Contrast the direction of stress and displacement along normal, reverse, and strike-slip faults.
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Contrast the direction of stress and displacement along normal, reverse, and strike-slip faults.
Faulting occurs in regions where the crust is weak. The rock breaks and either one side of the suspension or both sides get displaced at such places. Based on the direction and angle of movement, faults are divided widely into four main types.
- Normal faults
- Reverse faults
- Thrust faults
- Strike-slip faults
Normal faults: These faults are forming due to the expansion in the crust. It creates an extremely precipitous fault zone that results in the part of the land on the side being pushed up compared to the amount of land thrown down on the other side.
Reverse faults: This causes due to stress created by firmness or compression. Here threw the block upraises very precipitously over the block thrown down.
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