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Volcán Ecuador

Ecuador

Shield volcano · Ecuador · 790m

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. · Photo: Photo by Patricio Ramon, 2005 (Instituto Geofisca, Escuela Politecnica Nacional). · Wikimedia Commons
Type
Shield volcano
Country
Ecuador
Region
Eastern Pacific Volcanic Regions / Galapagos Hotspot Volcano Group
Elevation
790m
Coordinates
-0.020, -91.546
Last eruption
1150
Tectonic setting
Rift zone / Oceanic crust (< 15 km)
Landform
Shield
Major rock type
Basalt / Picro-Basalt
Geological summary

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.

From Wikipedia

Volcán Ecuador, also known as Cape Berkeley Volcano, is the smallest of the six shield volcanoes on Isabela Island, one of the Galápagos Islands, with an elevation of 790 m (2,590 ft). It is situated in the west of the Galapagos, straddling the equator, and is the northwestern most point of Isabela Island.

Wikipedia · CC BY-SA · Read full article

Eruption history

Summary (VEI over time)
Click a bar to see individual eruptions
1150~1150 · 1 eruptions · max VEI 011501150115111511151

Detailed timeline

  1. 1150VEI 0Geological estimate
    1150 – Ongoing

External links

⚠ For reference only. Not for emergency response.