It was here before anyone made a map and called this corner of it the Pacific Northwest.
Research published in the May 6 edition of Science indicates that slow-motion earthquakes or "slow-slip events" can rupture the shallow portion of a fault that also moves in large, tsunami-generating earthquakes. The finding ...
A new paper titled "Experimental study of the electrical conductivity of hydrous minerals in the crust and the mantle under high pressure and high temperature," published in Science China Earth Sciences, overviews the studies ...
When Jerry Paros shipped a seafloor sensor from his plant in Redmond to Japan in 2010, he never expected to see it again.
Deep beneath Alaska's Aleutian Islands, down where the pressure and temperatures have become so high that rock starts to flow, new continental crust is being born.
Make no mistake. Once a tsunami has formed, it cannot be stopped. But those in charge of keeping communities safe when one strikes should listen to experts' warning signs and take the necessary precautions to prevent an already ...
Geologists from Brown University may have finally explained what triggers certain earthquakes that occur deep beneath the Earth's surface in subduction zones, regions where one tectonic plate slides beneath another.
As military helicopters ferry search and rescue teams over the Pacific Northwest, below them are scenes of devastation from a giant earthquake that could strike the region at any time.
Research teams have evaluated the major 7.8 magnitude subduction zone earthquake in Gorkha, Nepal, in April 2015, and identified characteristics that may be of special relevance to the future of the Pacific Northwest.
The bottom of the ocean just keeps getting better. Or at least more interesting to look at.