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ミーガー山

Meager

複成火山 · 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. · 写真: Photo by Willie Scott, 1990 (U.S. Geological Survey). · Wikimedia Commons
タイプ
複成火山
Canada
地域
North America Volcanic Regions / Garibaldi Volcanic Arc
標高
2680m
座標
50.630, -123.500
最終噴火
-410年
テクトニクス環境
Subduction zone / Continental crust (> 25 km)
火山地形
Composite
主要岩石
Dacite
地質学的概要

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.

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
410 BCE~410 BCE · 1件 · 最大 VEI 5410 BCE410 BCE409 BCE409 BCE409 BCE

詳細タイムライン

  1. 紀元前 410年 (±200年)VEI 5地質学的推定
    BCE 410 ~ 進行中
    NE flank of Plinth Peak

外部リンク

⚠ 参考情報です。緊急対応には使用しないでください。