Tectonic plates float on the magma of the Earth's mantle, and move because of convection currents in the magma.
Normal faults occur at divergent boundaries, where tectonic plates are moving apart. This type of fault results from tensional stress pulling the plates in opposite directions, causing the hanging wall to move downward relative to the footwall.
In a normal fault, the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of fault is associated with divergent plate boundaries or areas where the Earth's crust is being pulled apart.
A normal fault causes land to move downward due to tensional forces pulling the Earth's crust apart. This type of fault is commonly associated with divergent plate boundaries where tectonic plates are moving away from each other.
When two plates move past each other, a transform fault boundary is formed. This boundary is characterized by horizontal motion, and the friction between the plates causes earthquakes along the fault line.
A rift valley is formed by a divergent boundary fault, specifically a normal fault. This type of fault occurs when two tectonic plates move apart, creating tensional stress that leads to the pulling apart of the Earth's crust and the formation of a rift valley.
Tensional boundary is the meeting zone of two tectonic plates at a normal fault; the plates move apart
Tensional boundary is the meeting zone of two tectonic plates at a normal fault; the plates move apart
A normal
Fault line between the plates
a normal fault
In a reverse fault, compression (plates crashing together) causes the hanging wall to move up. In a normal fault, tension ( plates pulling apart) causes the footwall to push up.
A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
Where two plates move away from each other tension forces create many normal faults.
Normal faults occur at divergent boundaries, where tectonic plates are moving apart. This type of fault results from tensional stress pulling the plates in opposite directions, causing the hanging wall to move downward relative to the footwall.
In a normal fault the hanging wall moves downward. With this type of fault, the hanging wall also shifts horizontally away from the fault line.
When plates move apart or diverge, it is called a normal fault (happens along a divergent boundary). When plates collide or converge, a reverse fault occurs (when the hanging wall pushes up, and the foot wall pushes down). When plates slide past each other, it is called a strike-slip fault, which typically occurs at a transform plate boundary.Also, if you are still having doubts, do more research on strike-slip faults, normal faults, and reverse faults by just typing it in.
In a normal fault, the hanging wall moves down relative to the footwall due to tensional forces pulling the plates apart. This type of fault is associated with divergent plate boundaries or areas where the Earth's crust is being pulled apart.