Volcanoes Of Japan
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Volcanoes Of 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 ...
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Volcano
A volcano is a rupture in the Crust (geology), crust of a Planet#Planetary-mass objects, planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and volcanic gas, gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where list of tectonic plates, tectonic plates are divergent boundary, diverging or convergent boundary, 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 ...
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Nigorigawa Caldera
Nigorigawa Caldera (Japanese: 濁川カルデラ, ''Nigorigawa karudera'') is a volcanic crater in Oshima, Hokkaido, Japan. It has an elevation of 1,168 ft (356m) and it last erupted 12,000 years ago. The caldera has a diameter of 3km. A town of the same name is located at the caldera. East of Nigorigawa is the town of Mori Mori is a Japanese and Italian surname, and also a Persian pet name for Morteza. It is also the name of two clans in Japan, and one clan in India. Italian surname *Barbara Mori, Uruguayan-Mexican actress * Camilo Mori, Chilean painter * Cesare ... and an active volcano known as Koma-ga-take. References {{Hokkaido-geo-stub Calderas of Hokkaido Volcanoes of Hokkaido Volcanic craters Pleistocene calderas ...
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Mount Shiretoko
is a volcano located on the Shiretoko Peninsula in Hokkaidō, Japan. The mountain consists of non-alkali mafic rocks and andesite. Mount Shiretoko is in Shari town, in Shari District of Abashiri Subprefecture. See Also *List of volcanoes in Japan *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 pro ... References External links Shiretoko Dake- Geological Survey of Japan * Mountains of Hokkaido Volcanoes of Hokkaido Stratovolcanoes of Japan Pleistocene stratovolcanoes {{Hokkaido-geo-stub ...
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Mount Shari
is a quaternary stratovolcano and one of Japan's 100 famous mountains. Its summit is . The summit consists of Mount Shari, and the western ridge. It is located on the Hokkaidō's Shiretoko Peninsula on the border of Shari and Kiyosato in Shari District, Abashiri and Shibetsu in Shibetsu District, Nemuro. Naming Its former name in the Ainu language was Onnenupuri. The name ''Shari'' in Ainu means ''marshes where reeds are growing''. It is also known by the names or . Geology The mountain is made mainly of andesite, dacite, and basalt. Climbing routes The most popular ascent route starts from the Kiyosato side. A public bus ( Sharibus) runs three times a day (first at 6:30) from Shiretokoshari Station to the start of the trail. See also *List of mountains in Japan *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 H ...
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Hokkaido Koma-ga-take
, also , , or just is a andesitic stratovolcano on the border between Mori, Shikabe, and Nanae, all within the Oshima Subprefecture of Hokkaidō, 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 n .... Occurrence of volcanic activity started some 30,000 years ago. Following roughly 5,000 years of dormancy, volcanic activity at Mount Koma-ga-take restarted at the start of the 17th century, triggering the Kan'ei Great Famine in 1640. Since then, there have been at least 50 recorded volcanic events at Mount Koma-ga-take.神沼克伊,小山悦郎 ''日本の火山を科学する 日本列島津々浦々、あなたの身近にある108の活火山とは?'' ソフトバンククリエイティブ 2011. . File:Hokkaido-Komagatake Relief Map, SRTM-1.jpg, Relief Map File:Red h ...
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Lake Tōya
is a volcanic caldera lake in Shikotsu-Toya National Park, Abuta District, Hokkaidō, Japan. It is part of "Toya Caldera and Usu Volcano Global Geopark" which joins in Global Geoparks Network. The stratovolcano of Mount Usu lies on the southern rim of the caldera. The lake is nearly circular, being 10 kilometers in diameter from east–west and 9 kilometers from north–south. The town of Tōyako comprises most of the area surrounding the lake and the town of Sōbetsu is located on the eastern side. Lake Tōya is said to be the northernmost lake in Japan that never ices (with competing claim by nearby Lake Shikotsu), and the second most transparent lake in Japan. Nakajima Island (not to be confused with another island of the same name in Lake Kussharo) is a recursive island in the middle of the lake which houses the ''Tōya Lake Forest Museum''. Lake Tōya was called ''Kim'un-to'' (キムウン (kim'un) means "in the mountain"Batchelor, John. (1905) ''An Ainu-English-Jap ...
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Mount Shiribetsu
Mount Shiribetsu ( ja, 尻別岳) is a volcano on the Japanese island of Hokkaido. The volcano last erupted hundreds of thousands of years before present. See also * List of mountains in Japan * 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 Archipelag ... References External links Shiribetsu Dake- Geological Survey of Japan Global Volcanism Program page for Mount Shiribetsu{{DEFAULTSORT:Shiribetsu Volcanoes of Hokkaido Mountains of Hokkaido ...
