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Global Volcanism Program | Image GVP-04429

Fumaroles rise above a small crater (right center) at the base of the headwall of the 6-km-wide summit caldera of Guagua Pichincha volcano.  The breached caldera seen here from the east was formed about 50,000 years ago.  Subsequent late-Pleistocene and Holocene eruptions from the central vent in the breached caldera consisted of explosive activity with pyroclastic flows that accompanied periodic growth and destruction of a lava dome.   Photo by Minard Hall, 1975 (Escuela Politécnica Nacional, Quito).

Fumaroles rise above a small crater (right center) at the base of the headwall of the 6-km-wide summit caldera of Guagua Pichincha volcano. The breached caldera seen here from the east was formed about 50,000 years ago. Subsequent late-Pleistocene and Holocene eruptions from the central vent in the breached caldera consisted of explosive activity with pyroclastic flows that accompanied periodic growth and destruction of a lava dome.

Photo by Minard Hall, 1975 (Escuela Politécnica Nacional, Quito).


Guagua Pichincha