Fonuafoʻou
Fonuafo'ou
Stratovolkan · Tonga · 17 m (bawah laut)

- Tipe
- Stratovolkan
- Negara
- Tonga
- Wilayah
- Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
- Ketinggian
- 17 m (bawah laut)
- Koordinat
- -20.320, -175.420
- Letusan terakhir
- 1936
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
Ringkasan geologi
The ephemeral Fonuafo'ou island in the central part of the Tonga Islands is also known as Falcon Island, named after the British vessel H.M.S. Falcon, which reported a shoal in 1865. Islands up to 6 km long were formed in 1885 and 1927 eruptions; in 1933 the island had a height of more than 145 m. Passing ships often reported "smoke" issuing from the site. The latest explosive activity was reported in 1936. By 1949 the island had eroded beneath sea level, but the summit remains at shallow depths.
Ringkasan Wikipedia
Ringkasan InggrisFonuafo‘ou, formerly known as Falcon Island, is a submarine volcano in the western part of the Ha'apai group in Tonga. The volcano has created an island several times throughout history.
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Riwayat letusan
Garis waktu rinci
- 1936VEI 2Teramati1936-06 – Berlangsung
- 1933VEI 2Teramati1933-04 – Berlangsung
- 1927VEI 2Teramati1927-10-04 – 1928-09
- 1921VEI 0Perkiraan geologi1921-11 – Berlangsung
- 1894VEI 0Perkiraan geologi1894-12 – Berlangsung
- 1885VEI 3Teramati1885-10-12 – 1886
- 1877VEI 2Teramati1877 – Berlangsung
- 1865VEI 0Perkiraan geologi1865 – Berlangsung
- 1781VEI 0Perkiraan geologi1781 – Berlangsung
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.