Fault line between the plates
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.
The movement of the Hanging wall in the normal fault downward with the gravity whereas in the Reverse fault the hanging wall moved upward against the gravity
they can shake in reverse fault, normal fault, strike-slip fault.
Earthquake/volcanic activity occur almost exactly the fault line where plates about
Along fault lines.
Normal Fault
normal and rivesre fault, thrust fault, dip-strike fault.
Earthquakes occur along a fault. Near the San Andreas fault lots of earthquakes occur.
No, the San Andreas Fault is a strike-slip fault, not a normal fault.
That the hanging wall is moved downward. They occur were two blocks of rock pull apart, by tension.
parallel normal faults.
A normal fault.
it is a normal fault.
At a divergent boundary, faults known as normal faults occur. These faults form as tectonic plates move away from each other, leading to the stretching and thinning of the Earth's crust. This results in the upper plate sliding down along the fault plane relative to the lower plate.
In a normal fault, the fault is at an angle, so one block of rock lies above the fault while the other lies below it. The rock above it is the hanging wall and the rock below it is the footwall. In a normal fault, the hanging wall moves downwards relative to the footwall.
Where two plates move away from each other tension forces create many normal faults.
a pulling motion causes a normal fault