How strong is a 9 earthquake?

A magnitude 9.0 earthquake can last for five minutes or longer, and the amount of energy released is about 1,000 times greater than that of a 7.0. According to the U.S. Geological Survey, the most powerful quakes could leave few if any masonry buildings standing, destroy bridges and toss objects into the air.

opb.org - What Is A 9.0 Earthquake? - OPB

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Monday, January 26, marks 315 years since a major Cascadia Subduction Zone earthquake shook Oregon. Geologists believe that quake was around a magnitude 9.0 — and that another one is looming for the region. Understanding the level of destruction associated with these types of temblors makes it clear why geologists are so concerned.

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What is a subduction zone earthquake?

A subduction zone is a large area where two plates of the Earth's crust meet and one is forced under the other. The plates sliding past each other cause extreme amounts of force to build up as friction restricts the movement. When the amount of force built up exceeds the friction holding it back, the plates slide past each other, causing the ground to rumble. Subduction zone earthquakes typically break across a much larger area than fault-line "bullseye" quakes (like the San Andreas), and can affect an area hundreds of miles long.

How do we know the subduction zone exists here?

Mostly because of geological data left behind by subduction zone earthquakes, known as megathrust earthquakes. Subduction zones are the only type of plate meeting that can cause earthquakes greater than magnitude 8.5, according to the Pacific Northwest Seismic Network. The last one off the Oregon coast happened January 26, 1700.

Why do scientists worry that we'll have a 9.0 earthquake off the Oregon Coast?

Geological evidence shows that earthquakes at or near a magnitude 9.0 have been happening along the Cascadia Subduction Zone for thousands of years. Scientists have even been able to figure out how often they happen along the fault section that spans the Oregon Coast — an average of every 234 years. Since the last one happened 315 years ago, Oregon is due for a major event. A timeline of documented earthquakes along the Cascadia Subduction Zone throughout history. Oregon State University and DOGAMI

How is a 9.0 different from a 6.0, or a 7.0?

There is a significant difference in the damage caused by a magnitude 9.0 earthquake and a more common magnitude 6.0 or 7.0. In the latter, the shaking does not last as long and it may only damage poorly built structures. Sometimes a magnitude 7.0 earthquake can be strong enough to damage earthquake-resistant structures, however. A magnitude 9.0 earthquake can last for five minutes or longer, and the amount of energy released is about 1,000 times greater than that of a 7.0. According to the U.S. Geological Survey, the most powerful quakes could leave few if any masonry buildings standing, destroy bridges and toss objects into the air.

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What causes earthquake?

The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.

usgs.gov - What is an earthquake and what causes them to happen? - USGS.gov

An earthquake is caused by a sudden slip on a fault. The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel. In California there are two plates - the Pacific Plate and the North American Plate. The Pacific Plate consists of most of the Pacific Ocean floor and the California Coast line. The North American Plate comprises most the North American Continent and parts of the Atlantic Ocean floor. The primary boundary between these two plates is the San Andreas Fault. The San Andreas Fault is more than 650 miles long and extends to depths of at least 10 miles. Many other smaller faults like the Hayward (Northern California) and the San Jacinto (Southern California) branch from and join the San Andreas Fault Zone. The Pacific Plate grinds northwestward past the North American Plate at a rate of about two inches per year. Parts of the San Andreas Fault system adapt to this movement by constant "creep" resulting in many tiny shocks and a few moderate earth tremors. In other areas where creep is NOT constant, strain can build up for hundreds of years, producing great earthquakes when it finally releases.

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