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Chachimbiro

Estratovolcán · Ecuador · 4106 m

Part of the Chachimbiro volcanic complex, located about 25 km NW of the city of Ibarra, is seen from the south.  The late Pleistocene-to-Holocene, NNE-trending dacitic Chachimbiro-Pucará line of lava domes includes the Pitzantzi lava dome, which erupted about 5700 years ago, producing an ash deposit that extends to the NW.   Hot springs and thermal areas are present at the Chachimbiro complex. Quarries in the foreground are cut into deposits from the caldera-forming eruption of Cuicocha volcano.
Part of the Chachimbiro volcanic complex, located about 25 km NW of the city of Ibarra, is seen from the south. The late Pleistocene-to-Holocene, NNE-trending dacitic Chachimbiro-Pucará line of lava domes includes the Pitzantzi lava dome, which erupted about 5700 years ago, producing an ash deposit that extends to the NW. Hot springs and thermal areas are present at the Chachimbiro complex. Quarries in the foreground are cut into deposits from the caldera-forming eruption of Cuicocha volcano. · Foto: Photo by Lee Siebert, 2006 (Smithsonian Institution). · Wikimedia Commons
Tipo
Estratovolcán
País
Ecuador
Región
South America Volcanic Regions / Northern Andean Volcanic Arc
Altitud
4106 m
Coordenadas
0.468, -78.287
Última erupción
-3740
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Dacite
Resumen geológico

The Chachimbiro volcanic complex lies about 25 km NW of the city of Ibarra. Late Pleistocene collapse of the andesitic Huanguillaro stratovolcano produced a 6.8 km3 debris-avalanche deposit and a 4-km-wide avalanche caldera open to the east that has largely been filled by lava domes, including the rhyodacitic Hugá dome. The avalanche deposit is overlain by three large ignimbrites and pyroclastic-flow deposits related to dome growth. The late Pleistocene-to-Holocene, NNE-trending, dacitic Chachimbiro-Pucará line of lava domes includes the Pitzantzi dome, which erupted about 5,700 years ago, producing an ash deposit that extends to the NW. Hot springs and thermal areas are present in the complex.

Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
3740 BCE~3740 BCE · 1 erupciones · VEI máx. 33740 BCE3740 BCE3739 BCE3739 BCE3739 BCE

Línea de tiempo detallada

  1. 3740 a. C.VEI 3Estimación geológica
    BCE 3740 – En curso
    NNE flank (Pitzantzi lava dome)

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.