compression
compression
shearing
The type of stress force that produces a strike-slip fault is transform stress. This stress occurs when two tectonic plates slide past each other horizontally, causing displacement along a fault line. Strike-slip faults are often associated with transform plate boundaries, such as the San Andreas Fault in California.
Tensile stress is the force that pulls rock apart, causing it to break or fracture. This type of stress occurs when rocks are stretched in opposite directions, leading to the formation of cracks or faults in the rock.
Shear Stress.
extensional
Tectonic stress, caused by the movement of Earth's tectonic plates, produces the most significant crustal deformation. This stress results in the formation of features like mountains, faults, and earthquakes as the Earth's crust responds to the forces generated by tectonic plate interactions.
Strike-slip Faults
The force that produces a strike slip fault is a shearing force.
Transform Boundary
Two types of stress are compressional and tensional stress. Shear stress also plays a significant role in deformations in the Earth's crust at transform and strike slip faults.
Shear force is a load (pounds, or newtons) in plane of the object which produces shear stress ( pounds per sq inch, or Pascals). Shear force is related to shear stress as STRESS = FORCE/AREA