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Minor earthquakes Tuesday shake the Nickel City

Separate afternoon quakes measure 3.3 and 3.8 on Richter Scale.

Greater Sudburians felt the Earth move Tuesday afternoon when two minor earthquakes struck northwest of Lively, events big enough to rattle some windows, but not do any serious damage.

The first at 1:55 p.m. measured 3.3 on the Richter Scale, while the second at 2:15 p.m. measured 3.8.

According to Earthquakes Canada, the epicentre was seven kilometres northwest of Lively. The latitude was 46.48, the longitude was 81.19, and it took place at a depth of 5.4 kilometres below ground.

Catherine Woodgold, a seismologist with Earthquakes Canada, said Tuesday that reports from this area are common but are normally related to mining.

“But this one was bigger, so we’re presuming it was an earthquake,” Woodgold said. “Mining blasts don’t usually get this large. (Although) that magnitude is not expected to cause damage.”

She said there are normally about four earthquakes this size in Canada each year, mostly in parts of British Columbia and Quebec. With the geology in Northern Ontario, the risk of a serious event is low.

“There’s a very small possibility of having damaging earthquakes in that area,” Woodgold said.

About 80 online reports have been filed with them so far, she said. An earthquakes that registers higher than 4 may cause some minor damage, while things get more serious at 5.

Overall, the northeastern Ontario Seismic Zone has a low level of seismic activity, according to the Earthquakes Canada website.

The zone runs from Sudbury in the east, Fort Frances and Red Lake in the West, Winisk in the North and south of the Sault in the south. Between 1970 and 1999, on average, only one or two magnitude 2.5 or greater earthquakes have been recorded in the zone per year.

“By comparison, over the same time period, the smaller region of Western Quebec experienced 15 magnitude 2.5 or greater earthquakes per year,” according to information on the website.

Since they began keeping statistics, two magnitude 5 earthquakes – one in 1905 in northern Michigan, and again in 1928, northwest of Kapuskasing — have occurred in the region. The biggest in eastern Canada was recorded in 1935, when Temiscaming was shaken by an earthquake of magnitude 6.2.

Quick facts:

Besides Tuesday’s events, there is one other earthquake
in the magnitude 3 range in the last 10 years in the area close to Sudbury, a magnitude 3.1 in 2001. Here’s a full list:

July 11, 1997: 2.1, 26 km east of Espanola
July 29, 1997; 2.7, 64 km southeast of Lively
Aug. 12, 1997: 2.6, 50 km southeast of Sudbury
July 27, 1998: 2.0, 45 km southeast of Sudbury
Dec. 23, 1999: 2.3, 58 km west of North Bay
Feb. 19, 2000: 2.3, 61 km west of North Bay
Sept. 26, 2001: 3.1, 50 km west of North Bay
Dec. 27, 2002: 2.2, 60 km west of North Bay
March 26, 2003: 2.3, 20 km east of Sudbury
Sept. 2, 2003: 2.5, 24 km southwest of Sudbury
May 27, 2007: 2.1, 53 km southwest of Sturgeon Falls
Aug. 5, 2014: 3.3, 6 km northwest of Lively
Aug. 5, 2014: 3.8, 7 km northwest of Lively

Source: http://www.northernlife.ca/news/localNews/2014/08/05-earthquake-sudbury.aspx

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5.9 magnitude Gulf of Alaska earthquake rocks Yukoners again

5.9 magnitude Gulf of Alaska earthquake rocks Yukoners again

It follows a 5.7 magnitude earthquake June 4, at almost exactly the same time of day, in same area.

An earthquake with a magnitude 5.9 about 150 kilometres southwest of Haines, Alaska woke up many people in Whitehorse at 4:54 MT this morning, according to the U.S. Geological Survey.

Many Yukoners got a similar wake-up when a 5.7 magnitude earthquake struck about 73 kilometres southwest of Haines at almost exactly the same time of day on June 4.

That event was followed by aftershocks.

The U.S. Geological Survey warns on its website that the same thing could happen this time.

