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Global Volcanism Program | Image GVP-01888

Taal caldera, seen here from its NW rim, is a 15 x 20 km caldera of Pleistocene and Holocene age. Volcano Island, in the north-central part of Lake Taal, is constructed of coalescing small tuff  and scoria cones. Powerful phreatomagmatic explosive eruptions from several locations on the 5-km-wide island have produced deadly pyroclastic surges. Photo by Chris Newhall, 1978 (U.S. Geological Survey).

Taal caldera, seen here from its NW rim, is a 15 x 20 km caldera of Pleistocene and Holocene age. Volcano Island, in the north-central part of Lake Taal, is constructed of coalescing small tuff and scoria cones. Powerful phreatomagmatic explosive eruptions from several locations on the 5-km-wide island have produced deadly pyroclastic surges.

Photo by Chris Newhall, 1978 (U.S. Geological Survey).

Creative Commons Icon This image is made available as a Public Domain Work, but proper attribution is appreciated.


Taal