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As seismologists gained more experience from earthquake records, it became obvious that the problem could not be reduced to a single peak acceleration. In fact, a full frequency of vibrations occurs. ↗
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I suggested that we might compare earthquakes in terms of the measured amplitudes recorded at these stations, with an appropriate correction for distance. ↗
If one introduces the concept of energy of an earthquake then that is a theoretically derived quantity. ↗
This advice comes as a surprise: job searching is not joblessness; it is a job in itself and should be structured to resemble one, right down to the more regrettable features of employment, like having to follow orders--orders which are in this case self-generated. ↗
