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Tourist attractions in Iinan, Shimane

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1.Iinan, Shimane
Iinan (飯南町, Iinan-chō) is a town located in Iishi District, Shimane Prefecture, Japan. It was formed on January 1, 2005 from the merger of the towns of Tonbara and Akagi, both from Iishi District. As of March 1, 2017 the town has a population of 4,908 and a density of 20 persons per km². The area is 242.84 km².
population:4,391人 area:242.88km2
Official site  Wikipedia

Iinan, Shimane in park

1.Mount Sanbe  ・
Mount Sanbe, also known as Sanbesan, is an active stratovolcano in Ōda, Shimane Prefecture. The highest peak, Osanbe, has an elevation of 1,126 m (3,694 ft). At the center of the volcano is a caldera 1 km (0.62 mi) across. The volcano's composition is mainly dacite and andesite. Volcanic activity was believed to have started 100 thousand years ago. The volcano frequently produces explosive eruptions with several classified as Plinian eruptions. All of these explosive eruptions occurred during the Pleistocene while one occurred in the Holocene at the Taiheizan lava dome approximately 3,700 years ago. The Holocene eruption triggered pyroclastic flows down the northeastern and southeastern flanks, reaching the Hayamizu River in the south. More recent eruptions have taken place but they are not precisely dated.[1][2]
Wikipedia    Details  

Iinan, Shimane in Mountain

2.Mount Sanbe
Mount Sanbe, also known as Sanbesan, is an active stratovolcano in Ōda, Shimane Prefecture. The highest peak, Osanbe, has an elevation of 1,126 m (3,694 ft). At the center of the volcano is a caldera 1 km (0.62 mi) across. The volcano's composition is mainly dacite and andesite. Volcanic activity was believed to have started 100 thousand years ago. The volcano frequently produces explosive eruptions with several classified as Plinian eruptions. All of these explosive eruptions occurred during the Pleistocene while one occurred in the Holocene at the Taiheizan lava dome approximately 3,700 years ago. The Holocene eruption triggered pyroclastic flows down the northeastern and southeastern flanks, reaching the Hayamizu River in the south. More recent eruptions have taken place but they are not precisely dated.[1][2]
Wikipedia    Details