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".
This is known as a fault.
Strike slip fault
This is called a fault.== ==
Yes, that is correct. In a Strike Slip fault, the rocks on either side of the fault move horizontally past each other in a predominantly lateral motion. This is in contrast to other types of faults where rocks move vertically or at different angles in relation to each other.
A fault line, or plate boundary.
When rocks break, they move along the surface in a process known as faulting. This movement can occur due to tectonic forces, causing the rocks to break and move along fractures known as faults.
Strike Slip Fault
Rocks on either side of a fault move along the surface of the fault.
This is known as a fault.
Strike Slip Fault
Strike Slip Fault
Transform fault
This kind of fault is called a normal fault and is usually a sign of crustal extension.
No
A fault.
Strike Slip Fault.
well, a fault pretty much does break or crack along wich rocks move.