#31

strike slips faults are most likely to occur along which type of plate boundary?
a. convergent
b. transform
c. transcontinental
d. divergent

To determine the answer to this question, we need to understand the different types of plate boundaries and the characteristics of strike-slip faults.

Strike-slip faults occur when two blocks of rock on either side of a fault line move horizontally relative to each other. There are three types of plate boundaries: convergent boundaries, divergent boundaries, and transform boundaries.

Convergent boundaries occur when two plates move towards each other. In this type of boundary, one plate is usually forced beneath the other in a process called subduction. Strike-slip faults are less likely to occur along convergent boundaries, as the movement is primarily vertical rather than horizontal.

Divergent boundaries occur when two plates move away from each other. These boundaries are characterized by the formation of new crust as magma rises to fill the gap between the separating plates. Strike-slip faults are also less likely to occur along divergent boundaries, as the movement is primarily parallel to the boundary rather than horizontal.

Transform boundaries occur when two plates slide past each other horizontally. This type of boundary is characterized by strike-slip faults, as the plates are moving in opposite directions along the boundary. Typically, the movement is remarkably horizontal along the fault line.

Based on the above information, the most likely type of plate boundary for strike-slip faults to occur along is b. transform boundaries.