Strong earthquake hits near volcanic Alaskan islands

Strong earthquake hits near volcanic Alaskan islands

A strong earthquake shook volcanic islands between Alaska and Russia yesterday in the northern part of the Pacific Ring of Fire.

A 6.5-magnitude earthquake occurred at 12:35 p.m. local time (1:35 p.m. B.C. time) on April 2, according to the U.S. Geological Survey.

The epicenter was located in the Rat Island of the Aleutian Islands at a depth of 19 kilometres (12 miles) and 93 kilometres (58 miles) northwest of Amchitka, Alaska.

A tsunami was not expected from the quake, according to the U.S. Tsunami Warning System.

Source: https://www.straight.com/news/1222971/strong-earthquake-hits-near-volcanic-alaskan-islands

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2.2 magnitude earthquake ‘lightly felt’ in Salmon Arm

2.2 magnitude earthquake ‘lightly felt’ in Salmon Arm

A 2.2 magnitude earthquake was felt by some residents of Salmon Arm, B.C. on Saturday night.

According to Earthquakes Canada, the quake was “lightly felt” around 8:40 p.m. There were no reports of damage.

Many residents said they felt their houses shake, and heard something that sounded like an explosion.

Source: https://www.cbc.ca/news/canada/british-columbia/earthquake-salmon-arm-1.5040985

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Fracking connection probed in 4.6-magnitude earthquake near Sylvan Lake

Fracking connection probed in 4.6-magnitude earthquake near Sylvan Lake

The Alberta Energy Regulator is working to determine if a fracking operation caused an earthquake near Sylvan Lake and Red Deer on Monday.

Natural Resources Canada said a 4.6-magnitude earthquake rocked parts of central Alberta just before 6 a.m. The federal department’s website said the tremor was classified as a light earthquake.

The AER has confirmed Vesta Energy had been fracking in the area just prior to the quake, which was detected by the company’s private seismic monitoring devices around 12 kilometres south of Sylvan Lake at a magnitude of 4.16.

The AER said the earthquake was reported to them by the company at 6:20 a.m.

“We are currently reviewing the events to determine if the incident is due to hydraulic fracturing activities or natural causes,” said Natalie Brodych, spokeswoman with the AER.

The regulator said Vesta has stopped work at the site while the AER investigates whether fracking led to the quake.

Earthquakes Canada initially had trouble pinpointing the earthquake, locating it first northeast of Red Deer, then south of the city. The most recent update has placed it 19 kilometres west of Red Deer, near Sylvan Lake. The earthquake occurred about a kilometre below the surface.

There were no immediate reports of damage, but power was knocked out for about 4,600 FortisAlberta customers. A spokesperson said the disruption lasted for a little more than an hour.

AltaLink said a transformer at a substation south of Sylvan Lake tripped around the same time of the quake. The transmission company is still investigating exactly what caused the outage.

The U.S. Geological Survey website says an earthquake similar to the one that struck Alberta has a sensation like a heavy truck striking a building; it can rattle windows and may break some dishes or windows.

Debbi McGillicky, who lives in the Mountain View area of Red Deer, said she and her husband were jarred awake by the quake.

“My husband and I were awakened at 5:55 a.m. when our bed began to shake violently. My husband shot up out of bed and exclaimed, ‘What the hell was that?’,” she told Postmedia. At the time, she thought the quake was some sort of explosion.

Linda Borsato lives in Sylvan Lake and said she was eating breakfast when the earthquake hit.

“There was a pop and the power went out, and right after the power went out the whole house shook from one end to the other,” she said.

“It was pretty freaky to say the least. We didn’t really know what to do when it first happened. . . It was enormous.”

Earthquakes are rare for the Red Deer area; the last recorded quake was in 2016. There was a 4.0-magnitude quake on March 31, 1997.

However, Joanne Gaudet, communications officer for the town of Sylvan Lake, said there has been seismic activity in the past between Sylvan Lake and Rocky Mountain House to the west.

Source: https://calgaryherald.com/news/local-news/red-deer-hit-with-earthquake-monday-morning

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Developing Story: Seismic swarm in progress between Cascadia and San Andreas Faults

Developing Story: Seismic swarm in progress between Cascadia and San Andreas Faults

Four Magnitude-3.4 and larger quakes have struck in two hours, all south of Cape Mendocino, and west of the town of Petrolia, California. Based on the earthquake locations and their focal mechanisms (both by the USGS), the swarm appears to be occurring on a right-lateral reverse fault that connects the northernmost San Andreas-Mendocino Fracture Zone with the shallow portion of the Cascadia Megathrust (as shown by the black half- arrows in the map).

