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Kisar Island
Kisar, also known as ''Yotowawa'', is a small island in the Southwestern Moluccas in Indonesia, located to the northeast of Timor Island. Most of the island is included within the Southernmost Islands District ('' Kecamatan Pulau Pulau Terselatan'') within the Southwest Islands Regency of Maluku Province. The District previously also includes the larger (but less populated) Romang Island further north, but this with its own outliers was subsequently split off to form its own district (''Kecamatan Kepulauan Romang''). The rest of the island forms the North Kisar District (''Kecamatan Kisar Utara'') within the regency. It is one of the 92 officially listed outlying islands of Indonesia. The principal town is Wonreli, with 6,652 inhabitants at the 2010 Census. Geography, geology and ecology Kisar is similar geographically and geologically to the nearby islands of Timor, Leti, and Moa. The interior of the island is hilly, with several small mountains lined roughly east–west. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maluku Islands
The Maluku Islands (; Indonesian: ''Kepulauan Maluku'') or the Moluccas () are an archipelago in the east of Indonesia. Tectonically they are located on the Halmahera Plate within the Molucca Sea Collision Zone. Geographically they are located east of Sulawesi, west of New Guinea, and north and east of Timor. Lying within Wallacea (mostly east of the biogeographical Weber Line), the Maluku Islands have been considered as a geographical and cultural intersection of Asia and Oceania. The islands were known as the Spice Islands because of the nutmeg, mace and cloves that were exclusively found there, the presence of which sparked colonial interest from Europe in the sixteenth century. The Maluku Islands formed a single province from Indonesian independence until 1999, when it was split into two provinces. A new province, North Maluku, incorporates the area between Morotai and Sula, with the arc of islands from Buru and Seram to Wetar remaining within the existing Maluku Province. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibolite
Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance. Amphibolite frequently forms by metamorphism of mafic igneous rocks, such as basalt. However, because metamorphism creates minerals entirely based upon the chemistry of the protolith, certain 'dirty marls' and volcanic sediments may also metamorphose to an amphibolite assemblage. Deposits containing dolomite and siderite also readily yield amphibolite (tremolite-schist, grunerite-schist, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses. Metamorphosed basalt (metabasalt) creates ''ortho-amphibolite'' and other chemically appropriate lithologies create ''para-amphibolite''. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vereenigde Oost-Indische Compagnie
The United East India Company ( nl, Verenigde Oostindische Compagnie, the VOC) was a chartered company established on the 20th March 1602 by the States General of the Netherlands amalgamating existing companies into the first joint-stock company in the world, granting it a 21-year monopoly to carry out trade activities in Asia. Shares in the company could be bought by any resident of the United Provinces and then subsequently bought and sold in open-air secondary markets (one of which became the Amsterdam Stock Exchange). It is sometimes considered to have been the first multinational corporation. It was a powerful company, possessing quasi-governmental powers, including the ability to wage war, imprison and execute convicts, negotiate treaties, strike its own coins, and establish colonies. They are also known for their international slave trade. Statistically, the VOC eclipsed all of its rivals in the Asia trade. Between 1602 and 1796 the VOC sent almost a million Eur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fataluku
Fataluku (also known as Dagaga, Dagoda', Dagada) is a Papuan language spoken by approximately 37,000 people of Fataluku ethnicity in the eastern areas of East Timor, especially around Lospalos. It is a member of the Timor-Alor-Pantar language family, which includes languages spoken both in East Timor and nearby regions of Indonesia. Fataluku's closest relative is Oirata, spoken on Kisar island, in the Moluccas of Indonesia. Fataluku is given the status of a national language under the constitution. Speakers of Fataluku normally have a command of Tetum and/or Indonesian. It has a considerable amount of Austronesian loanwords, and it has borrowed elements of Sanskrit and Arabic vocabulary via Malay. Phonology Vowels Consonants *¹ Spelled in Nácher orthography. *² Pronunciation of and varies in dialects. Words and phrases In the examples below, the letter 'c' and the letter combination 'tx' are pronounced as the 'ch' in the English word 'church'. Rau ana kapare? / ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oirata Language
Oirata or Woirata (also known as Maaro) is a Timor–Alor–Pantar language spoken on the island of Kisar in Indonesia, and by some people in Ambon. ''Ethnologue'' reports an SIL figure of 1,200 speakers from 1987. It is closely related to Fataluku Fataluku (also known as Dagaga, Dagoda', Dagada) is a Papuan language spoken by approximately 37,000 people of Fataluku ethnicity in the eastern areas of East Timor, especially around Lospalos. It is a member of the Timor-Alor-Pantar language fa ..., of which it is sometimes considered to be a dialect. Phonology Vowels Oirata has five vowels: Consonants Oirata has 13 consonants: References External links Oirata Wordlist at the Austronesian Basic Vocabulary DatabaseWoirata Maro (Oirata People) film {{West Trans–New Guinea languages Languages of Indonesia Oirata–Makasai languages ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kisar Language
