Sudden displacements along fault fissures can cause tremors and earthquakes.
When rocks on opposite sides of a fault move in opposite directions, it is called a strike-slip fault. When they move in the same direction, it is called a normal or reverse fault, depending on the type of stress causing the movement. The rate of movement can vary from slow creep to sudden jolts during an earthquake.
No. As a transform fault, the San Andreas Fault cannot produce volcanism.
A sudden movement along the boundary of a tectonic plate is known as an earthquake. This occurs when stress that has built up along a fault line is released, causing the rocks on either side of the fault to slip rapidly. Earthquakes can result in shaking of the ground, and potential damage and destruction to structures and properties.
Earthquake
A break or crack along which rocks move is called a fault. Sudden motion along the faults result to earthquakes.
A sudden jerk of land is called a fault. It occurs when there is a sudden release of energy along a fracture in the Earth's crust, resulting in seismic activity such as earthquakes.
A sudden movement of the Earth's crust is called an earthquake.
That's called an earthquake.
Sudden displacements along fault fissures can cause tremors and earthquakes.
It suddenly slips when the stress across it becomes too high, which produces a sudden series of shockwaves that radiate in all directions from the fault through the surrounding rock. The earthquake you feel happens when these shockwaves reach the surface.
A sharp cliff caused by sudden movements along dip-slip faults is called an earthquake. It causes the ground to shake for several seconds.
Earthquake
I'm not entirely certain, but probably about 95% sure that it's called a fault.
A Graben can produce a Normal Fault.
It is called a fault
When rocks on opposite sides of a fault move in opposite directions, it is called a strike-slip fault. When they move in the same direction, it is called a normal or reverse fault, depending on the type of stress causing the movement. The rate of movement can vary from slow creep to sudden jolts during an earthquake.