Global Volcanism Program | Image GVP-02719

The irregular mound in the center of the photo is Cinder Cone, a late-Pleistocene cone of the Garibaldi Lake volcanic field. The cone formed during two periods of activity, the latest of which produced a lava flow down the glaciated valley to the north. Photo by Lee Siebert, 1983 (Smithsonian Institution).

The irregular mound in the center of the photo is Cinder Cone, a late-Pleistocene cone of the Garibaldi Lake volcanic field. The cone formed during two periods of activity, the latest of which produced a lava flow down the glaciated valley to the north.

Photo by Lee Siebert, 1983 (Smithsonian Institution).

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Keywords: cone | erosion

Garibaldi Lake