The three faults are.... 1. Normal 2. Reverse 3. Strike-slip
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
-Normal Faults form when the hanging wall moves down. -Reverse Faults form when the hanging wall moves up. -Strike-Slip Faults have walls that moce sideways, instead of up or down.
A three-phase symmetrical fault exists when all three line conductors are short-circuited, sometimes to earth (ground). An unsymmetrical fault occurs when only one or two of the three lines are involved.
Convergence, divergence and strike slip.
There are strike- slip faults, normal faults, and reverse faults. A strike slip fault is where the ground moves past each other. A normal fault is where the plates move pull apart and the plates move up and down. A revers fault is where the plates push into each other and move up and down.
No. Your terminology is close but not quite right. The three main types of faults are normal faults, reverse faults, and strike-slip faults. Strike-slip faults may also be called transform faults.
The three types of faults are Normal faults, Reverse faults, and Strike and Slip fault
Faults are surfaces along the earths crust in which rocks have been fractured and displaced. There are three types of faults: strike-slip, normal and reverse.
three kinds of faults are normal fault, reverse fault, and strike-slip fault.
There are three types of fault lines in the crust. There are divergent boundaries, convergent boundaries, and transform boundaries.
refuse
the three types of faults are normal (colliding), reverse (moving apart), strike-slip (sliding past each other)
convergent plates produce thrust faults divergent plates form normal faults transform plates form strike/slip faults
Describe the three types of plate motion and the faults that are characteristic of each type of motion.
faults, dips and domes
Normal, Reverse, Wrench
They map faults, detect changes along faults, and develop a method of predicting earthquakes