Convergent plate margins
Explanation:
Reverse faults are usually found at convergent plate margins. In a convergent plate margin, compressive forces which squeezes rocks together are at work here. In this margin, plates are in head on collision.
- A reverse fault is a fault type in which the hanging wall moves up relative to the footwall moving downward.
- Here shortening of the earth occurs as the two blocks moves.
This can only be possible when there is compression. Two forces are directed towards each other.
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Good alternatives include dot density maps, graduated/proportional symbol maps, and cartograms
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