Fault The Hanging Wall Moves Downward Relative To The Footwall

When the hanging wall moves down in relative to the footwall it is called a fault. In dip slip faults if the hanging wall block moves downward relative to the footwall read more. Strike slip faults are right lateral or left lateral depending on whether the block on the opposite side of the fault from an observer has moved to the right or left.

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Normal Fault Geology Geology Teaching Geology Lessons Earth Science

In A Normal Fault The Blocks Are Being Pulled Apart So One Block Slides Down The Other Caption From Link Geophysics Earth Science Plate Tectonics

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Fault Types

When the hanging wall moves up in relative to the footwall it is called a fault.

Fault the hanging wall moves downward relative to the footwall.

The hanging wall moves down relative to the foot wall. In a normal fault the hanging wall moves downward relative to the footwall. Special type of reverse fault that is nearly horizontal angle has less than 45 degrees strike slip fault. The hanging wall moves up relative to the foot wall.

Formed by compressional stress rocks are pushed towards each other thrust fault. There is a normal fault which happens at a divergent boundary. A downthrown block between two normal faults dipping towards each other is a graben. There is a normal fault which happens at a divergent boundary.

An upthrown block between two normal faults dipping away from each other is a horst. In this fault the hanging wall moves down relative to the footwall. In this fault the hanging wall moves down relative to the footwall. These usually occur when tectonic forces cause tension that pulls rocks apart.

It is caused by tension. Low angle normal faults with regional tectonic significance may be designated detachment faults. It is caused by tension. To the dip is called dip slip faulting.