Trasform(plates sliding past each other.)
Converging(plates colliding.)
Divergent(plates moving away.)
These are 3 different types of plate boundries
The majority of faults occur in the plate boundaries.
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
The majority of faults occur in the plate boundaries.
No, faults are not the same as plate boundaries, though they are related. Faults are fractures in the Earth's crust where rocks have moved past each other, while plate boundaries are the edges where tectonic plates interact. Plate boundaries can give rise to faults due to the stress and movement of the plates, but not all faults are located at plate boundaries. Faults can also occur within tectonic plates away from these boundaries.
Yes, but not as often as earthquakes happen near plate boundaries
Earthquakes infrequently occur away from plate boundaries. Most earthquakes occur at plate boundaries because of the stress caused by the interacting plates.
yes
a. Transform:transform boundaries or motion creates strike-slip faults.b. Convergent:convergent boundaries or motion creates reverse faults.c. Divergent:divergent motion creates a normal fault.
No. Many faults, especially minor ones, are located far from plate boundaries.
The three types of faults are normal, reverse, 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.
Faults occur near plate boundaries because the earth is weaker there... The magma under the Earth's crust makes the plates move very slowly and sometimes two plates can crash into each other causing the ground to shake.
Normal faults occur when the hanging wall moves down relative to the footwall due to extensional forces, while reverse faults occur when the hanging wall moves up relative to the footwall due to compressional forces. Normal faults are associated with divergent plate boundaries, while reverse faults are associated with convergent plate boundaries.