Faial Island
Fayal
Stratovolcano · Portugal · 1041m

- Type
- Stratovolcano
- Country
- Portugal
- Region
- Atlantic Ocean Volcanic Regions / Azores-Terceira Rift Volcanic Province
- Elevation
- 1041m
- Coordinates
- 38.576, -28.713
- Last eruption
- 1958
- Tectonic setting
- Rift zone / Oceanic crust (< 15 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
The island of Fayal, also spelled Faial, is the nearest of the central Azorean islands to the Mid-Atlantic Ridge. The island is composed of a complex large andesitic-to-trachytic stratovolcano that contains a 2-km-wide summit caldera. Thick deposits of trachytic airfall pumice, pyroclastic flows, and lahars related to formation of the caldera cover the island. Formation of the steep-walled 400-m-deep caldera was followed by construction of fissure-fed basaltic lava fields and small volcanoes that form a peninsula extending to the west. This area is covered by the youngest volcanic products on the island. A submarine eruption at Capelinhos during 1957-58 created a new island that soon merged with the western peninsula.
From Wikipedia
Faial Island, also known as Fayal Island, is a Portuguese island contained within the Central Group or Grupo Central of the Azores, in the Atlantic Ocean.
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1957VEI 2Observed1957-09-27 – 1958-10-24West flank (Capelinhos) and summit
- 1672VEI 2Observed1672-04-24 – 1673-02-28West flank
External links
⚠ For reference only. Not for emergency response.