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Re: Astabula Ohio/Kermadec Is. earthquakes
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Posted by Lowell on June 04, 2001 at 15:30:07:
The idea of triggering of small earthquakes within 2,000-3,000 km of large earthquake is now generally accepted by geoscientists. What many do not realize is that the amplitude of seismic waves does not reduce monotonically with distance. There distances from the source where the amplitude of seismic waves is very high (called nodes) others where it is low. This variation in amplitude is caused by reflection and refraction off the internal boundaries of the earth and by geometric focussing. For example the calculated amplitude of surface waves near the antipode of an earthquake (180 degrees away), is very nearly the same as the amplitude 500 km away. If we can accept the idea that small earthquakes can be triggered at 500 km from a large source, why then, is it difficult to say that the same triggering mechanisms can exist at long distances where the ground motion is similar. Anyway, even if this is idle speculation, there is no better place for this kind of speculation than on this board. I hope that we all understand that the field of earthquake prediction is one of the few places left where speculation may actually lead to results (since none of the current theories seem to be leading anywhere except in circles - at least we can say they haven't been very successful at predicting earthquakes.) So I welcome harmless quantum leaps - bring them on if you have them.
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