Most faults are inactive and stand as geologic evidence of past structural deformation.

Name: Most faults are inactive and stand as geologic evidence of past structural deformation.
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Most faults are not currently active, meaning that they are not currently experiencing significant movement or causing earthquakes. Instead, they serve as evidence of past tectonic activity and can help geologists understand the history of an area's structural deformation.

Most Faults Are Inactive and Stand as Geologic Evidence of Past