Hokkaidō Komagatake
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Hokkaidō Komagatake
, also , , or just is a andesitic stratovolcano on the border between Mori, Shikabe, and Nanae, all within the Oshima Subprefecture of Hokkaidō, Japan. Occurrence of volcanic activity started some 30,000 years ago. Following roughly 5,000 years of dormancy, volcanic activity at Mount Koma-ga-take restarted at the start of the 17th century, triggering the Kan'ei Great Famine The Kan'ei Great Famine ( ') was a famine which affected Japan during the reign of Empress Meishō in the Edo period. The estimated number of deaths due to starvation is between 50,000 and 100,000. The famine is generally considered to have begun in ... in 1640. Since then, there have been at least 50 recorded volcanic events at Mount Koma-ga-take.神沼克伊,小山悦郎 ''日本の火山を科学する 日本列島津々浦々、あなたの身近にある108の活火山とは?'' ソフトバンククリエイティブ 2011. . File:Hokkaido-Komagatake Relief Map, SRTM-1.jpg, Relief Map File:Red ho ...
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List Of Mountains And Hills Of Japan By Height
The following is a list of the mountains and hills of Japan, ordered by height. Mountains over 1000 meters Mountains under 1000 meters As the generally accepted definition of a mountain (versus a hill) is 1000 m of height and 500 m of prominence, the following list is provided for convenience only. See also * List of Japanese prefectures by highest mountain References External links Mt. Nakanodake:Hiking route|Snow Country* * Japan 100 Mountains {{DEFAULTSORT:List Of Mountains And Hills Of Japan By Height Mountains of Japan Height Height is measure of vertical distance, either vertical extent (how "tall" something or someone is) or vertical position (how "high" a point is). For example, "The height of that building is 50 m" or "The height of an airplane in-flight is abou ...
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Mori, Hokkaidō
is a town located in Oshima Subprefecture, Hokkaido, Japan. The total area of the town is . As of September 2016, the town had a population of 16,299, and a population density of 44 persons per km2. Mount Komagatake, an active volcano, is located to the east of Mori, and much of the town is part of Ōnuma Quasi-National Park. Mori is the home of ikameshi, a squid and rice dish invented in the mid-20th century. Etymology The name of the town originates from the word "Oniushi", meaning "a forested area" in the Ainu language. In the Japanese language the name of the town is written as , meaning ''forest''. The suffix "", denoting town status in Japan, is pronounced as ''-chō'' in every municipality of Hokkaido with the exception of Mori, where it is read as ''-machi''. Geography Mori sits on the eastern coast of the Oshima Peninsula and overlooks Uchiura Bay ( in diameter). The bay, also known as Funka Bay, is rich in squid and is the site of scallop aquaculture, both a mains ...
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Pleistocene Stratovolcanoes
The Pleistocene ( , often referred to as the ''Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the two reg ...
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Mountains Of Hokkaido
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Volcanoes Of Hokkaido
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 pa ...
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Kan'ei Great Famine
The Kan'ei Great Famine ( ') was a famine which affected Japan during the reign of Empress Meishō in the Edo period. The estimated number of deaths due to starvation is between 50,000 and 100,000. The famine is generally considered to have begun in 1640 and lasted into 1643. It was named after the Kan'ei era (1624–1644). The ruling ''shōgun'' during the famine was Tokugawa Iemitsu. Events leading to the famine Due to large numbers of internally displaced persons in the aftermath of the Shimabara Rebellion, and the rinderpest epizooty, which broke out in Kyushu in 1638 and was impossible to contain, led to mass deaths of cattle in Western Japan, which reduced agricultural productivity in 1640 due to the scarcity of working animals. Also, motivation among farmers was weakening due to the extreme impoverishment of low-ranking samurai class members. The increased spending after the 1635 reformation of Sankin-kōtai (increasing frequency of ''daimyō'' annual trips to Edo) did not ...
