An earthquake hitting Fashion Island. This was its size

People reported their feeling of the earthquake until South Pears, north of Seattle and around Port Orkard.

Fashun Island, Washington – Fashion Island's earthquake later on Monday night, according to the northwestern seismic network in the Pacific Ocean (PNSN).

The tremors spread in a wide area, where people were informed in Takoma, Ranton, Seattle, Schorlain, Bethael, Ellac Park, that they felt the tremors.

Did you feel it? If so, you can fill a report with PNSN to help them learn more about the earthquake here.

The earthquake measured 3.3 on the Richter scale, which is simple. Earthquakes are observed on a wider scale once they reach a size 4, but until then, they usually cause little or non -damage.

The earthquake occurred more than 15 miles below the surface of the earth and hit around 11:10 pm, the earthquake center was placed in the water between the Beach of Magnolia and Perbin on Fashun Island.

To date this year, there have been earthquakes in Sequim, OCS Island, Bremerton so far this year. This is normal for the active area of ​​seismic terms such as Washington State. Earthquakes occur almost every day in our area, but most of them are very small so that they cannot be felt or cause damage, according to the Ministry of Natural Resources (DNR).

How common is earthquakes in western Washington?

Several earthquakes in Washington state are connected to the movement of the Juan de Voca plate and the North American continental plate moving against each other while the Juan de Voca plate slides under the continent of North America, according to PNSN. This is called Cascadi's criticism.

Washington has the highest danger in the United States to experience a large and destroyed earthquake due to its geological situation.

Northwest Pacific usually test three types of earthquakes:

Shallow rift earthquakes: rupture in errors at the highest 18 miles of the Earth's crust. These earthquakes usually last from 20 to 60 seconds and shake is translated into the area near the error, according to DNR. Deep earthquakes: deep errors occur when two tectonian panels collide and slide one plate under the other. These earthquakes can affect a large but less intense space. Integration area earthquakes: This earthquake is caused by a peripheral plate tension sliding under a continental plate. When it builds enough stress, the error will extend, which releases a huge amount of energy. CASCADIA has the possibility of these types of earthquakes and has been torn in the past. It is one of Washington State, according to DNR.

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