Several people went on Twitter to record their observations.

Source: http://www.cbc.ca/news/canada/north/5-9-magnitude-gulf-of-alaska-earthquake-rocks-yukoners-again-1.2717780

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Engineers want to help mitigate B.C.’s seismic risk

Engineers want to help mitigate B.C.’s seismic risk

Ann English, CEO and registrar at the Association of Professional Engineers and Geoscientists of B.C. (APEGBC), says her association can help British Columbia prepare for a catastrophic earthquake when The Big One hits the province.

English said Emergency Management B.C. (EMBC), which is developing a provincial earthquake preparedness plan, should be put to use The Seismic Mitigation Program for B.C. Schools, which was created 10 years ago by APEGBC, the Ministry of Education and the University of B.C.

“APEGBC will recommend that the B.C. government apply the school seismic mitigation model to all public buildings and critical economic infrastructure in the province,” English said.

“Adopting the application of common risk evaluation guidelines will allow all levels of government and the private sector to better organize and target limited resources.”

English said that APEGBC also recommends that the core operations of government be included in the evaluation.

“If, for example, an earthquake were to hit lower Vancouver Island while the legislature was in session, the damage to B.C.’s Parliament buildings could have severe consequences on the operation of government in an emergency,” she said.

APEGBC is participating in the B.C. government’s earthquake consultation process, which is part of the preparedness plan, through the Earthquake Review Board.

“We’re currently discussing with EMBC the ways in which APEGBC could support efforts to improve public safety related to earthquakes,” English said.

“If adopted for public buildings, the Seismic Retrofit Guidelines would need to be adapted for use with other building types. They are currently intended solely for use in the seismic retrofitting of schools.”

The origins of the school seismic upgrade program date back to 2004, when the Ministry of Education engaged APEGBC and UBC’s Earthquake Engineering Research Institute in a two-pronged mission:

To conduct a comprehensive update of how B.C. schools can be expected to perform in a major earthquake and to upgrade the technical guidelines for seismic retrofits.

The program that resulted from the collaboration contains assessment tools and procedures for engineers to determine how different sections of school buildings in different parts of B.C.’s seismic zones will withstand different types of earthquakes.

It also has technical guidelines for engineers to follow when planning school retrofits, and access to support from APEGBC’s technical review committee.

In addition, a data analyzer gives engineers access to more than eight million sets of seismic retrofit analysis to help them in the assessment and retrofit design of school structures.

“Because of the mitigation program, B.C. has a smart, science-based approach to protect our children in an earthquake, allowing government to efficiently target resources where they’re most needed,” English said.

APEGBC made its suggestions to the government following a March 2014 report by B.C.’s auditor general Russ Jones, which said EMBC wasn’t prepared for a catastrophic earthquake.

In reply to the report, EMBC has started working on a long-term earthquake response plan, a province-wide consultation on earthquake preparedness and a public education campaign.

EMBC spokesman Jeff Groot said the agency is planning to develop an immediate earthquake response plan by the end of March 2015, a sustained response plan by the end of March 2016 and long-term recovery plan by the end of March 2017.

Consultation chairman Henry Renteria, the former director of California’s Office of Emergency Services, has been holding community consultations around the province.

Renteria is meeting with more than a dozen communities in B.C., including Chilliwack, Metro Vancouver, Victoria, Nanaimo, Port Alberni, Courtenay, Port McNeil, Terrace, Prince Rupert, Queen Charlotte Village on Haida Gwaii and Kelowna.

Meetings started May 29 in Kelowna and continue until the end of July.

The consultations will wrap up with a report to government by the end of 2014.

English said the threat of an earthquake in B.C. is not hypothetical.

“The question is not if a significant earthquake will hit, but when,” she said

“Since 1872, nine earthquakes greater than magnitude 6.0 have shaken our region, most recently near Haida Gwaii in 2012.”

English said the only question is when our luck runs out and a big earthquake hits a populated area.

“As the 6.3-magnitude earthquake that shook Christchurch, New Zealand, in 2011 shows, when such an earthquake hits, the result is significant damage,” she said.

