A fault is a crack or fracture in the earth's crust. In geology, a fault or fault line is a planar fracture in rock in which the rock on one side of the fracture has moved with respect to the rock on the other side. Large faults within the Earth's crust are the result of differential or shear motion and active fault zones are the causal locations of most earthquakes. Earthquakes are caused by energy release during rapid slippage along a fault. A fault that runs along the boundary between two tectonic plates is called a transform fault.
In social studies, the term "fault" can refer to a break or fracture in the Earth's crust where rocks have slipped past each other. It is commonly associated with earthquakes and tectonic plate movements.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
The earth's crust is not stress
because is he mad
continental crust
A crack in the Earth's crust is a fracture where rocks have pulled apart, whereas a fault is a fracture where there has been movement along the fracture plane. In other words, a fault is a type of crack in the Earth's crust that has undergone displacement.
This is known as a fault. A fault is a fracture in the Earth's crust along which movement has occurred. Movement along faults can result in earthquakes.
The Earths crust is approximately 650 km deep.
A break in the Earth's crust is called a fault. It is a fracture where the two sides of the rock move in relation to each other. Faults are a common feature in tectonically active regions where there is movement of the Earth's plates.
In social studies, the term "fault" can refer to a break or fracture in the Earth's crust where rocks have slipped past each other. It is commonly associated with earthquakes and tectonic plate movements.
fault
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
mantle
The earth's crust is not stress
The fracture along blocks of crust (tectonic plates) is called a "fault" or "fault line".
because is he mad
half of earths layer