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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 ... [...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] |
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] |
Chino, Nagano
is a city located in Nagano Prefecture, Japan. , the city had an estimated population of 55,673 in 23,236 households, and a population density of 210 persons per km². The total area of the city is . Geography Chino is located in a mountainous area of the east-central Nagano prefecture. Notable mountains within the city limits include Mount Yatsugatake, Mount Tateshina, and Mount Kirigamine. Chino city hall is located at an elevation of 801 meters and is thus the highest city hall location in Japan. Climate The city has a climate characterized by hot and humid summers, and relatively mild winters (Köppen climate classification ''Cfa''). The average annual temperature in Chino is 10.9 °C. The average annual rainfall is 1310 mm with September as the wettest month. The temperatures are highest on average in August, at around 23.6 °C, and lowest in January, at around -1.8 °C. The mountainous portions of the city are considered part of the snow country of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Koumi, Nagano
is a town located in Nagano Prefecture, Japan. , the town had an estimated population of 4,676 in 2012 households, and a population density of 41 persons per km². The total area of the town is . The town mascot is "Ptylitza", an imaginary small gnome-like creature, images of which can be seen all over the town. Geography Koumi is located in the far east of Nagano. The nearest city is Saku, about 40 minutes drive away. Nagano city is about 100 km away. Mount Tengu (2646 meters) is located on the border of Koumi with Chino. the Chikuma River flows through the town. Surrounding municipalities *Nagano Prefecture ** Chino ** Minamimaki ** Kitaaiki ** Minamiaiki ** Sakuho Climate The town has a humid continental climate characterized by warm and humid summers, and cold winters with heavy snowfall (Köppen climate classification ''Dfb''). The average annual temperature in Koumi is 8.2 °C. The average annual rainfall is 1398 mm with September as the wettest month. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nagano Prefecture
is a landlocked prefecture of Japan located in the Chūbu region of Honshū. Nagano Prefecture has a population of 2,052,493 () and has a geographic area of . Nagano Prefecture borders Niigata Prefecture to the north, Gunma Prefecture to the northeast, Saitama Prefecture to the east, Yamanashi Prefecture to the southeast, Shizuoka Prefecture and Aichi Prefecture to the south, and Gifu Prefecture and Toyama Prefecture to the west. Nagano is the capital and largest city of Nagano Prefecture, with other major cities including Matsumoto, Ueda, and Iida. Nagano Prefecture has impressive highland areas of the Japanese Alps, including most of the Hida Mountains, Kiso Mountains, and Akaishi Mountains which extend into the neighbouring prefectures. The abundance of mountain ranges, natural scenic beauty, and rich history has gained Nagano Prefecture international recognition as a world-class winter sports tourist destination, including hosting the 1998 Winter Olympics and a new ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 toward the East China Sea, Philippine Sea, and Taiwan in the south. Japan is a part of the Ring of Fire, and spans Japanese archipelago, an archipelago of List of islands of Japan, 6852 islands covering ; the five main islands are Hokkaido, Honshu (the "mainland"), Shikoku, Kyushu, and Okinawa Island, Okinawa. Tokyo is the Capital of Japan, nation's capital and largest city, followed by Yokohama, Osaka, Nagoya, Sapporo, Fukuoka, Kobe, and Kyoto. Japan is the List of countries and dependencies by population, eleventh most populous country in the world, as well as one of the List of countries and dependencies by population density, most densely populated and Urbanization by country, urbanized. About three-fourths of Geography of Japan, the c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Yatsugatake Volcanic Group
is a volcanic group of stratovolcanoes and lava domes located in Nagano Prefecture on Honshū in Japan. Description The Northern Yatsugatake Volcanic Group is part of the Yatsugatake Mountains. The northern group is defined as the mountains from Mount Futago to Natsuzawa Pass. The highest peak of the mountains is Mount Tengu and the elevation is 2,646 metres. The southern Yatsugatake mountains are steep and have alpine characteristics. The mountains of the Northern Yatsugatake Volcanic Group are gentler and lower. Yatsugatake is listed among the 100 famous mountains in Japan, but this refers to the Southern Yatsugatake Volcanic Group. Mount Tateshina is also mentioned as one of the 100 famous mountains, and it is part of the Northern Yatsugatake mountains, but is listed separately. These mountains are part of the Yatsugatake-Chūshin Kōgen Quasi-National Park. Geology and volcanic activity The volcanoes are stratovolcanos that are 1 million to 200,000 years old. The rock ... [...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] |
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] |
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] |
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] |
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] |
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