The Christchurch earthquake damaged more than 10,000 homes, destroyed 7,500 more, and resulted in the demolition of 1,400 buildings.

The total loss: more than $30 billion or 10 per cent of New Zealand’s GDP.

“That was in a city the size of Victoria,” English said.

“Imagine the economic impact if a similar-sized earthquake hit Metro Vancouver.”

Source: http://www.journalofcommerce.com/Associations/News/2014/7/Engineers-want-to-help-mitigate-BCs-seismic-risk-1000469W/

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Magnitude-6.0 earthquake near Yukon-Alaska border

WHITEHORSE — A magnitude-6.0 earthquake rattled parts of Yukon early Thursday morning.

The earthquake was recorded just before 5 a.m. along the Yukon-Alaska border. The U.S. Geological Survey placed the epicentre on the Alaska side of the border about 300 kilometres west of Whitehorse.

An earthquake report on Natural Resources Canada’s website said the quake was felt in Whitehorse and surrounding areas.

The quake was enough to wake up Hardy Ruf, whose home near Haines Junction, Yukon, is about 200 kilometres east of the epicentre.

“We woke up and the house was shaking and the lamp was swinging from one side to another above our heads,” said Ruf, 60, who runs the Dalton Trail Lodge.

Ruf said he didn’t notice any damage.

Earthquakes are not unusual in the region. Ruf said he feels about one or two a year.

“I’d say this was about average,” he said. “We’re kind of used to it.”

Darren Moorhouse, 46, was asleep in his home north of Whitehorse when the shaking began.

“I was dreaming about some weird thing with noises and stuff in it, and I woke up and the dream continued on and it was my place shaking,” said Moorhouse.

“You just lie there and wait for it to run its course hoping nothing worse happens.”

The U.S. Geological Survey’s website said there were more than a dozen smaller quakes after the initial one.

Source: http://www.ctvnews.ca/canada/magnitude-6-0-earthquake-near-yukon-alaska-border-1.1918408

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Preparing for the Big One never ends

Preparing for the Big One never ends

If there were a catastrophic earthquake this week, is B.C. prepared for it? The question was put point-blank to the director of Emergency Management B.C. on Wednesday during a committee meeting, and the answer was: “No, we are not.”

And with full candour, Pat Quealey’s more extensive reply was that B.C. will never be fully prepared. The catastrophic damage from an offthe-charts quake would overwhelm any jurisdiction that sustains it. That premise is proven every time one strikes.

The concept of preparing for the Big One is a never-ending road, and you never get to the destination where readiness can be declared.

Quealey, who has been on the job as an assistant deputy minister for four months, told MLAs that preparing for catastrophe is ongoing. “There will never be that end state of preparedness where I will be able to answer your questions and say: ‘Yes, we are.’ “The idea is to continue planning and modelling for resiliency, so that when a portion of the province is overwhelmed by catastrophe, the systems can be adaptive and bounce back.

“Next year, I will not categorically tell you that we are prepared, but I will say that we will be better prepared than we are today,” said Quealey.

His appearance stemmed from the auditor general’s report on earthquake readiness last

March that condemned the state of preparation. A similar audit 17 years earlier produced dozens of recommendations, but not much came of any of them. Despite reassuring news releases over the years, the audit found B.C. is not ready for a big quake and its lack of preparedness has not been publicly disclosed. Emergency Management B.C. has so many other responsibilities that it runs earthquake readiness “off the side of the desk,” with a $6-million budget that has remained unchanged for several years.

What they are supposed to be planning for is the kind of earthquake that flattens buildings, alters river courses and topography and results in high numbers of casualties and evacuees. Responsibility for dealing with the aftermath response follows a hierarchy.

If individuals are overwhelmed, local governments are expected to respond. If they are overwhelmed, the province is legislated to act, and if the province needs help, it asks the federal government or other jurisdictions for aid.

But the audit found B.C.’s preparation for the role it legally has to play is inadequate. The analyses of risk and hazard are out of date. The plans don’t detail everything that has to happen. There’s little integration of planning, and the training exercises and public education programs are inadequate.

