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← GeographyWhich outcome results when regional stress exceeds a fault's static friction?
A)Abrupt release triggers seismic waves✓
B)Creep deformation minimizes energy release
C)Gradual folding creates monoclines slowly
D)Mantle convection plate velocity stalls
💡 Explanation
Seismic waves are triggered because elastic rebound along the fault overcomes static friction. The Fault rupture progresses as stored stress exceeds the frictional strength, causing a sudden slip; therefore, seismic energy is released, rather than gradual creep, folding or mantle changes.
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