How To Tell Difference Between Hanging Wall And Footwall

An arcuate cliff called the headwall.

How to tell difference between hanging wall and footwall.

As nouns the difference between hangingwall and footwall is that hangingwall is while footwall is geology the section of rock that extends below a diagonal fault line the corresponding upper section being the hanging wall. In a non vertical fault where the fault plane dips the footwall is the section of the fault that lies under the fault while the hanging wall lies over the fault the names come about from the. That is the slip occurs along the strike not up or down the dip. In a fault plane that dips 45 degrees the overlying rock unit is the hanging wall and the underlying rock unit is the footwall.

In these faults the fault plane is usually vertical so there is no hanging wall or footwall. In normal faulting the hanging wall moves downwards in relation to the footwall. Difference between hanging wall and footwall. An upthrown block between two normal faults dipping away from each other is a horst.

In a non vertical fault where the fault plane dips the footwall is the section of the fault that lies under the fault while the hanging wall lies. A downthrown block between two normal faults dipping towards each other is a graben. Strike slip faults have walls that move sideways not up or down. Draw a normal and reverse fault label the hanging wall and footwall for each also show how they move for each fault.

In reverse thrust faulting the hanging wall moves upward in relation to the footwall. In an ideal cirque the headwall is semicircular in plan view. 48 the footwall exhibits a general trend of higher porosity and lower resistivity compared to the hanging wall and the clear contrast between the hanging wall and footwall may account for the difference in maximum burial accumulation of strain and structural variation across the thrust. This situation however is generally found only in cirques cut into flat plateaus.

Other articles where hanging wall is discussed. Low angle normal faults with regional tectonic significance may be designated detachment faults. In a normal fault the hanging wall moves downward relative to the footwall.