Tonga · Stratovolkan
Kao
- Tipe
- Stratovolkan
- Ketinggian
- 1009 m
- Letusan terakhir
- 1847

- Tipe
- Stratovolkan
- Negara
- Tonga
- Wilayah
- Tonga & Kermadec / Tofua Volcanic Arc
- Ketinggian
- 1009 m
- Koordinat
- -19.668, -175.016
- Letusan terakhir
- 1847
- Kondisi tektonik
- Zona subduksi / Kerak samudra (< 15 km)
- Bentuk lahan
- Komposit
- Batuan utama
- Andesit / Andesit basaltik
Ringkasan geologi
The symmetrical Kao rises steeply from the ocean about 6 km N of Tofua Island in Tonga. It is elongated NNE-SSW and, with the exception of a small flat area on the SSW coast, rises at angles exceeding 35° to the summit, which has a series of small coalescing craters. The lower flanks of the basaltic andesite volcano are densely jungled, but the upper slopes are almost vegetation free. There are no fresh-looking lava flows, although the absence of sufficient time for erosion to produce deep gullies or high sea cliffs suggests a very recent origin. A missionary on a ship anchored at Tofua reported that "smoke" was "pouring forth" from Kao on 10 July 1847.
Riwayat letusan
1 tercatatGlosariumRingkasan (VEI dari waktu ke waktu)
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Garis waktu rinci
- 1847VEI 2Teramati1847-07-10 – akhir tidak diketahui
Gunung api terdekat
Tautan eksternal
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