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Originally posted by collietta
reply to post by JoeP2247
No problem. I think another thread was started on the same quake, and they called it Sacramento area.
Where I'm from (the earthquake area) we call Sac the bay area, and the people who live there flat landers. At least we did a decade ago.
glad you specified Westwood LA.
There's a Westwood between Susanville and Chester, about 30 odd miles from Canyon dam epicenter.
Originally posted by calstorm
reply to post by JoeP2247
That would be like an earthquake in Massachusetts setting of quakes in Florida. It is doubtful especially since this quake is not on a fault so it is most likely volcanic activity.
"Diane Johnson, Geologist:Zone is called the Mohawk Valley fault zone."
Originally posted by g146541
Originally posted by calstorm
Given the location of people posting, I should have felt it. Neither my fiance nor myself felt it. I was sitting here on ATS when it happened. *sigh*
Don't feel so alone, I did not know about it until my wife called and told me.
My dogs had been lying on the same spot on the bed for quite awhile and no jumping up and barking.
Come to think of it, no animals going nuts.
Fair Oaks here.
(Edit)
I've a suggestion to keep all of you occupied, learn to swimedit on 23-5-2013 by g146541 because: by the way...
Originally posted by applesthateatpeople
Originally posted by facelift
Originally posted by applesthateatpeople
reply to post by usaman1983
An earthquake in California?
Imagine that.
Another watered down comment?
Imagine that.
And your comment was what? Pure?
Earthquakes are part of life on Earth. Especially in California.
Eta: oh, I get it. You like stars. Gotcha now.
Sorry.edit on 23-5-2013 by applesthateatpeople because: (no reason given)
Volcanic earthquakes are common, although most are too small to be felt. Non-volcanic earthquakes along regional faults also occur—earthquake swarms in 1936, 1945-1947, and 1950 included several events above magnitude 4.0, with the two largest registering 5.0 and 5.5. Ground surveys show localized subsidence of the volcano, probably due to motion on regional faults.