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Santa Cruz Islands
The Santa Cruz Islands form an archipelago in Temotu Province, Solomon Islands. They lie approximately to the southeast of the Solomon Islands (archipelago), Solomon Islands archipelago, just north of the archipelago of Vanuatu and are considered part of the Vanuatu rain forests ecoregion. The term Santa Cruz Islands is sometimes used to encompass all the islands of Temotu Province, Solomon Islands. Geography The largest island is Nendo Island, Nendö, which is also known as Santa Cruz Island proper. Lata, Solomon Islands, Lata, located on Nendö, is the largest town, and is the capital of Temotu Province. Other islands belonging to the Santa Cruz group are Vanikoro (which is actually made up of two islands, Banie (island), Banie and its small neighbour Teanu (island), Teanu) and Utupua. The table below provides basic data on these three islands. The Santa Cruz Islands are less than five million years old and were pushed upward by the Plate tectonics, tectonic subduction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Map Of The Santa Cruz Islands (Solomon Islands)
A map is a symbolic depiction of interrelationships, commonly spatial, between things within a space. A map may be annotated with text and graphics. Like any graphic, a map may be fixed to paper or other durable media, or may be displayed on a transitory medium such as a computer screen. Some maps change interactively. Although maps are commonly used to depict geographic elements, they may represent any space, real or fictional. The subject being mapped may be two-dimensional such as Earth's surface, three-dimensional such as Earth's interior, or from an abstract space of any dimension. Maps of geographic territory have a very long tradition and have existed from ancient times. The word "map" comes from the , wherein ''mappa'' meant 'napkin' or 'cloth' and ''mundi'' 'of the world'. Thus, "map" became a shortened term referring to a flat representation of Earth's surface. History Maps have been one of the most important human inventions for millennia, allowing humans t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Puma (village)
Puma is the only inhabited village of the island of Teanu, in the Vanikoro group located in the Solomon Islands Solomon Islands, also known simply as the Solomons,John Prados, ''Islands of Destiny'', Dutton Caliber, 2012, p,20 and passim is an island country consisting of six major islands and over 1000 smaller islands in Melanesia, part of Oceania, t .... The language spoken there has been sometimes referred to as ''Puma'' (or wrongly ''Buma''), and is now known as Teanu. References External links Maps of Vanikoro, showing location of Puma on Teanu island Satellite photo of Puma village Populated places in Temotu Province {{SolomonIslands-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gerd Koch
Gerd Koch (11 July 1922 – 19 April 2005) was a German cultural anthropologist best known for his studies on the material culture of Kiribati, Tuvalu and the Santa Cruz Islands in the Pacific. He was associated with the Ethnological Museum of Berlin (; until 1999 ''Museum für Völkerkunde''). His field work was directed to researching and recording the use of artefacts in their indigenous context, to begin to understand these societies. His work in cultural and social anthropology extended to researching and recording the music and dance of the Pacific Islands. He collaborated with Dieter Christensen, a music-ethnologist, on ''The Music of the Ellice Islands'' (German: ''Die Musik der Ellice-Inseln'') (1964) and Koch also published the ''Songs of Tuvalu'' (translated by Guy Slatter) (2000). In Tuvalu he was also known as 'Keti'. Biography As a child Gerd Koch was fascinated by accounts of explorers including the Pacific voyages of James Cook. After he completed his s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polynesian Outliers
Polynesian is the adjectival form of Polynesia. It may refer to: * Polynesians, an ethnic group * Polynesian culture, the culture of the indigenous peoples of Polynesia * Polynesian mythology, the oral traditions of the people of Polynesia * Polynesian languages, a language family spoken in geographical Polynesia and on a patchwork of outliers Other * Polynesian (horse), an American Thoroughbred racehorse and sire * Polynesian Leaders Group, an international governmental cooperation group * Polynesian Triangle, a region of the Pacific Ocean with three island groups at its corners * ''The Polynesian ''The Polynesian'' was a 4-8 page weekly newspaper published in Honolulu, that had two periods of publication: from June 6, 1840, to December 11, 1841, and then from May 18, 1844, to February 6, 1864. From 1845 to 1861, it was the official publicat ...'', a Honolulu-based newspaper published in the mid-nineteenth century See also * {{disambiguation Language and nationality disambi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tepukei
