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Periodic collapse of the oversteepend front of the dome produced pyroclastic flows that traveled progressively farther down the Mizunashi valley.

Photo courtesy Shimbara Earthquake and Volcano Observatory, 1991.

This was near the beginning of a period of renewed activity at the Caliente vent, on the eastern side of Santiaguito.

Growth of the composite Santiaguito lava dome has been occurring since 1922.

Dome formation is often preceded or accompanied by explosive eruptions, and dome collapse can produce pyroclastic flows and debris avalanches.

Incandescent rockfalls accompanying slow growth of the summit lava dome descend from beneath a cloudcap covering the summit of Merapi volcano in this 1993 nighttime view.

Periodic collapse of Merapi's lava dome has produced pyroclastic flows down the western and southern flanks that have devastated populated areas and agricultural lands.

Cerro Sincholagua (left) and Loma la Marca (right) are the southernmost of a group of lava domes pre-dating the formation of Pululagua's caldera.

The Novy lava dome at Kamchatka's Bezymianny volcano has been growing since 1956 within a large horseshoe-shaped crater.

The 1.8 x 2.5 km crater formed during the catastrophic 1956 eruption when the summit of the volcano collapsed, producing a debris avalanche and lateral blast that swept to the east.

Photo by Charles Pineo, 1967 (Dartmouth College, courtesy of Dick Stoiber).

A small blocky lava dome fills the crater of Caliente vent on the Santiaguito lava dome of Guatemala's Santa María volcano on July 18, 1969.




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(Photo by Chris Hondros/Newsmakers) KSTW is Seattle’s home for The CW Network!