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English: Izu Oshima in Izu Islands, Tokyo, Japan. ... Description= {{en|Relief map of Izu Ōshima island, Izu Islands, Tokyo, Japan. From "SRTM-1 (30m Mesh) ...
Izu Ōshima (伊豆大島, Izu-ōshima) is an inhabited volcanic island in the Izu archipelago in the Philippine Sea, off the coast of Honshu, Japan, 22 km (14 mi) east of the Izu Peninsula and 36 km (22 mi) southwest of Bōsō Peninsula. [1]
The Izu Islands are divided into two towns (Oshima and Hachijojima) and six villages (the remaining inhabited islands.) Three subprefectures are formed above the municipalities as branch offices of the metropolitan government. [citation needed] All the islands (more than a dozen in total) lie within the Fuji-Hakone-Izu National Park.
1986 Izu Ōshima eruption. Mount Mihara's major eruption in 1986 saw lava fountains up to 1.6 kilometres (1.0 mi) high. The eruption had a Volcanic Explosivity Index of 3, and involved a central vent eruption, radial fissure eruption, explosive eruption, lava flows, and a lava lake eruption. There was also a 16 km high subplinian plume. All of ...
Izu-Torishima Island seen from the west, 2002 Tori-shima is located in the Philippine Sea approximately 600 km (373 mi) south of Tokyo and 76 km (47 mi) north of Lot's Wife . The roughly circular-shaped island is listed as a Class A active volcano by the Japan Meteorological Agency .
As this name of the Seven Islands of Izu continued to be used even today, the islanders of the islands other than the Seven Islands feel discriminated., [1] and the Aogashima villagers in particular have petitioned not to use it at every opportunity. In connection with this, the affiliated organization of Tokyo, the "Izu Seven Islands Tourism ...
After the start of the Meiji period, in 1878, the island came under the control of Tokyo-fu and was organized into six villages (Okada, Motomura, Senzu, Nomashi, Sashikiji and Habuminato) under Oshima subprefecture on April 1, 1908. The six villages were merged to form Ōshima Town on April 1, 1955.
Relief Map. Tanna Fault (right) Tanna Fault surface rupture Ravine of Tanna Fault viewed from N. Tanna Fault (丹那断層, Tanna Dansō) is a left lateral strike-slip fault which runs along the northeast side of Izu Peninsula south 30 km to Izu City in Japan. It was responsible for the magnitude 7.0 1930 North Izu earthquake (北伊豆地震). [1]