![]() In transform or strike-slip faults, one block moves laterally relative to the other block – it does not matter which one is the hanging wall or footwall. Thrust Fault.ģD interactive model of Figure 16: Transform or Strike-slip Faults Reverse Fault.Ī reverse fault that has a shallowly dipping fault plane (perhaps less than about 45 degrees) is called a thrust fault (Figure 16). In map view, the hanging wall rocks will be older than the footwall rocks, due to erosion of the uplifted side ( Figure 15). This motion can be determined by tracing the offset of the beds in a vertical motion in a block diagram. In reverse faults, the hanging wall moves upwards relative to the footwall. ![]() Normal Fault.ģD interactive model of Figure 14: Reverse Faults In map view, the hanging wall rocks will be younger than the footwall rocks, due to erosion of the uplifted side. In normal faults, the hanging wall moves downward relative to the footwall ( Figure 13 and Figure 14). There are three main types of faults: normal faults, reverse faults, and transform or strike-slip faults. A good way to remember this is to imagine a mine tunnel running along a fault the hanging wall would be where a miner would hang a lantern and the footwall would be at the miner’s feet.įigure 13 (Click on link): Hanging wall, footwall, and scarp of a normal fault. In a dip-slip system, the footwallis below the fault plane and the hanging wall is above the fault plane. Dip-slip motion consists of relative up-and-down movement along a dipping fault between two blocks, the hanging wall and footwall. Normal and reverse faults display vertical, also known as dip-slip, motion. If it is visible at the surface, it is called a fault scarp (Figure 13). The plane along which motion occurs is called the fault plane. ![]() Faults are the places in the crust where brittle deformation occurs as two blocks of rocks move relative to one another.
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