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Bizarre Earthquakes Off Oregon Coast

Posted on: Monday, 14 April 2008, 00:25 CDT

A peculiar swarm of earthquakes have been occurring off of Oregon’s central coast, resembling those that happen just prior to a volcanic eruption. However, scientists are baffled as there are no volcanoes in the area.  

There have been more than 600 quakes during the past 10 days in an area 150 miles southwest of Newport. The largest quake was a magnitude of 5.4, with two others measuring greater than magnitude 5.0, OSU reported.

Few of the quakes have been strong enough to be felt on land, and they have not shown the typical pattern of a major shock followed by a series of diminishing aftershocks.

Robert Dziak, a geophysicist for the National Oceanic and Atmospheric Administration and Oregon State University, suspects the quakes could be the result of molten rock rumbling away from the established faults in the area.

The scientists used underwater microphones called hydrophones to listen to the earthquakes.  Dziak told the Associated Press the quakes sound like low thunder on the hydrophones, and are unlike anything scientists have heard in 17 years of listening.   

Some of the quakes have also been detected by earthquake instruments on land.

The hydrophones are left over from a network the Navy used to listen for submarines during the Cold War
. The devices were also used to detect passing ships, whales calling out to one another and earthquakes on the ocean’s floor.

Dziak said the scientists hope to deploy an OSU research ship to gather water samples, searching for evidence of stirred up sediment and chemicals indicating magma is moving up through the Juan de Fuca Plate.

The Earth's crust is made up of plates that rest on molten rock, known as magma. The plates are constantly rubbing together.   When the magma erupts through the crust it creates volcanoes, which can occur in the middle of a plate. It’s possible that such an event would cause the plates lurch against each other, creating earthquakes along the edges.

Off the Oregon coast, the Juan de Fuca Plate is a small piece of crust being crushed between the Pacific Plate and North America, Dziak said.

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Image Caption: Satellite imagery of the northeast Pacific Ocean and western North Pacific Plate. Explorer, Juan de Fuca, and Gorda Ridges make up the plate boundary between the Pacific Plate and the Juan de Fuca/ Explorer/ Gorda Plates. The Cascadia Subduction Zone is also highlighted, which is the area where oceanic crust is subducting beneath the North American Plate. Courtesy NOAA

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On the Net:

National Oceanic and Atmospheric Administration

Juan de Fuca Plate - Wikipedia

Associated Press

Source: redOrbit Staff and Wire Reports

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User Comments (3)

3. Posted by hanna on 05/06/2008, 14:51
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2. Posted by tont on 04/18/2008, 08:45
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1. Posted by John Delano on 04/15/2008, 07:12
For 33 years I have researched landforms and the 20 mile deep and 20 mile high ice shell that moved based on the Milankovich Orbits. The asemetric distribution of original ice shell or ice cap on 1/2 of planet Earth was the 20 mile deep lithosphere and moving art 6 inches per year, crust and ice shell , the mamimum spped would have to "rift" sidways [fracture zone -transcurrent fault] when the extreme 413,000 year elytical orbitasl cycle ocurred. You only have to look inland at the physical results laid down by the retreating ice shell. The Columbia Plateau ,is a direct mirror image of the 413,000 year eliptical cycle. All 23 steps of the Columbia Plateau are 45 to 60 feet high. All were laid down 413,000 years apart, and took 9.3 million years to creat. Its the retreating end of the ice shell movement, emitting under pressure from twenty miles down maga, lava onto the surface to be smoothed by the ice above into a step,again and again. This is original thoughs from the author Delano's Discovery- lulu.com

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