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A force that acts on rock to change its shape or volume is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
The fastest seismic waves that compress and expand are called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
A fault where tension causes the hanging wall to slip below the footwall at a divergent plate boundary is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
A wave or series of waves produced by an earthquake or a landslide is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
The point directly above the focus where seismic waves release the most energy during an earthquake is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
Stress that squeezes a rock until it bends or breaks is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
The slowest seismic waves that move side to side are called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
A fault where the compression causes the hanging wall to slide up and over the footwall at a convergent boundary is called
Normal fault
Compression
Primary (P) waves
Stress
Secondary (S) waves
Tsunami
Epicenter
Reverse Fault
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