Geology and oceanography have come together this year in the Ocean Observatories Initiative, an unprecedented new tool for monitoring our coast. It will improve the already comprehensive seismic network throughout the Northwest and California.
Currently, some 240 seismometers have been installed throughout Washington and Oregon to detect vibrations. They send readings to a computer at the UW, where the regional seismic network creates an automated report within about 10 minutes after any seismic event.
Brian Atwater found evidence of repeating full rip subduction zone earthquakes on the shore. Atwater linked the evidence of the 1700 Cascadia earthquake on the West Coast on January 26, 1700, to the tsunami arrival in Japan, that hit some 24 hours later.
Chris Goldfinger found evidence of the same full rip subduction zones off the West coast using deep sea drilling, about 19 times over the last 10,000 years.
But in addition to the full rip, Goldfinger found another 21 past earthquakes in the southern Oregon coast.
The geologic evidence of nineteen subduction zones over 10,000 years is about every 500 years. About every 250 years if you count the smaller, southern Oregon subduction events. Since we’re about 317 years since the last (big) subduction event in 1700, the southern coast looks overdue. But a full-rip, 9.0 event could also happen relatively soon. Nobody knows when, but it WILL HAPPEN.
The Pacific Northwest Seismology Network (PNSN) recently implemented an earthquake warning system to predict the strength and location of earthquakes and provide short-term warnings. The earthquake warning system is under development, but not yet available to the public.
ShakeAlert would use a network of high-end sensors placed by a consortium that includes the Berkeley Seismological Laboratory, the U.S. Geological Survey, the Caltech Seismological Laboratory, University of Washington and the University of Oregon.
It might give Seattle and Portland as much as three or four minutes’ warning for a big offshore quake near the Bay Area, and as much as 30 seconds for an earthquake on one of the onshore faults. But there’s no funding to make it public. The Cascadia Region Earthquake Workgroup has more. Here are the Latest Earthquakes in the North Pacific.
The Cascadia Initiative (pdf) is assembling a much more complete scientific picture of the Northwest’s most dangerous fault — including what to expect the next time it ruptures. It’s deployed more than 60 ocean-bottom seismometers and pressure gauges and is now receiving a “live” profile of events off our coast.
The Ocean Observatories Initiative has wired up the west coast, from California to Canada. It’s the most extensive ocean monitoring system yet devised. Rutgers plans to hook up their ocean observatory to similar projects on the East coast and will deliver OOI’s Cyberinfrastructure. Woods Hole, Oregon State University and Scripps are responsible for the OOI coastal and global arrays and their autonomous vehicles.
Sensors on the Axial Seamount on the Juan de Fuca spreading center are now live. Axial is the most active volcanic site in the North Pacific.
Join the crew on the April-May 2015 Axial Seamount expendition, mapping, and sampling the new lava flows from the 2015 eruption. In the summer of 2014, Bill Chadwick and colleagues correctly predicted that Axial Seamount would erupt in 2015.
Maybe they’ll bring back some hyperthermophiles, one of many weirdly amazing extremophiles. They can live in temperatures above boiling, in crushing depth and blackness. They’re surrounded by sub-freezing water kept liquid by immense pressure.
How did they get there?
CRISPR was named Science’s Breakthrough of the Year. The “molecular scalpel for genomes” can edit the DNA of fertilized human embryos and has already helped create a menagerie of genetically new organisms. MIT’s Technology Review calls it “the biggest biotech discovery of the century“.
The Wild West.
John Delaney, father of deep-sea, fiber-fed observatories, explains it all.