The type of force found in a strike slip fault is lateral force.
The bending and buckling of rocks under great force produces a fold.
Higher frictional resistance along a fault can inhibit the fault from slipping smoothly, causing stress to accumulate over time. When this stress is eventually released as an earthquake, the force released can be higher if the resistance was greater. Conversely, lower frictional resistance can allow the fault to slip more easily, potentially leading to a lower force released during an earthquake.
Tensional stress from divergent plate boundaries causes a normal fault to form. This stress pulls rocks apart along a fault line, causing the hanging wall to drop relative to the footwall.
Strike-slip faults are caused by horizontal shear stress along the fault plane, which results in horizontal movement of the rocks on either side of the fault. The movement can be either left-lateral (sinistral) or right-lateral (dextral), depending on the direction of the shear stress.
The force that causes rocks on either side of a fault to slide past each other is the built-up stress along the fault line, which is released as the two sides move in opposite directions. This stress can accumulate due to tectonic plate movements, leading to the sudden release of energy in the form of an earthquake.
shearing
The force that produces a strike slip fault is a shearing force.
compression
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
A Force applied to an object will cause a displacement. Strain is effectively a measure of this displacement (change in length divided by original length). Stress is the Force applied divided by the area it is applied to. (eg. pounds per square inch) So, to answer the question, it is the applied Force that produces both stress and strain. Stress and strain are linked together by various material properties such as Poisson's ratio and Young's Modulus.
The bending and buckling of rocks under great force produces a fold.
There is NO SUCH THING as "strain energy"Strain is the response of a system to an applied stress. When a material is loaded with a force, it produces a stress, which then causes a material to deform. Engineering strain is defined as the amount of deformation in the direction of the applied force divided by the initial length of the material.Thus the energy is the FORCE - the stress.The stresses present in a fault system are caused by the convection currents in Earth's mantle (driven by the heat in Earth's core). Once the stress builds up to a point that exceeds the strength of the rocks comprising the fault system, the rock fractures and moves and this is the strain.
Higher frictional resistance along a fault can inhibit the fault from slipping smoothly, causing stress to accumulate over time. When this stress is eventually released as an earthquake, the force released can be higher if the resistance was greater. Conversely, lower frictional resistance can allow the fault to slip more easily, potentially leading to a lower force released during an earthquake.
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
Tensional stress from divergent plate boundaries causes a normal fault to form. This stress pulls rocks apart along a fault line, causing the hanging wall to drop relative to the footwall.
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
The San Andreas Fault is a transform fault where tectonic plates slide past each other horizontally. The force at the fault is primarily due to the movement of the North American Plate and the Pacific Plate, causing stress to build up until it is released in the form of earthquakes.