Pulau Faial
Fayal
Stratovolkan · Portugal · 1041 m

- Tipe
- Stratovolkan
- Negara
- Portugal
- Wilayah
- Samudra Atlantik / Azores-Terceira Rift Volcanic Province
- Ketinggian
- 1041 m
- Koordinat
- 38.576, -28.713
- Letusan terakhir
- 1958
- Kondisi tektonik
- Rift zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
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.
Ringkasan Wikipedia
Ringkasan InggrisFaial 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.
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Riwayat letusan
Garis waktu rinci
- 1957VEI 2Teramati1957-09-27 – 1958-10-24West flank (Capelinhos) and summit
- 1672VEI 2Teramati1672-04-24 – 1673-02-28West flank
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.