Final answer:
Normal faulting is associated with divergent boundaries, where tectonic plates move apart and new crust is formed. These faults occur due to extensional forces that pull the crust apart, unlike at convergent or transform boundaries where different types of faults are found.
"The correct option is approximately option b"
Step-by-step explanation:
The tectonic setting where you would typically see normal faulting is at a divergent boundary. In geological terms, a normal fault occurs when the crust is extended and broken, resulting in one block of crust dropping down relative to the other block.
This type of faulting is most common at divergent boundaries, also known as rift zones, where tectonic plates are moving away from each other, leading to the formation of new crust. Examples of divergent boundaries include the Mid-Atlantic Ridge and the East African Rift Valley.
Conversely, at convergent boundaries and subduction zones, which are areas where one tectonic plate is being pushed under another, you often find reverse or thrust faults due to the compressional forces.
Transform boundaries, such as the San Andreas Fault in California, are characterized by strike-slip faulting where plates slide past one another horizontally.