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Oshima Subprefecture
is a subprefecture of Hokkaido Prefecture, Japan. As of 2004 it had a population of 456,621 and an area of 3,715.38 km2. Hakodate Airport is located in the City of Hakodate. Geography The subprefecture is located on the Oshima Peninsula The Oshima Peninsula (渡島 半島 ''Oshima-hantō'') is the southernmost part of Hokkaidō, the northernmost of the Japanese islands. Where the peninsula starts is open to interpretation. A more generous interpretation is to draw a line southe .... Municipalities Mergers History *1897: Hakodate Subprefecture, Kameda Subprefecture, and Matsumae Subprefecture was established. *1899: Hakodate Subprefecture was abolished. Kameda Subprefecture was transferred to Hakodate and renamed Hakodate Subprefecture. *1903: Matsumae Subprefecture was merged into Hakodate Subprefecture. *1922: Hakodate Subprefecture changed its name to Oshima Subprefecture. External links Official website (Matsumae General Branch Office) Subprefectures ...
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Nanae, Hokkaidō
is a town located in Oshima Subprefecture, Hokkaido, Japan. In April 2017, the town had an estimated population of 28,514, with 13,639 households, and a density of 130 persons per km2. The total area is 216.61 km2. Geography Nanae is at the southern end of the Oshima Peninsula, about 16 km away from Hakodate. The name of is derived from two former villages, and . *Highest mountain: 1133m, a stratovolcano History *1897: Nanae village and Iida village was merged to form Nanae village. *1902: Nanae village was merged with neighboring villages and became a Second Class Village. *1957: Nanae village became Nanae town. Transportation * Hakodate Main Line: Ōnakayama - Nanae - Oshima-Ōno( Hokuto) - Niyama - Ōnuma - Ōnuma-Kōen * Hakodate Main Line (Sawara Branch Line): Ōnuma - Ikedaen - Nagareyama Onsen - Chōshiguchi * Route 5 Education * High school ** Hokkaido Nanae High School Sister cities * Concord, Massachusetts (United States) * Miki, Kagawa ...
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Shikabe, Hokkaidō
is a town located in Oshima Subprefecture, Hokkaido, Japan. The town has a total area of . Geography Shikabe is located in northeast of Oshima Peninsula. There is Hokkaido Koma-ga-take on northwest of the town. The name of "Shikabe" is derived from Ainu word "sikerpe", meaning "Place with Phellodendron amurense". Neighboring municipalities * Hakodate * Mori * Nanae Demographics On August 1, 2019, the town had an estimated population of 3,920 and a density of 37 persons per km². History *1666: Ito Genguro, Shogunate of Tsugaru, discovers a deer healing itself in a hot spring in the area now called Shikabe. The legend of Shikabe Onsen begins. *1906: Shikabe became a Second Class village. *1945: Hakodate Main Line Sawara Branch Line and Shikabe Station were opened. *1983: Shikabe village became Shikabe town. *1990: The founding of Shikabe Park. Education * Shikabe Junior High School * Shikabe Elementary School Economy The economy of Shikabe is dominated by fishing, with ...
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Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of the fe ...
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List Of Volcanoes In Japan
This is a list of active and extinct volcanoes in Japan. An Orange background indicates a volcano considered active by the Japan Meteorological Agency. Hokkaido Honshū Izu Islands Ogasawara Archipelago The Ogasawara Archipelago include the Bonin Islands and Volcano Islands. Kyūshū Ryūkyū Islands See also * Notes and references Notes References External links Quaternary Volcanoes of Japan- Geological Survey of Japan - Geological Survey of Japan * ttp://www.data.jma.go.jp/svd/vois/data/tokyo/STOCK/souran_eng/souran.htm The National Catalogue of the Active Volcanoes in Japan- Japan Meteorological Agency 日本の主な山岳標高 (Elevation of Principal Mountains in Japan)- Geospatial Information Authority of Japan {{Asia topic, List of volcanoes in Japan Lists of coordinates Volcanoes 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 ...
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