GEOLOGY

Detailed explanation-1: -Plates can move past each other in the same plane at a boundary. This type of boundary is called a transform boundary . This type of boundary is dominated by strike-slip faulting, although other types of faulting may be observed. Where two plates slide past each other, earthquakes originate at shallow depths.

Detailed explanation-2: -Transform faults are found where plates slide past one another. An example of a transform-fault plate boundary is the San Andreas fault, along the coast of California and northwestern Mexico. Earthquakes at transform faults tend to occur at shallow depths and form fairly straight linear patterns.

Detailed explanation-3: -The third type of plate boundary occurs where tectonic plates slide horizontally past each other. This is known as a transform plate boundary. As the plates rub against each other, huge stresses can cause portions of the rock to break, resulting in earthquakes.

Detailed explanation-4: -A transform fault is a plate boundary along which the relative motion between the two plates is parallel to the strike of the fault and is geometrically the arc of a small circle about the pole of rotation between two plates.

Detailed explanation-5: -Shallow, low-magnitude earthquakes commonly occur at divergent plate boundaries. Earthquakes at divergent plate boundaries are distributed with predictable locations and depths. Earthquakes at divergent plate boundaries occur as new crust is created and other crust is pushed apart.