Pulau Faial
Fayal
Stratovolkan · Portugal · 1041 m

- Tipe
- Stratovolkan
- Negara
- Portugal
- Wilayah
- Atlantic Ocean Volcanic Regions / 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
Pulau Faial adalah sebuah pulau di kepulauan Azores, Portugal. Gunung berapi Capelinhos, titik paling barat dari pulau itu, mungkin juga menjadi titik paling barat di Eropa, jika Kepulauan Monchique, dekat Pulau Flores, dianggap sebagai bagian dari Amerika Utara, karena ia berada di Lempeng Amerika Utara.
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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.