A fault zone is created when directed stress (as opposed to isotropic stress that simply compacts materials) overcomes the physical strength of the rock to withstand pressure leading to a pervasive crack.
If the stress that created the fault is pulling the rock apart, the block that lies above the fault (the hanging wall) is bound to sink and the rocks below the fault will move upwards relative to the hanging wall. This situation is termed a "normal fault" and occurs for example in rift zones all over the world.
If confining pressure produces a fault, the hanging wall is pushed on top of the rocks below the fault. This is known as a "reverse fault" and is a common phenomenon in many mountain ranges.
In a special type of stress regime, faults are created along which rocks are sliding past each other horizontally. They are called "transform faults".
Strike slip fault
This is known as a fault.
This is called a fault.== ==
A fault line, or plate boundary.
strike slip fault
A fault fault fault fault
Strike Slip Fault
Rocks on either side of a fault move along the surface of the fault.
Strike Slip Fault
Transform fault
Strike Slip Fault
This kind of fault is called a normal fault and is usually a sign of crustal extension.
A fault.
No
Strike Slip Fault.
well, a fault pretty much does break or crack along wich rocks move.
Strike slip fault