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Quilotoa

Caldera · Ecuador · 3914 m

Quilotoa is a truncated, forested dacitic cone containing a steep-walled, 3-km-wide caldera filled by a 250-m-deep lake.  Lava domes form the caldera's perimeter and occupy its floor.  Its most recent large eruption about 800 years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes.  Reports of historical eruptions from the caldera lake are somewhat ambiguous.  Fumaroles are present on the lake floor and hot springs occur on the eastern flank.
Quilotoa is a truncated, forested dacitic cone containing a steep-walled, 3-km-wide caldera filled by a 250-m-deep lake. Lava domes form the caldera's perimeter and occupy its floor. Its most recent large eruption about 800 years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes. Reports of historical eruptions from the caldera lake are somewhat ambiguous. Fumaroles are present on the lake floor and hot springs occur on the eastern flank. · Foto: Photo by Minard Hall, 1973 (Escuela Politécnica Nacional, Quito). · Wikimedia Commons
Tipo
Caldera
Paese
Ecuador
Regione
South America Volcanic Regions / Northern Andean Volcanic Arc
Altitudine
3914 m
Coordinate
-0.859, -78.904
Ultima eruzione
1280
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Caldera
Roccia principale
Dacite
Sintesi geologica

Quilotoa is a truncated, dacitic cone in the Western Cordillera of Ecuador, 35 km WNW of the city of Latacunga, that contains a 3-km-wide caldera with steep-sided walls that rise 400 m above the surface of 240-m-deep caldera lake. Multiple lava domes are present along the caldera's perimeter. This small volcano has produced eight major explosive eruptions during the past 200,000 years. Its most recent major eruption about 800 radiocarbon years ago produced voluminous pyroclastic flows, lahars that reached the Pacific Ocean, and one of the largest airfall-tephra deposits of the northern Andes. Formation of the caldera was followed by extrusion of a small lava dome. Reports of observed eruptions from the caldera lake are somewhat ambiguous. Fumaroles are present on the lake floor and hot springs occur on the E flank.

Sintesi da Wikipedia

Il Quilotoa è un lago di origine vulcanica dell'Ecuador, situato nella provincia del Cotopaxi, nella parte occidentale delle Ande ecuadoriane.

Wikipedia · CC BY-SA · Leggi l'articolo completo

Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
1280~1332 · 1 eruzioni · VEI max. 61694~1745 · 2 eruzioni · VEI max. 21745~1797 · 2 eruzioni · VEI max. 212801383153916421745

Cronologia dettagliata

  1. 1797VEI ?Stima geologica
    1797-02-04 – In corso
  2. 1759VEI 2Stima geologica
    1759 – In corso
  3. 1740VEI 2Stima geologica
    1740-12 – In corso
  4. 1725VEI 2Stima geologica
    1725 – In corso
  5. 1280VEI 6Stima geologica
    1280 – In corso

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