This area has highest quake rate in all of California (http://temblor.net/earthquake-insights/m6-5-earthquake-stresses-offshore-san-andreas-fault-aka-mendocino-fault-zone-1917/). That’s because the two fastest-slipping faults in the western U.S. join, or nearly join, here. It’s also because the bend in both the San Andreas and Cascadia Faults mean that the crust here is being crushed, distorted, and fractured. This distortion cannot be accommodated solely along the great faults, and so there is a plethora of small faults like this one that distribute the stress.

What this event means for the Cascadia and San Andreas Faults is unknown, but it is certainly a swarm to watch.

Source: http://temblor.net/earthquake-insights/developing-story-seismic-swarm-in-progress-in-cascadia-8323/

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3.8 magnitude earthquake hits area northwest of Hampton, NB

3.8 magnitude earthquake hits area northwest of Hampton, NB

Earthquakes Canada has confirmed a 3.8 magnitude earthquake hit an area 17 kilometres northwest of Hampton in southern New Brunswick this morning.

Nick Ackerley, an Earthquakes Canada seismologist, said the earthquake happened at 9:49 a.m. AT, approximately 17 kilometres west-northwest of Hampton and 35 kilometres north of Saint John.

Its preliminary magnitude was reported as 3.7, but Earthquakes Canada upgraded it later Thursday.

It was an “intraplate earthquake,” a type that happened inside the tectonic plate, as opposed to an interplate earthquake, which occurs in areas at the edge of a tectonic plate.

“The causes include things like long-dormant faults from previous mountain-building episodes, and glacial rebound,” Ackerley said.

“This part of Canada was under glaciers until about 10,000 years ago, and when the weight of the ice was lifted off, the Earth is slowly springing back, and that causes stress in the crust of the Earth.”

The government of New Brunswick tweeted officials are aware and are monitoring the earthquake.

Earthquakes Canada has confirmed a 3.8 magnitude earthquake hit an area 17 kilometres northwest of Hampton in southern New Brunswick this morning.

Nick Ackerley, an Earthquakes Canada seismologist, said the earthquake happened at 9:49 a.m. AT, approximately 17 kilometres west-northwest of Hampton and 35 kilometres north of Saint John.

Its preliminary magnitude was reported as 3.7, but Earthquakes Canada upgraded it later Thursday.

It was an “intraplate earthquake,” a type that happened inside the tectonic plate, as opposed to an interplate earthquake, which occurs in areas at the edge of a tectonic plate.

“The causes include things like long-dormant faults from previous mountain-building episodes, and glacial rebound,” Ackerley said.

“This part of Canada was under glaciers until about 10,000 years ago, and when the weight of the ice was lifted off, the Earth is slowly springing back, and that causes stress in the crust of the Earth.”

The government of New Brunswick tweeted officials are aware and are monitoring the earthquake.

Hughes said there’s no visible damage to her home.

Lee Jacobs said she and her husband heard a low rumbling that lasted for several seconds before the house starting “shaking violently.”

“I said, ‘What is that?’ And as soon as I said those words, the house started shaking. You could hear the sound before the shaking started.”

She called the earthquake an “unnerving” experience

3.8-magnitude quake considered minor

A 3.8 magnitude quake “could be widely felt,” according to Ackerley, depending on the depth at which it occurred.

That being said, a 3.8 magnitude is still considered to be a minor earthquake and unlikely to cause damage.

Earthquakes, while rarely severe, aren’t unheard of in New Brunswick.

In the spring of 2018, Earthquakes Canada recorded a “swarm” of 22 minor quakes on the western edge of the province near McAdam, a village also also rattled by a 3.3 magnitude earthquake in 2016.

In November 2016, a magnitude 3.1 earthquake was recorded 23 kilometres west-northwest of Miramichi.

But the last major earthquake, a magnitude 5, hit the Miramichi area in the 1980s, the largest earthquake to have affected the Maritimes since 1929.

Source: https://www.cbc.ca/news/canada/new-brunswick/earthquake-hits-northwest-of-hampton-1.4972818

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A low-intensity hum near Vancouver Island may help predict the next killer earthquake

A low-intensity hum near Vancouver Island may help predict the next killer earthquake

There has not been a major earthquake in the Cascadia subduction zone since 1700. But every year or so, there is a month-long ‘slow slip’ of tectonic plates.

