Hirogawa, Wakayama
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Hirogawa, Wakayama
270px, Inamura no hi no yakata is a town in Arida District, Wakayama Prefecture, Japan. , the town had an estimated population of 6,778 in 2833 households and a population density of 100 persons per km². The total area of the town is . Geography Hirogawa is located on the coast in north-central Wakayama Prefecture, facing the Kii Channel. The Hirogawa River flows through the town. The climate is moderated by the influence of the Kuroshio Current offshore. Neighboring municipalities Wakayama Prefecture * Yuasa * Aridagawa * Yura * Hidaka * Hidakagawa Climate Hirogawa has a Humid subtropical climate (Köppen ''Cfa'') characterized by warm summers and cool winters with light to no snowfall. The average annual temperature in Hirogawa is 15.7 °C. The average annual rainfall is 1878 mm with September as the wettest month. The temperatures are highest on average in August, at around 26.0 °C, and lowest in January, at around 5.8 °C. The area is subject to t ...
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Towns Of Japan
A town (町; ''chō'' or ''machi'') is a local administrative unit in Japan. It is a local public body along with prefecture (''ken'' or other equivalents), city (''shi''), and village (''mura''). Geographically, a town is contained within a district. Note that the same word (町; ''machi'' or ''chō'') is also used in names of smaller regions, usually a part of a ward in a city. This is a legacy of when smaller towns were formed on the outskirts of a city, only to eventually merge into it. Towns See also * Municipalities of Japan * Japanese addressing system The Japanese addressing system is used to identify a specific location in Japan. When written in Japanese characters, addresses start with the largest geographical entity and proceed to the most specific one. When written in Latin characters, ad ... References {{reflist External links "Large_City_System_of_Japan";_graphic_shows_towns_compared_with_other_Japanese_city_types_at_p._1_[PDF_7_of_40/nowiki>">DF_7_of_4 ...
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Aridagawa, Wakayama
file:Aragijima003.JPG, 270px, Aragijima rice terraces is a List of towns in Japan, town located in Arida District, Wakayama, Arida District, in central Wakayama Prefecture, Japan. , the town had an estimated population of 25,940 in 10680 households and a population density of 74 persons per km². The total area of the town is . Geography Aridagawa is located in the north-center of Wakayama prefecture, with the Aridagawa River running through the center of the town. Although there are some flatlands along the Aridagawa River, most of the town tends to be mountainous. * Mountains: Mt. Washigamine (589m) * Flatlands: Aridagawa Plain * Rivers: Aridagawa River (Futagawa Dam)It was established on January 1, 2006, by the merger of the towns of Kanaya, Wakayama, Kanaya, Kibi, Wakayama, Kibi and Shimizu, Wakayama, Shimizu, all from Arida District, Wakayama, Arida District. Neighboring municipalities Wakayama Prefecture :Arida, Wakayama, Arida, Kainan, Wakayama, Kainan, Tanabe, Wakayama, ...
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Tsunami
A tsunami ( ; from ja, 津波, lit=harbour wave, ) is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations, landslides, glacier calvings, meteorite impacts and other disturbances) above or below water all have the potential to generate a tsunami. Unlike normal ocean waves, which are generated by wind, or tides, which are in turn generated by the gravitational pull of the Moon and the Sun, a tsunami is generated by the displacement of water from a large event. Tsunami waves do not resemble normal undersea currents or sea waves because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide. For this reason, it is often referred to as a tidal wave, although this usage is not favoured by the scientific community because it might give ...
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The Fire Of Rice Sheaves
is a story based on the events of the 1854 Nankai earthquake's tsunami. This story explains the importance of alertness to the tsunami after the earthquake and early evacuation, and the sacrificial spirit for saving lives. When the 1854 tsunami, In Hiro (now Hirogawa), Goryo Hamaguchi set fires using rice straw to help guide villagers to safety. This story was turned into "A living god" by the Greek-born writer Lafcadio Hearn. Hamaguchi saved the lives of many of his fellow villagers of Hiro, Kii Province (current Hirogawa, Wakayama), when a massive tsunami struck the Kii Peninsula in 1854. He set fire to stacks of rice sheaves as landmarks to guide villagers to safety. Lafcadio Hearn wrote a story about him in ''Gleanings in Buddha-Fields: Studies of Hand and Soul in the Far East'' (1897), called "Inamura no Hi: The burning rice fields". Overview Thanks to the story ''Inamura no Hi: The Burning Rice Fields'' by Tsunezo Nakai (translated and published in English by Sara C ...
