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도시마섬

Toshima

성층화산 · Japan · 508m

Steep cliffs up to 300-m-high surround the small island of Toshima. Toshimamura, the port village of the island, is to the far left in this view from the west. Toshima lies about 20 km W of the main volcanic front of the Izu-Marianas arc. Recent activity occurred between about 8,000 and 40,00 years ago.
Steep cliffs up to 300-m-high surround the small island of Toshima. Toshimamura, the port village of the island, is to the far left in this view from the west. Toshima lies about 20 km W of the main volcanic front of the Izu-Marianas arc. Recent activity occurred between about 8,000 and 40,00 years ago. · 사진: Copyrighted photo by Shun Nakano (Japanese Quaternary Volcanoes database, RIODB, http://riodb02.ibase.aist.go.jp/strata/VOL_JP/EN/index.htm and Geol Surv Japan, AIST, http://www.gsj.jp/). · Wikimedia Commons
화산 유형
성층화산
국가
Japan
지역
Northwestern Pacific Volcanic Regions / Izu Volcanic Arc
해발
508m
좌표
34.520, 139.279
마지막 분화
-4550년
판구조 환경
Subduction zone / Oceanic crust (< 15 km)
화산 지형
Composite
주요 암석
Basalt / Picro-Basalt
지질학적 요약

The small 2 x 2.4 km island of Toshima is located in the northern Izu Islands south of Izu-Oshima Island about 20 km W of the main volcanic front. Steep cliffs up to 300 m high ring the basaltic to basaltic andesite island on three sides. The summit is asymmetrically located opposite the more gentle slopes of the northern side of the island, where the village of Toshima is located. The latest known eruption of this stratovolcano occurred sometime between about 9,000 and 4,000 years ago, producing a lava flow from Kajiana crater.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
4550 BCE~4550 BCE · 1건 · 최고 VEI 04550 BCE4550 BCE4549 BCE4549 BCE4549 BCE

상세 타임라인

  1. 기원전 4550년 (±2550년)VEI 0지질학적 추정
    BCE 4550 ~ 진행 중
    Kajiana crater

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