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Volcán Ecuador

Ecuador

Volcán en escudo · Ecuador · 790 m

An aerial view of Volcán Ecuador from the south shows the large horseshoe-shaped caldera breached to the west that was formed when the volcano collapsed, producing a large submarine debris avalanche.  The volcano straddles the equator at the NW end of Isabela Island.  Two large pyroclastic cones were constructed along the coast, and smaller cones are found on the caldera floor.  Extensive dark-colored lava flows (right) originate from a NE-trending line of fissures that extends from the outer eastern flanks of the main edifice.
An aerial view of Volcán Ecuador from the south shows the large horseshoe-shaped caldera breached to the west that was formed when the volcano collapsed, producing a large submarine debris avalanche. The volcano straddles the equator at the NW end of Isabela Island. Two large pyroclastic cones were constructed along the coast, and smaller cones are found on the caldera floor. Extensive dark-colored lava flows (right) originate from a NE-trending line of fissures that extends from the outer eastern flanks of the main edifice. · Foto: Photo by Patricio Ramon, 2005 (Instituto Geofisca, Escuela Politecnica Nacional). · Wikimedia Commons
Tipo
Volcán en escudo
País
Ecuador
Región
Eastern Pacific Volcanic Regions / Galapagos Hotspot Volcano Group
Altitud
790 m
Coordenadas
-0.020, -91.546
Última erupción
1150
Contexto tectónico
Rift zone / Oceanic crust (< 15 km)
Forma volcánica
Shield
Roca principal
Basalt / Picro-Basalt
Resumen geológico

Volcán Ecuador straddles the equator at the NW end of Isabela Island. The western side of the volcano, the smallest of the six large shield volcanoes on the island, is broadly breached by edifice collapse, and youthful lava flows cover much of the caldera floor. Two large pyroclastic cones were constructed along the coast, and several chains of spatter cones and small scoria cones cross the caldera floor, which has a prominent bench on its southern side. A single dark-colored aa lava flow covers about half of the caldera floor. A number of young lava flows reach the coast to form Cape Berkeley, W of a large youthful-looking tuff cone. Extending from the outer eastern flanks of the main edifice is a line of NE-trending fissure-fed vents that connect Volcán Ecuador (also known as Cape Berkeley volcano) with Volcán Wolf. The only Isabela Island volcano without historical eruptions, the youthful morphology of its most recent lava flows nevertheless resembles those of very recent flows on other Isabela Island volcanoes.

Resumen de Wikipedia

Volcán Ecuador es el nombre que recibe un volcán en escudo activo localizado en el norte de la isla Isabela la mayor del archipiélago y parque nacional de las islas Galápagos, que pertenece al país sudamericano de Ecuador y se tiene una elevación máxima de 790 metros sobre el nivel del mar. El volcán contiene flujos de lava, conos de salpicadura y conos pequeños de escoria. No se han registrado erupciones desde que se "descubrieron" las islas en 1535.

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Historial de erupciones

Resumen (VEI en el tiempo)
Haga clic en una barra para ver erupciones individuales
1150~1150 · 1 erupciones · VEI máx. 011501150115111511151

Línea de tiempo detallada

  1. 1150VEI 0Estimación geológica
    1150 – En curso

Enlaces externos

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