:nl: tepukei A tepukei, tepuke or TePuke is a Polynesian boat type, characterized by its elaborate decking, its submerged hulls and symmetrical "crab claw" sail slender foil or radically extended tips claw sail (Te Laa). ''Tepukei'' boats are produced primarily by the Polynesian-speaking inhabitants of Taumako (Duff Islands), and have been occasionally borrowed by other Polynesian and Melanesian societies. Name The word comes from the phrase ''te puke'' in Vaeakau-Taumako and other Polynesian languages. Removing the noun article , the original meaning of ''puke'' , as reconstructed for the ancestor Proto-Polynesian is “bow and stern decking on a canoe”.Entry ''puke'' in ''Pollex'' (the Comparative Polynesian Lexicon). By |
Austronesian Languages
The Austronesian languages ( ) are a language family widely spoken throughout Maritime Southeast Asia, parts of Mainland Southeast Asia, Madagascar, the islands of the Pacific Ocean and Taiwan (by Taiwanese indigenous peoples). They are spoken by about 328 million people (4.4% of the world population). This makes it the fifth-largest language family by number of speakers. Major Austronesian languages include Malay (around 250–270 million in Indonesia alone in its own literary standard named " Indonesian"), Javanese, Sundanese, Tagalog (standardized as Filipino), Malagasy and Cebuano. According to some estimates, the family contains 1,257 languages, which is the second most of any language family. In 1706, the Dutch scholar Adriaan Reland first observed similarities between the languages spoken in the Malay Archipelago and by peoples on islands in the Pacific Ocean. In the 19th century, researchers (e.g. Wilhelm von Humboldt, Herman van der Tuuk) started to apply the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oceanic Languages
The approximately 450 Oceanic languages are a branch of the Austronesian languages. The area occupied by speakers of these languages includes Polynesia, as well as much of Melanesia and Micronesia. Though covering a vast area, Oceanic languages are spoken by only two million people. The largest individual Oceanic languages are Eastern Fijian with over 600,000 speakers, and Samoan with an estimated 400,000 speakers. The Gilbertese (Kiribati), Tongan, Tahitian, Māori and Tolai (Gazelle Peninsula) languages each have over 100,000 speakers. The common ancestor which is reconstructed for this group of languages is called Proto-Oceanic (abbr. "POc"). Classification The Oceanic languages were first shown to be a language family by Sidney Herbert Ray in 1896 and, besides Malayo-Polynesian, they are the only established large branch of Austronesian languages. Grammatically, they have been strongly influenced by the Papuan languages of northern New Guinea, but they retain a rema ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reef Islands – Santa Cruz Languages
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic (non-living) processes such as deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite near to the surface, but not all definitions require this ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Ash
Volcanic ash consists of fragments of rock, mineral crystals, and volcanic glass, produced during volcanic eruptions and measuring less than 2 mm (0.079 inches) in diameter. The term volcanic ash is also often loosely used to refer to all explosive eruption products (correctly referred to as '' tephra''), including particles larger than 2 mm. Volcanic ash is formed during explosive volcanic eruptions when dissolved gases in magma expand and escape violently into the atmosphere. The force of the gases shatters the magma and propels it into the atmosphere where it solidifies into fragments of volcanic rock and glass. Ash is also produced when magma comes into contact with water during phreatomagmatic eruptions, causing the water to explosively flash to steam leading to shattering of magma. Once in the air, ash is transported by wind up to thousands of kilometres away. Due to its wide dispersal, ash can have a number of impacts on society, including animal a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
