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Chachimbiro

Stratovolcano · Ecuador · 4106m

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. · Photo: Photo by Lee Siebert, 2006 (Smithsonian Institution). · Wikimedia Commons
Type
Stratovolcano
Country
Ecuador
Region
South America Volcanic Regions / Northern Andean Volcanic Arc
Elevation
4106m
Coordinates
0.468, -78.287
Last eruption
-3740
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Landform
Composite
Major rock type
Dacite
Geological summary

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.

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
3740 BCE~3740 BCE · 1 eruptions · max VEI 33740 BCE3740 BCE3739 BCE3739 BCE3739 BCE

Detailed timeline

  1. 3740 BCEVEI 3Geological estimate
    BCE 3740 – Ongoing
    NNE flank (Pitzantzi lava dome)

External links

⚠ For reference only. Not for emergency response.