiu, on the island of Rotuma, one of the islands of Fiji. Rotuma is made up of two volcanic landmasses connected by a sandy isthmus, on which Motusa is located. For this reason it has one of the islands longest white sandy beach. Motusa also sits between the Islands two largest bay; Maka Bay to the North and Hapmafau Bay to the South. Motusa consists of the following places: * Ạilala *Agai Maftoa *Atapisi *Elsee *Elsio *Fagmạn *Farsạu *Fonmạn *Hamatua *Haroa *Islepi *Jumjumi *Leitunoa *Lum'ava *Malniu *Mofmanu *Tạnmohini *Tia *Tuifiriga *Salagvaka *Samoa *Uanheta *Upu Motusa also has a primary school known as Motusa District School, that consist of Year 1 to Year 8. Motusa is about one kilometer southwest of Ahau, the government station, which is also the location of the island's post office, and a small hospital. Ahau is now the administrative center of Rotuma, although for a long time Motusa, being the ...
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Rotuma
Rotuma is a Fijian dependency, consisting of Rotuma Island and nearby islets. The island group is home to a large and unique Polynesian indigenous ethnic group which constitutes a recognisable minority within the population of Fiji, known as "Rotumans". Its population at the 2017 census was 1,594, although many more Rotumans live on mainland Fijian islands, totaling 10,000. Geography and geology The Rotuma group of volcanic islands are located (Suva to Ahau) north of Fiji. Rotuma Island itself is long and wide, with a land area of approximately , making it the 12th-largest of the Fiji islands. The island is bisected by an isthmus into a larger eastern part and a western peninsula. The isthmus is low and narrow, only wide, and is the site of Motusa village ( Itutiu district). North of the isthmus is Maka Bay, and in the south is Hapmafau Bay. There is a large population of coral reefs in these bays, and there are boat passages through them. Rotuma is a shield volcano m ...
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Fiji
Fiji ( , ,; fj, Viti, ; Fiji Hindi: फ़िजी, ''Fijī''), officially the Republic of Fiji, is an island country in Melanesia, part of Oceania in the South Pacific Ocean. It lies about north-northeast of New Zealand. Fiji consists of an archipelago of more than 330 islands—of which about 110 are permanently inhabited—and more than 500 islets, amounting to a total land area of about . The most outlying island group is Ono-i-Lau. About 87% of the total population of live on the two major islands, Viti Levu and Vanua Levu. About three-quarters of Fijians live on Viti Levu's coasts: either in the capital city of Suva; or in smaller urban centres such as Nadi—where tourism is the major local industry; or in Lautoka, where the Sugarcane, sugar-cane industry is dominant. The interior of Viti Levu is sparsely inhabited because of its terrain. The majority of Fiji's islands were formed by Volcano, volcanic activity starting around 150 million years ago. Some geo ...
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Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ...
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Isthmus
An isthmus (; ; ) is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. A tombolo is an isthmus that consists of a spit or bar, and a strait is the sea counterpart of an isthmus. Isthmus vs land bridge vs peninsula ''Isthmus'' and ''land bridge'' are related terms, with isthmus having a broader meaning. A land bridge is an isthmus connecting Earth's major landmasses. The term ''land bridge'' is usually used in biogeology to describe land connections that used to exist between continents at various times and were important for migration of people and various species of animals and plants, e.g. Beringia and Doggerland. An isthmus is a land connection between two bigger landmasses, while a peninsula is rather a land protrusion which is connected to a bigger landmass on one side only and surrounded by water on all other sides. Technically, an isthmus can have canals running from coast to coast (e.g. the Panama ...
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Mooring (watercraft)
A mooring is any permanent structure to which a vessel may be secured. Examples include quays, wharfs, jetties, piers, anchor buoys, and mooring buoys. A ship is secured to a mooring to forestall free movement of the ship on the water. An ''anchor mooring'' fixes a vessel's position relative to a point on the bottom of a waterway without connecting the vessel to shore. As a verb, ''mooring'' refers to the act of attaching a vessel to a mooring. The term likely stems from the Dutch verb ''meren'' (to ''moor''), used in English since the end of the 15th century. Permanent anchor mooring These moorings are used instead of temporary anchors because they have considerably more holding power, for example because of lesser damage to the marine environment, and are convenient. Where there is a row of moorings they are termed a tier. They are also occasionally used to hold floating docks in place. There are several kinds of moorings: Swing moorings Swing moorings also known a ...
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Wesleyan Theology
Wesleyan theology, otherwise known as Wesleyan– Arminian theology, or Methodist theology, is a theological tradition in Protestant Christianity based upon the ministry of the 18th-century evangelical reformer brothers John Wesley and Charles Wesley. More broadly it refers to the theological system inferred from the various sermons (e.g. the Forty-four Sermons), theological treatises, letters, journals, diaries, hymns, and other spiritual writings of the Wesleys and their contemporary coadjutors such as John William Fletcher. In 1736, the Wesley brothers travelled to the Georgia colony in America as Christian missionaries; they left rather disheartened at what they saw. Both of them subsequently had "religious experiences", especially John in 1738, being greatly influenced by the Moravian Christians. They began to organize a renewal movement within the Church of England to focus on personal faith and holiness. John Wesley took Protestant churches to task over the nature of s ...
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William Des Vœux
Sir George William Des Vœux (22 September 1834 – 15 December 1909) was a British colonial administrator who served as governor of Fiji (1880–1885), Newfoundland (1886–1887), and Hong Kong (1887–1891). Early life Des Vœux was born as the eighth of nine children of Reverend Henry Des Vœux (1786–1857) and his second wife Fanny Elizabeth Hutton in Baden-Baden, Germany, on 22 September 1834. His grandfather was Irish politician Sir Charles des Voeux, 1st Baronet.im Thurn, E. F.; Milne, Lynn, rev. "Des Vœux, Sir (George) William". ''Oxford Dictionary of National Biography'' (2004 ed.). Oxford University Press. . Retrieved 9 May 2020. His great-grandfather was a Huguenot from Normandy, France, who settled in Ireland in the early 18th century. Des Vœux attended a public school in London before starting his studies at Charterhouse School (1845–1853) and Balliol College, Oxford (1854–1856), but left without a degree after his father gave him the choice of finishing h ...
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