Most of the deficiencies were noted by EMBC itself, after a 7.7 earthquake off Haida Gwaii in October 2012.

Wednesday’s session was the first chance for Opposition MLAs to go over the report in detail, and the budgeting caught some attention.

NDP MLA David Eby said government priorities can be ranked by the money allocated.

By that measure, B.C. spent twice as much on the Bollywood awards show and $14 million on advertising the jobs plan. He noted the $6 million for earthquake readiness is the same amount as a different agenda item that occupied the committee earlier – the legal bills, covered by taxpayers, of the two corrupt aides who pleaded guilty in the B.C. Rail case.

Quealey came armed with a strategic plan to show MLAs. It was completed in the months following release of the audit findings. It’s been posted on the EMBC website and preparation for a catastrophic seismic event is listed as a priority. (There are actually 57 specific relevant potential hazards in B.C.) Just So You Know: The audit compared preparedness with Washington, Oregon and California and came to an interesting conclusion – they spend much more money there, but don’t believe they are prepared, either.

Direct comparisons are different because the structure of governments are different. But all the U.S. agencies that have roles are well-funded, yet they recently self-assessed themselves as not being prepared. When it comes to preparing readiness, the audit official said: “What B.C. should be doing is meeting its own expectations.”

Source: http://www.avtimes.net/preparing-for-the-big-one-never-ends-1.1195505

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Alaska hit with 8.0 magnitude earthquake; no tsunami threat for coastal B.C.

Alaska hit with 8.0 magnitude earthquake; no tsunami threat for coastal B.C.

An 8.0 earthquake off the Aleutian Islands triggered a tsunami warning for parts of Alaska this afternoon

The U.S.’s National Weather Service initially issued a warning for coastal areas of Alaska from Nikolski to Attu— but it’s has since been downgraded to a tsunami advisory.

The B.C. coast is outside of the tsunami advisory area.

The Pacific Tsunami Warning Center says the earthquake is too deep, 114 kilometres down, to pose a tsunami threat along the Pacific Coast areas of Canada and U.S.

Dr. Brent Ward, earth scientist at Simon Fraser University, says it sounds like the earthquake occurred in the subduction plate — as opposed to along the subduction zone — which means there wouldn’t have been much seafloor movement.

“You need the seafloor movement to generate a tsunami,” Ward said. “When you move the seafloor — punching up from the bottom — it displaces the water and that’s what generates the wave.”

Still, an 8.0 quake is a very significant event, said Ward.

“Anything over 8.0 we call a great earthquake and we only get about 15 or so of those a year of that magnitude around the world” — Brent Ward, SFU

There have been no immediate reports of damage, but Natasha Ruppert, a seismologist with the Alaska Earthquake Center, told the Associated Press that the communities that would have suffered damage are also under tsunami warnings, so people may not have been able to get out and check for damage yet.

From the AP story: “The National Tsunami Warning Center in Palmer, Alaska, issued a tsunami warning for coastal areas between Nikolski to Attu, on the Aleutian Islands. A warning means significant inundation is possible or occurring. Residents are being warned to move inland toward higher ground.
A tsunami advisory was also issued for coastal areas stretching from Nikolski to Unimak Pass. An advisory means strong currents or dangerous waves are expected, but widespread inundation isn’t likely.”

CNN is reporting that the town of Adak evacuated its 150 residents to a shelter about 600 feet above sea level.

Google has a live epicenter map of the quake that was centred 24 kilometres southeast of Little Sitkin Island, Alaska.

Source: http://blogs.vancouversun.com/2014/06/23/alaska-hit-with-8-0-magnitude-earthquake/

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B.C.’s slow earthquakes fuelled by fluid

If you live in Victoria or Nanaimo in B.C., you experience the equivalent of a magnitude-7 earthquake every 14 months – it just happens so slowly that you don’t notice it.

Now, scientists at the University of Ottawa and the University of California, Berkeley, have figured out what makes bizarre “slow earthquakes” recur so regularly and why some happen more frequently than others. They published their findings online Wednesday in the journal Nature.

