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.

Friday, February 26, 2016

Many of Our Grandchildren Are Going To Die, Any Day Now


Great Earthquakes of the Pacific Northwest & Western Canada
Suggested by: CWU – CentralWashU - Central Washington University A Natural Obsession
It is well worth your time to watch this.
If you have interrupted reception, it may be because your internet speed is lower than my original post. To correct, once the video is started, click on gear icon (show at the bottom of the video, and lower the resolution. I, and many others have begun photographing and videographing in HD - High Definition 1080p (pixels) and higher; but you can view in as low as 144p for viewing.
>> Sound On >> Best viewed Full Screen >> Darkened Room
(1:04:00 minutes YouTube Video, it's quite long: being 1 hour and four minutes)

Published on Feb 16, 2016 
Central Washington University geology professor Nick Zentner presents “Great Earthquakes of the Pacific Northwest”.
Field data discussed includes Brian Atwater’s buried soils onshore, Chris Goldfinger’s turbidites offshore, and CWU Geology’s PANGA data from GPS receivers from across the Pacific Northwest. 250 folks attended the lecture at the Hal Holmes Center in downtown, Ellensburg, Washington. February 10, 2016.
Engineering
 
If you have interrupted reception, it may be because your internet speed is lower than my original post. To correct, once the video is started, click on gear icon (show at the bottom of the video, and lower the resolution. I, and many others have begun photographing and videographing in HD - High Definition 1080p (pixels) and higher; but you can view in as low as 144p for viewing.
>> Sound On >> Best viewed Full Screen >> Darkened Room

Because earthquake magnitudes are measured on a logarithmic scale, there is a thirty times (30x) increase in the amount of energy released in an earthquake of magnitude 7.0 to magnitude 8.0. There is a thirty times (30x) increase in the energy released in an earthquake of magnitude 8.0 to magnitude 9.0. So, there is a 30x30; a 900 times times increase in the amount of energy released in an earthquake of magnitude 7.0 to magnitude 9.0.

Albeit this discussion is very United States, America-centric, discussing the U.S. Pacific Northwest: Washington State, Oregon and Northern California, that very same Cascadia Subduction Zone continues up into British Columbia to Nootka Fault, about half way up Vancouver Island. Just north of that Nootka Fault is another Subduction Zone, caused by the Explorer Plate Subducting under the North American Plate; and, even further north the Pacific Plate Subducts directly under the North American Plate, at the Queen Charlotte Fault (soon to be renamed the Haida Gwaii Fault).

Seismicity of Canada (corrected hyperlink Natural Resources Canada – Earthquakes . Earthquakes Canada:

Seismologists locate an average of 1,500 earthquakes each year in Canada. Only about 100 of these measure more than magnitude 3 on the Richter scale or are felt by humans. Earthquakes of magnitude 6 or greater are strong enough to cause a significant damage. Geological Survey of Canada (GSC) is a Natural Resources Canada agency with a mandate to study and record earthquakes in Canada. The text and the figures presented in this section are a modified version of the material presented at the GSC's web site. For more information on seismic hazard in Canada and British Columbia refer to the (corrected hyperlink) Natural Resources Canada – Earthquakes . Earthquakes Canada: for recent earthquakes reports, with magnitude and location ...” ~ British Columbia Institute of Technology, Department of Civil Engineering


For an artists interpretation of all of this see: Icelandic native, Björk, provides an artists interpretation of plate tectonics : Björk Icelandic pronunciation: [ˈpjœr̥k ˈkvʏðmʏntsˌtoʊhtɪr] - Mutual Core - Tectonic Plates, Chords

Knowing that this topic is very scary for many people, that does not mean we should look away. My old Boy Cub training was all about being prepared. Over the next while I hope that I can help you do just that.

Please make certain to voice your comments, concerns, recommendations and suggestions in the comment section, at the bottom of each post.

1 comment:

  1. Knowing that the second topic is very scary for many people, that does not mean we should look away. My old Boy Cub training was all about being prepared. Over the next while I hope that I can help you do just that.

    Please make certain to voice your comments, concerns, recommendations and suggestions in the comment section, at the bottom of each post.

    ReplyDelete