We can find strike slip fault between two tectonic plates.
For exemple; San Andreas fault in California is a strike slip fault and represent the limit between America plate and Pacifique plate. These two plates move with an inverse movement(~1 towards the north and ~1 toward the south).
But we can also find this kind of fault in other context like in a colision.
The San Andreas Fault is a strike slip fault.
LATERAL A+
Strike slip faults occur where there are large shear stresses in the earth's crust. This includes places such as transform boundaries.
Directly above the focus on the surface of Earth
Slip-strike faults always occur at transform boundaries. The San Andreas Fault is a famous transform boundary in located in southern California.
Horizontal faults can be refered to as lateral faults or strike-slip faults.
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.
transform
bobobobobo
Slip-strike faults always occur at transform boundaries. The San Andreas Fault is a famous transform boundary in located in southern California.
Convergence, divergence and strike slip.
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.