The fault locks, and stress builds up until an earthquake occurs.
Pressure, more accurately described as stress, eventually overpowers the weight of the rock strata along the fault, and it moves. This usually results in an earthquake.
The rocks easily slide past each other.
reverse fault
Strain builds up until the release is shocking.
Usually along a fault the rock layers are broken and displaced in some manner so that the rock layers are not continuous across the fault.
They cannot determine which point along a fault has the most pressure.
They cannot determine which point along a fault has the most pressure.
The fault will be locked until the pressure builds up enough until it breaks.
reverse fault
Because of friction and the rigidity of the rock, the rocks cannot glide or flow past each other. Rather, stress builds up in rocks and when it reaches a level that exceeds the strain threshold, the accumulated potential energy is dissipated by the release of strain, which is focused into a plane along which relative motion is accommodated-the fault.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
Earthquakes occur along the San Andreas Fault because of the tectonic plates. When the plates slip or shift, an earthquake happens.
The rock gets farther a part from the fault
If the fault is responsible for the earthquake, there will be movement (displacement) along the fault.
Earthquake.
Reverse fault
Strain builds up until the release is shocking.
Usually along a fault the rock layers are broken and displaced in some manner so that the rock layers are not continuous across the fault.