Slow earthquakes are a strange phenomenon discovered only a dozen years ago, said Pascal Audet, lead author of the new study.

The first one was found on Vancouver Island.

“Victoria is right at the epicentre of these things,” Audet said.

Like the sudden, violent earthquakes we are familiar with, they are caused by two tectonic plates on the surface of the earth sliding against each other at a boundary called a fault.

Regular earthquakes happen at seemingly random intervals, last just seconds to minutes and produce seismic waves that move through the Earth.

hi-seismograph-cp1456684
A regular earthquake registers on a seismograph. Slow earthquakes are detectable, but look like background “noise.” (Associated Press)

Slow earthquakes, on the other hand, recur regularly – every 14 months in the case of the slow earthquakes on Vancouver Island.

“These slow earthquakes typically last for several days – 10 days to two weeks,” said Audet, an assistant professor in the Earth Sciences department at the University of Ottawa.

In that time, the tectonics plates can slide as much as they do in a big, regular earthquake. For example, the slow earthquake on Vancouver Island produces a movement equivalent to a magnitude-7 regular earthquake, Audet said. That’s bigger than the magnitude-6.6 quake that hit Port Alice, B.C. in April and similar to the Mexican earthquake a few days earlier that knocked down walls and was felt across six states.

The first slow earthquake ever discovered was detected on Vancouver Island from seismometer and GPS measurements along part of the Cascadia subduction zone that runs from B.C. to California. Subduction zones are faults where a plate on the bottom of the ocean is sliding down under the plate of a continent. More recently, other slow earthquakes have been found around the Pacific Ocean in other subduction zones.

All around Pacific

But they all happen at different intervals – for example, one in Japan happens every six months and some slow earthquakes happen as infrequently as every two years.

Audet wanted to know why.

To find out, he looked at seismic data from slow earthquakes in B.C., Japan, Mexico, Costa Rica and New Zealand. With some help from University of California, Berkeley, researcher Roland Burgmann, he compared the frequency of the slow earthquakes with other characteristics indicating the structure and composition of the plates.

What the researchers found is that higher levels of quartz in the crust corresponded to more frequent slow earthquakes. Quartz is known to be formed when fluids in the Earth’s crust cool rapidly, so that provided clues to what could be happening.

“Oceanic crust is full of fluids,” Audet said.

Based on their evidence, the researchers came up with an explanation that seemed to fit their observations.

As the oceanic crust is pushed down into the subduction zone, it’s subjected to higher and higher temperatures and pressures. Those cause the fluids to push back up toward the surface.

But the fault between two plates acts as a seal, Audet said: “It prevents the fluids from migrating up.”

That causes the buildup of pressure until the fault slips. The fluid bursts out, cools and crystallizes into quartz.

The higher the levels of fluid circulation, the more quickly pressure builds up. The more quickly the pressure builds up, the more quickly it reaches the threshold where the fault slips, generate a slow earthquake. That in turn causes more quartz to be deposited.

Predicting the ‘big one’

The results not only provide an explanation of how slow earthquakes work, but a better understanding of faults in general. That, in turn, may help scientists predict big, violent, ordinary earthquakes in the future.

Like slow earthquakes, regular earthquakes are caused by a buildup of pressure, but solid pressure that isn’t directly due to a buildup of fluids. Nevertheless, the two are related.

“Every time there is a slow earthquake that happens, it also puts a little bit more pressure on the part of the fault that produces the regular earthquakes,” Audet said. “It puts the fault closer towards the next big earthquake.”

However, scientists don’t yet know for sure if slow earthquakes can directly lead to a “big one” because up until now, instruments that could measure the data necessary to show that haven’t been well-placed during major earthquakes.

Audet added, “We’ll have to wait for a really big earthquake again to test that.”

Source: http://www.cbc.ca/news/technology/b-c-s-slow-earthquakes-fuelled-by-fluid-1.2679669

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2.4-magnitude earthquake hits outside Victoria

2.4-magnitude earthquake hits outside Victoria

An earthquake just outside of Victoria, B.C. rattled homes in the Vancouver Island city Monday afternoon.

