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Ndoi Island
Ono-i-Lau is a group of islands within a barrier reef system in the Fijian archipelago of Lau Islands (''ono'' means "six" in the Fijian language). There are four central volcanic islands: Onolevu, Doi (or Ndoi) Lovoni and Ndavura, the uppermost parts of the volcanic edifice rising from the Lau Ridge slightly more than below sea level and on which the reef and other islands are built. There are also three clusters of coral limestone islets, Yanuya (50 islets) and Mana (46 islets) on the barrier reef and Niuta (7 tiny islets). A sand cay, Udui, is not counted as one of the six “islands”. The group forms one of the southernmost of the Lau Islands; it is located at 20.80° South and 178.75° West, and occupies an area of . It has a maximum elevation of . It is south-southwest of Vatoa, the nearest largish island; the only land further south in the Lau Group is in the two small Tuvana islands of coral limestone and sand. There are four villages in the group – Nukuni and Lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ono I LauISS002-E-9864
ONO, Ono or Ōno may refer to: Places Fiji * Ono Island (Fiji) Israel * Kiryat Ono * Ono, Benjamin, ancient site Italy * Ono San Pietro Ivory Coast * Ono, Ivory Coast, a village in Comoé District Japan * Ōno Castle, Fukuoka * Ōno District, Fukui * Ōno District, Gifu * Ōno District, Ōita * Ōno, Chita District, Aichi * Ōno, Fukui * Ono, Fukushima * Ōno, Gifu * Ōno, Hiroshima * Ōno, Hokkaidō * Ono, Hyōgo * Ōno, Ibaraki * Ōno, Iwate * Ōno, Ōita * Ōno River, in Ōita Prefecture United States * Ono Island (Alabama) * Ono, Kentucky * Ono, Pennsylvania * Ono, Wisconsin People and language * Ono (surname), including a list of people bearing the name *Ono language ONO * The FAA identifier of Ontario Municipal Airport in Ontario, Oregon * Organization of News Ombudsmen (ONO) * ONO (Spain), a Spanish cable company ** ONO Estadi, a football stadium in Mallorca, Spain, named for the cable company * ONO, the name Yoko Ono uses for releasing remixes of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barrier Reef
A coral reef is an underwater ecosystem characterized by reef-building corals. Reefs are formed of colonies of coral polyps held together by calcium carbonate. Most coral reefs are built from stony corals, whose polyps cluster in groups. Coral belongs to the class Anthozoa in the animal phylum Cnidaria, which includes sea anemones and jellyfish. Unlike sea anemones, corals secrete hard carbonate exoskeletons that support and protect the coral. Most reefs grow best in warm, shallow, clear, sunny and agitated water. Coral reefs first appeared 485 million years ago, at the dawn of the Early Ordovician, displacing the microbial and sponge reefs of the Cambrian. Sometimes called ''rainforests of the sea'', shallow coral reefs form some of Earth's most diverse ecosystems. They occupy less than 0.1% of the world's ocean area, about half the area of France, yet they provide a home for at least 25% of all marine species, including fish, mollusks, worms, crustaceans, echino ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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 volcanic activity starting around 150 million years ago. Some geothermal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lau Islands
The Lau Islands aka little Tonga (also called the Lau Group, the Eastern Group, the Eastern Archipelago) of Fiji are situated in the southern Pacific Ocean, just east of the Koro Sea. Of this chain of about sixty islands and islets, about thirty are inhabited. The Lau Group covers a land area of 188 square miles (487 square km), and had a population of 10,683 at the most recent census in 2007. While most of the northern Lau Group are high islands of volcanic origin, those of the south are mostly carbonate low islands. Administratively the islands belong to Lau Province. History The British explorer James Cook reached Vatoa in 1774. By the time of the discovery of the Ono Group in 1820, the Lau archipelago was the most mapped area of Fiji. Political unity came late to the Lau Islands. Historically, they comprised three territories: the Northern Lau Islands, the Southern Lau Islands, and the Moala Islands. Around 1855, the renegade Tongan prince Enele Ma'afu co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fijian Language
Fijian (') is an Austronesian language of the Malayo-Polynesian family spoken by some 350,000–450,000 ethnic Fijians as a native language. The 2013 Constitution established Fijian as an official language of Fiji, along with English and Fiji Hindi and there is discussion about establishing it as the "national language". Fijian is a VOS language. Standard Fijian is based on the speech of Bau, which is an East Fijian language. A pidginized form is used by many Indo-Fijians and Chinese on the islands, while Pidgin Hindustani is used by many rural ethnic Fijians and Chinese in areas dominated by Indo-Fijians. History Phonology The consonant phonemes of Fijian are as shown in the following table: The consonant written has been described as a prenasalized trill or trilled affricate . However, it is only rarely pronounced with a trilled release; the primary feature distinguishing it from is that it is postalveolar, , rather than dental/alveolar. The sounds a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 pla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, mountain glaciers and the polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlement and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coral
Corals are marine invertebrates within the class Anthozoa of the phylum Cnidaria. They typically form compact colonies of many identical individual polyps. Coral species include the important reef builders that inhabit tropical oceans and secrete calcium carbonate to form a hard skeleton. A coral "group" is a colony of very many genetically identical polyps. Each polyp is a sac-like animal typically only a few millimeters in diameter and a few centimeters in height. A set of tentacles surround a central mouth opening. Each polyp excretes an exoskeleton near the base. Over many generations, the colony thus creates a skeleton characteristic of the species which can measure up to several meters in size. Individual colonies grow by asexual reproduction of polyps. Corals also breed sexually by spawning: polyps of the same species release gametes simultaneously overnight, often around a full moon. Fertilized eggs form planulae, a mobile early form of the coral polyp which, whe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vatoa
Vatoa (pronounced ) (known as Turtle Island after Cook's visit) is an outlier of Fiji's Lau Group. History Vatoa was the only island of present-day Fiji visited by James Cook. The island was sighted on 2 July 1774. The next day, a Sunday, the Master and some of Cook's crew went ashore: Cook's chart shows the name Turtle Isle. Geography Vatoa has varied rainfall and is usually cool because of trade winds. The island has an area of and rises to more than above sea level. It is composed wholly of limestone (Koroqara Limestone, Tokalau Limestone Group), probably Late Miocene The Late Miocene (also known as Upper Miocene) is a sub-epoch of the Miocene Epoch made up of two stages. The Tortonian and Messinian stages comprise the Late Miocene sub-epoch, which lasted from 11.63 Ma (million years ago) to 5.333 Ma. The ... in age. A single village has a population around 300. Interesting old fortifications occupy the highest part of the island. Government Viliame Naupoto, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fijians
Fijians ( fj, iTaukei, lit=Owners (of the land)) are a nation and ethnic group native to Fiji, who speak Fijian and share a common history and culture. Fijians, or ''iTaukei'', are the major indigenous people of the Fiji Islands, and live in an area informally called Melanesia. Indigenous Fijians are believed to have arrived in Fiji from western Melanesia approximately 3,500 years ago, though the exact origins of the Fijian people are unknown. Later they would move onward to other surrounding islands, including Rotuma, as well as blending with other (Polynesian) settlers on Tonga and Samoa. They are indigenous to all parts of Fiji except the island of Rotuma. The original settlers are now called "Lapita people" after a distinctive pottery produced locally. Lapita pottery was found in the area from 800 BCE onward. As of 2005, indigenous Fijians constituted slightly more than half of the total Fijian population. Indigenous Fijians are predominantly of Melanesian extrac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
