GEOLOGY

Detailed explanation-1: -In terms of faulting, compressive stress produces reverse faults, tensional stress produces normal faults, and shear stress produces transform faults .

Detailed explanation-2: -A transform fault will form between tectonic plates where each plate moves away from the divergent plate boundary. The earthquakes that occur at boundaries cause stress through the crust of the Earth; rocks at the surface will break in response to the stress-forming faults.

Detailed explanation-3: -Figure 10.6: Faults can form in response to any one of the three types of forces: compression, tension and shear: The type of fault produced, however, depends on the type of force exerted.

Detailed explanation-4: -Faults which move horizontally are known as strike-slip faults and are classified as either right-lateral or left-lateral. Faults which show both dip-slip and strike-slip motion are known as oblique-slip faults.

Detailed explanation-5: -A strike-slip fault is formed by shear stress, which occurs whenever two blocks of rock slide past one another. The hanging wall does not lie above or below the footwall at a strike-slip fault. These types of faults occur along boundaries known as transform boundaries.