THRUST
A normal fault
strike-slip fault
Stike slip fault
strike-slip
Shearing
THRUST
Friction This movement is also known as Transform plat boundary Movement
The movement of earth's crust along a fault is called a transform fault. At a transform fault, the plates slide past each other and crust is neither destroyed nor created. If there geological structures don't "slip" easily, energy can build up as the plates try to slide past each other. Eventually the "stuck" parts of the fault will fail and the energy stored there will be released quickly in a seismic event. An earthquake can result.
The fault locks, and stress builds up until an earthquake occurs.
Astrike-slip fault it when the hanging wall and the footwall slide past each other.
Transform fault/boundary. Its when two plates slide past each other.
an earthquake
A lateral fault is when Shearing causes rock blocks to slide horizontally past each other.
transform fault
Slip/slide fault
When rocks move in to each other. When two plates are constantly hitting each other, they form a convergent boundary, which forms a reverse fault. The Compression between these plates (or push) makes one slide above the other. If this happens continuously, one will be above the other, resting on it. This creates a hanging and foot wall.
At these boundaries, the rocks grind and slide against each other, causing earthquakes.
Earthquakes with "Faults" or "Fault Lines"
sounds like, if the rocks are plates, an earthquake... assuming this "crack" is a fault?? does this help?
Friction This movement is also known as Transform plat boundary Movement
Friction This movement is also known as Transform plat boundary Movement
one has rocks and the other doesnt
In geology, shearing occurs when rocks slide past each other horizontally in opposite directions. The kind of fault created by shearing is called a strike-slip fault.