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Mount Nasu
is a group of complex volcanoes located in the northeast part of Nikkō National Park, Japan. The tallest peak is Sanbonyari Peak at a height of . Mount Nasu is one of the 100 Famous Japanese Mountains. Major peaks Mount Nasu has the following major peaks: * Sanbonyari Peak – 1916.9 m * Chausu Peak – 1915 m * Asahi Peak – 1896 m * Minamigatsusan – 1776 m * Kuro-oya Peak – 1589 m These peaks are known collectively as . Climate Eruption It is estimated that Mount Nasu started erupting 600 thousand years ago. The eruption started from the north end of the mountain range, at Kashi-Asahi Peak. Only Chausu Peak is active today. Access * Nasu Sancho Station of Nasu Ropeway * Sandogoya Onsen Bus Stop of Kanto Transportation Gallery File:Mt.Chausu&Mt.Asahi.jpg, Chausu lava dome and Asahi Peak File:Nasu chausudake.jpg, Chausu lava dome and fumes File:Nasu asahidake.jpg, Asahi Peak Image:Nasudake02.JPG, West view from Sanbonyari Peak Image:Nasudake03.JPG, Sanbony ...
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Ōu Mountains
The are a mountain range in the Tōhoku region of Honshū, Japan. The range is the longest range in Japan and stretches south from the Natsudomari Peninsula of Aomori Prefecture to the Nasu volcanoes at the northern boundary of the Kantō region. Though long, the range is only about wide. The highest point in the range is Mount Iwate, . The range includes several widely known mountains: Hakkōda Mountains, Mount Iwate, Mount Zaō, Mount Azuma, Mount Yakeishi, and Mount Adatara. Naming These mountains previously formed the boundary between historical provinces of Mutsu (陸奥国) and Dewa (出羽国). The ''kanji'' for the name of the mountain range was created from one ''kanji'' of the two provinces, 奥 and 羽, respectively. Geology The Ōu Mountains began to form in the Pliocene. They sit over the middle of the inner arc of the Northeastern Japan Arc. This is the result of the Pacific Plate subducting under the Okhotsk Plate The Okhotsk Plate is a minor tect ...
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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 documentaries, and other hiking books. An English edition, ''One Hundred Mountains of Japan'', translated by Martin Hood, was published in 2014 by the

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Volcanoes Of Tochigi 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 (geology), hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tecto ...
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Mountains Of Fukushima 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 Tochigi 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 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 abou ...
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Michinori Holdings#Kanto Transportation
Michinori (written: 道教, 通教, 通憲 or 倫範) is a masculine Japanese given name. Notable people with the name include: * (1106–1160), Japanese scholar and Buddhist monk * (1315–1349), Japanese ''kugyō'' * (1910–1945), Japanese military officer * (born 1990), Japanese mixed martial artist * (born 1953), Japanese mathematician {{given name Japanese masculine given names ...
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Michinori Holdings
is a holding company headquartered in Chiyoda, Tokyo, and a wholly owned subsidiary of Industrial Growth Platform, Inc. Michinori Holdings rehabilitates deficit companies which have so much liability that they cannot act as an administrator of assets. It manages them by acquiring and holding their shares until they return to financial stability and viability. As of 2022, Michinori Holdings currently holds and operates subsidiaries in the transportation sector, including bus, railway, and monorail companies. They are: * Fukushima Transportation, since 2008 * Shonan Monorail, since 2015 * Sado Kisen (ferry company), since 2022 * Aizu Bus, since 2011 * Kanto Transportation, since 2012 * Northern Iwate Transportation, since 2010 * Ibaraki Kotsu (bus company), since 2009 * Higashinihon Kotsu (bus company), since 2018 Some expressway bus routes operated by affiliated companies of Michinori Holdings are named "Michinori Express" (MEX), designed by Yasuyuki Kawanishi, who also design ...
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Japan Meteorological Agency
The , abbreviated JMA, is an agency of the Ministry of Land, Infrastructure, Transport and Tourism. It is charged with gathering and providing results for the public in Japan that are obtained from data based on daily scientific observation and research into natural phenomena in the fields of meteorology, hydrology, seismology and volcanology, among other related scientific fields. Its headquarters is located in Minato, Tokyo. JMA is responsible for gathering and reporting weather data and forecasts for the general public, as well as providing aviation and marine weather. JMA other responsibilities include issuing warnings for volcanic eruptions, and the nationwide issuance of earthquake warnings of the Earthquake Early Warning (EEW) system. JMA is also designated one of the Regional Specialized Meteorological Centers of the World Meteorological Organization (WMO). It is responsible for forecasting, naming, and distributing warnings for tropical cyclones in the Northwestern ...
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Nikkō National Park
is a national park in the Kantō region, on the main island of Honshū in Japan. The park spreads over three prefectures: Tochigi Prefecture, Tochigi, Gunma Prefecture, Gunma and Fukushima Prefecture, Fukushima, and was established in 1934. History The establishment of Nikkō National Park dates to the early 20th century. The Diet of Japan designated Nikkō an in 1911. The National Parks Law was passed in 1931, and Nikkō National Park was established in 1934. The park was expanded throughout the 20th century. Oze National Park was once part of Nikkō National Park, but became a separate national park in 2007. Description The park is considered one of the most beautiful in Japan, and is a popular tourist destination.Nikko National Park
Beyond its striking scenery, the park is noted for its historical Buddhist temp ...
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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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