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Mount Meager

Meager

복합화산 · Canada · 2680m

The Mount Meager volcanic complex is the northernmost major volcanic center in the Canadian part of the Cascade Range. This Tertiary to Holocene complex has erupted mafic to felsic magmas from at least eight vents. The most recent eruption produced a pyroclastic flow and lava flow from a NE-flank vent about 2,350 years ago. This view from the Lillooet River valley to the west shows, from left to right, the glacially eroded volcanic necks of Mount Capricorn, Meager Mountain, and Plinth Mountain.
The Mount Meager volcanic complex is the northernmost major volcanic center in the Canadian part of the Cascade Range. This Tertiary to Holocene complex has erupted mafic to felsic magmas from at least eight vents. The most recent eruption produced a pyroclastic flow and lava flow from a NE-flank vent about 2,350 years ago. This view from the Lillooet River valley to the west shows, from left to right, the glacially eroded volcanic necks of Mount Capricorn, Meager Mountain, and Plinth Mountain. · 사진: Photo by Willie Scott, 1990 (U.S. Geological Survey). · Wikimedia Commons
화산 유형
복합화산
국가
Canada
지역
North America Volcanic Regions / Garibaldi Volcanic Arc
해발
2680m
좌표
50.630, -123.500
마지막 분화
-410년
판구조 환경
Subduction zone / Continental crust (> 25 km)
화산 지형
Composite
주요 암석
Dacite
지질학적 요약

Mount Meager volcanic complex, of Pliocene-to-Holocene age, forms a dissected andesitic-to-rhyodacitic stratovolcano with multiple eroded summit lava domes and volcanic necks. It lies in the Garibaldi volcanic belt and is the northernmost volcano of the Cascade arc that extends to northern California. The summit of the complex consists of overlapping piles of andesitic lava flows and younger dacitic lava domes and flows. Quaternary basalts underlying the uppermost 22 km of the Elaho valley originated at the 1375 m level in the South Fork Meager River. The most recent activity, about 2350 years ago, produced Canada's largest known Holocene explosive eruption and an associated welded block-and-ash flow and a lava flow from a vent on the NE flank of Plinth Peak. Two clusters of hot springs occur within the complex, which has been investigated for potential geothermal power.

분화 이력

요약 (VEI 시계열)
막대를 클릭하면 개별 분화가 표시됩니다
410 BCE~410 BCE · 1건 · 최고 VEI 5410 BCE410 BCE409 BCE409 BCE409 BCE

상세 타임라인

  1. 기원전 410년 (±200년)VEI 5지질학적 추정
    BCE 410 ~ 진행 중
    NE flank of Plinth Peak

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