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Hamaguchi Goryō
was a village headman in Hiro, Kii Province (current Hirogawa, Wakayama) noted for his role in saving villagers from a tsunami during the 1854 Ansei-Nankai earthquake. In the Meiji period, he became an entrepreneur, the seventh owner of Yamasa, the noted soy sauce brewer, philanthropist and politician. Biography Early history Hamaguchi Goryō was born to a cadet branch of the Hamaguchi family in what is now Yuasa, Wakayama. The Hamaguchi family were soy sauce brewers and merchants, and had operations in both Shimosa and Kii Province. At the age of 12, he was adopted by the main family, which was based at what is now Chōshi, Chiba, where he relocated. In October 1839, he married a daughter of Ikenaga Umetaro in Yuasa at the age of 20. After staying in Hiro-mura for another six months, he returned to Chōshi via Edo in the following spring. By the time, he already mastered techniques of martial arts, especially ''kendo''. In addition, he was very good at composing and writing ...
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1854 Ansei-Nankai Earthquake
The 1854 Nankai earthquake occurred at about 16:00 local time on 24 December. It had a magnitude of 8.4 and caused a damaging tsunami. More than 30,000 buildings were destroyed and there were at least 3,000 casualties. It was the second of the three Ansei great earthquakes; the 1854 Tōkai earthquake of identical magnitude had hit northwest the previous morning, and the third 1855 Edo earthquake would strike less than a year later. Background The southern coast of Honshu runs parallel to the Nankai Trough, which marks the subduction of the Philippine Sea Plate beneath the Eurasian Plate. Movement on this convergent plate boundary leads to many earthquakes, some of them of the megathrust type. The Nankai megathrust has five distinct segments (A–E) that can rupture independently, the segments have ruptured either singly or together repeatedly over the last 1300 years. Megathrust earthquakes on this structure tend to occur in pairs, with a relatively short time gap between them. ...
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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 the Tok ...
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Kofun Period
The is an era in the history of Japan from about 300 to 538 AD (the date of the introduction of Buddhism), following the Yayoi period. The Kofun and the subsequent Asuka periods are sometimes collectively called the Yamato period. This period is the earliest era of recorded history in Japan, but studies depend heavily on archaeology since the chronology of historical sources tends to be distorted. The word '' kofun'' is Japanese for the type of burial mound dating from this era. It was a period of cultural import. Continuing from the Yayoi period, the Kofun period is characterized by influence from China and the Korean Peninsula; archaeologists consider it a shared culture across the southern Korean Peninsula, Kyūshū and Honshū. On the other hand, the most prosperous keyhole-shaped burial mounds in Japan during this period were approximately 5,000 in Japan from the middle of the 3rd century in the Yayoi period to the 7th century in the Asuka period, and many of them had huge t ...
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Jōmon Period
The is the time in Japanese history, traditionally dated between   6,000–300 BCE, during which Japan was inhabited by a diverse hunter-gatherer and early agriculturalist population united through a common Jōmon culture, which reached a considerable degree of sedentism and cultural complexity. The name "cord-marked" was first applied by the American zoologist and orientalist Edward S. Morse, who discovered sherds of pottery in 1877 and subsequently translated it into Japanese as ''Jōmon''.Mason, 14 The pottery style characteristic of the first phases of Jōmon culture was decorated by impressing cords into the surface of wet clay and is generally accepted to be among the oldest in the world. The Jōmon period was rich in tools and jewelry made from bone, stone, shell and antler; pottery figurines and vessels; and lacquerware.Imamura, K. (1996) ''Prehistoric Japan: New Perspectives on Insular East Asia''. Honolulu: University of Hawaii Press It is often compared to pre-C ...
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Kii Province
, or , was a province of Japan in the part of Honshū that is today Wakayama Prefecture, as well as the southern part of Mie Prefecture. Nussbaum, Louis-Frédéric. (2005). "''Kii''" in . Kii bordered Ise, Izumi, Kawachi, Shima, and Yamato Provinces. The Kii Peninsula takes its name from this province. During the Edo period, the Kii branch of the Tokugawa clan had its castle at Wakayama. Its former ichinomiya shrine was Hinokuma Shrine. The Japanese bookshop chain Kinokuniya derives its name from the province. Historical districts * Wakayama Prefecture ** Ama District (海部郡) - merged with Nagusa District to become Kaisō District (海草郡) on April 1, 1896 ** Arida District (有田郡) ** Hidaka District (日高郡) ** Ito District (伊都郡) ** Naga District (那賀郡) - dissolved ** Nagusa District (名草郡) - merged with Ama District to become Kaisō District on April 1, 1896 * Mixed ** Muro District (牟婁郡) *** Higashimuro District (東牟婁郡) ...
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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 thr ...
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Humid Subtropical Climate
A humid subtropical climate is a zone of climate characterized by hot and humid summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates. It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classification was officially created under the Trewartha climate classification. In this classification, climates are termed humid subtropical when the ...
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