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Global Volcanism Program | Image GVP-01324

Ikedako is a 4.5-km-wide lake-filled caldera that was formed as a result of a major explosive eruption about 4,600 years ago. Kaimon is the highest peak of the Ibusuki volcanic field, rising to the SW above the caldera rim. The eruption of the 3 km3 Ikeda pumice was the the largest Holocene eruption in the Ibusuki volcanic field, which consists of a group of small central volcanoes and maars, along with Ikedako caldera and Kaimon. Photo by Lee Siebert, 1988 (Smithsonian Institution).

Ikedako is a 4.5-km-wide lake-filled caldera that was formed as a result of a major explosive eruption about 4,600 years ago. Kaimon is the highest peak of the Ibusuki volcanic field, rising to the SW above the caldera rim. The eruption of the 3 km3 Ikeda pumice was the the largest Holocene eruption in the Ibusuki volcanic field, which consists of a group of small central volcanoes and maars, along with Ikedako caldera and Kaimon.

Photo by Lee Siebert, 1988 (Smithsonian Institution).

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Galleries: Calderas

Keywords: caldera | volcanic field


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