Wiki User
∙ 7y agoThe wave is a Tsunami
Wiki User
∙ 7y agoSudden 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.
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.
Faults are breaks in the crust where the crust has moved. The types of dip-slip faults are normal and reverse faults. In both of these, the movement is along the slope of the fault. Sudden movements along these faults can produce fault scarps. Layers of rock being misaligned is evidence of fault movement. Fault creep is caused by slow movement along the fault.In a normal fault, the plates are moving away from each other. This is due to tension. When the fault moves, the footwall rises relative to the hanging wall. Normal faults occur at divergent boundaries, such as ocean ridges. Normal faults can produce fault-block mountains.In a reverse fault, the plates are moving towards each other. This is due to compression. Here, the footwall falls relative to the hanging wall. A thrust fault is a special type of reverse fault, where the angle is shallow. Reverse faults occur at convergent boundaries, like subduction zones.A strike-slip fault is where the two plates move horizontally past each other. The force between them is called shearing. This type of fault is often called a transform fault, because they occur at transform boundaries.