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Q: What is the movement along slide slip faults?
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What is a fault with horizontal movement called?

Horizontal faults can be refered to as lateral faults or strike-slip faults.


What does normal faulting mean?

Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.


How do strike slip faults?

strike-slip faults move along each other from shearing


What type of fault has side to side movement?

Strike-slip (transcurrent) faults. Oblique faults exhibit some strike-slip movement, but they also have a dip-slip component.


What does faults mean?

Normal faults are when you have hanging walls that slide down relative to and below the footwall. Dip-slip faults are normal faults.


Faults undergoing movement that is horizontal and parallel to the strike of the fault surface are called?

Faults which appear to have displaced rock strata horizontally are called strike slip faults. The two blocks that have been displaced move in opposite directions along the fault line.


How does the movement along a strike-slip fault cause the one slide to go up?

shearing made the rock slip past each other


What type of plate motion causes a strike slip fault?

Also called transform faults, strike-slip faults involve a movement that is horizontal with a block of rock on one side of the fault moving in one direction, the other block of rock moving in the other direction. --> <--


What is the definition for a strike slip fault?

Dip-slip faults is the term used for any fault that has movement in the vertical direction. One side moves up where as the other side moves down. Examples are Normal Fault and Reverse fault.


Strike slip plate explain?

Strike-slip faults indicate rocks are sliding past each other horizontally, with little to no vertical movement. Both the San Andreas and Anatolian Faults are strike-slip.


What are the different types of faults?

The 4 main types of fault are summarised below:Dip-slip faultsStrike-slip / transcurrent faultsOblique-slip faultsListric faultDip slip faults are those where the relative motion on the fault is broadly vertical. Examples include normal faults where the hanging wall moves down relative to the foot wall. Reverse faults have the opposite sense of motion, with the hangingwall moving up relative to the footwall. Thrust faults are a special type of reverse fault where the dip of the fault plane is at a shallower angle than 45 degrees from the horizontal.Strike slip or transcurrent faults are those where the relative motion on the fault is broadly horizontal. The fault plane in these types of faults is normally near vertical and the sense of motion is described in terms of the relative movement of the rockmass on the far side of the fault plane. If this relative movement is to the left, then it is known as a sinistral fault. If he motion is to the right it is a dextral fault.Oblique slip faults are those have have a significant component of both vertical and horizontal movement. They can be thought of a composite of the dip slip and strike slip faults.Listric faults are characterised by a curved fault plane surface. They usually start of relatively steep and then become more shallow with increased depth and may ultimately become horizontal.Previous Answer:The four different types of faults are normal, reverse, transcurrent (also known as strike-slip), and thrust. Normal faults are so named because movement follows what would be expected from normal effects of gravity--one plate slides downward, pulled by gravity, and the other plate forms a cliff face. The reverse fault, then, is the opposite of a normal fault--one plate moves against gravity and slides over the other. Transcurrent faults feature horizontal movement rather than up/down movement; plates slide along each other, resulting in offset roads and such. Finally, thrust faults are similar to reverse faults--one plate moves over the other--but the angles of movement for thrust faults are generally less steep, and thrust faults are more commonly associated with geographical features such as mountain ranges.


A sharp cliff caused by sudden movements along dip-slip faults is called a .?

A sharp cliff caused by sudden movements along dip-slip faults is called an earthquake. It causes the ground to shake for several seconds.