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The formal investigation by each side prior to trial is called .
Strike-Slip Fault
A type of fault where two blocks of the Earth's crust slide past one another horizontally, with little to no vertical movement.
Normal Fault
A type of fault where the hanging wall has moved downward relative to the footwall due to tensional forces.
Horizontal Compression
The force that acts in parallel opposition across the Earth's crust, leading to folding, faulting, or shortening of geological formations.
Horizontal Tension
Refers to the stress acting parallel to the Earth's surface, which can cause stretching and fracturing of geological structures.
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