Minamiizu Town Hall
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Minamiizu Town Hall
is a List of towns in Japan, town located at the southern tip of Izu Peninsula in Kamo District, Shizuoka, Kamo District, Shizuoka Prefecture, Japan. , the town had an estimated population of 8,231 in 3895 households, and a population density of 74 persons per km². The total area of the town is Geography Minamiizu occupies the southern tip of Izu Peninsula, a hilly region with an indented ria coastline facing the Philippine Sea of the Pacific Ocean. The area has numerous hot springs. Warmed by the warm Kuroshio Current, the area enjoys a warm maritime climate with hot, humid summers and mild, cool winters. Parts of the town are within the borders of Fuji-Hakone-Izu National Park, and the historic Irōzaki Lighthouse is located at the tip of Cape Irōzaki, to the south of town. Neighboring municipalities Shizuoka Prefecture *Shimoda, Shizuoka, Shimoda *Matsuzaki, Shizuoka, Matsuzaki Climate The city has a climate characterized by hot and humid summers, and relatively mild win ...
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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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Population
Population typically refers to the number of people in a single area, whether it be a city or town, region, country, continent, or the world. Governments typically quantify the size of the resident population within their jurisdiction using a census, a process of collecting, analysing, compiling, and publishing data regarding a population. Perspectives of various disciplines Social sciences In sociology and population geography, population refers to a group of human beings with some predefined criterion in common, such as location, race, ethnicity, nationality, or religion. Demography is a social science which entails the statistical study of populations. Ecology In ecology, a population is a group of organisms of the same species who inhabit the same particular geographical area and are capable of interbreeding. The area of a sexual population is the area where inter-breeding is possible between any pair within the area and more probable than cross-breeding with in ...
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Izu Province
was a province of Japan in the area of Shizuoka Prefecture. Nussbaum, Louis-Frédéric. (2005). "''Izu''" in . Izu bordered on Sagami and Suruga Provinces. Its abbreviated form name was . The mainland portion of Izu Province, comprising the Izu Peninsula, is today the eastern portion of Shizuoka Prefecture and the Izu Islands are now part of Tokyo. History In 680 A.D., two districts of Suruga Province, Tagata District and Kamo District, were separated into the new Izu Province. At some point between the year 701 and 710, Naka District was added. The capital of the new province was established at Mishima, which also had the ''Kokubun-ji'' and the Ichinomiya ( Mishima Taisha) of the province. Under the ''Engishiki'' classification system, Izu was ranked as a "lesser country" (下国). Under the ''ritsuryō'' legal system, Izu was one of the preferred locations for exile for those convicted of political crimes by the Heian period court. In the Kamakura period, Izu was rule ...
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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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Matsuzaki, Shizuoka
270px, Matsuzaki Town Hall is a town located in on the southwest coast of Izu Peninsula in Kamo District, Shizuoka Prefecture, Japan. , the town had an estimated population of 6,563 in 2969 households, and a population density of 77 persons per km². The total area of the town is . ''Sakuramochi'' is a noted local specialty. Matsuzaki is listed as one of The Most Beautiful Villages in Japan. Geography Matsuzaki is located on the southwest coast of Izu Peninsula, facing Suruga Bay on the Pacific Ocean. It is a hilly region with an indented ria coastline. The area has numerous hot springs. Warmed by the warm Kuroshio Current, the area enjoys a warm maritime climate with hot, humid summers and mild, cool winters. Parts of the town are within the borders of Fuji-Hakone-Izu National Park. Neighboring municipalities Shizuoka Prefecture * Shimoda *Minamiizu * Kawazu * Nishiizu Demographics Per Japanese census data, the population of Matsuzaki has been in slow decline over the past 50 ...
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Shimoda, Shizuoka
270px, Shimoda City Hall is a city and port located in Shizuoka Prefecture, Japan. , the city had an estimated population of 21,402 in 10,787 households, and a population density of 200 persons per km2. The total area of the city is . In the 1850s, Japan was in political crisis over its increasing inability to maintain its national seclusion policy and the issue of what relations, if any, it should have with foreign powers. For a few years, Shimoda was central to this debate. Geography Shimoda is located at the southern tip of the Izu Peninsula about 100 kilometres southwest of Tokyo. Shimoda's location, with the Amagi Mountains to the north, and the warm Kuroshio Current to the south give the city a humid, sub-tropical climate. Surrounding Municipalities *Shizuoka Prefecture **Minamiizu ** Kawazu ** Matsuzaki Demographics Per Japanese census data, the population of Shimoda has been in slow decline over the past 40 years. Climate The city has a climate characterized by ...
