A normal fault is in a zone of tensional faulting rocks in the.
In a reverse fault where does the hanging wall move relative to the footwall.
Mike dunning dorling kindersle getty images reverse faults form when the hanging wall moves up.
True the oldest sedimentary rock strata are exposed along the axial parts of deeply eroded anticlines.
In a normal fault the hanging wall of the fault moves down relative to the foot wall.
In a reverse fault the hanging wall right slides over the footwall left due to compressional forces.
Another type of fault is the thrust fault where ground on one side of the fault moves up and over adjacent ground.
A normal fault is in a zone of tensional faulting rocks in the.
Alternatively such a fault can be called an extensional fault.
In a reverse fault the hanging wall moves upward relative to the foot wall.
In a normal fault the hanging wall of the fault moves down relative to the foot wall.
In a reverse fault the hanging wall moves upward relative to the foot wall.
A reverse fault is in a zone of compressional faulting rocks in the hanging wall are pushed up relative to rocks in the footwall.
A reverse fault is in a zone of compressional faulting rocks in the hanging wall are pushed up relative to rocks in the footwall.
What types of faults would you.
The hanging wall moves downward relative to the footwall.