Please keep this secret and under your hat, for awhile. We are still doing ongoing research, editing, writing and are in production. Those who dance with earthquakes and volcanoes are considered mad by those who cannot smell the sulfur. <a href="https://mountbakerstratovolcano.blogspot.com/">Simon Fraser University (foreground) Kulshan Stratovolcano© / Mount Baker Stratovolcano (background)/</a> ~ Image by <a href="https://stangwebb.blogspot.com/">Stan G. Webb - In Retirement©</a> Learn more about <a href="https://mountmeagermassif.blogspot.com/">Mount Meager Massif©, part of the Cascadia Volcanic Arc©</a><a href="https://manfromminto.blogspot.com/">Man From Minto© - A Prospector Who Knows His Rocks And Stuff©</a>
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Friday, June 21, 2019
Saturday, June 15, 2019
Mount Meager Massif©

As with Kulshan Stratovolcano© /Mount Baker Stratovolcano©, Mount Meager Massif© is related to
where the westward moving North America Tectonic Plate collides with,
and rises above the eastward moving Explorer and Juan de Fuca
Tectonic Plates. The 7th vent of the volcano blew north, into the
Bridge River Valley. The Goldbridge Golf Course is largely talus.
Images
are via Wikipedia List
of iconic photographs
books
have been produced about iconic photographs and giving
suggested examples. The list of iconic photographs provides an
index to articles
The
Mount Meager massif as seen from the east near Pemberton.
Summits left to right are Capricorn
Mountain,
Mount Meager and Plinth
Peak.
The
Mount
Meager massif
is a group of volcanic peaks in the Pacific
Ranges
of the Coast
Mountains
in southwestern British
Columbia,
Canada. Part of the Cascade
Volcanic Arc
of western North America, it is located 150 km (93 mi) north of
Vancouver
at the northern end of the Pemberton
Valley
and reaches a maximum elevation of 2,680 m (8,790 ft). The massif is
capped by several eroded volcanic edifices, including lava
domes,
volcanic
plugs
and overlapping piles of lava flows; these form at least six major
summits
including Mount Meager which is the second highest of the massif.
The
Garibaldi
Volcanic Belt
(GVB) has a long history of eruptions and poses a threat to the
surrounding region. Any volcanic
hazard
ranging from landslides
to eruptions could pose a significant risk to humans and wildlife.
Although the massif has not erupted for more than 2,000 years, it
could produce a major eruption; if this were to happen, relief
efforts would be quickly organized. Teams such as the Interagency
Volcanic Event Notification Plan
(IVENP) are prepared to notify people threatened by volcanic
eruptions in Canada.
The
Mount Meager massif produced the largest volcanic eruption in Canada
in the last 10,000 years. About 2,400 years ago, an explosive
eruption
formed a volcanic
crater
on its northeastern flank and sent avalanches of hot ash, rock
fragments and volcanic
gases
down the northern flank of the volcano. Evidence for more recent
volcanic activity has been documented at the volcano, such as hot
springs
and earthquakes.
The Mount Meager massif has also been the source of several large
landslides in the past, including a massive debris
flow
in 2010 that swept down Meager
Creek
and the Lillooet River.
8th Vent, Bridge River Volcanic Vent
https://en.wikipedia.org/wiki/Bridge_River_Vent
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 Bridge River Valley, with ash reaching Alberta; perhaps some into nearby Pemberton Valley, to the south.