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El Salvador · Stratovolcano

San Vicente

Type
Stratovolcano
Elevation
2149m
Last eruption
Unknown
San Vicente
Photo: Kristal Dorion, (U.S. Geological Survey) · Public domain · Wikimedia Commons
Type
Stratovolcano
Country
El Salvador
Region
Middle America & Caribbean / Central America Volcanic Arc
Elevation
2149m
Coordinates
13.597, -88.838
Last eruption
Unknown
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Andesite / Basaltic andesite
Geological summary

San Vicente stratovolcano, also known as Chichontepec, is ~20 km SE of Lake Ilopango. The andesitic edifice with two summit peaks was constructed within the Pleistocene La Carbonera caldera, whose rim is visible only on its SW side. The N and S flanks are covered by lava flows from the central vent, but lava flows on the eastern side originated from a vent on the upper flank. Volcanism has continued into the Holocene, but the latest lava flows are covered by deposits from the major Tierra Blanca eruption from Ilopango around 450 CE. Reports of eruptions in 1643 CE and 1835 CE are false (Catalog of Active Volcanoes of the World; Sapper, 1917), but numerous hot springs and fumaroles are found on the N and W flanks.

From Wikipedia

San Vicente is a stratovolcano in central El Salvador. It is located next to the town of San Vicente and is the second highest volcano in El Salvador. In the indigenous language Nahuat, Chichontepec means the mountain of the two breasts, because its double summit resembles a woman's bosom. The volcano has two craters, one located in each summit, although not exactly at the top. A dense jungle covers both summits. Numerous hot springs and fumaroles are found on the northern and western flanks of the volcano. To the northeast, at 820 metres in a ravine of 180 metres longitude, there are fumaroles—fountains of clear and muddy water or small volcanoes of mud.

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Eruption history

Glossary

Detailed timeline

No eruption records available.

Nearby volcanoes

External links

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