The 2.4-magnitude quake hit 11 kilometres northeast of the capital city around 1:40 p.m., according to the Pacific Geoscience Centre.

Affected residents quickly took to Twitter to report shaking windows and floors in their homes. Others said they could hear a rumbling noise when the quake hit.

There have been no reports of injuries or damage caused by the shaking.

Source: http://bc.ctvnews.ca/2-4-magnitude-earthquake-hits-outside-victoria-1.1871607

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Watch: SFU ’50s-style earthquake video wins major award

Watch: SFU ’50s-style earthquake video wins major award

A 1950s-style, black and white, two-minute video about earthquake preparedness, starring Simon Fraser University mascot McFogg the Dog, has won a major award.

Drop, Cover and Hold On! has been awarded a 2013 Video Award in the public service announcement category by PR Daily, a communications news site.

The video was created jointly by the SFU Creative Services and Safety & Risk Services departments. The SFU video was up against submissions from the U.S. Department of Labor, Office of Public Affairs, and the University of Colorado, Health, Management.

See the video here: Drop, Cover, Hold on!

© Copyright (c) The Vancouver Sun

Source: http://www.vancouversun.com/news/Watch+style+earthquake+video+wins+major+award/9911363/story.html

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The Big One – Examining the risk of an earthquake in the region

The Big One – Examining the risk of an earthquake in the region

Erin Edwards – As a longtime resident of British Columbia, I feel as though I live in one of the most beautiful places in the world. I am grateful to call the west coast my home, but its picturesque landscapes have the subtle ability to make me forget about the natural hazards that are prominent to this area.

British Columbia sits on Canada’s most active earthquake zone, making the threat of a large seismic event in our lifetime a very real possibility, and one that all British Columbians should be prepared for.

Earthquakes are caused by the movement of the tectonic plates that comprise the Earth’s surface. There are three types of plate boundaries at play along the west coast of B.C.: convergent (plates move together), divergent (plates move apart) and transform (plates slide past each other). However, the boundary that has the most potential to cause what scientists have termed “The Big One” is a convergent boundary.

“The Big One” refers to a large megathrust earthquake that scientists predict will at sometime hit the southwest coast of B.C. A megathrust earthquake occurs along a subduction zone that is found at a convergent boundary, where tectonic plates collide and one is subducted underneath the other, sinking down into the Earth’s mantle.

Subduction generally occurs when an oceanic plate, which is comparatively dense, and a continental plate collide. It is along this type of subduction zone that the largest earthquakes in the world are found, usually measuring a magnitude 9.0 or greater on the Richter Scale. An example of this event would be the 9.0 earthquake that hit Japan in 2011.

The Cascadia Subduction Zone (CSZ) separates the Juan de Fuca plate from the North American plate, extending approximately 1,000 kilometres from Vancouver Island to California. The Juan de Fuca plate is moving towards the North American plate at a rate of two to five centimetres per year. As the plates meet, the Juan de Fuca descends below the North American, currently 45 kilometres deep beneath Victoria and 70 kilometres deep beneath Vancouver.

Tectonic plates do not slide past each other smoothly. Rather their movement is discontinuous and in many cases they lock together. There is comprehensive evidence showing that the Juan de Fuca and North American plates are currently locked, causing strain to build up within the Earth’s crust.

When the fault’s frictional strength is exceeded, these locked plates will snap loose, causing a megathrust earthquake to occur.

Although predicting an earthquake is next to impossible, scientists have gathered diverse evidence that has identified 13 megathrust events along the CSZ over the last 6,000 years, occurring anywhere from 300 to 800 years apart, with the most recent occurrence in 1700.

Although there is nothing we can do to stop or control these types of natural events from occurring, we can be prepared for them. Do you have your earthquake preparedness kit ready?

Source: http://www.piquenewsmagazine.com/whistler/the-big-one/Content?oid=2552616

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