Makian Island
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Makian Island
Makian (also Machian), known to local people as Mount Kie Besi, is a volcanic island, one of the Maluku Islands within the province of North Maluku in Indonesia. It lies near the southern end of a chain of volcanic islands off the western coast of the province's major island, Halmahera, and lies between the islands of Moti and Tidore to the north and Kayoa and the Bacan Group to the south. The island, which forms two districts (''Pulau Makian'' and ''Makian Barat'') within South Halmahera Regency of North Maluku Province, covers an area of 84.36 sq.km, and had a population of 12,394 at the 2010 Census, which rose to 14,000 at the 2020 Census. The island is wide, and its high summit consists of a large wide crater, with a small lake on its Northeast side. There are four parasitic cones on the western slopes of Makian. Makian volcano is also known as Mount Kiebesi (or Kie Besi). Volcanic history Makian volcano A volcano is a rupture in the crust of a planetary-mass obj ...
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Southeast Asia
Southeast Asia, also spelled South East Asia and South-East Asia, and also known as Southeastern Asia, South-eastern Asia or SEA, is the geographical United Nations geoscheme for Asia#South-eastern Asia, south-eastern region of Asia, consisting of the regions that are situated south of mainland China, east of the Indian subcontinent, and north-west of mainland Australia. Southeast Asia is bordered to the north by East Asia, to the west by South Asia and the Bay of Bengal, to the east by Oceania and the Pacific Ocean, and to the south by Australia (continent), Australia and the Indian Ocean. Apart from the British Indian Ocean Territory and two out of atolls of Maldives, 26 atolls of Maldives in South Asia, Maritime Southeast Asia is the only other subregion of Asia that lies partly within the Southern Hemisphere. Mainland Southeast Asia is completely in the Northern Hemisphere. East Timor and the southern portion of Indonesia are the only parts that are south of the Equator. Th ...
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South Halmahera Regency
South Halmahera Regency ( id, Kabupaten Halmahera Selatan) is a regency of North Maluku Province, Indonesia. It lies partly on Halmahera Island and partly on smaller islands to the west and south of Halmahera. It covers a land area of 8,779.320 km2, and at the 2010 Census it had a population of 198,911 people, while the 2020 Census showed that this had risen to 248,395 and the official estimate in mid 2021 was 251,690. The capital lies at the town of Labuha on Bacan Island. Islands Besides the southern part of Halmahera Island, the regency includes a number of archipelagoes and islands. These comprise: * Obi Islands, including Obira (main), Bisa, Obilatu and other small islands, comprising in all five ''kecamatan'' with 51,510 people in mid 2021. * Bacan Islands, including: ** Bacan Island itself, comprising 7 ''kecamatan'' with 84,011 people (in mid 2021) ** Bacan Lomang Island, comprising 1 ''kecamatan'' with 7,735 people ** Mandioli, comprising 2 ''kecamatan'' with 10,843 ...
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List Of Volcanoes In Indonesia
The geography of Indonesia is dominated by volcanoes that are formed due to subduction zones between the Eurasian plate and the Indo-Australian plate. Some of the volcanoes are notable for their eruptions, for instance, Krakatoa for its global effects in 1883, the Lake Toba Caldera for its supervolcanic eruption estimated to have occurred 74,000 years before present which was responsible for six years of volcanic winter, and Mount Tambora for the most violent eruption in recorded history in 1815. Volcanoes in Indonesia are part of the Pacific Ring of Fire. The 150 entries in the list below are grouped into six geographical regions, four of which belong to the volcanoes of the Sunda Arc trench system. The remaining two groups are volcanoes of Halmahera, including its surrounding volcanic islands, and volcanoes of Sulawesi and the Sangihe Islands. The latter group is in one volcanic arc together with the Philippine volcanoes. The most active volcano is Mount Merapi on Java. ...
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West Makian Language
West Makian (also known by the endonym MoiKlamer, Marian; Ger Reesink; and Miriam van Staden. 2008. East Nusantara as a Linguistic Area. In Pieter Muysken (ed.), ''From linguistic areas to areal linguistics'', 95-149. Amsterdam: John Benjamins.) is a divergent North Halmahera language of Indonesia. It is spoken on the coast near Makian Island, and on the western half of that island. West Makian has been strongly influenced by a neighboring Austronesian language or languages to the extent that it was once classified as Austronesian, as East Makian (Taba) still is. As a family-level isolate, it is not closely related to any other language. A brief description of the language can be found in Voorhoeve (1982). Much influence comes from Taba, as well as Malay, Ternate, Dutch, and potentially Portuguese. Phonology Vowels West Makian has 5 or 6 vowels: /a, e, ə, i, o/, and /u/, with /ə/ not recorded by Watuseke. Voorhoeve states that /ə/ is only found in Indonesian loans. ...
