Mount Tengu (Ishikari)
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Mount Tengu (Ishikari)
is a mountain on the border of Chino and Koumi of Nagano in Japan. This mountain is the highest mountains of Northern Yatsugatake Volcanic Group, and consists of two peaks, ''Mount Nishi Tengu'', and ''Mount Higashi Tengu'', . Mount Tengu is named for the mythical Tengu of Japanese folklore. Description Mount Tengu is a stratovolcano. The mountain forms part of Yatsugatake-Chūshin Kōgen Quasi-National Park, and is one of . Mount Neishi, , is located just to the south of Mount Hisashi Tengu. , , is located to the north of Mount Hisashi Tengu. Access * or of Alpico Kōtsū from Chino Station Mountain Climbing The main traverse route of the Yatsugatake Mountain Range passes through the eastern summit of Mount Tengu. In addition, there are mountain trails on the western side of Mount Tengu from Shibunoyu, , in Oku-Tateshina Onsen Village and from Karasawa Kosen, and on the eastern side from Inakoyu via Honzawa Onsen. A mountain hut, ''Kuroyuri Hutte'', , is ...
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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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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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Volcanoes Of Nagano Prefecture
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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Mountains Of Nagano Prefecture
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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Chino Station
is a railway station on the Chūō Main Line in the city of Chino, Nagano, Japan, operated by East Japan Railway Company (JR East). Lines Chino Station is served by the Chūō Main Line, and is 195.2 kilometers from the terminal station, terminus of the line at Tokyo Station. Station layout The station consists of one ground level side platform and one ground level island platform, connected by a footbridge. The station has a ''Midori no Madoguchi'' staffed ticket office. A JNR Class C12 steam locomotive is preserved in the plaza outside the station's east entrance. Platforms Bus terminal Highway buses * Chūō Kōsoku Bus; For Shinjuku Station * ''Alpen Suwa''; For Kyoto Station, Momoyamadai Station, Shin-Ōsaka Station, and Umeda Station Route buses *JR BUS **For Takatō Bus Terminal, Senryuso *Alpico Kotsu **For Mugikusa Pass **For Lake ShirakabaTransferring onto Tateshina Smile Kotsu and Toshin Kanko Bus at this bus stop enables you to go to Oya Station (Nagano), Sakud ...
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Alpico Kōtsū
is a public transport company in Nagano Prefecture, Japan. It is the core company of Alpico Group and is wholly owned by Alpico Holdings Co., Ltd. The company was known as until its merger with two affiliate companies on April 1, 2011. Headquarters The company's headquarters are at 1-1 Igawajō 2-chōme, Matsumoto, Nagano Prefecture 390-8518 Japan. Area served The company serves the cities of Chino, Nagano, Matsumoto, Nagano, Okaya, Nagano, Suwa, Nagano, and their vicinities. History *May 29, 1920 - Incorporated as Chikuma Railway (筑摩鉄道) *October 2, 1921 - Opens Shimashima Line railway between Matsumoto and Niimura. *May 3, 1922 - Extends Shimashima Line from Niimura to Hata. *September 26, 1922 - Extends Shimashima Line from Hata to Shimashima. *October 31, 1922 - Renamed as Chikuma Electric Railway (筑摩電気鉄道) *April 19, 1924 - Opens Asama Line tramway between Matsumoto and Asama-onsen.Wakuda, ''supra'', p. 48 *December 2, 1932 - Renamed as Matsumoto Elec ...
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Mount Neishi
{{nihongo, Mount Neishi, 根石岳, Neishi-dake is a 2,603m mountain on the border of Chino and Koumi of Nagano in Japan. This mountain belongs to Northern Yatsugatake Volcanic Group. Description Mount Neishi is a stratovolcano. This mountain is a part of the Yatsugatake-Chūshin Kōgen Quasi-National Park. Access * Tatsunokan Bus Stop of Suwa Bus had been a bus company in Suwa area Nagano Prefecture, Japan until March 2011 because the company has been be taken over by Alpico Kotsu. After merging to Alpico Kotsu, Suwa Bus is a nickname which Alpico Kotsu Group operates on Suwa area. Hist ... Gallery Image:Neishi02.JPG, The top of Mount Neishi Image:Neishi03.JPG, Mount Nishi-Tengu from Mount Neishi Image:Neishi04.JPG, Mount Higashi-Tengu from Mount Neishi Image:Neishi05.JPG, Neishi Hut from Mount Neishi References Ministry of Environment of JapanOfficial Home Page of the Geographical Survey Institute in Japan ‘Yatsugatake, Tateshina, Utsukushigahara, Kirigamine 200 ...
