Normal Fault
a reverse fault
A normal fault.
Horizontal shearing can result in strike-slip faults, where two plates slide past each other horizontally. This type of fault is common along transform boundaries, such as the San Andreas Fault in California.
It is called a normal fault.
A reverse fault is a type of fault where the hanging wall moves up relative to the footwall due to compression forces in the Earth's crust. This type of fault is typically found in regions undergoing compression, such as at convergent plate boundaries where tectonic plates collide. Reverse faults are characterized by a steep fault plane and can result in uplift and mountain building.
A normal fault.
Normal faults are the result of tensile stresses.
the upper wall of an inclined fault
normal
a reverse fault
A normal fault moves because of tension. In this type of fault, the hanging wall moves down relative to the footwall due to the stretching and pulling apart of the Earth's crust.
Normal faults
Rocks being pulled apart are under tension. This is found at divergent plate boundaries. It is a tension fault.
Normal Thrust
A normal fault is a type of fault in which the hanging wall drops down relative to the footwall due to tensional forces in the Earth's crust. This type of fault is commonly associated with extensional tectonic settings, where the crust is being pulled apart.
tension (Dip-Slip Normal fault)
A tension fault occurs when there is stretching or pulling apart of the Earth's crust, which can lead to earthquakes as the rock breaks under the stress. This type of fault is associated with tectonic plate movements and occurs along divergent plate boundaries.