Nankaidō in the context of "Awa province (Tokushima)"

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⭐ Core Definition: Nankaidō

Nankaidō (南海道; Japanese pronunciation: [naŋ.kaꜜi.doː], lit.'Southern Sea Circuit') is a Japanese geographical term. It means both an ancient division of the country and the main road running through it. The road connected provincial capitals in this region. It was part of the Gokishichidō system.

The Nankaidō encompassed the pre-Meiji provincial lands of Kii and Awaji, plus the four provinces that made up the island of Shikoku: Awa, Sanuki, Tosa, and Iyo.

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Nankaidō in the context of Awa Province (Tokushima)

Awa Province (阿波国, Awa no Kuni; Japanese pronunciation: [aꜜ.wa (no kɯ.ɲi)]) was a province of Japan in the area that is today Tokushima Prefecture on the island of Shikoku. Awa was bordered by Tosa, Sanuki, and Iyo Provinces. Its abbreviated form name was Ashū (阿州). In terms of the Gokishichidō system, Awa was one of the provinces of the Nankaidō circuit. Under the Engishiki classification system, Awa was ranked as one of the 35 "superior countries" (上国) in terms of importance, and one of the "middle countries" (中国) in terms of distance from the capital. The provincial capital was located in what is now the city of Tokushima.

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Nankaidō in the context of Tosa Province

Tosa Province (土佐国, Tosa no Kuni; Japanese pronunciation: [toꜜ.sa (no kɯ.ɲi), to.saꜜ (no kɯ.ɲi)]) was a province of Japan in the area of southern Shikoku. Tosa bordered on Awa to the northeast, and Iyo to the northwest. Its abbreviated form name was Doshū (土州). In terms of the Gokishichidō system, Tosa was one of the provinces of the Nankaidō circuit. Under the Engishiki classification system, Tosa was ranked as one of the "middle countries" (中国) in terms of importance, and one of the "far countries" (遠国) in terms of distance from the capital. The provincial capital was located in what is now the city of Nankoku. The ichinomiya of the province is the Tosa shrine located in the city of Kōchi.

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Nankaidō in the context of Sanuki Province

Sanuki Province (讃岐国, Sanuki no Kuni; Japanese pronunciation: [saꜜ.nɯ.kʲi (no kɯ.ɲi), sa.nɯ.kʲiꜜ (no kɯ.ɲi)]) was a province of Japan in the area of northeastern Shikoku. Sanuki bordered on Awa to the south, and Iyo to the west. Its abbreviated form name was Sanshū (讃州). In terms of the Gokishichidō system, Sanuki was one of the provinces of the Nankaidō circuit. Under the Engishiki classification system, Sanuki was ranked as one of the "upper countries" (上国) in terms of importance, and one of the "middle countries" (中国) in terms of distance from the capital. The provincial capital was located in what is now the city of Sakaide, but its exact location was only identified in 2012. The ichinomiya of the province is the Tamura jinja located in the city of Takamatsu.

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Nankaidō in the context of Iyo Province

Iyo Province (伊予国, Iyo no Kuni; Japanese pronunciation: [iꜜ.jo (no kɯ.ɲi)]) was a province of Japan in the area of northwestern Shikoku. Iyo bordered on Sanuki Province to the northeast, Awa to the east, and Tosa to the south. Its abbreviated form name was Yoshū (予州). In terms of the Gokishichidō system, Iyo was one of the provinces of the Nankaidō circuit. Under the Engishiki classification system, Iyo was ranked as one of the "upper countries" (上国) in terms of importance, and one of the "far countries" (遠国) in terms of distance from the capital. The provincial capital was located in what is now the city of Imabari, but its exact location is still unknown. The ichinomiya of the province is the Ōyamazumi Shrine located on the island of Ōmishima in what is now part of Imabari. The people spoke Iyo dialect.

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Nankaidō in the context of Nankai Trough

The Nankai Trough (南海トラフ, Nankai Torafu; Southern Sea Trough) is a submarine trough located south of the Nankaidō region of Japan's island of Honshu, extending approximately 900 km (559 mi) offshore. The underlying fault, the Nankai megathrust, is the source of the devastating Nankai megathrust earthquakes, while the trough itself is potentially a major source of hydrocarbon fuel, in the form of methane clathrate.

In plate tectonics, the Nankai Trough marks a subduction zone that is caused by subduction of the Philippine Sea plate beneath Japan, part of the Eurasian plate (Kanda et al., 2004). This plate boundary would be an oceanic trench except for a high flux of sediments that fills the trench. Within the Nankai Trough there is a large amount of deformed trench sediments (Ike, 2004), making one of Earth's best examples of accretionary prism. Furthermore, seismic reflection studies have revealed the presence of basement highs that are interpreted as seamounts that are covered in sediments (Ike, 2004). The northern part of the trough is known as the Suruga Trough, while to the east is the Sagami Trough. The Nankai Trough runs roughly parallel to the Japan Median Tectonic Line.

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