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 and transform faults are associated with shear stress.
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
three kinds of faults are normal fault, reverse fault, and strike-slip fault.