| Kaimondake | |
|---|---|
| 開聞岳 | |
 Seen from the NNW | |
| Highest point | |
| Elevation | 924 m (3,031 ft) |
| Coordinates | 31°10′48″N 130°31′42″E / 31.18000°N 130.52833°E |
| Geography | |
| Geology | |
| Mountain type | stratovolcano |
| Last eruption | 885 CE[1] |
Kaimondake (開聞岳, Kaimon-dake), or Mount Kaimon, is an undissected[i] volcano – consisting of a basal stratovolcano and a small complex central lava dome[2] – which rises to a height of 924 metres above sea level near the city of Ibusuki in southern Kyūshū, Japan. The last eruption occurred in the year 885 CE. Because of its conic shape, Mt. Kaimon is sometimes referred to as "the Fuji of Satsuma".
- ^ "Ata: Eruptive History". Global Volcanism Program. Smithsonian Institution. Retrieved 2021-06-24.
- ^ Okuno, M.; Nakamura, T.; Kobayashi, T. (1997). "AMS 14C Dating of Historic Eruptions of the Kirishima, Sakurajima and Kaimondake Volcanoes, Southern Kyushu, Japan". Radiocarbon. 40 (2): 825–832. doi:10.1017/S0033822200018786. S2CID 133569925.
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