aftershock
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The Landers fault (red lines at left) and the Hector
Mine fault and its aftershocks (red lines and circles at right). The
Hector Mine earthquake was a magnitude 7.1, and it produced thousands
of aftershocks. Image credit: Egill Hauksson, Caltech
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An earthquake that follows the largest
shock of an earthquake sequence. Aftershocks are smaller than the mainshock
and within 1–2 fault lengths distance from the mainshock fault. Aftershocks
can continue over a period of weeks, months, or years. In general, the larger
the mainshock, the larger and more numerous the aftershocks, and the longer
they will continue. Related category
• GEOLOGY
AND PLANETARY SCIENCE Source: U.S.
Geological Survey
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