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Makian
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 has had infrequent, but violent eruptions that destroyed villages o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Maluku
North Maluku ( id, Maluku Utara) is a province of Indonesia. It covers the northern part of the Maluku Islands, bordering the Pacific Ocean to the north, the Halmahera Sea to the east, the Molucca Sea to the west, and the Seram Sea to the south. The provincial capital is Sofifi on the largest island of Halmahera, while the largest city is the island city of Ternate. The population of North Maluku was 1,038,087 in the 2010 census,Central Bureau of Statistics: ''Census 2010'' , retrieved 17 January 2011 making it one of the least-populous provinces in Indonesia, but by the 2020 Census the population had risen to 1,282,937, and the official estimate as at mid 2021 was 1,299,177. North Maluku was originally the centre of the four largest Islamic sultanates in the eastern Indonesian archi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halmahera
Halmahera, formerly known as Jilolo, Gilolo, or Jailolo, is the largest island in the Maluku Islands. It is part of the North Maluku province of Indonesia, and Sofifi, the capital of the province, is located on the west coast of the island. Halmahera has a land area of ; it is the largest island of Indonesia outside the five main islands. It had a population of 162,728 in 1995; by 2010, it had increased to 449,938 for the island itself (excluding the tip which is considered part of the Joronga Islands, but including Gebe and Ju islands) and 667,161 for the island group (including all of South Halmahera and Tidore, but not Ternate). Approximately half of the island's inhabitants are Muslim and half are Christian. History Sparsely-populated Halmahera's fortunes have long been closely tied to those of the smaller islands of Ternate and Tidore, both off its west coast. These islands were both the sites of major kingdoms in the era before Dutch East India Company colonized the e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moti Island
Moti or Motir is a volcanic island in the western side of Halmahera island, Indonesia. While administratively part of the city of Ternate, it is situated between the islands of Tidore to its north and Makian to its south. The 5 km wide island is surrounded by coral reefs. Its summit is truncated and the volcano contains a crater at the south-west side. Moti has an area of 24.78 km2 and had a population of 4,811 at the 2020 Census;Badan Pusat Statistik, Jakarta, 2021. it is governed as the district (''kecamatan'') of Moti within the City ('' kota'') of Ternate. See also * 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 globa ... References Stratovolcanoes of Indonesia Volcanoes of Halmahera Mountains of Indonesia Ternate Islands of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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 plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
