Mount Myōgi
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Mount Myōgi
is one of the major mountains in Gunma Prefecture, Japan. Its straddles the border between the municipalities of Annaka, Shimonita and Tomioka. Well known for its rocks weathered into fantastic forms, this famous peak is ranked among Japan's three most noted places of rugged beauty. There are many hiking courses, and when the foliage changes color there are splendid views to be seen. The highest point is the peak of the Mt. Sōmadake (相馬岳) reaching .It is also a National Place of Scenic Beauty as determined by the Agency for Cultural Affairs in Japan in 1923. Mount Myōgi, along with Mount Akagi and Mount Haruna, is one of the "Three Mountains of Jōmō". (Jōmō is an old name for Gunma.). It is also featured on the 'mo' card in Jomo Karuta. Overview Mount Myōgi is composed of many different peaks: Hakuun-zan (白雲山), Kondō-san (金洞山), Kinkei-san (金鶏山), Sōma-dake (相馬岳), Mitake-san (御岳山), Chōsunokashira (丁須ノ頭), Yakyu-san (谷急 ...
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Gunma Prefecture
is a prefecture of Japan located in the Kantō region of Honshu. Gunma Prefecture has a population of 1,937,626 (1 October 2019) and has a geographic area of 6,362 km2 (2,456 sq mi). Gunma Prefecture borders Niigata Prefecture and Fukushima Prefecture to the north, Nagano Prefecture to the southwest, Saitama Prefecture to the south, and Tochigi Prefecture to the east. Maebashi is the capital and Takasaki is the largest city of Gunma Prefecture, with other major cities including Ōta, Isesaki, and Kiryū. Gunma Prefecture is one of only eight landlocked prefectures, located on the northwestern corner of the Kantō Plain with 14% of its total land being designated as natural parks. History The ancient province of Gunma was a center of horse breeding and trading activities for the newly immigrated continental peoples. The arrival of horses and the remains of horse tackle coincides with the arrival of a large migration from the mainland. From this point forward, the hor ...
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Mount Fuji
, or Fugaku, located on the island of Honshū, is the highest mountain in Japan, with a summit elevation of . It is the second-highest volcano located on an island in Asia (after Mount Kerinci on the island of Sumatra), and seventh-highest peak of an island on Earth. Mount Fuji is an active stratovolcano that last erupted from 1707 to 1708. The mountain is located about southwest of Tokyo and is visible from there on clear days. Mount Fuji's exceptionally symmetrical cone, which is covered in snow for about five months of the year, is commonly used as a cultural icon of Japan and it is frequently depicted in art and photography, as well as visited by sightseers and climbers. Mount Fuji is one of Japan's along with Mount Tate and Mount Haku. It is a Special Place of Scenic Beauty and one of Japan's Historic Sites.
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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 terrain ...
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List Of Places Of Scenic Beauty Of Japan (Gunma)
This list is of the Monuments of Japan, Places of Scenic Beauty of Japan located within the Prefectures of Japan, Prefecture of Gunma Prefecture, Gunma. National Places of Scenic Beauty As of 1 August 2020, eight Places have been Cultural Properties of Japan, designated at a national level; Sanbaseki Gorge spans the prefectural borders with Saitama Prefecture, Saitama. Prefectural Places of Scenic Beauty As of 1 May 2019, five Places have been Cultural Properties of Japan, designated at a prefectural level. Municipal Places of Scenic Beauty As of 1 May 2019, twenty-seven Places have been Cultural Properties of Japan, designated at a municipal level. See also * Cultural Properties of Japan * :en:Parks and gardens in Gunma Prefecture, List of parks and gardens of Gunma Prefecture * List of Historic Sites of Japan (Gunma) References External links * {{in lang, ja}Cultural Properties in Gunma Prefecture
Tourist attractions in Gunma Prefecture Places of Scenic Beaut ...
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Myōgi, Gunma
was a town located in Kanra District, Gunma Prefecture, Japan. On March 27, 2006, Myōgi was merged into the expanded city of Tomioka. In 2003, the town had an estimated population of 4,901 and a density of 170.41 persons per km². The total area was 28.76 km². See also * Mount Myōgi is one of the major mountains in Gunma Prefecture, Japan. Its straddles the border between the municipalities of Annaka, Shimonita and Tomioka. Well known for its rocks weathered into fantastic forms, this famous peak is ranked among Japan's th ... External links Tomioka official website Dissolved municipalities of Gunma Prefecture Tomioka, Gunma {{Gunma-geo-stub ...