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Yatsugatake-Chūshin Kōgen Quasi-National Park
is a quasi-national park on Honshū in Japan. It is rated a protected landscape (category V) according to the IUCN. The park includes the Yatsugatake Mountains and the surrounding lava plateaus: Tateshina plateau, Kirigamine, and Utsukushigahara. It straddles the border between Nagano and Yamanashi prefectures. Mount Aka is the highest point in the park at 2,899 m. The volcanoes of the Yatsugatake mountains erupted from the middle of the Fossa Magna ( ja) and spread skirts of lava south, east and west. Lake Matsubara, Shirakoma Pond, and Lake Shirakaba attract tourists to the region for boating, skating, and camping. Utsukushigahara is a lava plateau at the northern end of the park and offers views of the Northern Alps. The extensive lava plateau of Kirigahara is popular for hiking. There are also a number of onsens in addition to the hotsprings at Tateshina. The park was designated a quasi-national in 1964. Like all quasi-national parks in Japan, the park is managed by th ...
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Japanese Folklore
Japanese folklore encompasses the informally learned folk traditions of Japan and the Japanese people as expressed in its oral traditions, customs, and material culture. In Japanese, the term is used to describe folklore. The academic study of folklore is known as . Folklorists also employ the term or to refer to the objects and arts they study. Folk religion Men dressed as namahage, wearing ogre-like masks and traditional straw capes (''mino'') make rounds of homes, in an annual ritual of the Oga Peninsula area of the Northeast region. These ogre-men masquerade as kami looking to instill fear in the children who are lazily idling around the fire. This is a particularly colorful example of folk practice still kept alive. A parallel custom is the secretive ritual of the Yaeyama Islands, Okinawa which does not allow itself to be photographed. Many, though increasingly fewer households maintain a kamidana or a small Shinto altar shelf. The Shinto version of the kitchen go ...
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Japanese Language
is spoken natively by about 128 million people, primarily by Japanese people and primarily in Japan, the only country where it is the national language. Japanese belongs to the Japonic or Japanese- Ryukyuan language family. There have been many attempts to group the Japonic languages with other families such as the Ainu, Austroasiatic, Koreanic, and the now-discredited Altaic, but none of these proposals has gained widespread acceptance. Little is known of the language's prehistory, or when it first appeared in Japan. Chinese documents from the 3rd century AD recorded a few Japanese words, but substantial Old Japanese texts did not appear until the 8th century. From the Heian period (794–1185), there was a massive influx of Sino-Japanese vocabulary into the language, affecting the phonology of Early Middle Japanese. Late Middle Japanese (1185–1600) saw extensive grammatical changes and the first appearance of European loanwords. The basis of the standard dialect moved f ...
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Tengu
are a type of legendary creature found in Japanese folk religion (Shinto). They are considered a type of ''yōkai'' (supernatural beings) or Shinto ''kami'' (gods). The ''Tengu'' were originally thought to take the forms of birds of prey and a monkey deity, and they are traditionally depicted with human, monkey, and avian characteristics. Sarutahiko Ōkami is considered to be the original model of Konoha-Tengu (a supernatural creature with a red face and long nose), which today is widely considered the ''Tengu''s defining characteristic in the popular imagination. He is the Shinto monkey deity who is said to shed light on heaven and earth. Some experts theorize that Sarutahiko was a sun god worshiped in the Ise region prior to the popularization of Amaterasu. Buddhism long held that the ''Tengu'' were disruptive demons and harbingers of war. Their image gradually softened, however, into one of protective and even manifestations of Buddhist deities, if still dangerous, spirits ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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