During an eruption, if the wind is from the east at 10,000 feet (outflow), the tephra will fall on Vancouver, Canada in about an hour. This Page Hyperlinked [click on] Mount Baker Stratovolcano (background)© ™ ®/ Kulshan Stratovolcano© ™ ®, Simon Fraser University (foreground)© ™ ® ~ Image by Stan G. Webb - In Retirement© ™ ®, An Intelligent Grandfather's Guides© ™ ® next, The Man From Minto© ™ ® - A Prospector Who Knows His Rocks And Stuff© ™ ®
Learn more about the Cascadia Volcanic Arc© ™ ® (Part of Pacific Ring of Fire) Cascadia Volcanoes© ™ ® and the currently active Mount Meager Massif© ™ ®, part of the Cascadia Volcanic Arc© ™ ® [ash flow, debris flows, fumaroles and hot springs], just northwest of Pemberton and Whistler, Canada ~ My personal interest in the Mount Meager Massif© is that the last volcanic vent blew north, into the Bridge River Valley [The Bridge River Valley Community Association (BRVCA), [formerly Bridge River Valley Economic Development Society], near my hometown. I am the Man From Minto© ™ ® - A Prospector Who Knows His Rocks And Stuff© ™ ® The 2010 Mount Meager landslide was a large catastrophic debris avalanche that flowed to the south, into the Lillooet Valley British Columbia, Canada, on August 6 at 3:27 a.m. PDT (UTC-7). More than 45,000,000 m3 (1.6×109 cu ft) of debris slid down Mount Meager, temporarily blocking Meager Creek and destroying local bridges, roads and equipment. It was one of the largest landslides in Canadian history and one of over 20 landslides to have occurred from the Mount Meager massif in the last 10,000 years. Although voluminous, there were no fatalities caused by the event due in part to its remote and uninhabited location. The landslide was large enough to send seismic waves more than 2,000 km (1,200 mi) away into the neighboring U.S. states of Alaska and Washington and beyond. Multiple factors led to the slide: Mount Meager's weak slopes have left it in a constant state of instability. The massif has been a source of large volcanic debris flows for the last 8,000 years, many of which have reached several tens of kilometres downstream in the Lillooet River valley., to the south. It is arguably the most unstable mountain massif in Canada and may also be its most active landslide area. And on the north side lies Downton Lake Hydro Reservoir, impounded by the La Joi Dam, the uppermost of the Bridge River Project dams. The earliest identified Holocene landslide was in 7900 BP (before the present, or read it as the number of years ago). Further landslides occurred in 6250 BP, 5250 BP, 4400 BP, 2600 BP, 2400 BP, 2240. BP BP, 2170 BP, 1920 BP, 1860 BP, 870 BP, 800 BP, 630 BP, 370 BP, 210 BP, 150 BP and in 1931, 1947, 1972, 1975, 1984, 1986 and 1998. These events were attributed to structurally weak volcanic rocks, glacial unloading, recent explosive volcanism and glacial activity. Those who dance with earthquakes and volcanoes are considered mad by those who cannot smell the sulfur. We begin to deal with BIG (MEGA) EARTHQUAKES at Simon Fraser University (foreground) Kulshan Stratovolcano© / Mount Baker Stratovolcano (background)©New Cascadia Dawn© - Cascadia Rising - M9 to M10+, An Intelligent Grandfather's Guide© next, ~ Images by Stan G. Webb - In Retirement©, An Intelligent Grandfather's Guides©Countdown to Earthquake Drill - International Great ShakeOut Day is on Thursday, October 20, 2022 at 10:20AM, and annually on the 3rd Thursday in October thereafter - - I grew up in small towns and in the North where the rule is share and share alike. So, I'm a Creative Commons type of guy. Copy and paste ANY OF MY MATERIAL anywhere you want. Hyperlinks to your own Social Media are at the bottom of each post. Creative Commons License
This work is licensed under my Creative Commons Attribution 4.0 International License.

Thursday, July 11, 2019

The Big Quake - TechKnow

https://youtu.be/TuOfZWkeRi8    [24:09 minutes]

AlJazeera English

Published on Oct 9, 2016
The 1,130 km stretch of coastline from Vancouver, Canada to Mendocino, California, harbours an underwater threat just over 110km offshore - the seismic fault, Cascadia. Places like Japan, Chile and North America's Pacific Northwest all fall in what's known as subduction zones - ie, where one tectonic plate dives under another. The potential seismic activity from one of these plates 'popping' from on top of the other equates to an entire region affected by earthquake symptoms. The Cascadia Initiative (CI) is a years-long project that has been developed to study the effects of the fault and the two plates responsible for the action: Juan de Fuca and Gorda. From the data collected, it is confirmed that the Cascadia will only cause large magnitude earthquakes, ranging between every 300 to 500 years. The last noted eruption of the Cascadia was in the 1700s, making Western Canada and the US Pacific Northwest overdue for the next quake. But alongside the shaking, the movement of the sea floor is also set to generate a tsunami wave that will reach Northwestern shores within minutes of the explosion. Impact studies are under way at Oregon State University, where civil engineer Daniel Cox utilises a wave laboratory to gauge the effect of different sized tsunamis. Replicas of towns based on actual layouts of coastal cities that could be affected by a Cascadia-triggered tsunami are used to collect data that is then input into a computer, simulating potential situations and scanning for the worst areas of damage. The results, even on a small scale, are terrifying, and the fear doesn't lie only in the force of the tsunami waves, but also in the projectiles that get swept up in it, including vehicles or temporary buildings that could crash and, ultimately, obliterate permanent structures. With knowledge of the mass panic caused during evacuation due to natural disasters, even this facet of the event has been mapped out by experts at Oregon State. Combining elements of how the water moves onto land and factoring in human behaviour leads to the conclusion that most people are still unaware of how to react should an event of this large scale arise. How likely is it that there will be a 9.0 magnitude earthquake on the Pacific Northwest within the next 50 years? "Somewhere within one in seven chance within the next 50 years," says Daniel Cox. "These odds are way too high for us to accept. There's too many lives at risk. We have to come up with some better ideas." - Subscribe to our channel:  http://aje.io/AJSubscribe
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