JMA reported that minor eruptive activity continued at Suwanosejima’s Ontake crater during 28 June-3 July. Eruptions were recorded during 28-29 June and on 2 July. Ash plumes at 0952 and 1638 on 28 June rose up to 1.2 km above the crater and drifted NE. The next day, at 1232 and 2129 on 29 June, ash plumes rose up to 1 km above the crater and drifted NE. Ash plumes rose to 1.5 km and drifted NE at 2025 on 2 July. The Alert Level remained at 2 (on a 5-level scale) and the public was warned to stay at least 1 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 active summit craters. The summit is truncated by a large breached crater extending to the sea on the E 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 covered 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 an open collapse scarp extending 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.

Source: Japan Meteorological Agency (JMA)