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Midai River Embankments
The was a system of flood control levees constructed by the Sengoku period warlord Takeda Shingen to protect the central Kōfu Basin in the Chūbu region of Japan. These levees were located in what is now the cities of Nirasaki and Minami-Alps in Yamanashi Prefecture. The remnants were designated a National Historic Site of Japan in 2003, with the area under designation expanded in 2009. Overview The Midai River is an 18.6 kilometer long tributary of the Kamanashi River which originates in the Southern Alps. It was subject to flash flooding due to snow melt off in spring and typhoons in summer and autumn. Massively flooding had been known to occur since ancient times, and even the name of the Midai River (御勅使川) comes from the fact that an Imperial envoy was sent to the area in 825 AD to investigate a flood disaster. The warlord of Kai Province, Takeda Shingen, considered that control of the river was essential for his clan to prosper and to control the province, ...
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Nirasaki, Yamanashi
is a city in Yamanashi Prefecture, Japan. , the city had an estimated population of 29,483 in 12662 households, and a population density of 210 persons per km². The total area is . Geography Nirasaki is located in the northwestern end of the Kofu Basin in Yamanashi Prefecture, bordered to the east by the Minami Alps National Park and the west by the Minami Alps Koma Prefectural Natural Park. Surrounding municipalities Yamanashi Prefecture * Hokuto * Minami-Alps * Kai Climate The city has a climate characterized by characterized by hot and humid summers, and relatively mild winters (Köppen climate classification ''Cfa''). The average annual temperature in Nirasaki is 13/0 °C. The average annual rainfall is 1278 mm with September as the wettest month. Demographics Per Japanese census data, the population of Nirasaki has remained relatively steady in recent decades. History The area around present-day Nirasaki was the ancestral homeland of the Takeda clan, wh ...
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Typhoon
A typhoon is a mature tropical cyclone that develops between 180° and 100°E in the Northern Hemisphere. This region is referred to as the Northwestern Pacific Basin, and is the most active tropical cyclone basin on Earth, accounting for almost one-third of the world's annual tropical cyclones. For organizational purposes, the northern Pacific Ocean is divided into three regions: the eastern (North America to 140°W), central (140°W to 180°), and western (180° to 100°E). The Regional Specialized Meteorological Center (RSMC) for tropical cyclone forecasts is in Japan, with other tropical cyclone warning centers for the northwest Pacific in Hawaii (the Joint Typhoon Warning Center), the Philippines, and Hong Kong. Although the RSMC names each system, the main name list itself is coordinated among 18 countries that have territories threatened by typhoons each year. Within most of the northwestern Pacific, there are no official typhoon seasons as tropical cyclones form th ...
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Historic Sites Of Japan
is a collective term used by the Japanese government's Law for the Protection of Cultural Properties to denote Cultural Properties of JapanIn this article, capitals indicate an official designation as opposed to a simple definition, e.g "Cultural Properties" as opposed to "cultural properties". as historic locations such as shell mounds, ancient tombs, sites of palaces, sites of forts or castles, monumental dwelling houses and other sites of high historical or scientific value; gardens, bridges, gorges, mountains, and other places of great scenic beauty; and natural features such as animals, plants, and geological or mineral formations of high scientific value. Designated monuments of Japan The government ''designates'' (as opposed to '' registers'') "significant" items of this kind as Cultural Properties (文化財 ''bunkazai'') and classifies them in one of three categories: * * , * . Items of particularly high significance may receive a higher classification as: * * * ...
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History Of Yamanashi Prefecture
History (derived ) is the systematic study and the documentation of the human activity. The time period of event before the invention of writing systems is considered prehistory. "History" is an umbrella term comprising past events as well as the memory, discovery, collection, organization, presentation, and interpretation of these events. Historians seek knowledge of the past using historical sources such as written documents, oral accounts, art and material artifacts, and ecological markers. History is not complete and still has debatable mysteries. History is also an academic discipline An academy (Attic Greek: Ἀκαδήμεια; Koine Greek Ἀκαδημία) is an institution of secondary education, secondary or tertiary education, tertiary higher education, higher learning (and generally also research or honorary membershi ... which uses narrative to describe, examine, question, and analyze past events, and investigate their patterns of cause and effect. Histori ...
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List Of Historic Sites Of Japan (Yamanashi)
This list is of the Historic Sites of Japan located within the Prefecture of Yamanashi. National Historic Sites As of 1 June 2022, sixteen Sites have been designated as being of national significance, including Mount Fuji, which spans the prefectural borders with Shizuoka. Prefectural Historic Sites As of 1 April 2022, twenty-eight Sites have been designated as being of prefectural importance. Municipal Historic Sites As of 1 May 2021, a further one hundred and ninety-six Sites have been designated as being of municipal importance. Registered Historic Sites As of 17 June 2022, one Monument has been registered (as opposed to designated) as an Historic Site at a national level. See also * Cultural Properties of Japan * Kai Province * List of Places of Scenic Beauty of Japan (Yamanashi) * Yamanashi Prefectural Museum opened in Fuefuki, Yamanashi Prefecture, Japan in 2005. The collection relates to the natural history, history, and culture of Yamanashi Pr ...
