Almolonga
Stratovulcano · Guatemala · 3173 m

- Tipo
- Stratovulcano
- Paese
- Guatemala
- Regione
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- Altitudine
- 3173 m
- Coordinate
- 14.797, -91.519
- Ultima eruzione
- 1818
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Dacite
Sintesi geologica
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.
Storia delle eruzioni
Cronologia dettagliata
- 1818VEI 2Osservata1818-01-16 – 1818-06-19East flank of Cerro Quemado
- 1765VEI 2Osservata1765-10-24 – 1765-10-25Cerro Quemado
- 800 (±50 anni)VEI 3Stima geologica800 – In corsoCerro Quemado
Link esterni
⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.