Kisar is a Central Malayo-Polynesian language spoken on Kisar Island, northeast of East Timor in Maluku, Indonesia. It shares the island with Oirata, which is a Papuan language The Papuan languages are the non- Austronesian and non-Australian languages spoken on the western Pacific island of New Guinea in Indonesia and Papua New Guinea, as well as neighbouring islands, by around 4 million people. It is a strictly geogra .... References Further reading * Taber, Mark (1993).Toward a Better Understanding of the Indigenous Languages of Southwestern Maluku" ''Oceanic Linguistics'', Vol. 32, No. 2 (Winter, 1993), pp. 389–441. University of Hawai'i. Timor–Babar languages Languages of Indonesia {{Au-lang-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Timor Monitor
''Varanus timorensis'', the Timor monitor or spotted tree monitor, is a species of small monitor lizards native to the island of Timor and some adjacent islands. Taxonomy Kimberley rock monitors (''Varanus glauerti''), banded tree monitors (''Varanus scalaris''), and spotted tree monitors (''Varanus similis'') were once considered subspecies of the Timor monitor, but have since been elevated to full species status. Currently, the peacock monitor (''Varanus auffenbergi'') is sometimes considered a subspecies, but is usually considered its own species. Description The Timor monitor is a dwarf species of monitor lizard belonging to the subgenus '' Odatria''. Generally, it is dark greenish-gray to almost black in background color, with bright gold-yellow or sometimes bluish spotting along its dorsal surface and a lighter straw-yellow color on its ventral side. It has a pointed snout, excellent eyesight and hearing, sharp teeth, and a prehensile tail that measures two-thirds of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Banda Arc
The Banda Arc (main arc, Inner, and Outer) is a set of island arcs in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active arc is located on what appears to be oceanic crust whereas the associated subduction trench is underlain by continental crust. The convergence of the Indo-Australian plates and Eurasia resulted in the formation of the Sunda and Banda island arcs. The transitional zone between the arcs is located south of Flores Island and is characterized by the change in the tectonic regime along the boundary. Terminology Some academic literature refers to the arcs by location – so that main arc can be referred to as the 'southern', the 'western' Situated at the centre of three converging and colliding major tectonic plates, Indo-Australia, Eurasia, Pacific, the Banda arc includes young oceanic crust enclosed by a volcanic inner arc, outer arc islands and a trough parallel to the Australian contine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inner Banda Arc
The Banda Arc (main arc, Inner, and Outer) is a set of island arcs in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active arc is located on what appears to be oceanic crust whereas the associated subduction trench is underlain by continental crust. The convergence of the Indo-Australian plates and Eurasia resulted in the formation of the Sunda and Banda island arcs. The transitional zone between the arcs is located south of Flores Island and is characterized by the change in the tectonic regime along the boundary. Terminology Some academic literature refers to the arcs by location – so that main arc can be referred to as the 'southern', the 'western' Situated at the centre of three converging and colliding major tectonic plates, Indo-Australia, Eurasia, Pacific, the Banda arc includes young oceanic crust enclosed by a volcanic inner arc, outer arc islands and a trough parallel to the Australian contin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outer Banda Arc
The Banda Arc (main arc, Inner, and Outer) is a set of island arcs in eastern Indonesia. It is the result of the collision of a continent and an intra-oceanic island arc. The presently active arc is located on what appears to be oceanic crust whereas the associated subduction trench is underlain by continental crust. The convergence of the Indo-Australian plates and Eurasia resulted in the formation of the Sunda and Banda island arcs. The transitional zone between the arcs is located south of Flores Island and is characterized by the change in the tectonic regime along the boundary. Terminology Some academic literature refers to the arcs by location – so that main arc can be referred to as the 'southern', the 'western' Situated at the centre of three converging and colliding major tectonic plates, Indo-Australia, Eurasia, Pacific, the Banda arc includes young oceanic crust enclosed by a volcanic inner arc, outer arc islands and a trough parallel to the Australian continen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geochemistry
Geochemistry is the science that uses the tools and principles of chemistry to explain the mechanisms behind major geological systems such as the Earth's crust and its oceans. The realm of geochemistry extends beyond the Earth, encompassing the entire Solar System, and has made important contributions to the understanding of a number of processes including mantle convection, the formation of planets and the origins of granite and basalt. It is an integrated field of chemistry and geology. History The term ''geochemistry'' was first used by the Swiss-German chemist Christian Friedrich Schönbein in 1838: "a comparative geochemistry ought to be launched, before geognosy can become geology, and before the mystery of the genesis of our planets and their inorganic matter may be revealed." However, for the rest of the century the more common term was "chemical geology", and there was little contact between geologists and chemists. Geochemistry emerged as a separate discipline after ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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