Bridge River Vent
http://dbpedia.org/resource/Bridge_River_Vent an entity of type: Thing
The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located 51 km (32 mi) west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of 1,524 m (5,000 ft), it lies on the steep northern face of Plinth Peak, a 2,677 m (8,783 ft) high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif.
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Bridge River Vent
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Bridge River Vent
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Bridge River Vent
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Bridge River eruption
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Canadian Cascade ArcGaribaldi Volcanic Belt
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A geologist next to a tree trunk that was buried by pyroclastic fall deposits from the Plinian phase of the eruption and then overrun by a pyroclastic flow.
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British Columbia, Canada
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Location of the Bridge River Vent in southwestern British Columbia
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Bridge River Vent ice and debris.jpg
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Meager ash-fall and pyroclastic flow deposits.jpg
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A photo of the northern flank of the Mount Meager massif. The Bridge River Vent is the bowl-shaped depression in the middle of this image.
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The Bridge River Vent is a volcanic crater in the Pacific Ranges of the Coast Mountains in southwestern British Columbia, Canada. It is located 51 km (32 mi) west of Bralorne on the northeastern flank of the Mount Meager massif. With an elevation of 1,524 m (5,000 ft), it lies on the steep northern face of Plinth Peak, a 2,677 m (8,783 ft) high volcanic peak comprising the northern portion of Meager. The vent rises above the western shoulder of the Pemberton Valley and represents the northernmost volcanic feature of the Mount Meager massif. At least eight volcanic vents compose the Meager massif, with the Bridge River Vent being the most recent to form. It is the only vent of the massif to exhibit volcanic activity in the past 10,000 years and one of the several vents in the Garibaldi Volcanic Belt to erupt since the end of the last glacial period. The crater constitutes a bowl-shaped depression overlain by glacial ice and volcanic debris that were deposited during volcanic activity. Its breached northern rim has been a pathway for lava and ash flows that have traveled throughout the nearby Pemberton Valley.
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A glaciated mountain rising over a forested valley.
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