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Why the 7.0 earthquake felt different from Anchorage – and why it has the potential for more large after scaling

The earthquake 7.0 just north of Anchorage on Friday morning crushed the earth with 2 million tons of explosive power…

The earthquake 7.0 just north of Anchorage on Friday morning crushed the earth with 2 million tons of explosive power and generated 650 aftershocks within 30 hours, some of them big enough for raging residents again, experts say.

There is a good chance that more nervous scaling will not yet come.

A forecast issued Saturday by the United States Geological Survey provides a 88 percent chance for more magnitude 5.0 aftershocks, as the two shook the city and surroundings late Friday night.

Five aftershocks with magnitudes between 5.1 and 5.7 had occurred from Saturday night

The aftershocks have generally decreased in intensity and are expected to continue to do so. It is much less likely that a 6.0 aftershock or higher will occur, says the weekly forecast.

But residents should be careful because the power released by the earthquake fades, experts said.

People should keep a security plan in mind, as any desk or desk they should dash under for protection, “said Geoffrey Geyser, a geophysicist for research with the USGS National Earthquake Information Center

” It’s hard to handle after scaling because you never how long they will be, “he said.

After the earthquake on Friday morning, the geologists fought to analyze the aftershave mushrooms and other details. On Saturday they offered explanations why it felt different throughout the region and appeared to be longer for some people than others.

A person’s view is critical, but other factors are also counting, said Hayes, who said that he heard intervals of duration lasting 30 seconds to a few minutes.

“Time slowly slows down when you’re in an earthquake so,” Hayes said. “It has a lot to do with personal perception and where you are in Anchorage, and about the specific features of the local geologist you are on top of.”

The crime occurred as a huge disc about 30 miles below the ground where it was pulled out as a Snickers bar, “said Peter Haeussler, an American research geologist in Anchorage. That album sits in the southern part of Alaska.

The crime stretched for about 19 miles.

It’s a fraction of the crime during the massive 1964 shot, which extended 500 miles and was much founder, he said.

Anchor residents felt the shake for four minutes – much longer than Friday’s movement – in part because the 64-crash dropped energy over a wild field, from Prince William Sound to Kodiak.

On Friday, the first waves of energy issued by the earthquake would have reached Anchorage in about seven seconds, in the form of primary waves, Hayes said.

There are sound waves. When they arrive, people can hear something like a loud truck that rubs up the street.

The secondary waves come after, and should have reached Anchorage in about 13 seconds, Hayes said.

“It’s the big shake” when there’s suddenly a violent shot that leaves without a doubt a shake is going on, “said Haeussler.

The difference between the waves is like thunder and lightning – geologists can appreciate an earthquake mode by measuring the difference in the arrival time between the wave types, Haeussler said.

The different arrival times are also a reason why some felt that the shake of Friday lasted different lengths.

People further from the epicenter could have experienced the earthquake anymore as the difference between different types of waves is prolonged.

A major factor is the different types of materials under Southcentral Alaska, geologists said. People in permanent bedrock homes experience shaking faster, such as sudden drift. People on clay soils, like in West Anchorage, experience a longer, jiggling movement.

The seismic waves change as they move from silty basins like Cook Inlet and Strike Rock, bouncing back. It keeps the ground moving for longer periods in certain areas.

“They are like a wave in water striking a stock in a dam. It just runs back, he said.”

Data he has seen shows “really shaking less than a minute” in the Anchorage area, Tape said

However, the simulation also shows that the ground is kept moving for two minutes in some areas. It can also help explain why the shroud seemed longer for some people than others, he said.

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