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Chūō Main Line
The , commonly called the Chūō Line, is one of the major trunk railway lines in Japan. It connects Tokyo and Nagoya, although it is the slowest direct railway connection between the two cities; the coastal Tōkaidō Main Line is slightly faster, and the Tōkaidō Shinkansen is currently the fastest rail link between the cities. The eastern portion, the , is operated by the East Japan Railway Company (JR East), while the western portion, the , is operated by the Central Japan Railway Company (JR Central). The dividing point between the two companies is , where express trains from both operators continue to the Shinonoi Line towards the cities of Matsumoto and Nagano. Compared to the huge urban areas at either end of the Chūō Line, its central portion is very lightly traveled; the Shiojiri-Nakatsugawa corridor is only served by one limited express and one local service per hour. The Chūō Main Line passes through the mountainous center of Honshu. Its highest point (near ) ...
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JR Central
is the main railway company operating in the Chūbu (Nagoya) region of central Japan. It is officially abbreviated in English as JR Central and in Japanese as JR Tōkai ( ja, JR東海, links=no). ''Tōkai'' is a reference to the geographical region in which the company chiefly operates. JR Central's operational hub is Nagoya Station and the company's administrative headquarters are located in the JR Central Towers above the station. The busiest and longest railway line operated by JR Central is the Tōkaidō Main Line between and . The company also operates the Tōkaidō Shinkansen between and . Additionally it is responsible for the Chūō Shinkansen—a maglev service between Tokyo and Osaka, which is due to start operation between Tokyo and Nagoya in 2027. JR Central is Japan's most profitable and highest throughput high-speed-rail operator, carrying 138 million high-speed-rail passengers in 2009, considerably more than the world's largest airline. Japan recorded a ...
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Kōfu Station
is the main railway station in the city of Kōfu, Yamanashi Prefecture, Japan. It is managed by the East Japan Railway Company (JR East). Lines Kōfu Station is served by the JR East Chūō Main Line and is 134.1 kilometers from the starting point of the line at . It is also the northern terminus of the 83.1 kilometer JR Central Minobu Line. Layout The station has one side platform and two island platforms which are shared by both JR East and JR Central. The ticket offices and gates are located on a bridge over the tracks. The station has a ''Midori no Madoguchi'' staffed ticket office. Platforms History Kōfu Station was opened on 11 June 1903 with the extension of government railway (later named Chūō Main Line) from Hajikano Station (now Kai-Yamato Station). The line was later extended from Kōfu Station to Nirasaki Station on 15 December 1903. The privately-owned Fuji-Minobu Railway connected Ichikawa-Daimon Station to Kōfu on 30 March 1928. This line was nationa ...
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Edo Period
The or is the period between 1603 and 1867 in the history of Japan, when Japan was under the rule of the Tokugawa shogunate and the country's 300 regional ''daimyo''. Emerging from the chaos of the Sengoku period, the Edo period was characterized by economic growth, strict social order, isolationist foreign policies, a stable population, perpetual peace, and popular enjoyment of arts and culture. The period derives its name from Edo (now Tokyo), where on March 24, 1603, the shogunate was officially established by Tokugawa Ieyasu. The period came to an end with the Meiji Restoration and the Boshin War, which restored imperial rule to Japan. Consolidation of the shogunate The Edo period or Tokugawa period is the period between 1603 and 1867 in the history of Japan, when Japan was under the rule of the Tokugawa shogunate and the country's regional ''daimyo''. A revolution took place from the time of the Kamakura shogunate, which existed with the Tennō's court, to th ...
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Matsuri
Japanese festivals are traditional festive occasions often celebrated with dance and music in Japan. Many festivals have their roots in traditional Chinese festivals, but have undergone extensive changes over time to have little resemblance to their original form, despite sharing the same name and date. There are also various local festivals (e.g. Tobata Gion) that are mostly unknown outside a given prefecture. Unlike most people in East Asia, Japanese people generally do not celebrate the Lunar New Year, its observance having been supplanted by the Western New Year's Day on January 1 in the late 19th century (see Japanese New Year); however, many continue to observe several of its cultural practices. Many Chinese residents in Japan, as well as more traditional shrines and temples, still celebrate the Lunar New Year in parallel with the Western New Year. In Yokohama Chinatown, Japan's biggest Chinatown, tourists from all over Japan come to enjoy the festival, similar to Nagasak ...
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Shogi
, also known as Japanese chess, is a strategy board game for two players. It is one of the most popular board games in Japan and is in the same family of games as Western chess, '' chaturanga, Xiangqi'', Indian chess, and '' janggi''. ''Shōgi'' means general's (''shō'' ) board game (''gi'' ). Western chess is sometimes called (''Seiyō Shōgi'' ) in Japan. Shogi was the earliest chess-related historical game to allow captured pieces to be returned to the board by the capturing player. This drop rule is speculated to have been invented in the 15th century and possibly connected to the practice of 15th century mercenaries switching loyalties when captured instead of being killed. The earliest predecessor of the game, chaturanga, originated in India in the sixth century, and the game was likely transmitted to Japan via China or Korea sometime after the Nara period."Shogi". ''Encyclopædia Britannica''. 2002. Shogi in its present form was played as early as the 16th century, ...
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Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where flow emerges from a confined channel and is free to spread out and infiltrate the surface. This reduces the carrying capacity of the flow and results in deposition of sediments. The flow can take the form of infrequent debris flows or one or more ephemeral or perennial streams. Alluvial fans are common in the geologic record, such as in the Triassic basins of eastern North America and the New Red Sandstone of south Devon. Such fan deposits likely contain the largest accumulations of gravel in the geologic record. Alluvial fans have also been found on Ma ...
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