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 © ™ ® the next website to look at is New Cascadia Dawn © ™ ® - Cascadia Rising - M9 to M10+, An Intelligent Grandfather's Guide © ™ ® The next website to look at is 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 © ™ ® NEW this year If You Have a Mobility Disability (Earthquake Safety Video Series), on Youtube << slide Image Left On The Website Mastheads (here and elsewhere) Image by Stan G. Webb is of Kulshan (Mt. Baker) an active, live stratovolcano about 108 kilometres east of Vancouver, Canada. Simon Fraser University is in the foreground. 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 New Cascadia Dawn© - Cascadia Rising - M9 to M10+, An Intelligent Grandfather's Guide© next, Simon Fraser University (foreground) Kulshan Stratovolcano© / Mount Baker Stratovolcano (background)© ~ 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©

I experienced my first magnitude 7.0-7.5 earthquake when I was almost 23 months old. It almost knocked me to the ground. That 1946 Vancouver Island earthquake struck Vancouver Island on June 23 at 10:15 a.m.[1] with a magnitude estimated at 7.0 Ms[2] and 7.5 Mw.[6] The main shock epicenter occurred in the Forbidden Plateau area northwest of Courtenay. While most of the large earthquakes in the Vancouver area occur at tectonic plate boundaries, the 1946 Vancouver Island earthquake was a crustal event. Shaking was felt from Portland, Oregon, to Prince Rupert, British Columbia. This is one of the most damaging earthquakes in the history of British Columbia, but damage was restricted because there were no heavily populated areas near the epicentre, where severe shaking occurred. There were, however, a whole series of landslides in the Forbidden Plateau area there were a whole series of landslides blocked streams and rivers to create lakes. The first hikers into the area gave them great names, Landslide Lake, Rock Fall Lake, Earthquake Lake etc.; over time these natural dams were eroded to nothing, leaving nothing but fading memories of those lakes. This earthquake is Canada's largest historic onshore earthquake.[1] Three years later, an earthquake, an M8.1, struck at 8:01 p.m. PDT on August 2, 1949 in Haida Gwaii [formerly Queen Charlotte Islands], an interplate earthquake that occurred on the ocean bottom just off the west coast of the main south island [Graham Island]. The shock had a surface wave magnitude of 8.1 and a maximum Mercalli Intensity of VIII (Severe).
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.

Sunday, July 24, 2022

Morning Over Tsleil-Waututh Nation And Me © ™ ®


 

Tsleil-Waututh Nation left foreground on the north side Burrard Inlet in the trees opposite these petrochemical processes, Simon Fraser University top left, West Coast (Canada) Tidewater Terminal Alberta Tar-Sands, Petrochemical Processing including Chevron Oil Refinery centre right, also in the foreground on the north side Burrard Inlet is Hooker Chemical, in the trees opposite these petrochemical processes.

For 34 years I was an auditor of this regions First Nations and their related First entities ~ companies, co-ops, reserve lands and all related matters. For 34 years I looked for the documents recording these land sales to any government, indeed, to anyone, whatsoever. NOPE! 

under Simon Fraser University, Canada is building the West Coast Oceanside Terminal for export of Alberta Tar Sands right on an active seismic zone

See, Earthquake Risk Reduction

extract from

The 11th Canadian Conference on Earthquake Engineering

Canadian Association for Earthquake Engineering

https://www.caee.ca/pdf/Paper_94158.pdf

EARTHQUAKE RISK MODELLING AND DISASTER RESILIENCE
PLANNING AT THE COMMUNITY LEVEL

Page 7 of 10
Fig. 4 – Indicator charts summarizing risk reduction potential through structural mitigation.
3.2.2. Building Performance
Building performance directly influences the safety and security of individuals, the extent of social
disruption following an earthquake, and the longer-term economic security of a community. Key
performance measures include the number of structures likely to sustain extensive and/or complete
damage (resistance), and the number of days needed to restore baseline levels of functionality (recovery)
for both baseline and mitigation scenarios.
For current baseline conditions, It is estimated that ~840 buildings would sustain extensive or complete
damage in the Georgia Strait M7.3 scenario earthquake. The majority of these are older concrete and
unreinforced masonry structures in business precincts along the waterfront (~600 buildings), More than
215 residential structures and 25 public sector buildings are also likely to be damaged beyond repair in
isolated hotspots of severe shaking and ground failure throughout the District.


