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Massiccio del monte Meager

Meager

Vulcano complesso · 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
Vulcano complesso
Paese
Canada
Regione
North America Volcanic Regions / Garibaldi Volcanic Arc
Altitudine
2680 m
Coordinate
50.630, -123.500
Ultima eruzione
-410
Contesto tettonico
Subduction zone / Continental crust (> 25 km)
Forma vulcanica
Composite
Roccia principale
Dacite
Sintesi geologica

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.

Sintesi da Wikipedia

Il massiccio del monte Meager è un gruppo di picchi vulcanici nelle Pacific Ranges delle Montagne Costiere nel sud-ovest della Columbia Britannica, in Canada. Compreso nell'arco vulcanico delle Cascate del Nord America occidentale, si trova 150 km a nord di Vancouver all'estremità settentrionale della valle di Pemberton e raggiunge un'elevazione massima di 2.680 m. Il massiccio è ricoperto da diversi edifici vulcanici erosi, tra cui duomi di lava, colli vulcanici e cumuli sovrapposti di colate laviche; questi formano almeno sei grandi vette, compreso il monte Meager che è il secondo più alto del massiccio.

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Storia delle eruzioni

Riepilogo (VEI nel tempo)
Fai clic su una barra per vedere le singole eruzioni
410 BCE~410 BCE · 1 eruzioni · VEI max. 5410 BCE410 BCE409 BCE409 BCE409 BCE

Cronologia dettagliata

  1. 410 a.C. (±200 anni)VEI 5Stima geologica
    BCE 410 – In corso
    NE flank of Plinth Peak

Link esterni

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