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Taba Language
Taba (also known as East Makian or Makian Dalam) is a Malayo-Polynesian language of the South Halmahera–West New Guinea group. It is spoken mostly on the islands of Makian, Kayoa and southern Halmahera in North Maluku province of Indonesia by about 20,000 people. Dialects There are minor differences in dialect between all of the villages on Makian island in which Taba is spoken. Most differences affect only a few words. One of the most widespread reflexes is the use of /o/ in Waikyon and Waigitang, where in other villages /a/ is retained from Proto-South Halmaheran.Bowden 2001, p. 190 Geographic distribution As of 2005, Ethnologue lists Taba as having a speaking population of approximately 20,000, however, it has been argued by linguists that this number could in reality be anywhere between 20,000 and 50,000. The language is predominantly spoken on Eastern Makian island, although it is also found on Southern Mori island, Kayoa islands, Bacan and Obi island and along the west ...
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Eruption
Several types of volcanic eruptions—during which lava, tephra (ash, lapilli, volcanic bombs and volcanic blocks), and assorted gases are expelled from a volcanic vent or fissure—have been distinguished by volcanologists. These are often named after famous volcanoes where that type of behavior has been observed. Some volcanoes may exhibit only one characteristic type of eruption during a period of activity, while others may display an entire sequence of types all in one eruptive series. There are three different types of eruptions: * Magmatic eruptions are the most well-observed type of eruption. They involve the decompression of gas within magma that propels it forward. * Phreatic eruptions are driven by the superheating of steam due to the close proximity of magma. This type exhibits no magmatic release, instead causing the granulation of existing rock. * Phreatomagmatic eruptions are driven by the direct interaction of magma and water, as opposed to phreatic erupti ...
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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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Parasitic Cone
A parasitic cone (also adventive cone or satellite cone) is the cone-shaped accumulation of volcanic material not part of the central vent of a volcano. It forms from eruptions from fractures on the flank of the volcano. These fractures occur because the flank of the volcano is unstable. Eventually, the fractures reach the magma chamber and generate eruptions called flank eruptions, which, in turn, produce a parasitic cone. A parasitic cone can also be formed from a dike or sill cutting up to the surface from the central magma chamber in an area different from the central vent. A peculiar example of multiple parasitic cones is Jeju Island in South Korea. Jeju features 368 " oreums" (; "mount"), which lie in a roughly lateral line on either side of the island's central dormant shield volcano Hallasan. See also *Flank crater A volcanic crater is an approximately circular depression in the ground caused by volcanic activity. It is typically a bowl-shaped feature containing ...
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Bacan
The Bacan Islands, formerly also known as the Bachans, Bachians, and Batchians, are a group of islands in the Moluccas in Indonesia. They are mountainous and forested, lying south of Ternate and southwest of Halmahera. The islands are administered by the South Halmahera Regency of North Maluku Province. They formerly constituted the Sultanate of Bacan. Bacan ( nl, Batjan), formerly also known as Bachian or Batchian, is the group's largest island. The second and third-largest islands are Kasiruta and Mandioli. Bacan Island in 2020 included about 82,387 people, of which about 10,000 live in the capital Labuha; it is subdivided into seven districts. Kasiruta and Mandioli each have over 10,000 inhabitants, and each is subdivided into two districts. A fourth island, Bacan Lomang, forms a twelfth district within the group. There are dozens of smaller islands in the group, which had a total population of 84,075 at the 2010 Census, but by the 2020 Census had risen to 111,517. The offic ...
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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. ...
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Kayoa
Kayoa (also Kaioa), or in the native language Pulau Urimatiti, is a group of 66 islands, part of the Maluku Islands. It is located in South Halmahera Regency, part of North Maluku Province of Indonesia. Geography The Kayoa Islands are near the southern end of a chain of volcanic islands off the western coast of Halmaherato (Halmahera region), to the south of Makian and to the north of Bacan. The 66 islands cover a land area of 179.97 km2. The main island is about 10 miles (16 km) long, about 9 miles (14.5 km) south of Makian with a line of hills along most of its length. The group forms four districts within South Halmahera Regency (although Kayoa Barat District - comprising Muari Island and 4 smaller islands - is actually closer to the Bacan Islands than to Kayoa Island), and it had a total population of 20,176 at the 2010 Census and 23,111 at the 2020 Census. The official estimate for mid 2021 was 23,226. The islands were for centuries the only place in the world ...
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