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Mount Azumaya
is one of the 100 Famous Japanese Mountains. The peak lies on the border of Nagano Prefecture and Gunma Prefecture. There exist alternative spellings of the mountain's name, like: 吾妻山 and 吾嬬山 which is read as "Agatsuma-yama" (Mount Agatsuma). In the village Tsumagoi, the mountain is spelled 吾妻山. The mountain should not be confused with of which there are two, one in Nagano Prefecture and the other in Saitama Prefecture. Though the reading is the same, the name written in Kanji differs from the mountain in this article. Outline Mount Azumaya was formed between 900,000 and 300,000 years ago by andesite lava flowing out of a Stratovolcano. An eruption 340,000 years ago formed a caldera of circa 3 kilometers in diameter. Through erosion the mountain has arrived at its present form with several peaks. is the general term for the following peaks lying roughly on a circle: , Mount Azumaya, , . The famous Sugadaira Kōgen ski area is found on the mountain's sou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
100 Famous Japanese Mountains
is a book written in 1964 by mountaineer and author Kyūya Fukada.Hyakumeizan, Hiking Japan! . Japan Gazetteer. Accessed June 27, 2008. The list became famous when , now Emperor, took note of it. The list has been the topic of NHK documentaries, and other hiking books. An English edition, ''One Hundred Mountains of Japan'', translated by Martin Hood, was published in 2014 by the |
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] |
Volcanoes Of Gunma 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Gunma 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 ... [...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] |
Volcanoes Of Honshū
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 sli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Japan ...
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 ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Neko
is a mountain in Jōshin'etsu-kōgen National Park with an elevation of , located near Ueda and Suzaka in Nagano Prefecture, Japan. It is one of the because of the flowers of Parnassia palustris which bloom in September. Along with Mount Azumaya, Mount Neko is one of the published by The Shinano Mainichi Shimbun. The mountain should not be confused with a similarly named Mount Neko (根子岳) in Kumamoto Prefecture. Mount Neko forms the western peak along the rim of the caldera. This volcano was active 900,000–300,000 years ago. Other peaks on the caldera are Mount Azumaya () to the south, () to the east, and () to the north. Mount Azumaya is one of the 100 Famous Japanese Mountains. Mountain Climbing ; Ascent * One of the most frequently used trails begins at Sugadaira Farm (). From there, it is approximately 30 minutes to a birch forest, then one hour through the forest, and another 30 minutes from the tree line to the summit. ; Descent * From the summit, it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Japan's Top 100 Waterfalls
is a list of waterfalls in Japan compiled by the Japanese Ministry of the Environment in 1990. Background According to the Japanese government, there are 517 named waterfalls in Japan. Many of these waterfalls are located in remote mountain locations, but with an increase in hiking and tourism in recent years, the number of visitors has greatly increased, placing significant pressure on the surrounding environment. Listing Gallery File:Hagoromonotaki.jpg, 1. Hagoromo Falls File: Inkura.jpg, 2. Inkura Falls File:Garoh-Fall.jpg, 3. Garō Falls File:Ginganotaki.jpg, 4. Ryusei-Ginga Falls File:Asiribetu.jpg, 5. Ashiribetsu Falls File:Oshinkoshin-no-taki.jpg, 6. Oshinkoshin Falls File:Kurokumanotaki.jpg, 7. Kurokuma Falls File: Waterfall of Fudou in Hatimantai.JPG, 9. Fudō Falls File:Akiu Otaki.jpg, 10. Akiu Great Falls File:Sankai_no_taki_5nov07.jpg, 11. Sankai Falls File:Nanataki Falls 2008-02-29.jpg, 12. Nanataki Falls File:Chagamanotakiw.jpg, 13. Chagama Falls File:Hot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ski Area
A ski area is the terrain and supporting infrastructure where skiing and other snow sports take place. Such sports include alpine and cross-country skiing, snow boarding, tubing, sledding, etc. Ski areas may stand alone or be part of a ski resort. Scope of activities The US Forest Service defines a ski area as: "a site and associated facilities that has been primarily developed for alpine or Nordic skiing and other snow sports, but may also include, in appropriate circumstances, facilities necessary for other seasonal or year-round natural resource-based recreation activities, provided that a preponderance of revenue generated by the ski area derives from the sale of alpine and Nordic ski area passes and lift tickets, revenue from alpine, Nordic, and other snow sport instruction, and gross revenue from ancillary facilities that support alpine or Nordic skiing and other snow sports." Notable examples Ski areas can extend over several municipalities (ex: La Plagne in France, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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