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Macizo Mount Meager

Meager

Volcán complejo · Canada · 2680 m

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. · Foto: Photo by Willie Scott, 1990 (U.S. Geological Survey). · Wikimedia Commons
Tipo
Volcán complejo
País
Canada
Región
North America Volcanic Regions / Garibaldi Volcanic Arc
Altitud
2680 m
Coordenadas
50.630, -123.500
Última erupción
-410
Contexto tectónico
Subduction zone / Continental crust (> 25 km)
Forma volcánica
Composite
Roca principal
Dacite
Resumen geológico

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.

Historial de erupciones

Resumen (VEI en el tiempo)
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410 BCE~410 BCE · 1 erupciones · VEI máx. 5410 BCE410 BCE409 BCE409 BCE409 BCE

Línea de tiempo detallada

  1. 410 a. C. (±200 años)VEI 5Estimación geológica
    BCE 410 – En curso
    NE flank of Plinth Peak

Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.