one is the San Andreas Fault in California.
Some examples of strike-slip faults include the San Andreas Fault in California, the Anatolian Fault in Turkey, and the Great Glen Fault in Scotland.
strike-slip faults move along each other from shearing
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
The three faults are.... 1. Normal 2. Reverse 3. Strike-slip
Strike-slip faults generally do not produce tsunamis.
strike-slip faults move along each other from shearing
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
strike-slip faults where they move laterally
Strike-Slip faults are found at transform boundaries because strike slip faults push and pull on opposing forces HORIZONTALLY exactly like a transform boundary.
Horizontal faults can be refered to as lateral faults or strike-slip faults.
There are 6 types of fault lines. Strike-slip faults, dip-slip faults, oblique- slip faults, listric faults, ring faults, and synthetic and antithetic faults.
shear:)
Landslide
Strike-slip (transcurrent) faults. Oblique faults exhibit some strike-slip movement, but they also have a dip-slip component.
Strike-slip faults indicate rocks are sliding past each other horizontally, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.
The main direction of the stress on blocks of rock at normal faults, reverse faults and the strike slip faults usually happens at the weak areas.
Strike-slip faults cause shearing