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Global Volcanism Program | Image GVP-07860

Tolimán volcano is 4 km away beyond the summit of Atitlán. Atitlán was constructed over the approximate rim of the Atitlán III caldera, whereas Tolimán was built over the margin of Atitlán II caldera. The irregular Lake Atitlán shoreline to the left is formed by lava flows from Tolimán. The far Atitlán III caldera rim can be faintly seen across the lake. The two post-caldera cones have dramatically different eruptive styles, with lava flows dominating at Tolimán and pyroclastic eruptions at Atitlán.  Photo by Bill Rose, 1983 (Michigan Technological University).

Tolimán volcano is 4 km away beyond the summit of Atitlán. Atitlán was constructed over the approximate rim of the Atitlán III caldera, whereas Tolimán was built over the margin of Atitlán II caldera. The irregular Lake Atitlán shoreline to the left is formed by lava flows from Tolimán. The far Atitlán III caldera rim can be faintly seen across the lake. The two post-caldera cones have dramatically different eruptive styles, with lava flows dominating at Tolimán and pyroclastic eruptions at Atitlán.

Photo by Bill Rose, 1983 (Michigan Technological University).

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Keywords: stratovolcano | caldera


Tolimán