Faults and Earthquakes Note: you should also have pictures drawn in your notes about where earthquakes occur along other plate boundaries (ie divergent, convergent boundaries
How Seismographs Work
Seismic Waves
Locating Earthquakes
Locating Earthquakes - Depth
Elastic Rebound
Strike-Slip Fault – Left Lateral
Strike-Slip Fault – Right Lateral
Dip-Slip Fault - Normal Hanging wall footwall
Dip-Slip Fault - Reverse 3. Faults are classified by the kinds of movement that occur along them Hanging wall Foot wall
Oblique Slip Faults
Subduction zones
Waves Travel The Fastest Path
Shadow zones
tsunamis I will expect you to be able to draw/label this and understand how the tsunami wave changes (in height, speed and wavelength) as it moves from the ocean to the shore. Be sure to understand how the wave is generated (you should have a picture that we drew together in class)