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Chachimbiro

Stratovolkan · 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
Tipe
Stratovolkan
Negara
Ecuador
Wilayah
South America Volcanic Regions / Northern Andean Volcanic Arc
Ketinggian
4106 m
Koordinat
0.468, -78.287
Letusan terakhir
-3740
Kondisi tektonik
Subduction zone / Continental crust (> 25 km)
Bentuk lahan
Composite
Batuan utama
Dacite
Ringkasan geologi

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.

Riwayat letusan

Ringkasan (VEI dari waktu ke waktu)
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3740 BCE~3740 BCE · 1 letusan · VEI maks. 33740 BCE3740 BCE3739 BCE3739 BCE3739 BCE

Garis waktu rinci

  1. 3740 SMVEI 3Perkiraan geologi
    BCE 3740 – Berlangsung
    NNE flank (Pitzantzi lava dome)

Tautan eksternal

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