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Tokachi-Mitsumata Caldera
Tokachi-Mitsumata Caldera is an 8-km wide volcanic caldera in the Ishikari Mountains of Daisetsuzan National Park in Hokkaidō, Japan. The caldera is bounded to the north by the Central Ishikari Mountains, Ishikari Mountains and to the southwest by the Nipesotsu-Maruyama Volcanic Group. See also * List of volcanoes in Japan References Tokachi-Mitsumata Caldera Quaternary Volcanoes of Japan, Geological Survey of Japan, AIST, 2006 * Calderas of Hokkaido Volcanoes of Hokkaido Pleistocene calderas {{Japan-protected-area-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tokachi Mitsumata Caldera Relief Map, SRTM-1 (born 1973), Japanese cinematographer
{{geodis ...
is a place name used in or near Tokachi Subprefecture, Hokkaidō. It may also refer to: * Tokachi District, Hokkaido, in Tokachi Subprefecture * Tokachi Province (1869–1882), an old province of Hokkaidō * Tokachi Plain, a plain in eastern Hokkaidō * Mount Tokachi (Daisetsuzan), a volcano in central Hokkaidō * Mount Tokachi (Hidaka), a mountain in the Hidaka Mountains of eastern Hokkaidō * '' Super Tokachi'', a train service in Hokkaidō People * Tokachi Tsuchiya is a film maker. He was born in Kyoto in 1973. In 1997 he began his studies of cinema. Film career ''A Normal Life, Please'', his début film, focuses on a cement truck driver and the brutal conditions that he is subjected to by his employers, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caldera
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a Volcanic crater, crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish language, S ... [...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 Types of volcanic eruptions, volcanic eruptions and .... References Hokkaipedia, Daisetsuzan Mountains last access 2 July 2008. Mountain ranges of Hokkaido {{Hokkaido-geo-stub ... [...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] |
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 the isla ... [...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] |
Central Ishikari Mountains
The , or more commonly referred to simply as the {{nihongo, Ishikari Mountains, 石狩山地, Ishikari Sanchi, are a group of mountains in central Hokkaidō, Japan. List of peaks *Mount Ishikari * Mount Otofuke * Mount Mikuni * Mount Yuniishikari * Mount Numanohara Geography These mountains border Tokachi-Mitsumata Caldera to the south and Nipesotsu-Maruyama Volcanic Group Nipesotsu-Maruyama is a volcanic group situated in Hokkaidō, Japan. It is composed of several stratovolcanoes and lava domes, including: * Mount Nipesotsu * Mount Maru (Kamishihoro-Shintoku) * Mount Tengu * Mount Kotengu * Mount Gunkan * ... to the southwest. Mountain ranges of Hokkaido ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nipesotsu-Maruyama Volcanic Group
Nipesotsu-Maruyama is a volcanic group situated in Hokkaidō, Japan. It is composed of several stratovolcanoes and lava domes, including: * Mount Nipesotsu * Mount Maru (Kamishihoro-Shintoku) * Mount Tengu * Mount Kotengu * Mount Gunkan * 1332 Meter Peak * Mount Upepesanke 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 * External links Nipesotsu-Maruyama Volcano Group- Geological Survey of Japan Volcanoes of Hokkaido Volcanism of Japan Volcanic groups {{Hokkaido-geo-stub ... [...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 a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calderas Of Hokkaido
A caldera ( ) is a large cauldron-like hollow that forms shortly after the emptying of a magma chamber in a volcano eruption. When large volumes of magma are erupted over a short time, structural support for the rock above the magma chamber is gone. The ground surface then collapses into the emptied or partially emptied magma chamber, leaving a large depression at the surface (from one to dozens of kilometers in diameter). Although sometimes described as a crater, the feature is actually a type of sinkhole, as it is formed through subsidence and collapse rather than an explosion or impact. Compared to the thousands of volcanic eruptions that occur each century, the formation of a caldera is a rare event, occurring only a few times per century. Only seven caldera-forming collapses are known to have occurred between 1911 and 2016. More recently, a caldera collapse occurred at Kīlauea, Hawaii in 2018. Etymology The term ''caldera'' comes from Spanish ', and Latin ', meaning "c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Hokkaido
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] |
