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Magnitude 6.0
Date-Time Wednesday, February 15, 2012 at 03:31:20 UTC
Tuesday, February 14, 2012 at 07:31:20 PM at epicenter
Time of Earthquake in other Time Zones
Location 43.536°N, 127.381°W
Depth 10 km (6.2 miles)
Region OFF THE COAST OF OREGON
Distances 256 km (159 miles) W of Coos Bay, Oregon
293 km (182 miles) WSW of Newport, Oregon
302 km (187 miles) NW of Brookings, Oregon
380 km (236 miles) WSW of SALEM, Oregon
Location Uncertainty horizontal +/- 19.7 km (12.2 miles); depth +/- 6.2 km (3.9 miles)
Parameters NST=205, Nph=211, Dmin=282.8 km, Rmss=1.15 sec, Gp=180°,
M-type=regional moment magnitude (Mw), Version=6
Source Magnitude: USGS NEIC (WDCS-D)
Location: USGS NEIC (WDCS-D)
Event ID usb00080ib
Magnitude 4.2
Date-Time Tuesday, February 14, 2012 at 22:54:40 UTC
Tuesday, February 14, 2012 at 02:54:40 PM at epicenter
Time of Earthquake in other Time Zones
Location 49.214°N, 128.751°W
Depth 10 km (6.2 miles)
Region VANCOUVER ISLAND, CANADA REGION
Distances 191 km (118 miles) SSW of Port Hardy, British Columbia, Canada
235 km (146 miles) W of Ucluelet, British Columbia, Canada
268 km (166 miles) WSW of Campbell River, British Columbia, Canada
405 km (251 miles) WNW of VICTORIA, British Columbia, Canada
Location Uncertainty horizontal +/- 25 km (15.5 miles); depth +/- 2.7 km (1.7 miles)
Parameters NST= 33, Nph= 33, Dmin=268.3 km, Rmss=0.65 sec, Gp=212°,
M-type=body wave magnitude (Mb), Version=9
Source Magnitude: USGS NEIC (WDCS-D)
Location: USGS NEIC (WDCS-D)
Event ID usb00080ej
Magnitude 5.6
Date-Time Monday, February 13, 2012 at 21:07:02 UTC
Monday, February 13, 2012 at 01:07:02 PM at epicenter
Time of Earthquake in other Time Zones
Location 41.143°N, 123.790°W
Depth 28.2 km (17.5 miles)
Region NORTHERN CALIFORNIA
Distances 9 km (5 miles) SW (234°) from Weitchpec, CA
28 km (17 miles) NNW (343°) from Willow Creek, CA
29 km (18 miles) ENE (67°) from Westhaven-Moonstone, CA
50 km (31 miles) NE (38°) from Eureka, CA
349 km (217 miles) NW (326°) from Sacramento, CA
Location Uncertainty horizontal +/- 0.4 km (0.2 miles); depth +/- 1.2 km (0.7 miles)
Parameters Nph= 47, Dmin=20 km, Rmss=0.27 sec, Gp= 72°,
M-type=regional moment magnitude (Mw), Version=8
Source California Integrated Seismic Net:
USGS Caltech CGS UCB UCSD UNR
Event ID nc71734741
Originally posted by westcoast
The leading theory is that the Cascade Volcanic Chain is fed by the subduction zone
...that at the point of friction the rock becomes molten and has to find a way to the surface...hence a volcano.
There's no obvious "supercyle" of supergiant quakes, as Satake suggests, in Japan. But it is clear that quakes on Cascadia have varied in size, said USGS scientist Brian Atwater. Some geologists argue the magnitude-9 quake 300 years ago was simply average and that the Northwest has been slammed by quakes twice as big in the distant past.
“You have two hypotheses – movement along a fault on the mountain (and there are lots of faults up there) or movement of magma to the surface. Anytime they are small and a swarm, there is a strong possibility that it is magma moving.”
Kind of weird to think about hot magma moving underneath the cold, snowy mountain you’re skiing and snowboarding on, isn’t it?
All two dozen micro-quakes on Mt. Hood have been less than magnitude 2. Now let’s see how many of these earthquakes we have before the mountain goes silent again!
Several conclusions are apparent. First, Sisters is active and bears close monitoring. Second, were this injection to lead to an eruption, it might form a new vent, however it is important to remember that much more magma is injected into the crust than erupted on the surface. Third, the volume injected is modest, so that it would take many such injections to provide the magma for a significant eruption. Fourth, we cannot count on seismicity to provide clear signals of injection - study of deformation is a critical complement to seismic monitoring.