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Faults are the boundaries between tectonic plates and are not the cause of earthquakes. The motion of one plate against another or the subduction of one plate by another can eventually cause a slippage, and it is this slippage that causes earthquakes.
Faults are fractures in the Earth's crust where rocks have moved past each other. When the rocks along a fault suddenly shift, it can cause an earthquake. The movement along faults is what generates the energy that produces earthquakes.
The two types of faults that can result in mountains are thrust faults and normal faults. Thrust faults occur when older rock is pushed on top of younger rock, causing uplift and mountain formation. Normal faults occur when tensional forces cause one block of rock to drop down relative to another block, creating valleys and mountain ranges.
Reverse and thrust faults are both under compressive stress.
The force that causes earthquakes is primarily generated by the movement of tectonic plates along faults in the Earth's crust. As the plates move, stress builds up and eventually overcomes the friction holding the rocks together, causing them to break and release energy in the form of seismic waves, resulting in an earthquake.
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Shearing force can lead to faults like strike-slip faults, where rocks on either side of the fault move horizontally past each other. These faults can cause earthquakes and are common at tectonic plate boundaries.
Strike-slip faults cause shearing
a compression force would cause a normal fault. i rember by the name compress "press" together
Faults can create cracks in the earth and cause earthquakes.
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
compression
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.
It all depends on how big the fault is, bigger ones will cause bigger earthquakes, while smaller, or small ones may cause no earthquake at all.
Faults are the boundaries between tectonic plates and are not the cause of earthquakes. The motion of one plate against another or the subduction of one plate by another can eventually cause a slippage, and it is this slippage that causes earthquakes.
Earthquakes are typically caused by movement along a fault line, which is a fracture in the Earth's crust where rocks have shifted position relative to each other. The three main types of faults that can cause earthquakes are normal faults, reverse faults, and strike-slip faults.
So that geologist can predict how much force of pressure applied on the faults to predict how strong the earthquake.