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In a strike-slip fault the rocks on either side of the fault slip past each other sideways.?
=Yes!=
In a strike-slip fault the rocks on either side of the fault slip past each other sideways with the little?
up or down motion
What fault has little or no vertical movements?
A fault with little or no vertical movement is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past each other, usually in a side-to-side motion. This movement can cause earthquakes when the stress along the fault overcomes friction and the rocks suddenly slip.
What type of rock occurs on either side of a fault that move sideways past each other?
Rocks that occur on either side of a fault that move sideways past each other are typically classified as transform fault rocks. These rocks experience shearing forces as they slide horizontally past each other, leading to observable features like fault gouge and striations.
In a strike slip fault the rocks on either side of the slip past each other with little?
Strike-slip faults have little vertical motion.
What is the name of the fault where the rocks on either side move past each other during an earthquake?
strike slip fault---------------------------------------------------------------------------------------------------------------- BITCHOSAURUS REX
What type of fault rocks on either side of the fault surface moves past each other?
strike-slip
In a strike-slip fault the rocks on either side of the fault slip past each other sideways.?
=Yes!=
What fault causes rocks to become twisted and strained when they snag each other?
The fault type that causes rocks to become twisted and strained when they snag each other is a strike-slip fault. In a strike-slip fault, rocks on either side of the fault move horizontally past each other, leading to twisting and straining along the fault zone. This type of movement is typical in transform plate boundaries such as the San Andreas Fault in California.
When the rock on either side of a move in different direction what is that?
When rocks on either side of a fault move in different directions, it is known as a strike-slip fault. This type of fault occurs when the rocks slide past each other horizontally. Examples of strike-slip faults include the San Andreas Fault in California.
In a strike-slip fault the rocks on either side of the fault slip past each other sideways with the little?
up or down motion
What fault has little or no vertical movements?
A fault with little or no vertical movement is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past each other, usually in a side-to-side motion. This movement can cause earthquakes when the stress along the fault overcomes friction and the rocks suddenly slip.
A fault has a shearing force.?
strike-slip
What type of rock occurs on either side of a fault that move sideways past each other?
Rocks that occur on either side of a fault that move sideways past each other are typically classified as transform fault rocks. These rocks experience shearing forces as they slide horizontally past each other, leading to observable features like fault gouge and striations.
What is a fault with horizontal movement called?
A fault with horizontal movement is called a strike-slip fault. This type of fault occurs when the rocks on either side of the fault move horizontally past each other. Examples of strike-slip faults include the San Andreas Fault in California.
What is it called when the rocks on either side slips past each other sideways with little up and down motion at a?
This type of movement is known as strike-slip faulting, where rocks on either side of the fault move horizontally past each other with little vertical displacement. This typically occurs along transform plate boundaries where two tectonic plates slide horizontally against each other. An example of a strike-slip fault is the San Andreas Fault in California.
In a strike slip fault the rocks on either side of the slip past each other with little?
Strike-slip faults have little vertical motion.
