The difficulties associated with earthquake prediction are reviewed. The once-promising dilatancy theory has been displaced by monitoring of small earthquakes and earthquake swarms. While the ability to observe possible precursors has increased considerably, no reliable precursor has been found; without a long, detailed monitoring record, it is difficult to tell if some anomalous activity foretells a major earthquake. The existence of slow earthquakes would greatly complicate long-term prediction. (RWR)
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Richard A. Kerr (1978) studied this question.
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