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Matsuzaki, Shizuoka

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Matsuzaki ( 松崎町 , Matsuzaki-chō ) is a town located in on the southwest coast of Izu Peninsula in Kamo District , Shizuoka Prefecture , Japan . As of 31 July 2019, 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 85.23 square kilometres (32.91 sq mi). Sakuramochi is a noted local specialty. Matsuzaki is listed as one of The Most Beautiful Villages in Japan .

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17-509: 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 . Shizuoka Prefecture Per Japanese census data,

34-417: A major fault along only one of the boundaries, and these are known as half-graben. The polarity (throw direction) of the main bounding faults typically alternates along the length of the rift. The asymmetry of a half-graben strongly affects syntectonic deposition. Comparatively little sediment enters the half-graben across the main bounding fault because of footwall uplift on the drainage systems. The exception

51-573: A planet or moon, bordered by parallel normal faults . Graben is a loan word from German , meaning 'ditch' or 'trench'. The first known usage of the word in the geologic context was by Eduard Suess in 1883. The plural form is either graben or grabens . A graben is a valley with a distinct escarpment on each side caused by the displacement of a block of land downward. Graben often occur side by side with horsts . Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where

68-639: A result of its underlying geology, the peninsula is prone to frequent earthquake swarms and tsunamis , and it abounds in hot springs . All of Izu Peninsula is within Shizuoka Prefecture . It is administratively divided into eight cities and five towns: A popular resort region for tourists from the Kantō region , the Izu peninsula is primarily known for onsen hot spring resorts in Atami , Shuzenji , and Itō. The area

85-957: Is 103.3 km (64.2 mi) from the Yōga Interchange (用賀インター Yōga Intā ) on the Tokyo end of the Tōmei Expressway to Numazu. To get to the eastern side, a branch at Atsugi leads to the Odawara-Atsugi Road , which continues past Odawara to Yugawara, Atami , and Shimoda. Izu Peninsula is also served by Japan National Route 135 , Japan National Route 136 , and Japan National Route 414 . Izu also offers two scenic roads, called " Izu Skyline " (伊豆スカイライン) and " Western Izu Skyline " (西伊豆スカイライン) that offer beautiful views on nature and Mt. Fuji. Both skyline roads are favorite spots of car and motorcycle enthusiasts. The Odakyu Electric Railway runs local bus services from Odawara and Hakone , and there

102-401: Is also popular for sea bathing, surfing, golfing and motorcycle touring. The peninsula abuts Mount Fuji and is a part of Fuji-Hakone-Izu National Park . The southwest coast of Izu, from the municipalities of Matsuzaki, Nishiizu and Minamiizu was designated a National Place of Scenic Beauty in 1937. Aside from tourism, agriculture and fishing are the mainstays of the local economy. Izu

119-412: Is an extensive but infrequent internal bus network. On August 12, 1985, Flight JAL 123 , while crossing peninsular airspace, experienced an explosion in the aft pressure bulkhead, resulting in an accident that killed 520 people, becoming one of the deadliest air disasters in human history. Graben In geology , a graben ( / ˈ ɡ r ɑː b ən / ) is a depressed block of the crust of

136-533: Is one of the biggest producers of wasabi in Japan, and the local cuisine offers dishes flavored with wasabi . Nevertheless, these industries are not lucrative enough to prevent a heavy loss of population to Greater Tokyo and Shizuoka, particularly among the young. The northern parts of Izu peninsula is easily accessible from Tokyo and points west via the Tōkaidō Shinkansen , which has stations in both Atami in

153-693: The Edo period , all of Izu Province was tenryō territory under direct control of the Tokugawa shogunate , and the area now comprising Matsuzaki Town consisted of 21 villages. With the establishment of the modern municipalities system of the early Meiji period in 1889, the area was divided into 11 villages within Kamo District, and 10 villages within Naka District. After the abolishment of Naka District, all 21 villages were reunited under Kamo District. Matsuzaki Village

170-683: The Okhotsk Plate at the Nankai Trough . The Philippine Sea Plate, the Amurian Plate , and the Okhotsk Plate meet at Mount Fuji , a triple junction . The peninsula itself lies on the Philippine Sea Plate. The southern portion of the peninsula is composed largely of breccia , and the central and northern portions consist of numerous highly eroded volcanoes . The Amagi Mountain Range dominates

187-530: The area is forest. Matsuzaki has one public elementary school and one public junior high school operated by the town government. The town has one public high school operated by the Shizuoka Prefectural Board of Education. Izu Peninsula The Izu peninsula ( 伊豆半島 , Izu-hantō ) is a large mountainous peninsula with a deeply indented coastline to the west of Tokyo on the Pacific coast of

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204-479: The center of the peninsula with Mount Amagi (1,406 metres (4,613 ft)) and Mount Atami (773 metres (2,536 ft)) in the east and Mount Daruma (982 metres (3,222 ft)) in the west, with the eastern and western portions of the range extending underwater into Sagami Bay and Suruga Bay . The peninsula's major river, the Kano River in the north, flows through a graben valley created by plate tectonics. As

221-411: The displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides. Horsts are parallel blocks that remain between graben; the bounding faults of a horst typically dip away from the center line of the horst. Single or multiple graben can produce a rift valley . In many rifts , the graben are asymmetric, with

238-479: The island of Honshu , Japan . Formerly known as Izu Province , Izu peninsula is now a part of Shizuoka Prefecture . The peninsula has an area of 1,421.24 km (548.74 sq mi) and its estimated population in 2005 was 473,942 people. The peninsula's populated areas are located primarily on the north and east. Tectonically, the Izu peninsula results from the Philippine Sea Plate colliding with

255-534: The northeast and Mishima in the northwest. JR Itō Line and the Izu Kyūkō Line provides service along the east coast of the peninsula to Shimoda, however given the lack of population, these services are less regular. Central Izu is served by the Sunzu Line as far as Shuzenji. The west coast of the peninsula is less developed, and has no train service. Izu Peninsula is served by numerous expressways. By car, it

272-692: The population of Matsuzaki has been in slow decline over the past 50 years. The city has a climate characterized by hot and humid summers, and relatively mild winters ( Köppen climate classification Cfa ). The average annual temperature in Matsuzaki is 16.4 °C (61.5 °F). The average annual rainfall is 1,962.1 mm (77.25 in) with July as the wettest month. The temperatures are highest on average in August, at around 26.5 °C (79.7 °F), and lowest in January, at around 7.0 °C (44.6 °F). During

289-452: Was elevated to town status in 1901. The town annexed neighboring Nakagawa Village in 1955 and Iwashina Village in 1956. Around March 31, 2010, the city of Shimoda and three municipalities in Kamo District ( Kawazu , Matsuzaki, and Minamiizu ) were scheduled to merge . However, the merger backed out. The economy of Matsuzaki is dominated by commercial fishing , forestry and the tourist industry centered on hot spring resorts . Some 64% of

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