The Hanging Wall Has Moved Downward Relative To The Footwall
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Reverse in a fault the hanging wall block move up with respect to the footwall block.
The hanging wall has moved downward relative to the footwall. In a normal fault the hanging wall moves downward relative to the footwall. Two parallel normal faults form. A scientist observes a fault where the hanging wall has moved upward relative to the footwall. In a normal fault the hanging wall moves downward relative to the footwall.
An upthrown block between two normal faults dipping away from each other is a horst. Tension is stress that pulls rocks apart. A fault has little or no vertical movements of the two blocks. Along a normal fault the hanging wall moves down relative to the footwall.
A downthrown block between two normal faults dipping towards each other is a graben. Forces in earth s crust. The hanging wall moves down relative to the foot wall. Formed by tensional stress rocks are stretched away from each other.
The hanging wall on the left slides down relative to the footwall. The hanging wall on the right slides down relative to the footwall. Which type of fault is the scientist observing. Low angle normal faults with regional tectonic significance may be designated detachment faults.
The hanging wall on the right slides down relative to the footwall.
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