Kao
성층화산 · Tonga · 1009m

- 화산 유형
- 성층화산
- 국가
- Tonga
- 지역
- Tonga-Kermadec Volcanic Regions / Tofua Volcanic Arc
- 해발
- 1009m
- 좌표
- -19.668, -175.016
- 마지막 분화
- 1847년
- 판구조 환경
- Subduction zone / Oceanic crust (< 15 km)
- 화산 지형
- Composite
- 주요 암석
- Andesite / Basaltic Andesite
지질학적 요약
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.
Wikipedia 요약
영어 요약Kao 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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분화 이력
상세 타임라인
- 1847년VEI 2관측 기록1847-07-10 ~ 진행 중
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