1.) reverse fault A.) Compression forces a fault block upward. along a reverse fault at a transform boundary at a divergent boundary 2 See answers Answer 5.0 /5 1. sylvain96 +1 diavinad8 and 1 other learned from this answer ... Shearing often occur at a transform boundary. The difference between a reverse fault and a thrust fault is that a reverse fault has a steeper dip, more than 30°. In a strike-slip fault, the blocks of rock move in opposite horizontal directions.These faults form when crust pieces slide along each other at a transform plate boundary.

usually occurs at a transform boundary in the presence of high levels of friction. The major faults found in convergent plate boundaries are usually reverse or thrust faults, including a master thrust fault at the boundary between the two plates and typically several more major thrust faults running roughly parallel to the plate boundary.
B.) Match the types of faults with their descriptions. Let's look at faults: you have a block of material on one side and another block on the other side. Reverse faults are the result of compression (forces that push rocks together). Over time, this fault has caused the Mississippi River to run a different course. Really, it's scale. A thrust fault is a special kind of reverse fault where one or more plates are under the ocean. Reverse (thrust) faults are common in areas of compression. For example, reverse thrusts exist in areas with subducting plates such as along the coast of Japan. strike-slip fault 2.) At a thrust fault, a plate below the sea is moving under another plate, thrusting its edge upward.

Reverse faults are dip-slip faults in which the hanging wall moves up relative to the footwall. For example, the New Madrid Fault is a massive fracture in Missouri. A transform boundary is a place where two of the tectonic plates slide sideways past each other. Reverse and thrust faults form in sections of the crust that are undergoing compression. A reverse fault is usually associated with plates that are colliding. generally forms near a convergent boundary, where two plates collide. C.) often forms at a divergent boundary, where the crust stretches. The Sierra Madre fault zone of southern California is an example of reverse-fault movement. normal fault 3.) This type of fault happens in areas where the rocks are pushed together so that the rocky crust of an area must take up less space: Reverse fault This type of fault happens in areas where the rocks are being pushed in opposite directions: A convergent plate boundary is a zone of major reverse and thrust faults. Convergent plate boundaries are dominated by compression. The fault plane in a reverse fault is also nearly vertical, but the hanging wall pushes up, and the footwall pushes down.

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