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Originally posted by TrueAmerican
..... Why? Because all my study has been on my time, with my own techniques, and I am not publicly funded in any way, shape or form. I can't afford to do this, and yet still I persist. That is worth something, much the same way huge investments in seismo networks pay off for oil and mineral investment companies. And it is tedious work.
Originally posted by BO XIAN
I'm wondering . . . looking at the Pacific NW situation . . . do you imagine that such a sudden drop/rise as that cliff face might happen there?
Originally posted by westcoast
It is what it is. While I enjoy discussing all the possible indicators and raise awareness and educat; I surely do not want to panic anyone and cause them to uproot their lives based on nothing more than theories.
Originally posted by TrueAmerican
reply to post by BobAthome
Hopefully this thread was a waste of time, and so far it appears that way, thank God. The last thing I want to see, for real, is a massive quake out there. But again I say, I don't like it when things deviate from the norm.
Vital Signs.
Utilities and transportation in the I-5/Highway 99 corridor will be disrupted for months
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.