divergent-pullling apart
convergent-pushing together
transform-sliding past 1 another
Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
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.
Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.
Plate boundaries experience different types of forces, such as compression, tension, and shear, which can cause faults to form. In compression zones, faults like reverse and thrust faults can develop due to the plates being pushed together. In tension zones, normal faults form as plates are pulled apart. Shear forces along transform boundaries can create strike-slip faults.
The majority of faults occur in the plate boundaries.
The majority of faults occur in the 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.
No. Many faults, especially minor ones, are located far from plate boundaries.
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
Because most plates boundaries are also faults
The three main types of fault lines are normal faults, reverse faults, and strike-slip faults. Normal faults occur when rocks are pulled apart, reverse faults form when rocks are pushed together, and strike-slip faults happen when rocks slide past each other horizontally.