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Mount Tengu
is a 2,646m mountain on the border of Chino and Koumi of Nagano in Japan. This mountain is the highest mountains of Northern Yatsugatake Volcanic Group. Named for the mythical avian creatures of Japanese folklore, the Tengu. Description Mount Tengu is a stratovolcano. This mountain is a part of the Yatsugatake-Chūshin Kōgen Quasi-National Park. This mountain is on the list of the 200 famous mountains in Japan. This mountain has two major peaks, Mount Higashi Tengu, and Mount Nishi Tengu. Access * Tatsunokan Bus Stop of Suwa Bus Gallery Image:Iodake3.JPG, Mount Tengu from Mount Iō Image:Tengudake1.JPG, Mount Nishi-Tengu (Left) and Mount Higashi-Tengu from Mount Neishi Image:Tengudake2.JPG, Mount Nishi-Tengu from Mount Higashi-Tengu Image:Tengudake3.JPG, Mount Higashi-Tengu from Mount Nishi-Tengu Image:Tengudake4.JPG, Mount Nishi-Tengu from Mount Neishi Image:Tengudake5.JPG, Kuroyuri-daira, north of Mount Tengu Image:Tengudake6.JPG, Kuroyuri-daira, north of Mount Te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hida Mountains
The , or , is a Japanese mountain range which stretches through Nagano, Toyama and Gifu prefectures. A small portion of the mountains also reach into Niigata Prefecture. William Gowland coined the phrase "Japanese Alps" during his time in Japan, but he was only referring to the Hida Mountains when he used that name. The Kiso and Akaishi mountains received the name in the ensuing years. Geography The layout of the Hida Mountains forms a large Y-shape. The southern peaks are the lower portion of the Y-shape, with the northern peaks forming two parallel bands separated by a deep V-shaped valley. It is one of the steepest V-shaped valleys in Japan. The Kurobe Dam, Japan's largest dam, is an arch dam located in the Kurobe Valley in the central area of the mountains. The western arm of mountains, also known as the Tateyama Peaks (立山連峰 ''Tateyama Renpō''), are dominated by Mount Tsurugi and Mount Tate. The eastern arm, known as the Ushiro Tateyama Peaks (後立山連峰 ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tateshina
also Suwa Fuji is a complex volcano located on the border of the municipalities of Chino and Tateshina in Nagano Prefecture, Japan. It has an elevation of . This mountain is one of the 100 Famous Japanese Mountains. Outline Mount Tateshina is a typical complex volcano. About the origin of the name of this mountain, ''tate'' means water-pepper, and ''shina'' means steps or high places. So ''Tateshina'' is literally a high mountain of water-peppers. The other name of this mountain ''Suwa Fuji'', literally, ''Mount Fuji of the Suwa region''. Mount Tateshina is an important part of Yatsugatake-Chūshin Kōgen Quasi-National Park. Route Routes to climb up Mount Tateshina are well-developed. The most popular route is to start from the Nanagome parking lot. Gallery File:Tateshina4.jpg, Ruin of the volcanic crater of Mount Tateshina File:Tateshina1.jpg, Top of Mount Tateshina File:Yatsugatake from tateshina.jpg, Yatsugatake Mountains from Mount Tateshina File:Tateshina5.jpg, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. History *July 3, 1919 - Incorporation of Suwa Jidōsha K.K. *July 1941 - Setting of greater Suwa area as business area *December 1963 - Acquisition by Matsumoto Electric Railway as a subsidiary *May 1981 - Change of corporate name to Suwa Bus K.K. *December 1984 - Opening of Chuo Kosoku Bus Iida route (Iida– Shinjuku) *November 1986 - Opening of Chūō Expressway Bus Chino Route (Chūō Expressway Chino Bus Stop–Shinjuku) *July 1987 - Opening of Chūō Expressway Bus Suwa–Okaya Route (Kami-Suwa/Okaya–Shinjuku) *September 1988 - Opening of Misuzu Highway Bus *July 1989 - Opening of Chino–Nagoya route via Chūō Expressway (discontinued in April 1997) *December 1989 - Opening of Chino–Osaka route via Chūō Expressway *March 1993 - O ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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