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Mount Maru (Kamishihoro-Shintoku)
| Mount Maru | |
|---|---|
| 丸山 | |
| Highest point | |
| Elevation | 1,692.1 m (5,552 ft)[1] |
| Prominence | 421 m (1,381 ft)[1] |
| Parent peak | Mount Nipesotsu |
| Listing | List of mountains and hills of Japan by height List of volcanoes by elevation |
| Coordinates | 43°25′3″N 143°1′51″E / 43.41750°N 143.03083°E |
| Naming | |
| English translation | round mountain |
| Language of name | Japanese |
| Geography | |
| Location | Hokkaido, Japan |
| Parent range | Nipesotsu-Maruyama Volcanic Group |
| Topo map(s) | Geospatial Information Authority 25000:1 ニペソツ山 25000:1 ウペペサンケ山 50000:1 糠平 |
| Geology | |
| Rock age | Quaternary |
| Mountain type | lava dome |
| Volcanic arc | Kurile arc |
| Last eruption | 1898 |
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Mount Maru (丸山, Maru-yama) is a lava dome located in the Nipesotsu-Maruyama Volcanic Group of the Ishikari Mountains, Hokkaidō, Japan. Mount Maru is also known as Higashi-Tokachi-Maruyama (東十勝丸山)[2] or Higashi-Taisetsu-Maruyama (東大雪丸山)[3] to distinguish it from other mountains with the same name. Only in 1989 did scientists discover that Mount Maru is a quaternary volcano.[2] The mountain sits on the border between the towns of Kamishihoro and Shintoku.[1]
- ^ a b c Geospatial Information Authority topographic map ウペペサンケ山
- ^ a b "Maruyama". Global Volcanism Program. Smithsonian Institution. Retrieved 2010-04-30.
- ^ "HIGASHI-TAISETSU MARU-YAMA". Quaternary Volcanoes in Japan. Geological Survey of Japan, AIST. Archived from the original on 19 December 2012. Retrieved 30 April 2010.
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