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Global Volcanism Program | Image GVP-02675

These islands and peninsulas on the north coast of Augustine formed in 1883 when collapse of the summit produced a large debris avalanche. Deposits from the highly mobile avalanche extended the island up to 2 km beyond the pre-1883 shoreline. Pyroclastic flows from that eruption also reached the new coastline and emplaced the light-colored deposits to the lower left. Photo by Lee Siebert (Smithsonian Institution).

These islands and peninsulas on the north coast of Augustine formed in 1883 when collapse of the summit produced a large debris avalanche. Deposits from the highly mobile avalanche extended the island up to 2 km beyond the pre-1883 shoreline. Pyroclastic flows from that eruption also reached the new coastline and emplaced the light-colored deposits to the lower left.

Photo by Lee Siebert (Smithsonian Institution).

Creative Commons Icon This image is made available under the Public Domain Dedication CC0 license, but proper attribution is appreciated.

Galleries: debris avalanche deposit | deposit | debris avalanche


Augustine