It is well known that, off the coast of Vancouver Island, the massive undersea Juan de Fuca tectonic plate is slowly sliding under the larger North American plate, putting the west coast of Canada at grave risk of a megathrust earthquake and resulting tsunami.

What is lesser known about this process is the massive amount of energy that is unaccounted for, and might be building silently toward catastrophe. Newly published research based on artificial intelligence claims to have found it in a constant, low, background tremor, and, with it, a new way of predicting when the next big one might hit.

There has not been a major earthquake in what is known as the Cascadia subduction zone since about 9 p.m. on Jan. 26, 1700, long before Europeans first landed on Vancouver Island. The event is moderately well known to historians, however, for two reasons.

One is the oral histories and archeological remains of the various First Nations whose villages were swamped by a tsunami. Storytellers began to speak of dwarfs in the mountains who danced around a drum, causing the earth to shake and waters to rise. Others described a sea battle between a thunderbird and a whale that caused “a shaking, jumping up and trembling of the earth beneath, and a rolling up of the great waters,” according to research by Alan McMillan, who studies the archeology and ethnography of Vancouver Island First Nations at Simon Fraser University.

The other reason is that the tsunami also went the other way, westward to Japan, making landfall the next day, killing hundreds and sinking boats.

Ever since, Cascadia has been relatively quiet. But every year or so, there is a roughly month-long “slow slip,” when the North American plate lurches southwesterly over the Juan de Fuca plate.

This slip can account for as much as half of the total relative motion of the tectonic plates, as measured by displacement on the surface. It is usually accompanied by bursts of tremors, but the physics of “slow slip” is not well understood. It only occurs in some regions of the fault line between the plates, for example, while others appear to be “locked,” and only move in megathrust events.

This slip has been observed in advance of major earthquakes, which suggests it might be part of the process that causes them, according to a new paper by Bertrand Rouet-Leduc and Claudia Hulbert of the Los Alamos National Laboratory in New Mexico.

There is also a strange discrepancy between the amount of surface movement as measured by global positioning systems and the amount of energy measured by seismographs in tremors.

Somewhere in this process, a vast amount of energy has gone missing.

The key to finding it was to apply the tools of supervised machine learning, a kind of artificial intelligence that can separate a real signal from background noise. In a newly published paper, the researchers claim to have found that the Cascadia subduction zone is “continuously broadcasting a low-amplitude, tremor-like signal,” and that this low amplitude hum from the depths of the Earth “may account for most of this missing energy.”

Recognizing what this hum reveals about fault line physics might lead to something like an early warning system that “may prove useful in determining if and how a slow slip may couple to or evolve into a major earthquake,” the authors write in the journal Nature Geoscience.

They used seismic data from the Canadian National Seismograph Network and global positioning data from stations in the Western Canada Deformation Array, processed by the United States Geological Survey.

They found the Juan de Fuca plate is moving under the North American plate at around four centimetres a year as the North American plate slips over it. The highest slip speed for the North America plate, moving in the other direction, was also around four centimetres a year, which means that the transition zone between the plates — coastal British Columbia, basically — was slipping at around eight centimetres a year.

“The continuous tremor-like signal we identify tracks the slow slip rate, apparently at all times, and so provides real-time access to the physical state of the slowly slipping portion of the megathrust,” the authors write. “As the slow earthquakes transfer stress to the adjacent locked region where megaquakes originate, careful monitoring of this tremor-like signal may provide new information on the locked zone, with the potential to improve earthquake hazard assessment in Cascadia.”

Source: https://nationalpost.com/news/canada/a-strange-low-intensity-hum-near-vancouver-island-may-help-predict-when-the-next-killer-earthquake-will-strike

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Ontario town rattled by ‘mining-related’ earthquake

Ontario town rattled by ‘mining-related’ earthquake

It wasn’t a particularly strong quake, but it didn’t need to be for Kirkland Lake residents to feel the tremor on Wednesday night [December 12th, 2018] — it happened right underneath their feet.

According to Earthquakes Canada, the magnitude 3.2 earthquake was centred almost directly under the city, 2 km west-southwest of town, at a depth of 1.5 km. More than 100 people reported to Natural Resources Canada that they felt the quake, which struck at 11:16 EST Wednesday night. Weather Network viewers reported hearing a “loud blast that shook a lot of homes” at the time the quake was recorded.

