Fayal Volcano
Updated: 29 Ιουνίου 2024 13:39 GMT -
stratovolcano, lavadome 1043 m
Αζόρες (Πορτογαλία), 38.6°N / -28.83°W
Current status: normal or dormant (1 out of 5)
Αζόρες (Πορτογαλία), 38.6°N / -28.83°W
Current status: normal or dormant (1 out of 5)
Last update: 5 Mar 2022
The island of Fayal, also spelled Faial, is the nearest of the central Azorean islands to the Mid-Atlantic Ridge.
[smaller] [larger]
Fayal volcano eruptions: 1957-58
Latest nearby earthquakes
Ώρα | Mag. / Βάθος | Απόσταση / Τοποθεσία | |||
25 Ιου 08:40 (GMT -1) | 2.1 0 km | 29 km δυτικά | Portugal: W Faial | Περ. |
Background
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 blanket the island. Formation of the steep-walled 500-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 and has been the source of all historical eruptions. A dramatic submarine eruption at Capelinhos during 1957-58, the best-studied of historical eruptions in the Azores, created a new island that soon merged with the western peninsula.-----------------------------------
Source: Smithsonian GVP