Report on Suwanosejima (Japan) — 19 October-25 October 2022
Smithsonian Institution / US Geological Survey
Weekly Volcanic Activity Report, 19 October-25 October 2022
Managing Editor: Sally Sennert.
Please cite this report as:
Global Volcanism Program, 2022. Report on Suwanosejima (Japan) (Sennert, S, ed.). Weekly Volcanic Activity Report, 19 October-25 October 2022. Smithsonian Institution and US Geological Survey.
29.638°N, 129.714°E; summit elev. 796 m
All times are local (unless otherwise noted)
JMA reported that the eruption at Suwanosejima's Ontake Crater continued during 17-24 October. Crater incandescence was visible nightly. A total of 119 explosions during 17-21 October produced eruption plumes that rose as high as 2 km above the crater rim and ejected blocks as far as 800 m from the vent. Occasional rumbling noises and ashfall were reported in Toshima village (3.5 km SSW). Only one explosion was reported during 21-24 October. Plumes rose as high as 1.5 km and blocks were ejected as far as 200 m from the vent. Ashfall was reported in Toshima village. The Alert Level remained at 3 (on a 5-level scale), and residents were warned to stay 2 km away from the crater.
Geological Summary. The 8-km-long island of Suwanosejima in the northern Ryukyu Islands consists of an andesitic stratovolcano with two historically active summit craters. The summit is truncated by a large breached crater extending to the sea on the east flank that was formed by edifice collapse. One of Japan's most frequently active volcanoes, it was in a state of intermittent Strombolian activity from Otake, the NE summit crater, between 1949 and 1996, after which periods of inactivity lengthened. The largest recorded eruption took place in 1813-14, when thick scoria deposits blanketed residential areas, and the SW crater produced two lava flows that reached the western coast. At the end of the eruption the summit of Otake collapsed, forming a large debris avalanche and creating the open Sakuchi caldera, which extends to the eastern coast. The island remained uninhabited for about 70 years after the 1813-1814 eruption. Lava flows reached the eastern coast of the island in 1884. Only about 50 people live on the island.