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Global Volcanism Program | Image GVP-08055

The circular Apoyo caldera is filled by beautiful Laguna de Apoyo.  The NE caldera wall in the background rises about 120 m above the surface of the lake, which is only 78 m above sea level.  The only road access to the lake is along its western shore.  The caldera was formed by collapse along near-vertical faults following two major dacitic explosive eruptions about 23,000 years ago from a vent area inferred to be near the NE part of the caldera.  Photo by Jaime Incer.

The circular Apoyo caldera is filled by beautiful Laguna de Apoyo. The NE caldera wall in the background rises about 120 m above the surface of the lake, which is only 78 m above sea level. The only road access to the lake is along its western shore. The caldera was formed by collapse along near-vertical faults following two major dacitic explosive eruptions about 23,000 years ago from a vent area inferred to be near the NE part of the caldera.

Photo by Jaime Incer.

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Apoyo