friction
A fractured surface on the Earth's crust where a mass of rock is in motion is called a fault.
a pulling motion causes a normal fault
The type of fault that exhibits sideways motion is called a strike-slip fault. In this faulting mechanism, the movement of rocks on either side of the fault line occurs horizontally, parallel to the fault plane. An example of a strike-slip fault is the San Andreas Fault in California. These faults are typically associated with shear stress and are common at transform plate boundaries.
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Where 2 plates slide past each other in a horizontal motion that boundary is called a Transform Boundary, or a fault.
A fractured surface on the Earth's crust where a mass of rock is in motion is called a fault.
A break or crack along which rocks move is called a fault. Sudden motion along the faults result to earthquakes.
This area is called the fault line.
This area is called the fault line.
fault
a pulling motion causes a normal fault
Slip/slide fault
The type of fault that exhibits sideways motion is called a strike-slip fault. In this faulting mechanism, the movement of rocks on either side of the fault line occurs horizontally, parallel to the fault plane. An example of a strike-slip fault is the San Andreas Fault in California. These faults are typically associated with shear stress and are common at transform plate boundaries.
The place where an earthquake's slipping motion begins is called the focus or hypocenter. It is the exact point underground where the seismic energy is released.
A tectonic fault is a fracture in the Earth's crust where rocks on either side have moved relative to each other. This movement can occur horizontally (strike-slip fault), vertically (normal fault), or in a complex motion (thrust fault). Faults are a primary source of earthquakes.
The answer is by convergent plate motion.
It is called a fault