plates in the earth move and shift, cracking the crust.
Tension creates normal faults, where the hanging wall moves downward relative to the footwall. This type of fault is common in divergent boundary settings when tectonic plates move away from each other, causing extension and the rocks to be pulled apart.
A fault-block mountain is formed when higher blocks of land are displaced along a fault line, causing one side of the fault to rise relative to the other. This creates a steep-sided mountain range with a distinctive block-like structure.
Fault-block mountains are caused by normal faults, where blocks of the Earth's crust are tilted and uplifted along a fault line. As the hanging wall block moves downward relative to the footwall block, it creates a steep mountain range with a characteristic block-like appearance.
Rock layers cut by a fault formed as a result of tectonic forces. The faulting process involves rocks breaking and shifting along a fracture zone due to stress accumulation, leading to the development of a fault plane. Over time, this creates distinct layers on either side of the fault line due to the movement of the Earth's crust.
The San Andreas Fault is a result of the tectonic forces causing the Pacific Plate to move northwestward relative to the North American Plate. This movement creates significant stresses that are relieved through periodic earthquakes along the fault line.
Seismograph
compression
When compression pushes rocks together, it creates a reverse fault. In a reverse fault, the hanging wall moves up relative to the footwall due to compression forces pushing the rocks together.
In geology, shearing occurs when rocks slide past each other horizontally in opposite directions. The kind of fault created by shearing is called a strike-slip fault.
Tension creates normal faults, where the hanging wall moves downward relative to the footwall. This type of fault is common in divergent boundary settings when tectonic plates move away from each other, causing extension and the rocks to be pulled apart.
A fault-block mountain is formed when higher blocks of land are displaced along a fault line, causing one side of the fault to rise relative to the other. This creates a steep-sided mountain range with a distinctive block-like structure.
Fault-block mountains are caused by normal faults, where blocks of the Earth's crust are tilted and uplifted along a fault line. As the hanging wall block moves downward relative to the footwall block, it creates a steep mountain range with a characteristic block-like appearance.
Rock layers cut by a fault formed as a result of tectonic forces. The faulting process involves rocks breaking and shifting along a fracture zone due to stress accumulation, leading to the development of a fault plane. Over time, this creates distinct layers on either side of the fault line due to the movement of the Earth's crust.
The San Andreas Fault is a result of the tectonic forces causing the Pacific Plate to move northwestward relative to the North American Plate. This movement creates significant stresses that are relieved through periodic earthquakes along the fault line.
A reverse fault is caused by compressional forces in the Earth's crust, where rocks are pushed together, causing the overlying rock to move up and over the underlying rock along the fault plane. This results in a reverse fault where the hanging wall moves vertically upward in relation to the footwall.
Fault lines - are 'cracks' in the Earth's crust, which creates large 'plates'. The plates 'float' on the magma under the surface - allowing them to move. When these plates rub against each other - it causes earthquakes.
A reverse fault occurs when compression forces push one side of the fault upward and the other side downward. This motion creates a steep incline in the fault plane, with the hanging wall moving up and the footwall moving down. Reverse faults are typically associated with convergent plate boundaries where compression forces are high.