Earthquakes Canada lists the tremor as ‘mining-related’, although no confirmation has been released. Local resident Jeff Wilkinson told CTV News he was concerned it might have been a fracture related to mining. “As you may know,” Wilkinson told CTV, “we have had some fatal rockbursts in this area, so we’re all sort of wondering whether it has happened again.” A rock burst is a sudden, sometimes explosive, fracture that can happen in deep mines. The rock surrounding a mine shaft is under tremendous pressure from the rock surrounding it; sometimes this pressure can cause the rock surrounding the shaft to give way.

DOES MINING CAUSE EARTHQUAKES, OR IS IT THE OTHER WAY AROUND? 

There has definitely been a lot of coverage of fracking-related earthquakes in recent years, as geologists point to the oil-extraction process for the rising number of quakes in places like Ohio and Oklahoma. Earthquakes related to mineral mining are a slightly different animal, however.

As happens with rock bursts, since mining leaves empty spaces that change the balance of pressure on the surrounding rocks, it’s not unusually to get minor earthquakes related to the collapse of excavated regions. The excavation process itself can also result in events that register on the seismometer. According to a report from the Canadian Hazards Information Service, “Literally hundreds of [mining-induced activity] blasts are recorded and identified by the project on a yearly basis.”

Sometimes it’s a case of ‘the chicken and the egg’, however.

A lot of the minerals that people mine for are actually largely found along fault lines — gold being among them. As Daniel Jaska, of the Geoscience Australia Earthquake Alert Centre, put it talking to ABC, “we have mining because of earthquakes.”

“[Minerals like gold] are [along faults] because when and earthquake occurs, there is generally a flow of water or liquid that interacts with the rocks,” said Jaska, “and over many millions of years forms minerals.”

While seismic activity in central Canada tends to be fairly low, thanks to a lake of tectonic plate interactions in the area, there are ‘weak zones’ within plates that are subject to shifting when stress builds up in the interior of a plate, thanks to constant pushing at its edges.

Source: https://www.theweathernetwork.com/news/articles/earthquake-felt-in-kirkland-lake-officials-believe-mining-related-gold-mine-mining-seismicity-rockburst/119806

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Regulator halts fracking operations in northeastern B.C. while investigating earthquakes

Regulator halts fracking operations in northeastern B.C. while investigating earthquakes

The B.C. Oil and Gas Commission has shut down oilfield fracking operations for at least 30 days in northeastern British Columbia while it investigates earthquakes that occurred there on Nov. 29.

The regulator says the seismic events, which measured between 3.4 and 4.5 magnitude, took place near hydraulic fracturing operations being conducted about 20 kilometres southeast of Fort St. John by Calgary-based Canadian Natural Resources Ltd. The practice is also known as fracking.

It says the company immediately suspended work on Nov. 29 and it won’t be allowed to resume without the written consent of the commission. Six companies in or close to the area have also suspended fracking operations. 

The area closed off is 11.6 kilometres by 6.4 kilometres in size, says the regulator.

According to Natural Resources Canada, the 4.5 magnitude earthquake was felt in Fort St. John, Taylor, Chetwynd and Dawson Creek but did no damage. It was followed by two smaller aftershocks.

Fracking involves injecting large amounts of water, sand and chemicals into a well to break up tight rock underground and allow trapped oil and gas to flow.

The technology, along with injecting oilfield liquids into disposal wells, have been linked by the B.C. commission to previous incidents of “induced seismicity,” although it notes on its website none of the events in B.C. have resulted in hazards to safety or the environment or property damage.

Earthquakes usually small, shallow

Honn Kao, a seismologist with Natural Resources Canada, told CBC’s Daybreak North that most fracking operations don’t produce induced earthquakes, and when they do, they’re relatively small and shallow.

The earthquake last week came close to matching the world’s largest fracking-induced earthquake which occurred a little further north in 2015 and registered magnitude 4.6.

The Fort St. John and District Chamber of Commerce says the shutdown is an attack on the already suffering oil and gas industry.

“We’ve gone through three bad years,” said Ramona McDonald, the chamber’s president.

“We do not need to go through another three years or another month even of shutdowns, because people are finally just starting to get back to work.”

Shutdown hurting business owners

McDonald, who runs a business that serves the oil and gas industry, says the shutdown could cost her upwards of $100,000 in lost contracts.

She says the shutdown is unnecessary and that there’s already scientific evidence backing the link between fracking and earthquakes. 

