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Usulutan

Volcano
Usulután volcano is a stratovolcano in east-central El Salvador, at the SE end of a cluster of basaltic to basaltic-andesite stratovolcanoes between San Vicente and San Miguel volcanoes. The volcano contains a broad 1.3-km-wide summit crater breached to the east. The flanks of the forested Usulután volcano are strongly eroded and suggest a long repose interval, but young lava flows are present on its southern flanks. They are probably less than 10,000 years old. Cerro Nanzal is a flank cone on the lower SE flank and was mapped as Holocene.
Volcano typestratovolcano normal or dormant
LocationEl Salvador
Summit elevation1449 m / 4,754 ft
Usulutan volcano eruptionsunknown, less than 10,000 years ago
Typical eruption styleeffusive
 

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