Kao
Stratovolkan · Tonga · 1009 m

- Tipe
- Stratovolkan
- Negara
- Tonga
- Wilayah
- Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
- Ketinggian
- 1009 m
- Koordinat
- -19.668, -175.016
- Letusan terakhir
- 1847
- Kondisi tektonik
- Subduction zone / Oceanic crust (< 15 km)
- Bentuk lahan
- Composite
- Batuan utama
- Andesite / Basaltic Andesite
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.
Ringkasan Wikipedia
Ringkasan InggrisKao is an island and stratovolcano in the Haʻapai island group of Tonga. It lies about 6 km (3.7 mi) north of Tofua island and reaches 1,030 m (3,379 ft) above sea level, the highest point in Tonga.
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Riwayat letusan
Garis waktu rinci
- 1847VEI 2Teramati1847-07-10 – Berlangsung
Tautan eksternal
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