“This has been studied for a number of years … and has been going around and around in circles,” she said.

Natural Resources Canada says there’s still not complete certainty the earthquake was caused by fracking, although the two events seem strongly correlated.

“We need to do some more serious investigation to determine the physical mechanism that actually links these two phenomena together,” said Kao, the seismologist.

Injecting oilfield liquids can change the stress field in a location and dissipate in the vicinity, which is what investigators are looking at right now, Kao said. 

And although the earthquakes have so far been small, they suggest a greater risk of larger seismic activity, he said.

“The seismic risk associated with the development of shale gas and oil should not be overlooked.”

Source: https://www.cbc.ca/news/canada/british-columbia/bc-halts-northeast-fracking-operations-while-it-investigates-earthquakes-1.4937438

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Alaskans rattled by more than 2,100 aftershocks since last week’s earthquake

Alaskans rattled by more than 2,100 aftershocks since last week’s earthquake

Life was beginning to return to normal Monday in Alaska after a powerful earthquake near Anchorage on Friday, but people nervous about aftershocks were still grappling with damage that closed public buildings and schools, clogged roads and knocked homes off foundations.

Some residents went back to work. But state transportation officials again urged people who live north and south of Anchorage to take the day off or work from home to reduce traffic.

Rockfalls were still occurring along cliff-lined Seward Highway, while major repairs were underway on hard-hit Glenn Highway, the main road leading north of the city, Department of Transportation spokeswoman Meadow Bailey said.

“We don’t want the commute to be frustrating because people will experience delays,” she said.

Residents still jittery from the 7.0 quake on Friday have been rattled even further by more than 2,100 aftershocks. A dozen have had magnitudes of 4.5 or greater.

“Anything that moves, you’re on your last nerve,” said Anchorage resident Lyn Matthews, whose home sustained substantial structural damage, including a sunken foundation.

Matthews, who was back at work at a chiropractor’s office, and her husband have no earthquake insurance.

“I’m scared to death,” she said.

The earthquake struck 11 kilometres north of Anchorage, swaying buildings, disrupting power and causing heavy damage to Glenn Highway.

There were no reports of deaths, serious injuries or widespread catastrophic damage in the state with strict building codes implemented after a 1964 earthquake with a magnitude of 9.2 — the second most powerful of any quake ever recorded.

No outbreaks of disease or other major health problems have been reported.

Still, federal officials declared a public health emergency on Monday, saying the action will ensure that Medicaid funds continue to be issued despite the temporary closure of offices. Mental health aid is also available for people stressed by the disaster.

“Remember, whatever you’re feeling right now is valid,” Anchorage Health and Human Services director Natasha Pineda said at a weekend briefing.

Earthquake forecasts cited a 4 per cent chance of another earthquake with a magnitude of 7.0 or greater in the first week after the first quake.

“The chance is very small, but it’s not impossible,” U.S. Geological Survey Geophysicist Paul Caruso said.

The federal courthouse in Anchorage was among structures that remained closed. Officials said the U.S. District Court and the attached federal building in Anchorage will be closed at least through Thursday following a preliminary evaluation by the General Services Administration.

GSA spokesman Chad Hutson said boilers in the federal building were leaking, leaving it without heat.

The nearby Historic Federal Building, where the bankruptcy court is located, also remained closed. Officials said late Monday afternoon a detailed evaluation of the building found no structural deficiencies and the building is set to reopen Tuesday.

Schools in Anchorage have been closed until Dec. 10, which should also reduce traffic. An elementary school in the Anchorage suburb of Eagle River has been deemed unsafe to occupy, while multiple other campuses in the region are undergoing repairs and cleanup, according to the Anchorage School District.

A middle school in the small town of Houston north of Anchorage likely will remain closed through the year.

The supply chain of food and other goods delivered to the Port of Anchorage from the Lower 48 has not been disrupted.

About 90 per cent of all the goods sold in Alaska are delivered to the Port of Anchorage, where officials have completed a preliminary damage assessment. There were some structural issues with some trestles, but nothing that should impede operations, according to Municipal Manager Bill Falsey.

GSA spokesman Chad Hutson said boilers in the federal building were leaking, leaving it without heat.

The nearby Historic Federal Building, where the bankruptcy court is located, also remained closed. Officials said late Monday afternoon a detailed evaluation of the building found no structural deficiencies and the building is set to reopen Tuesday.

