Shaking or trembling of the earth caused by movement along a fault
Types of faults
Strike-slip fault
Normal fault
Reverse fault
Normal fault
The block above the fault has moved downward relative to the block below
Reverse fault
The block above the fault moves up relative to the block below the fault
Strike-slip faults
Vertical (or nearly vertical) fractures where the blocks have mostly moved horizontally
Dextral fault
A strike-slip fault where the blocks have moved horizontally in a right-handed sense
Sinistral fault
A strike-slip fault where the blocks have moved horizontally in a left-handed sense
Geological folding
1. Plastic deformation (bending, buckling) of a single or multiple (stack) strata
2. Structural failure and faulting
Folds
Classified according to size, fold shape, tightness, and dip of the axial plane
Pressure on rocks
Can deform or break them, causing folds or faults
Anticlines
Folds that go up
Synclines
Folds that go down
Fault line
Water can flow through the crack and form beautiful cave formations
Earthquakes
Occur when rock shifts or slips along fault lines
Earthquakes
1. Generate waves that travel through the earth's surface
2. These waves cause damage around the epicenter
Ground shaking
Consequence of movement of seismic waves through the ground
Seismic waves
Caused by the sudden movement of materials within the Earth, such as slip along a fault during an earthquake
waves
Primary body waves; first seismic wave detected; able to move through both liquid and solid rock
waves
Secondary body waves that oscillate the ground perpendicular to the direction of wave travel; travel about 1.7 times slower than P waves; will not travel through liquids
Love waves
Only form on the surface of the Earth after a large earthquake; have a horizontal back and forth motion
Rayleigh waves
Move the surface of the earth around in a circle, forward and down then back and up