extensional
Shear Stress.
Normal faults are associated with divergent plate boundaries, where two tectonic plates are moving away from each other. This type of boundary results in tensional stress that leads to the hanging wall moving down relative to the footwall, creating a normal fault.
The three types of faults are normal, reverse, and strike-slip faults. Normal faults are associated with divergent plate boundaries, reverse faults with convergent plate boundaries, and strike-slip faults with transform plate boundaries.
compression
Reverse and thrust faults are both under compressive stress.
When shear stress exceeds the shear strength of a material, it can cause the material to deform or fracture. This type of fault is often associated with strike-slip earthquakes, where two tectonic plates slide past each other horizontally. The most famous example of this type of fault is the San Andreas Fault in California.
compression
Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.
Faults form due to the movement of tectonic plates, which causes stress and deformation in the Earth's crust. When this stress exceeds the strength of the rocks, they fracture along pre-existing zones of weakness, creating faults. These faults can be normal, reverse, or strike-slip depending on the type of stress exerted during the movement.
Normal faults have a hanging wall and footwall Normal Faults are common at mid-ocean ridges Normal Faults occur where the crust is being pulled apart at the divergent plate boudary. Sorry i only have 3 facts, but I anyone with the question
Strike-slip Faults
Answer: Compressional stress.