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Titila

순상화산 · Russia · 1523m

Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right.
Titila volcano is viewed looking towards the SE. It started to erupt in the late Pleistocene and was active about 10,000-8,000 and 3,000-2,500 years ago. A flank vent (forming the peak to the right) formed during the early Holocene. Its lava flows dammed a river to form Glubokoye Lake to the right. · 사진: Copyrighted photo by Maxim Portnyagin (Holocene Kamchataka volcanoes; http://www.kscnet.ru/ivs/volcanoes/holocene/main/main.htm).
화산 유형
순상화산
국가
Russia
지역
Northwestern Pacific Volcanic Regions / Central Kamchatka Volcanic Arc
해발
1523m
좌표
57.406, 160.108
마지막 분화
-550년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Shield
주요 암석
Basalt / Picro-Basalt
지질학적 요약

Titila is a small basaltic shield volcano NW of Lake Glubokoye, west of the crest of the central Sredinny Range. Lava flows radiate from two summit craters, and cinder cones are prominent on its southern flank. Titila overlaps to the W with another small shield volcano, Rassoshina, along with other features in the Sedanka Lava Field to the south. The latest known eruption took place about 2,500 years ago.

Wikipedia 요약

영어 요약

Titila is a shield volcano located in the northern part of Kamchatka Peninsula, Russia. It comprises two shield volcanoes: Titila and Rassoshina, from which Titila is the higher one.

Wikipedia · CC BY-SA · 전체 기사 보기 →

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
550 BCE~550 BCE · 1건 · 최고 VEI ?550 BCE550 BCE549 BCE549 BCE549 BCE

상세 타임라인

  1. 기원전 550년VEI ?지질학적 추정
    BCE 550 ~ 진행 중

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