Induced Seismicity

Induced seismicity refers to typically minor earthquakes and tremors that are caused by human activity that alters the stresses and strains on the Earth's crust. Most induced seismicity is of an extremely low magnitude. A few sites regularly have larger quakes, such as The Geysers geothermal plant, which in the past 5 years has averaged 2 M4 events and 15 M3 events every year.

Read more about Induced Seismicity:  Causes, U.S. National Research Council Report

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