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Japan is known for its earthquakes. A quake releasing ten times as much energy leveled the city of Nobi in central Japan in 1891, and others struck in 1927, 1943, and 1948 at other locations. The intervals between these great earthquakes—thirty-five, sixteen, and five years—hardly form a simple, predictable sequence, as is typical of earthquakes everywhere. If the historian H. A. L. Fisher failed to see in history “a plot, a rhythm, a predetermined pattern,” then so too have geophysicists failed utterly, despite immense effort, to discern any simple pattern in the Earth’s seismic activity. Modern scientists can chart the motions of distant comets or asteroids with stunning precision, yet something about the workings of the Earth makes predicting earthquakes extremely difficult, if not altogether impossible.
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