Page 8 of 10
Specific measures that might be considered to increase building performance include: the strengthening
of foundation connections; bracing and/or anchoring of frame, floor and roof systems; the addition of
shear walls; and a variety of other measures to help dissipate seismic energy and resist the effects of
shear and lateral drift. With mitigation measures in place, all but 21 of the 839 buildings currently
exposed to extensive or complete damage from a major earthquake would be preserved from significant
damage (Figure 3). Fifteen of the buildings still in danger of collapse are situated along the industrial
waterfront with the remaining six in surrounding commercial precincts. Nearly all are larger unreinforced
masonry buildings that are likely to collapse from severe ground shaking and lateral spreading caused by
liquefaction.
Investments in seismic retrofits to the most vulnerable buildings in the District also have the effect of
reducing recovery times for homes and businesses. The greatest gains are in the residential sector,
where mean recovery times are reduced by almost 95% (See Fig. 4). Recovery times are reduced by ~4
months for single-family homes and over one year for multi-family residential buildings that have been
seismically retrofitted. Recovery times are reduced ~4 months for commercial and industrial buildings,
and ~1 week for public sector buildings.
3.2.3. Public Safety
Investments in seismic retrofits have the potential to reduce the number of people expected to sustain or
succumb to life-threatening injuries for a daytime earthquake scenario by 52 (Fig. 4). The greatest gains
are for older concrete and unreinforced masonry buildings, where safety performance levels increase by
17% and 28%, respectively. While this represents a significant reduction in the number of potential
fatalities, more than 1,300 people will still sustain injuries that require paramedic care and ~425 will need
emergency medical care at a hospital — even with mitigation measures in place.
Although most of the population is likely to shelter in place, it is expected that more than 3,000 residents
would likely be displaced from their homes for up to 20 days after the scenario earthquake to allow time
for building inspections and restoration of lifeline services. While the majority of those displaced will seek
temporary accommodation with friends and family, several hundred people would require emergency
shelter and social services from local authorities and supporting aid agencies. Seismic retrofit measures
are most effective in reducing the extent of social disruption for those displaced three months or more
(See Fig. 4). More than 13,000 people who would otherwise be displaced by the earthquake are expected
to return to their homes and places of work with mitigation measures in place. The most significant
reductions in social disruption are for residents displaced more than a year (~1,500 people), and for
employees displaced for 3 months or more (~16,500 workers).
3.2.4. Lifeline Resilience
Lifeline resilience measures the extent to which critical infrastructure systems can absorb the impacts of
sudden shocks that threaten structural coherence and functional integrity, and the capability of these
systems to provide access to essential services during the recovery process. Target criteria are
expressed in terms of performance measures that track the number of system components that are
expected to remain functional following a major earthquake (resistance), and the number of days required
to restore water and power services to the community (recovery).
Water utilities and related lifeline services are particularly vulnerable to earthquake damage and loss of
functionality in areas of severe ground shaking, and in older neighbourhoods where pipelines are
constructed of older brittle materials that are less resistant to settling and lateral displacements caused by
earthquake-triggered liquefaction. Earthquake damages are expected to result in leaks and breaks that
would require at least 100 repairs to restore potable water service, and ~250 repairs to restore
functionality for wastewater infrastructure. For current conditions, it is estimated that more than half of all
homes and businesses would be without water for up to 7 days after the earthquake. Depending on the
size and capacity of repair crews, it would take up to 18 days to restore full service capacity. Nearly 700
homes and businesses that would otherwise be without services would have access to potable water
within 7 days as a result of investments in seismic retrofits to pipelines and water facilities. In addition,
the time required to restore full service capacity is likely to be reduced by one week or more. This
represents a ~ 40% increase in service capacity for potable water systems and a ~70% increase for
wastewater systems.

Page 9 of 10

Our assessment of power system resilience is limited to an analysis of damages to electrical substations
within the District and does not account for upstream dependencies on power generation or distribution.
Electrical facilities are expected to sustain a ~50% drop in service capacity with as many as 18,000
homes and businesses without access to power immediately after the earthquake and ~3,500 without
power one week later. Investments in seismic retrofits to vulnerable facilities have the potential to
increase overall system resistance with ~7,000 fewer service interruptions immediately after the
earthquake, and a significantly shorter amount of time to restore full service capacity to the community.
Gains in system resilience have important implications on business interruption and overall economic
security during the recovery process.

See Geological Survey of Canada
Open File 7677 A Profile of Earthquake Risk for the District of North Vancouver, British Columbia

SCAN Search Results: Fastlink

Natural Resources Canada, Corporate Management and Services Sector, Chief Information Officer Branch

https://geoscan.nrcan.gc.ca/starweb/geoscan/servlet.starweb?path=geoscan%2Fshorte.web&search1=R%3D296264%3A296266

Dec 7, 2015 ... Survey of Canada, Open File 7677, 2015 p. 1-14, https://doi.org/10.4095/296264 Open Access. Download (whole publication) More Display on a map Community profile; Journeay, J M; Dercole, F; Mason, D; in, A profile of earthquake risk for the District of North VancouverBritish Columbia; Journeay, J M; Dercole, F; Mason, D; Westin, M; Prieto, J A; Wagner, C L



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