이스터섬
Rapa Nui
순상화산 · Chile · 501m

- 화산 유형
- 순상화산
- 국가
- Chile
- 지역
- 남태평양 / Salas y Gómez Ridge Volcano Group
- 해발
- 501m
- 좌표
- -27.114, -109.356
- 마지막 분화
- 미확인
- 판구조 환경
- Rift zone / Oceanic crust (< 15 km)
- 화산 지형
- Shield
- 주요 암석
- Basalt / Picro-Basalt
지질학적 요약
The triangular Rapa Nui (also known as Isla de Pascua, or Easter Island), is renowned for its dramatic megalithic statues of hand-carved basalt. The island sits atop the largely submarine Salas y Gómez Ridge, which trends eastward from the East Pacific Rise. It is composed of three principal volcanoes and more than 70 subsidiary vents. Rano Kau at the SW tip includes flat-bottomed crater 1.5 km wide, while Poike volcano is at the E point; both are of Pleistocene age. Terevaka is a broad shield volcano of Pliocene-to-Pleistocene age at the northern point of the island, which is capped by many pyroclastic cones; the last stage of activity consisted of eruptions from multiple rift zones. The latest lava flows, at Hiva-Hiva near the west-central coast, are thought to be less than 2,000 years old.
Wikipedia 요약
영어 요약Poike is one of the three main extinct volcanoes that form Rapa Nui, a Chilean island in the Pacific Ocean. At 370 metres above sea level, Poike's peak is the island's second-highest point after the peak of the extinct volcano Terevaka.
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