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Almolonga

Stratovolcano · Guatemala · 3173m

The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818.
The rounded hills in the middle of the photo are part of a chain of lava domes of the Almolonga volcanic field. Partial flank collapse of an edifice sometime prior to 84,000 years ago formed a 3.3-km-wide collapse scarp that is surrounded by a ring-dike configuration of dacite and rhyolite lava domes, seen here from the east. Cerro Quemado is a young dome near the center of the horizon, right of the larger Santa María, that produced a 2.5-km-long lava flow on its eastern flank in 1818. · Photo: Photo by Lee Siebert, 1988 (Smithsonian Institution). · Wikimedia Commons
Type
Stratovolcano
Country
Guatemala
Region
Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
Elevation
3173m
Coordinates
14.797, -91.519
Last eruption
1818
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Dacite
Geological summary

Volcán de Almolonga is an andesitic stratovolcano with a 3.3-km-wide late-Pleistocene central caldera that is located along the Zunil fault zone. The caldera is surrounded by a ring-dike configuration of dacitic and rhyolitic lava domes. The youngest and only historically active dome complex is Cerro Quemado (whose name means Burned Peak), located immediately south of Guatemala's second largest city, Quezaltenango. About 1200 radiocarbon years ago, part of the andesitic-to-dacitic Cerro Quemado dome collapsed, producing a debris avalanche and an associated lateral explosion that swept across the valley to the west as far as the flanks of Siete Orejas volcano. The latest eruption in 1818 produced a blocky 2.5-km-long lava flow. Hot springs are located on the northern and eastern flanks of Cerro Quemado, and the Zuníl geothermal field, the site of a geothermal exploration project, lies on the SE flank of Cerro Quemado.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
800~902 · 1 eruptions · max VEI 31716~1818 · 2 eruptions · max VEI 28001004130915131716

Detailed timeline

  1. 1818VEI 2Observed
    1818-01-16 – 1818-06-19
    East flank of Cerro Quemado
  2. 1765VEI 2Observed
    1765-10-24 – 1765-10-25
    Cerro Quemado
  3. 800 (±50 yrs)VEI 3Geological estimate
    800 – Ongoing
    Cerro Quemado

External links

⚠ For reference only. Not for emergency response.