Schools in Anchorage have been closed until Dec. 10, which should also reduce traffic. An elementary school in the Anchorage suburb of Eagle River has been deemed unsafe to occupy, while multiple other campuses in the region are undergoing repairs and cleanup, according to the Anchorage School District.

A middle school in the small town of Houston north of Anchorage likely will remain closed through the year.

The supply chain of food and other goods delivered to the Port of Anchorage from the Lower 48 has not been disrupted.

About 90 per cent of all the goods sold in Alaska are delivered to the Port of Anchorage, where officials have completed a preliminary damage assessment. There were some structural issues with some trestles, but nothing that should impede operations, according to Municipal Manager Bill Falsey.


Source: https://www.cbc.ca/news/canada/north/alaska-earthquake-aftermath-1.4931912

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Powerful quakes buckle Alaska roads, briefly trigger tsunami warning

Powerful quakes buckle Alaska roads, briefly trigger tsunami warning

Back-to-back earthquakes measuring 7.0 and 5.8 rocked buildings and shattered roads Friday morning, November 30, 2018 in Anchorage, Alaska, sending people running into the streets and briefly triggering a warning to residents in Kodiak to flee to higher ground for fear of a tsunami.

The warning was lifted a short time later. There were no immediate reports of any deaths or serious injuries.

The U.S. Geological Survey said the first and more powerful quake was centred about 12 kilometres north of Anchorage, Alaska’s largest city, with a population of about 300,000. People ran from their offices or took cover under desks.

Cracks could be seen in a two-story downtown Anchorage building, and photographs posted to social media showed fractured roads and collapsed ceiling tiles at an Anchorage high school. One image showed a car stranded on an island of pavement, surrounded by cavernous cracks where the earthquake split the road.

Cereal boxes and packages of batteries littered the floor of a grocery store, and picture frames and mirrors were knocked from living room walls.

People went back inside after the first earthquake struck, but the 5.8 aftershock about five minutes later sent them running back into the streets.

A tsunami warning was issued for the southern Alaska coastal areas of Cook’s Inlet and part of the Kenai peninsula. Kodiak police on Kodiak Island warned people in the city of 6,100 to “evacuate to higher ground immediately.”

The National Weather Service Seattle tweeted a tsunami warning is in effect for Cook Inlet, but it is not expected to affect Washington or B.C.

Anchorage lawyer Hank Graper was driving when the quake struck. He first thought his vehicle had a flat tire, then thought it was exploding. He realized it was an earthquake after he saw traffic poles swaying.

Graper called it the most violent earthquake he’s experience in his 20 years in Anchorage.

David Harper was getting some coffee at a store when the low rumble began and intensified into something that sounded “like the building was just going to fall apart.” Harper ran to the exit with other patrons.

“The main thought that was going through my head as I was trying to get out the door was, ‘I want this to stop,”‘ he said.

Harper said the quake was “significant enough that the people who were outside were actively hugging each other. You could tell that it was a bad one.”

Thrown from bathtub

In Kenai, north of Anchorage, Brandon Slaton was alone at home and soaking in the bathtub when the earthquake struck. Slaton, who weighs 209 pounds, said it created a powerful back-and-forth sloshing in the bath, and before he knew it, he was thrown out of the tub by the waves.

His 55-kilogram mastiff panicked and tried to run down the stairs, but the house was swaying back and forth so much that she was thrown off her feet and into a wall and tumbled to the base of the stairs.

“It was anarchy. There’s no pictures left on the walls, there’s no power, there’s no fish tank left. Everything that’s not tied down is broke,” Slaton said.

Slaton ran into his son’s room after the shaking stopped and found his fish tank shattered and the fish on the closet floor, gasping for breath.

He grabbed the Betta fish and put it in another bowl. He says the area was eerily quiet. His children’s school was evacuated.

Alaska averages 40,000 earthquakes per year, with more large quakes than the other 49 states combined. Southern Alaska has a high risk of earthquakes due to tectonic plates sliding past each other under the region.

According to the U.S. Geological Survey, the Pacific plate is sliding northwestward and plunges beneath the North American plate in southern Alaska, the Alaska Peninsula and the Aleutian Islands.

On March 27, 1964, Alaska was hit by a magnitude 9.2 earthquake, the strongest recorded in U.S. history, centred about 120 kilometres east of Anchorage. The quake and the tsunami it triggered claimed about 130 lives.

Source: https://www.cbc.ca/news/canada/north/earthquake-anchorage-1.4927624

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