A fault
A place where two tectonic plates meet is a fracture in the Earth.
faulting causes large blocks of the Earth's crust to drop down relative to other blocks
They are called fault lines.
== == A fault.
A fault is a break in Earth's crust along which blocks of rock slide relative to one another. A fault can occur within a tectonic plate's boundaries. Boundaries between tectonic plates are always faults.
The fracture along blocks of crust (tectonic plates) is called a "fault" or "fault line".
A fault is a fracture where blocks of the Earth's crust move relative to one another. This movement can be lateral, vertical, or diagonal, and it is often caused by tectonic forces. Earthquakes can occur along faults when the built-up stress is released suddenly.
That's called a 'fault line'.
That is called a fault. A fault is a fracture in the Earth's crust where movement has occurred along the fracture.
A deep crack in the earth's surface is a fault It can also be a joint.
The breaking and sliding surface between blocks of crust is known as a fault. Faults occur due to tectonic forces causing stress and releasing energy along these fracture zones. Movement along faults can result in earthquakes and the shifting of Earth's crust.
what are mountains formed by blocks of crust moving along a fault
The rift of an earthquake refers to the fracture or break along a fault line where the two blocks of the Earth's crust move relative to each other during an earthquake. This movement causes the release of energy in the form of seismic waves that produce the shaking felt on the Earth's surface.
A fault is a fracture in the Earth's crust where movement has occurred. This movement can be horizontal, vertical, or a combination of both. Faults can generate earthquakes when the stress along the fault is released suddenly, resulting in movement along the fault surface.
Large blocks of Earth's crust that drops down relative to other blocks, will form a rift valley (trench). The Great Rift Valley in Africa is one example.
Fault block mountains are formed when large blocks of the Earth's crust are uplifted along faults. Tensional forces cause the blocks to move vertically relative to each other, creating steep mountain ranges and valleys. As the blocks continue to move, the mountains can be further uplifted and shaped by erosion.
fault block