Question

1) Identify the three types of faults and discuss the sense of motion that occurs on each. Also, indicate which type of plate boundary each is commonly associated with and provide a real world example location where each occurs (e.g. eastern North America).

Answer 1

The three types of faults are normal faults, reverse faults, 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.

Step-by-step explanation:

The three types of faults are normal faults, reverse faults, and strike-slip faults. In a normal fault, the hanging wall moves downward relative to the footwall. This type of fault is commonly associated with divergent plate boundaries, where plates are moving apart, such as the Mid-Atlantic Ridge. A real-world example location is the Great Rift Valley in East Africa.

In a reverse fault, the hanging wall moves upward relative to the footwall. This type of fault is commonly associated with convergent plate boundaries, where plates are moving toward each other, such as the Himalayas. A real-world example location is the San Andreas Fault in California.

In a strike-slip fault, the two plates slide past each other horizontally. This type of fault is commonly associated with transform plate boundaries, where plates are moving horizontally past each other, such as the San Andreas Fault in California. Another real-world example location is the Anatolian Fault in Turkey.