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Asahidake
is a mountain located near the town of Higashikawa, Hokkaido and the tallest mountain on the Japanese island of Hokkaido. It is part of the Daisetsuzan Volcanic Group of the Ishikari Mountains, it is located in the northern part of the Daisetsuzan National Park. Its native Ainu name is ''Kamui-mintara'', which means "the playground of the gods". The mountain is popular with hikers in the summer and can be easily reached from Asahidake Onsen via Asahidake Ropeway. During winter, the mountain is open for use by skiers and snowboarders. Sugatami Pond, directly below the peak, is famous for its reflection of the peaks, snow, and steam escaping from the volcanic vents. History Sulphur was once mined in the fumarolic areas. Geology Mount Asahi is an active stratovolcano, in height that arose southwest of the Ohachi-Daira caldera. The Japan Meteorological Agency gave the region rank C in volcanic activity. The volcano consists mainly of andesite and dacite, Holocene volcanic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asahidake Ropeway
The is Japanese aerial lift line in Asahidake Onsen, Higashikawa, Hokkaidō, Higashikawa, Hokkaidō, operated by . The ropeway line, founded in 1968 and refurbished in 2000, climbs Mount Asahi-dake of Daisetsuzan Volcanic Group, Daisetsuzan Mountains, the tallest mountain in Hokkaidō. The line mainly transports spectators of alpine plants in summer and autumn leaf color, autumn colors in autumn, while there also is a ski area. During the summer months, the lift operates once every 15 minutes and every 20 minutes during the winter months. It takes 10 minutes to complete a one-way trip. Stations The two connecting stations at the foot and submit of the ropeway are: Sanroku Station (Asahi-dake Station) * Altitude 1,100m Main attractions and facilities in the surrounding area include: * Foothills shop * Foothills dining room "Alpine Flora" * Asahidake Onsen Sugatami Station (Sancho Station) * Altitude 1,600m Main attractions and facilities in the surrounding area include: * Moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Asahidake Onsen
is a small village in Daisetsuzan National Park, Kamikawa Subprefecture is a subprefecture of Hokkaido Prefecture, Japan. The name is derived from Kamikawa no hitobito no Shūraku (Village of the Upstream People), a translation of the Ainu Ainu or Aynu may refer to: *Ainu people, an East Asian ethnic group of Ja ..., Hokkaidō, Japan. The village consists of a few hotels and a youth hostel. It a popular base for hikers in the national park, and for tourists using Asahidake Ropeway to climb Asahi-dake, Hokkaidō's highest mountain peak. There are several natural primitive hot springs, and also a hot springs resort, with approximately twelve buildings. The nearby ropeway costs 1800 or 2800 yen, depending on the time of year. Hiking opportunities in the area range from 30- to 60-minute walks all the way up to one- or two-day tours of the area's mountains. The area is volcanic, and evidence of such activity is plentiful. There are also opportunities for skiing in the are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daisetsuzan National Park
, or Taisetsuzan is located in the mountainous center of the northern Japanese island of Hokkaidō. At , Daisetsuzan is the largest national park in Japan, and is approximately the size of Kanagawa Prefecture. Daisetsuzan, meaning "great snowy mountains", an apt description of these peaks. There are 16 peaks over in Daisetsuzan National Park, both with and without trails. The park offers some of the most rugged scenery in Japan. Asahidake (), located in the north of the park, is the highest peak in Hokkaidō. Daisetsuzan National Park spans two subprefectures of Hokkaidō, Kamikawa and Tokachi. Daisetsuzan National Park was established in 1934. Mountain groups Daisetsuzan National Park consists of three volcanic mountain groups. The groups consist of stratovolcanoes piled on top of each other. As one vent becomes active, it builds a peak then stops until a new vent appears. These groups are: #Daisetsuzan Volcanic Group — lies in the northern part of the park and includes H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Daisetsuzan Volcanic Group
The is a volcanic group of peaks arranged around the wide caldera in Hokkaidō, Japan. In the Ainu language it is known as ''Nutapukaushipe'' (which means "the mountain above the river"),Geographical Survey Institute website , last access 1 July 2008. ''Nutaku Kamushupe'', or ''Optateske''. These peaks are the highest in Hokkaidō. The group lends its name to the Daisetsuzan National Park in which the volcanic group is located. Geography The volcanic group lies at the north end of the Daisetsu-Tokachi on th ...[...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 ab ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ishikari Mountains
The is a range of volcanic mountains in central Hokkaidō, Japan. The mountain range is made up from the Daisetsuzan Volcanic Group and the Tomuraushi Volcanic Group. The volcanoes are part of the Kurile arc of the Pacific ring of fire The Ring of Fire (also known as the Pacific Ring of Fire, the Rim of Fire, the Girdle of Fire or the Circum-Pacific belt) is a region around much of the rim of the Pacific Ocean where many volcanic eruptions and earthquakes occur. The Ring .... References Hokkaipedia, Daisetsuzan Mountains last access 2 July 2008. Mountain ranges of Hokkaido {{Hokkaido-geo-stub ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hokkaidō
is Japan's second largest island and comprises the largest and northernmost prefecture, making up its own region. The Tsugaru Strait separates Hokkaidō from Honshu; the two islands are connected by the undersea railway Seikan Tunnel. The largest city on Hokkaidō is its capital, Sapporo, which is also its only ordinance-designated city. Sakhalin lies about 43 kilometers (26 mi) to the north of Hokkaidō, and to the east and northeast are the Kuril Islands, which are administered by Russia, though the four most southerly are claimed by Japan. Hokkaidō was formerly known as '' Ezo'', ''Yezo'', ''Yeso'', or ''Yesso''. Nussbaum, Louis-Frédéric. (2005). "Hokkaidō" in Although there were Japanese settlers who ruled the southern tip of the island since the 16th century, Hokkaido was considered foreign territory that was inhabited by the indigenous people of the island, known as the Ainu people. While geographers such as Mogami Tokunai and Mamiya Rinzō explored ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 No ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fumarole
A fumarole (or fumerole) is a vent in the surface of the Earth or other rocky planet from which hot volcanic gases and vapors are emitted, without any accompanying liquids or solids. Fumaroles are characteristic of the late stages of volcanic activity, but fumarole activity can also precede a volcanic eruption and has been used for eruption prediction. Most fumaroles die down within a few days or weeks of the end of an eruption, but a few are persistent, lasting for decades or longer. An area containing fumaroles is known as a fumarole field. The predominant vapor emitted by fumaroles is steam, formed by the circulation of groundwater through heated rock. This is typically accompanied by volcanic gases given off by magma cooling deep below the surface. These volcanic gases include sulfur compounds, such as various sulfur oxides and hydrogen sulfide, and sometimes hydrogen chloride, hydrogen fluoride, and other gases. A fumarole that emits significant sulfur compounds is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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