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Lake Shikotsu
is a caldera lake in Chitose, Hokkaidō, Japan. It is a part of the Shikotsu-Toya National Park. Geography Lake Shikotsu is located in the south-west part of Hokkaidō. It has an average depth of and a maximum depth of , making it the second deepest lake in Japan, after Lake Tazawa. It is the 8th-largest lake by surface area in Japan and the second largest of Japan's caldera lakes, surpassed only by Lake Kussharo. It is surrounded by three volcanos: Mount Eniwa to the north and Mount Fuppushi and Mount Tarumae to the south. The caldera formed in the holocene when the land between the volcanos subsided. Due to its depth, the volume of Lake Shikotsu reaches 3/4 of the volume of Lake Biwa, Japan's largest lake, despite of having only 1/9 of that lake's surface area. Due to the small surface area to depth ratio, the water temperature remains quite constant throughout the year, making it the northernmost ice-free lake in Japan. The Bifue, Okotanpe, Ninaru and Furenai rivers fe ...
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Shikaribetsu Volcanic Group
is a volcanic group of lava domes surrounding Lake Shikaribetsu in Hokkaidō, Japan. The Shikaribetsu volcanic group is located in Daisetsuzan National Park. The volcanic group lies on the Kurile arc of the Pacific ring of fire. The volcanic group includes the following peaks: * Mount Higashi Nupukaushi * Mount Nishi Nupukaushi * Mount Tenbo * Mount Hakuun See also *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 Archipelag ... References * Shikaribetsu Volcanic Group Quaternary Volcanoes of Japan, Geological Survey of Japan, AIST., 2006 Volcanoes of Hokkaido Pleistocene lava domes Volcanic groups Volcanism of Japan {{Hokkaido-geo-stub ...
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Mount Rishiri
is a Quaternary stratovolcano located off the coast of Hokkaidō, Japan in the Sea of Japan. It rises out of the Sea of Japan forming Rishiri Island. Because its cone shape resembles Mount Fuji it is sometimes referred to as Rishiri Fuji. It is one of the 100 famous mountains in Japan. Mount Rishiri's opening festival is held annually on July 2 and July 3. This festival officially opens the climbing season. Geology Mount Rishiri is made up of alkali and non-alkali mafic volcanic rock dating from the Late Pleistocene, 130,000–18,000 years ago. Otherwise it is covered in Quaternary volcanic rock debris. Climbing route The ascent of Rishiri is not suitable for novice hikers, because it is challenging in places. There is a campsite partway up the mountain from the dock, and an unmanned hut located a short distance below the summit. There is also a small shrine at the summit. On clear days the view extends to Hokkaidō, the adjacent island of Rebun, and as far as Sakha ...
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Mount Rausu
__NOTOC__ is a stratovolcano on the Shiretoko Peninsula in Hokkaidō, Japan. It sits on the border between the towns of Shari and Rausu. Mount Rausu is the northeasternmost Holocene volcano on Hokkaidō. It is one of the 100 famous mountains in Japan. Mount Rausu's opening festival is held annually on July 3. This day officially opens the climbing season. In the past 2200 years it is believed that Mount Rausu erupted thrice, with a Plinian Eruption roughly 1400 years ago and a pyroclastic flow about 500 years ago.神沼克伊,小山悦郎 ''日本の火山を科学する 日本列島津々浦々、あなたの身近にある108の活火山とは?'' ソフトバンククリエイティブ 2011. . History * June 1, 1964 - The region around Mount Rausu declared Shiretoko National Park * July 2005 - Shiretoko registered as a Natural World Heritage Site File:Rausu-Shiretoko Io Volcano Group Relief Map, SRTM-1.jpg, Rausu- Shiretoko Io Volcano Group. Rausu (lower left) ...
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Ōshima, Hokkaidō
(means "big island") is an uninhabited island in the Sea of Japan, to the west from Matsumae town and therefore the westernmost point of Hokkaido. It is part of the town of Matsumae in Oshima Subprefecture in Hokkaido, Japan. To distinguish Ōshima from other islands with the same name, it is sometimes known as or . At , Ōshima is the largest uninhabited island under Japanese sovereignty. The island is a double caldera with a scoria hill rising in the middle. It is the peak of two overlapping stratovolcanoes and their associated calderas, Mount Higashi and Mount Nishi. The highest peak, at , is part of a triple volcano. The peak rises close to from the sea floor. The island consists of mafic alkali and non-alkali volcanic rock, less than 18,000 years old. On the south side of the island at , there is a lighthouse and a heliport operated by Japan Coast Guard. Because of volcanic activity and nature conservation, landing on the island requires the approval of the Agency for ...
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