Chapter 6 Test Flashcards
Earthquake
Vibrations in the ground that result from movement along faults or breaks in earth’s lithosphere
Fault
A break in earth’s lithosphere
3 types of faults
Normal fault
Strike slip fault
Reverse fault
Normal fault
Forms when forces pull rocks along a divergent plate boundarie; block above fault moves down
Strike slip fault
Two blocks of rock slide horizontally past each other in opposite directions
Reverse
Forces pushes two blocks of rock together with the rock above the fault moving up
Focus
Point beneath earth’s surface where rock under stress breaks to cause an earthquake
Epicenter
Point on the surface directly above the focus
Seismic waves
Waves that carry energy of an earthquake away from the focus
What are the 3 kinds of seismic waves?
Primary waves
Secondary waves
Surface waves
Primary waves (p-waves)
Compression waves that travel through solids and liquids
Secondary waves (S-waves)
Only travels through solids and temporarily changes shape
Surface waves
Moves slower than P and S waves, but can produce severe ground movement with a wavelike motion
Seismometers
Devices that measure and record ground motion and helps determine the distance seismic waves travel (Lag time)
How do you locate an epicenter?
By triangulating the data from at least 3 seismometers
- Find the lag time
- Find the distance to the epicenter
- Use map scale to mark radius on compass then draw circle around each