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.
There are three types of fault lines in the crust. There are divergent boundaries, convergent boundaries, and transform boundaries.
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.
Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.
Strike-slips are common at transform boundaries because of Shear stress which pushes different parts of rock in different directions.
The majority of faults occur in the plate boundaries.
The majority of faults occur in the plate boundaries.
They are common at transform boundaries because strike-slip faults move up and down like transform 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
Most present-day faults occur along boundaries. The three types of geologic boundaries are transform boundaries, divergent boundaries and convergent boundaries.