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The buildup of stress in Earth's crust can become so great that rocks reach their __________.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
Normal faults are created by __________.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
Buildings collapse as soil beneath becomes liquid.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
The farther apart primary, secondary, and surface waves arrive, the __________ the epicenter is.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
The San Andreas Fault in California is an example of a __________.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
The slowest seismic waves are __________.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
__________ do not pass through liquid so they are stopped when they hit the liquid outer core.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
A reverse fault is often located where plates __________.
come together
elastic force
strike-slip fault
liquidity
Surface waves
tension
farther away
Secondary waves
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