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Southeast view of Hokkaido-Komagatake
Photo by T.Soya
Komagatake in summer is here.
The main stratovolcano edifice that consists of andesite lava and pyroclastics were formed several ten thousand (40-30 ka) years ago (Stage I).
After that stage, the activities of the volcano were becoming more explosive. Stage II activity started with the collapse of the summit and formed Komagatake Debris Avalanche Deposit (30-23ka). Subsequently, Plinian eruptions accompanying with pyroclastic flows occurred twice until 17ka. At 6ka and 3ka, Stage III activities were Plinian Eruptions with pyroclastic flows.
In Stage IV, historical records of the large eruptions are recorded in 1640, 1694, 1856, 1929 (see Table). These eruptions were Plinian eruptions with pyroclastic flows. It is characteristic that the precursors of eruption were recognized just before the eruptions (one day or several hours before) and the eruptions were become quiet in several days.
| 1640 | Collapse of the edifice, Kurumi-sawa Debris avalanche, Tsunami killed over 700 people. Ko-d pumice fall and pyroclastic flow. |
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| 1694 | Ko-c2 pumice fall and pyroclastic flow. | |
| 1765 | Small eruption? | |
| 1784 | Small eruption. | |
| 1856 | Ko-c1 pumice fall and pyroclastic flow. Ansei crater and lava dome were formed. Two people were killed by pumice fall and 20+ by pyroclastic flow. | |
| 1888 | Small eruption. | |
| 1905 | Small eruption. | |
| 1919-1924 | Small eruption. | |
| 1929 | Ko-a pumice fall and pyroclastic flow. Syowa-4 crater were formed. Two people were killed. | |
| 1935-1938 | Small eruption. | |
| 1942 | Middle eruption. Ash fall. Syowa-17 crater and 1.6km long fissure were formed. | |
| 1996 | Small eruption. Ash fall. |
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