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As the relatively young Pacific plate dives beneath the continental land mass, sudden slippages along the grinding rock faces breed swarms of earthquakes, big and small.
Similar(59)
Geological faults can release the pressure in three ways: a steady slippage called creep, a stuttering series of nearly imperceptible microquakes, or a sudden catastrophic earthquake.
Those slippages can be disappointing.
There have been notable slippages.
Sudden rise?
Sudden sensation.
The end was sudden.
It was random, sudden.
Fainting, sudden dizziness, weakness.
There were sudden avalanches.
Why the sudden interest?
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