Ch.2 Flashcards
Stress-
A force that acts on rock to change it’s shape and volume.
Earthquake-
The shaking and trembling that results from the movement of rock beneath earths surface
Convergent boundary =
Stress force. Fault. Movement
Compression. Reverse. Hanging
Wall up
Divergent=
Stress force. Fault. Movement
Tension. Normal. Hanging wall⬇️
Transform=
Stress force. Fault. Movement
Shearing. Strike slip. No hanging wall
Deformation
Change in the volume or shape of earths crust
Focus
The point beneath the surface where the earthquake begins
Epicenter-
The point directly above the focus on the surface
Seismic waves-
The energy wave made by an earthquake through the crust
Primary waves-
Fastest compression waves
Secondary waves
Next wave you feel, side to side, longitude wave
Surface wave-
-slowest wave; the combination of P&S waves, most destructive
Shearing-
Stress that pushes a mass of rock on two opposite directions
Tension-
Pulls on the crust, stretching rock so it becomes thinner in the middle
Compression-
Squeezes rock until it folds or breaks
De formation-
Any change in volume or shape of earths crust
Where do faults normally occur?
Along plate boundaries, where the forces of plate motion compresses or pulls the crust so much it breaks
Strike slip fault-
When rocks on either side I the fault slip past each other sideways with a little up or down motion
Normal fault-
A fault at an angle so one block of rock lies above the fault while the other block lies below.
Seismograph-
Instrument used to record ground movements cause by shock waves
3 types of scales used to measure shock waves-
Mecalli scale- 12 step scale
Richter scale - based on how min damage is done
Moment magnitude scale- estimates total energy released, each step is 100x stronger
Triangulation-
You have to Figure the distance from earthquakes and draw circles around seismic station that distance. Use 2 other station doing the same thing. Where the 3 circles meet is where the earthquakes occurred
Liquid faction -
Seismic waves turn loose, soft soil into non-liquid mud
After shocks
Occur after main shocks, usually smaller, hours or days later