Wiki User
∙ 14y agoDescribe the three types of plate motion and the faults that are characteristic of each type of motion.
Wiki User
∙ 14y agoconvergent plates produce thrust faults divergent plates form normal faults transform plates form strike/slip faults
One of the three types of plates are the transform plates slip past each other. The convergent plates push together. The divergent plates pull away from each other.
it is dishfunctional
the movement of convection currents in the mantle is the cause of plate motion.
A treadle is a foot operated plate, which when pressed, causes a rotary movement for a machine.The plate is connected, usually via a rod, to a crank. Pushing on the treadle in a careful, repeated manner, will move the crank and cause rotary motion in the machine.
convergent plates produce thrust faults divergent plates form normal faults transform plates form strike/slip faults
One of the three types of plates are the transform plates slip past each other. The convergent plates push together. The divergent plates pull away from each other.
The three types of plate boundaries are divergent, convergent, and transform boundaries. Divergent boundaries have normal faults, convergent boundaries have thrust faults, and transform boundaries have strike-slip faults.
One of the three types of plates are the transform plates slip past each other. The convergent plates push together. The divergent plates pull away from each other.
The majority of faults occur in the plate boundaries.
The majority of faults occur in the plate boundaries.
Reverse faults are created by compressional stress, where the rocks are pushed together, causing the hanging wall to move up relative to the footwall. This type of faulting is common in areas undergoing compression, such as at convergent plate boundaries or mountain-building regions.
No. Many faults, especially minor ones, are located far from plate boundaries.
A normal fault is a type of fault where the hanging wall moves downward relative to the footwall. They are typically associated with extensional tectonic forces, where the crust is being pulled apart. Normal faults are common at divergent plate boundaries, such as mid-ocean ridges. These faults often create valleys or rift valleys as the crust stretches and thins. They have a characteristic "step-like" pattern due to repeated faulting events. Earthquakes associated with normal faults tend to have vertical motion and are classified as dip-slip earthquakes.
Strike-slip faults are typically found at transform plate boundaries, where two tectonic plates slide past each other horizontally. This movement is characterized by parallel fault lines with little vertical motion.
False. Earthquakes mostly occur along faults that are at or very near to plate boundaries.
Faults occur because the forces of plate motion push or pull the crust so much that the crust breaks.