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Cape Irōzaki
is a headland on southernmost point on the Izu Peninsula on the island of Honshu in Japan. It is located within the borders of the town of Minamiizu, Shizuoka and is within the borders of the Fuji-Hakone-Izu National Park. The cape marks the border between Sagami Bay and Suruga Bay, and the border between the Philippine Sea and the Pacific Ocean. Irōzaki Lighthouse stands on the cape. The cape also contains a Shinto shrine, the Imuro Jinja, which claims to have been founded in the Nara period The of the history of Japan covers the years from CE 710 to 794. Empress Genmei established the capital of Heijō-kyō (present-day Nara). Except for a five-year period (740–745), when the capital was briefly moved again, it remained the cap .... Climate Gallery Irozaki 2013-08-11.jpg, From above Irozaki-Lighthouse.JPG, From offshore File:Irozaki Minamiizu Japan.jpg, NE view from Irōzaki References External links *{{Commons category inline, Cape IroJapan Travel Guide
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Irōzaki Lighthouse
is a lighthouse located on a hill at the outermost extremity of Cape Irōzaki south of the town of Minamiizu, Shizuoka Prefecture, Japan on the southernmost extremity of Izu Peninsula. It is located within the borders of the Fuji-Hakone-Izu National Park. History Although not one of the eight lighthouses stipulated specifically by the provisions of the Anglo-Japanese Treaty of Amity and Commerce of 1858, the Irōzaki Lighthouse was one of the earliest of the 26 lighthouses to be built in Meiji period Japan by British engineer Richard Henry Brunton, and was the tenth western style lighthouse to be completed in Japan. Its construction was given priority by the Meiji government due to the frequency of marine accidents off the Izu Peninsula. The original structure as designed by Brunton was octagonal, and was constructed of wood. Work began in July 1871. The Irōzaki lighthouse was completed on October 5, 1871. This structure was destroyed during a wind storm on November 14, 1932 ...
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Fuji-Hakone-Izu National Park
is a national park in Yamanashi, Shizuoka, and Kanagawa Prefectures, and western Tokyo Metropolis, Japan. It consists of Mount Fuji, Fuji Five Lakes, Hakone, the Izu Peninsula, and the Izu Islands. Fuji-Hakone-Izu National Park covers . Rather than being a specific spot, the park is a collection of dispersed tourist sites that dot the region. The farthest point south, the isle of Hachijō-jima, is several hundred kilometers from Mount Fuji. The park includes a variety of geographic features including natural hot springs, coastlines, mountainous areas, lakes, and more than 1000 volcanic islands. Vegetation in the park ranges from species of mountainous trees to the subtropical vegetation of the Izu Islands. Fuji-Hakone-Izu National Park was established on February 2, 1936, as Fuji-Hakone National Park, and is one of the first four national parks established in Japan. In 1950, the Izu islands were added to the park, and its name changed to its present designation. Due to its prox ...
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Maritime Climate
An oceanic climate, also known as a marine climate, is the humid temperate climate sub-type in Köppen classification ''Cfb'', typical of west coasts in higher middle latitudes of continents, generally featuring cool summers and mild winters (for their latitude), with a relatively narrow annual temperature range and few extremes of temperature. Oceanic climates can be found in both hemispheres generally between 45 and 63 latitude, most notably in northwestern Europe, northwestern America, as well as New Zealand. Precipitation Locations with oceanic climates tend to feature frequent cloudy conditions with precipitation, low hanging clouds, and frequent fronts and storms. Thunderstorms are normally few, since strong daytime heating and hot and cold air masses meet infrequently in the region. In most areas with an oceanic climate, precipitation comes in the form of rain for the majority of the year. However, some areas with this climate see some snowfall annually during winter. ...
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Kuroshio Current
The , also known as the Black or or the is a north-flowing, warm ocean current on the west side of the North Pacific Ocean basin. It was named for the deep blue appearance of its waters. Similar to the Gulf Stream in the North Atlantic, the Kuroshio is a powerful western boundary current that transports warm equatorial water poleward and forms the western limb of the North Pacific Gyre, North Pacific Subtropical Gyre. Off the East Coast of Japan, it merges with the Oyashio Current to form the North Pacific Current. The Kuroshio Current has significant effects on both physical and biological processes of the North Pacific Ocean, including nutrient and sediment transport, major pacific storm tracks and regional climate, and Pacific mode water formation.Terazaki, Makoto (1989) "Recent Large-Scale Changes in the Biomass of the Kuroshio Current Ecosystem" in Kenneth Sherman and Lewis M. Alexander (eds.), Biomass Yields and Geography of Large Marine Ecosystems (Boulder: Westview) AAA ...
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Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its ...
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