Contact | RSS | EN | DE | EL | ES | FR | IT | RU

Ilopango volcano

Updated: Mar 4, 2024 06:13 GMT -
caldera 450 m / 1,476 ft
El Salvador, 13.67°N / -89.05°W
Current status: normal or dormant (1 out of 5)

Ilopango volcano is a 8x11 km wide caldera at the eastern margin of San Salvador city, El Salvador. It is elongated to the east, has 150-500 m high walls and contains the scenic Lake Ilopango, one of El Salvador's largest.
The caldera is the result of at least 4 large plinian eruptions over the past few tens of thousands years. The lastest of these occurred in the 5th centruy AD. A historic eruption in 1879-80 formed Islas Quemadas ("burnt islands"), a group of islands in the center of the lake, corresponding to the summit of a mostly submerged post-caldera lava dome.

Show interactive Map
[hide map] [enlarge]
Typical eruption style: explosive
Ilopango volcano eruptions: 1879-80, 450 AD ±30 years

Latest nearby earthquakes

TimeMag. / DepthDistance/Location
Feb 26, 03:36 pm (El Salvador)
Feb 26, 21:36 GMT
3.3

5 km
26 km (16 mi) to the SW Departamento de La Libertad, 17 km southwest of San Salvador, El Salvador
I FELT IT
Info
Sunday, February 25, 2024 GMT (1 quake)
Feb 24, 11:36 pm (El Salvador)
Feb 25, 05:36 GMT
2.5

5 km
21 km (13 mi) to the NW 17 km north of San Salvador, San Salvador, El Salvador Info
Saturday, February 24, 2024 GMT (1 quake)
Feb 24, 08:34 am (El Salvador)
Feb 24, 14:34 GMT
2.7

7 km
21 km (13 mi) to the E 10.1 km northwest of San Vicente, San Vicente, El Salvador Info
Tuesday, February 20, 2024 GMT (1 quake)
Feb 20, 10:17 am (El Salvador)
Feb 20, 16:17 GMT
3.2

8 km
21 km (13 mi) to the E 10.5 km northwest of San Vicente, San Vicente, El Salvador Info
Wednesday, February 28, 2024 GMT (1 quake)
Feb 27, 06:06 pm (El Salvador)
Feb 28, 00:06 GMT
2.4

5 km
21 km (13 mi) to the E 8.7 km northwest of San Vicente, San Vicente, El Salvador Info
Saturday, February 24, 2024 GMT (1 quake)
Feb 24, 06:09 am (El Salvador)
Feb 24, 12:09 GMT
2.2

7 km
21 km (13 mi) to the E 12 km northwest of San Vicente, San Vicente, El Salvador Info

Background

The caldera is controlled by regional faults of the central Salvador graben. 4 major dacitic-rhyolitic explosive eruptions during the late Pleistocene and Holocene produced extensive pyroclastic-flow and pyroclastic-fall deposits that blanket much of El Salvador. The latest collapse of Ilopango caldera resulted from the massive 5th century AD Terra Blanca Joven (TBJ) eruption, which produced widespread pyroclastic flows and devastated early Mayan cities. Post-caldera eruptions formed a series of glassy dacitic and andesitic lava domes within the lake and near its shore.

Sources & further reading:
- Smithsonian / GVP Ilopango volcano information
- Golombek, M.P., and Carr, M.J. (1978) "Tidal triggering of seismic and volcanic phenomena during the 1879-1880 eruption of Islas Quemadas volcano in El Salvador, central America", Journal of Volcanology and Geothermal Research, v. 3, pp. 299-307
- Richer (2004) "Mafic magma injection triggers eruption at Ilopango Caldera, El Salvador, Central America", Geol. Soc. Special Paper, v 375, pp. 175-189
- Hart, W.J.E., and Steen-Mcintyre, V. (1983) "Tierra Blanca Joven tephra from the AD 260 eruption of Ilopango caldera", in: Sheets, P.D., ed. "Archeology and Volcanism in Central America", Austin, University of Texas Press, pp. 14-34
- Sheets, P.D. (1979) "Maya recovery from volcanic disasters, Ilopango and Ceren", Archaeology, v. 32, pp. 32-42
- Sheets, P.D. (1979) "Environmental and cultural effects of the Ilopango eruption in Central America", in: Sheets, P.D., ed. "Archeology and Volcanism in Central America", Austin, University of Texas Press, pp. 14-34

1879-80 eruption
The last eruption of Ilopango constructed a new lava dome which emerged above the caldera lake and formed the Islas Quemadas, the "burnt islands".
It has been speculated that the eruption was affected by solid-earth tides, but a much more convincing and likely explanation was provided by Richer et al (2004) who demonstrate that an injection of 2% of basaltic-andesitic magma at the base of partially crystallized dacite magma triggered the 1880 eruption, creating the necessary overpressure needed for an eruption. ...more

5th century eruption of Ilopango (around 450 AD)
A violent Plinian eruption occurred at Ilopango in the 5th century AD. It was the largest eruption in El Salvador during the past 10,000 years and one of the largest in Central America.
The eruption was larger than the Krakatau 1883 or Pinatubo in 1991, and probably more comparable to Tambora 1815. It ranks VEI 6-7. It erupted more than 70 cu km of tephra, produced major ash fall and large pyroclastic flows that covered 10,000 sq km under 50 cm or more of pumice and ash. Pyroclastic flows and ash fall devastated an area of up to 100 km radius around the volcano.
The eruption severely impacted the cultural history of the region: at the time, a sophisticated Mayan culture ruled and lived in the highlands of El Salvador. The eruption killed thousands, destroyed settlements and sent many to flee to the lowland areas in Guatemala and Belize. It ended the Mayan presence in the highlands, and it took probably several centuries for the region to recover.
A major trade route controlled by the Mayas was abandoned and power shifted to Tikal. Modern excavations of some of the buried settlements have been bringing light into Mayan culture.

See also: Sentinel hub | Landsat 8 | NASA FIRMS

No news in this list.