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Initial D
is a Japanese street racing manga series written and illustrated by Shuichi Shigeno. It was serialized in Kodansha's ''seinen'' manga magazine ''Weekly Young Magazine'' from 1995 to 2013, with the chapters collected into 48 ''tankōbon'' volumes. The story focuses on the world of illegal Japanese street racing, where all the action is concentrated in the mountain passes and rarely in cities or urban areas, and with the drifting racing style emphasized in particular. Professional race car driver and pioneer of drifting Keiichi Tsuchiya helped with editorial supervision. The story is centered on the prefecture of Gunma, more specifically on several mountains in the Kantō region and in their surrounding cities and towns. Although some of the names of the locations the characters race in have been fictionalized, all of the locations in the series are based on actual locations in Japan. ''Initial D'' has been adapted into several anime television and original video ...
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Tomioka Silk Mill
is Japan's oldest modern model silk reeling factory, established in 1872 by the government to introduce modern machine silk reeling from France and spread its technology in Japan. The factory is designated by the government as a National Historic Site and all its buildings are preserved in very good condition. It is located in the city of Tomioka, Gunma Prefecture, Japan, about 100 km northwest of Tokyo. It is also featured as the 'ni' card in Jomo Karuta playing cards. History Following the Meiji restoration, the new Meiji government needed export products to raise the monies necessary for the industrialization and westernization of Japan. Goods which were already produced in Japan and which could be exported for good profit included tea, silk thread and silkworm cocoons. Especially with the spread of the silkworm disease called pébrine in France and Italy, and the turmoil in China caused by the Taiping Rebellion, Japanese silk was in high demand. In 1862, shortly be ...
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100 Landscapes Of Japan (Shōwa Era)
The is a list of famous scenic sites in Japan. The 100 Landscapes or Views were selected alongside further sets of 8 Views and 25 Winning Sites in 1927, a year after Hirohito became Emperor. The selection was intended to "reflect the new taste of the new era". The nomination and voting process was sponsored by the Tokyo Nichi Nichi Shimbun and Osaka Mainichi Shimbun. The landscapes or views are divided into eight classes (1) Coastlines (2) Lakes (3) Mountains (4) Rivers (5) Gorges (6) Waterfalls (7) Onsen (8) Plains. Many of these landscapes are now included among Japan's National Parks. Eight Views Twenty-Five Winning Sites 100 Views See also * 100 Landscapes of Japan (Heisei era) * Three Views of Japan * 100 Soundscapes of Japan * Tourism in Japan * Meisho originally referred to sites in Japan famous for their associations with specific poetic or literary references. With the development of woodblock printing and newer styles of tourism during the Edo period, th ...
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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 ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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Tuff
Tuff is a type of rock made of volcanic ash ejected from a vent during a volcanic eruption. Following ejection and deposition, the ash is lithified into a solid rock. Rock that contains greater than 75% ash is considered tuff, while rock containing 25% to 75% ash is described as tuffaceous (for example, ''tuffaceous sandstone''). Tuff composed of sandy volcanic material can be referred to as volcanic sandstone. Tuff is a relatively soft rock, so it has been used for construction since ancient times. Because it is common in Italy, the Romans used it often for construction. The Rapa Nui people used it to make most of the ''moai'' statues on Easter Island. Tuff can be classified as either igneous or sedimentary rock. It is usually studied in the context of igneous petrology, although it is sometimes described using sedimentological terms. Tuff is often erroneously called tufa in guidebooks and in television programmes. Volcanic ash The material that is expelled in a volcanic ...
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Dacite
Dacite () is a volcanic rock formed by rapid solidification of lava that is high in silica and low in alkali metal oxides. It has a fine-grained (aphanitic) to porphyritic texture and is intermediate in composition between andesite and rhyolite. It is composed predominantly of plagioclase feldspar and quartz. Dacite is relatively common, occurring in many tectonic settings. It is associated with andesite and rhyolite as part of the subalkaline volcanic rock, subalkaline tholeiite, tholeiitic and calc-alkaline magma series. Composition Dacite consists mostly of plagioclase feldspar and quartz with biotite, hornblende, and pyroxene (augite or enstatite). The quartz appears as rounded, corroded phenocrysts, or as an element of the ground-mass. The plagioclase in dacite ranges from oligoclase to andesine and labradorite. Sanidine occurs, although in small proportions, in some dacites, and when abundant gives rise to rocks that form rhyodacite, transitions to the rhyolites. The rel ...
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