Mount Aka (Yatsugatake)
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Mount Aka (Yatsugatake)
is a 2,899m mountain on the border of Chino, Hara of Nagano, and Hokuto of Yamanashi in Japan. This mountain is the tallest mountain of Yatsugatake Mountains. Description Mount Aka is a stratovolcano. This mountain is a center of the Yatsugatake-Chūshin Kōgen Quasi-National Park. Climbing route There are several routes to reach to the top of Mount Aka. The most popular route is from Minoto. It takes about four and half hours. Access * Minotoguchi Bus Stop of Suwa Bus Gallery Image:Akadake1.JPG, Mount Aka from north side Image:Akadake2.JPG, Mount Amida from Mount Aka Image:Akadake3.JPG, Mount Asama from Mount Aka Image:Akadake4.JPG, Mount Iō and Mount Yoko from Mount Aka Image:Akadake5.JPG, Akaishi Mountains from Mount Aka Image:Akadake6.JPG, Mount Tateshina and Hida Mountains from Mount Aka Image:Akadake7.JPG, The top of Mount Aka Image:Akadake8.JPG, Akadake Shirine at the top of Mount Aka Image:Akadake01.JPG, Mount Aka (December 2006) See also * List of Ult ...
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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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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 ...
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Mountains Of Yamanashi 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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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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List Of Ultras Of Japan
This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Japan. See also *List of mountains in Japan Sources ListMap {{DEFAULTSORT:List Of Ultras Of Japan Japan Ultras Mountains of Japan Ultras Ultras are a type of association football fans who are renowned for their fanatical support. The term originated in Italy, but is used worldwide to describe predominantly organised fans of association football teams. The behavioural tende ...
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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 ' ...
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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, ...
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Akaishi Mountains
The are a mountain range in central Honshū, Japan, bordering Nagano, Yamanashi and Shizuoka prefectures. It is also called the , as it joins with the Hida Mountains ("Northern Alps") and the Kiso Mountains ("Central Alps") to form the Japanese Alps. Origin of the name There are a lot of red stones (赤石 Aka-Ishi) around the Akaishi River, a tributary of the Ōi River in the southern part of Southern Alps. Then it was said that the mountain of red stone came to be called Mount Akaishi. The mountain represents the mountain range and the name ''Akaishi'' is used for the whole range mountain range, Akaishi Mountains. Major peaks Almost all major peaks of the Akaishi Mountains are in Minami Alps National Park that was established on June 1, 1964.Minami Alps National Park
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Mount Yoko (Southern Yatsugatake)
{{nihongo, Mount Yoko, 横岳, Yoko-dake is located in the Southern Yatsugatake Volcanic Group of the Yatsugatake Mountains, Honshū, Japan Japan ( ja, 日本, or , and formally , ''Nihonkoku'') is an island country in East Asia. It is situated in the northwest Pacific Ocean, and is bordered on the west by the Sea of Japan, while extending from the Sea of Okhotsk in the north .... References Geographical Survey Institute Yoko Yoko ...
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Mount Iō (Yatsugatake)
is a mountain on the border of Chino and Minamimaki, Nagano Prefecture, Japan. This mountain is one of the major mountains of Yatsugatake Mountains. Mount Iō literally means, ''sulphur mountain''. Outline Mount Iō is a stratovolcano in Southern Yatsugatake Volcanic Group. This mountain also belongs to the Yatsugatake-Chūshin Kōgen Quasi-National Park. Route This mountain is one of the major mountains in Yatsugatake Mountains, which is easy for climbers to reach to the top. The easiest route is from Sakurazawa. Access * Minotoguchi Bus Stop of Suwa Bus * 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 File:Mt.Iodake 08.jpg, Summit of Mount Iō from the SSE File:Mt.Iodake 02.jpg, View from summit of Mount Iō. Mount Amida o ...
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Mount Asama
is an active complex volcano in central Honshū, the main island of Japan. The volcano is the most active on Honshū. The Japan Meteorological Agency classifies Mount Asama as rank A. It stands above sea level on the border of Gunma and Nagano prefectures. It is included in ''100 Famous Japanese Mountains''. Geology Mount Asama sits at the conjunction of the Izu–Bonin–Mariana Arc and the Northeastern Japan Arc. The mountain is built up from non-alkali mafic and pyroclastic volcanic rocks dating from the Late Pleistocene to the Holocene. The main rock type is andesite and dacite. Scientists from the University of Tokyo and Nagoya University completed their first successful imaging experiment of the interior of the volcano in April 2007. By detecting sub-atomic particles called muons as they passed through the volcano after arriving from space, the scientists were able gradually to build up a picture of the interior, creating images of cavities through which lava was passin ...
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