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Originally posted by TrueAmerican
reply to post by PuterMan
Oh for Pete's sakes, stop being so grumpy and let me play. I might just surprise the crap out of you in the next months.
Also in regards to:
reply to post by PuterMan
When I said frequency was increasing, I didn't mean long term averages, at all. I know you are the long term average king, but I am talking about when in a short period of time they increase in frequency. Like two quakes on different parts of the fault within hours of each other. That's what I meant, sweetheart.edit on Sat Feb 4th 2012 by TrueAmerican because: (no reason given)
Originally posted by steve95988
I live in norcal and think its about over due for a large earthquake along the westcoast..
In-fact it may be a blessing in disguise,, shake some of these idiots up a lil!!
Originally posted by Tw0Sides
I have a theory, probably nothing.
Originally posted by TrueAmerican
A suite of 15 Episodic Tremor and Slip events imaged between 1997 and 2008 along the northern Cascadia subduction zone suggests future coseismic rupture will extend to 25 km depth, or ~60 km inland of the Pacific coast, rather than stopping offshore at 15 km depth. The ETS-derived coupling profile accurately predicts GPS-measured interseismic deformation of the overlying North American plate, as measured by ~50 continuous GPS stations across western Washington State.
When extrapolated over the 550-year average recurrence interval of Cascadia megathrust events, the coupling model also replicates the pattern and amplitude of coseismic coastal subsidence inferred from previous megathrust earthquakes here. For only the Washington State segment of the Cascadia margin, this translates into an Mw=8.9 earthquake, with significant moment release close to metropolitan regions.
www.geodesy.cwu.edu...
Visit link to see some charts.
In other words, there are good reasons to believe a future big quake could occur either very close to shore, or under land itself. The good news is that the further inland it occurs, the deeper that it is likely to be, because of the dip angle of the subducting slab.
The worst case scenario in my opinion is a very big quake, literally right offshore, making it quite shallow, and allowing only minutes or seconds reaction time to a very big tsunami.
The transition starts offshore near 10 km depth, with 100% "locked"-coupling dropping smoothly to half by 25 km depth. However, unlike previous models, the lower limit of the effective transition zone here is constrained by repeated ETS events to be near 25 km depth. To fit the interseismic GPS data while matching the estimate of moment release by ETS, plate coupling must drop abruptly from 50% up-dip of the 25 km depth to less than 15% within the ETS zone, before trending smoothly to 0 (i.e., "freely sliding") by 70 km depth.
A suite of 15 Episodic Tremor and Slip events imaged between 1997 and 2008 along the northern Cascadia subduction zone suggests future coseismic rupture will extend to 25 km depth, or ~60 km inland of the Pacific coast, rather than stopping offshore at 15 km depth.
The most important aspect for northern Cascadia is that stronger coupling between 15 and 25 km implies greater coseismic slip near major population centers, and provides an estimate of future coseismic slip along this region. 50% coupling suggests 9 meters of slip should be expected directly up-dip of 25 km. This lies well inland of the coast, directly west of the greater Seattle-Tacoma metropolitan basin.
Originally posted by Olivine
reply to post by zworld
Hi zworld, thanks for all of the information and associated articles. The CSZ is absolutely a catastrophe in the making.
I interpret this study a little differently, although the awful conclusions are still the same.
To me, the author is saying that instead of anticipating "only" a rupture of the "100% locked zone", which is the area from the trench/toe/accretionary wedge, then inland to a depth of 10-15 km (still offshore in most of the northern CSZ); but now, because of ETS data, they anticipate the ruptured fault area to include the above plus the area in the "transition zone" to a depth of 25km, which, at the surface, is approximately 60 km inland.
So, a much larger fault surface area than previously thought possible, and closer to Seattle-Tacoma.
Originally posted by TrueAmerican
reply to post by westcoast
Best I can tell through spectrum, it appears to be either a very small seismic event or even an ice quake. Heh, and Lord knows we have experience with those now... But you sure those UTC times match up to the exact time you heard this? Cause right after that there appears to be some kind of long, 9 Hz or so, narrow band hum of some kind coming from that station- or from something.
Magnitude
3.0
Date-Time
Thursday, February 09, 2012 at 21:58:41 UTC
Thursday, February 09, 2012 at 01:58:41 PM at epicenter
Time of Earthquake in other Time Zones
Location
40.334°N, 125.195°W
Depth
0.6 km (~0.4 mile) (poorly constrained)
Region
OFFSHORE NORTHERN CALIFORNIA
Distances
77 km (48 miles) W (271°) from Petrolia, CA
83 km (52 miles) WSW (251°) from Ferndale, CA
93 km (58 miles) WSW (253°) from Fortuna, CA
101 km (63 miles) WSW (240°) from Eureka, CA
372 km (231 miles) NW (321°) from San Francisco City Hall, CA
Location Uncertainty
horizontal +/- 3.2 km (2.0 miles); depth +/- 8 km (5.0 miles)
Parameters
Nph= 32, Dmin=76 km, Rmss=0.25 sec, Gp=263°,
M-type=duration magnitude (Md), Version=1
Source
California Integrated Seismic Net:
USGS Caltech CGS UCB UCSD UNR
Event ID
nc71727275