A Tectonic fault is where the different tectonic plates meet and it is a fault because one may be higger or thicker than the other.
The type of tectonic stress that forms fault-block mountains is known as extensional stress. This stress occurs when the Earth's lithosphere is being pulled apart, causing blocks of crust to move vertically. As the blocks are uplifted and tilted along fault lines, fault-block mountains are created.
Fault lines exist where one tectonic plate meets another. For example the San Andreas Fault in California is the boundary between the North American plate (on the east of the fault line) and the Pacific plate (on the west of the fault line)
Fold mountains are formed when tectonic plates collide, causing compression and the folding of rock layers. Fault mountains are created by the movement along fault lines, where one side of the fault is pushed up relative to the other. Both types of mountains result from the Earth's tectonic activity.
The San Andreas Fault is a strike-slip fault, where two tectonic plates move horizontally past each other. The main force causing movement along the fault is the tectonic forces generated by the motion of the Pacific Plate relative to the North American Plate.
Two actions of Earth's crust that can create a fault are tectonic plate movement and stress buildup. When two tectonic plates collide or slide past each other, it can cause the crust to fracture and create a fault. Additionally, the accumulation of stress along existing faults due to pressure from tectonic forces can also lead to fault formation.
Tectonic plates and fault lines created by the movement of tectonic plates.
A fault is where to tectonic plates meet but a fault zone is the area around a fault.
Tectonic plates
by tectonic plates
Japan sit on the Median Tectonic Fault Line
A fault line is the boundary between two tectonic plates; fault lines do not ordinarily appear on maps.
The force that is causing movement at this fault is called tectonic force. These forces are generated by the movement and interaction of the Earth's tectonic plates.
A fault line becomes active when the stress accumulated along the fault exceeds the strength of the rocks, causing them to break and move. This movement can result from tectonic forces, such as the shifting of tectonic plates. When the stress is released, it often leads to earthquakes. Continuous tectonic activity can keep a fault line active over time, leading to repeated seismic events.
The type of tectonic stress that forms fault-block mountains is known as extensional stress. This stress occurs when the Earth's lithosphere is being pulled apart, causing blocks of crust to move vertically. As the blocks are uplifted and tilted along fault lines, fault-block mountains are created.
Fault lines exist where one tectonic plate meets another. For example the San Andreas Fault in California is the boundary between the North American plate (on the east of the fault line) and the Pacific plate (on the west of the fault line)
A Fault(:
Shifting,sliding,diverging ,converging etc . of tectonic plates.