The distance from the epicenter to a place where the earthquake is recorded through a seimograph is called:
A. focus
B. epicenter
C. focal depth
D. epicenter depth
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The depth between focus and epicenter is called :
A. focal depth
B. epicenter depth
C. focus
D. epicenter
The point at which the vibration initiates and thus the energy is released in the crust or mantle is called:
A. epicenter
B. epicenter distance
C. focal depth
D. focus
The elastic rebound theory was proposed to explain why earthquake occur based on the observation of the earthquake happened on the San Andreas Fault that devastated San Francisco in 1906.
The elastic rebound theory was proposed to explain why earthquakes occur based on the observations of the earthquake on the San Andreas Fault that devastated San Francisco in 1906.