A high-angle fault under compression
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A thrust fault forms when compression forces in the Earth's crust cause one block of rock to move up and over another block of rock at a low angle. This results in older rock layers being pushed on top of younger rock layers. Thrust faults are common in areas where tectonic plates are colliding.
Thrust faults are faults which "thrust" older rocks above and/or over younger rocks. They are often steep having a angle greater than 30 degrees from horizontal. There are a variety of types which are easy to research on Wikipedia, Geology.com or USGS.com, the United States Geologic Sureveys web site which has a vast wealth of information.
the movement along the thrust fault is the foot wall goes down and the hanging wall goes up. its also called a reverse fault because a normal fault has the foot wall going up and the hanging wall going down
Reverse
This is called a reverse or thrust fault.
The movement of the crust along a thrust fault is usually a reverse movement unlike the movement along a normal fault.
False
A fault that occurs on folded rock layers is likely to be a thrust fault, where one block of rock is pushed up and over the other. This type of fault is common in areas where horizontal compression forces have folded the rock layers.