Chinameca
Stratovolcano · El Salvador · 1300m

- Type
- Stratovolcano
- Country
- El Salvador
- Region
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- Elevation
- 1300m
- Coordinates
- 13.478, -88.330
- Last eruption
- Unknown
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The small Chinameca stratovolcano (also known as El Pacayal) lies across a low saddle abotu 7 km NW of the large San Miguel volcano. A 2-km-wide, steep-sided caldera, Laguna Seca el Pacayal, truncates the summit, whose flanks are covered with coffee plantations. The Holocene cone of Cerro el Limbo on the W flank rises above the level of the caldera rim, and a Holocene lava flow extends from a NNW-flank vent into the lowlands to the N beyond the town of Chinameca (Weber and Weisemann, 1978). A group of fumarole fields on the N flank surrounds the city of Chinameca, and the volcano has been the site of a geothermal exploration program.
From Wikipedia
Chinameca is a stratovolcano in central-eastern El Salvador. It lies north of San Miguel volcano and rises over the town of Chinameca. The volcano is topped by a 2 kilometres (1.2 mi) wide caldera known as Laguna Seca el Pacayal, and a satellite cone on the west side, Cerro el Limbo, rises higher than the caldera rim. Fumaroles can be found on the north side, and it has been the site of a geothermal exploration program.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
No eruption records available.
External links
⚠ For reference only. Not for emergency response.