Stress forces affect rocks in various ways. The most common effects include cracking, breaking, shrinking or total change in their composition among others.
Reverse fault
The rock moves because forces deep inside earth create stress or pressure in the rock when the pressure in the rock builds up enough,the rock breaks or changes shape releasing energy in the form of waves
The stress that squeezes rock until it folds or breaks is called compressional stress. This type of stress occurs when forces push together in opposite directions, causing rocks to deform under pressure.
erosion happens
Sediment builds up over time and expands. Probably like a huge rock or a giant elephant.
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.
It could help you relax and relieve stress.
Ductile deformation is when rock is given enough stress to break. If the stress is less, it will bend but not break.
I found that folding happens
Elastic rebound. This phenomenon occurs when stress builds up in a rock mass and causes it to deform, then suddenly release that stress by rebounding to its original shape. Elastic rebound is often associated with earthquakes and fault movements.
When rock layers are folded, a geological fold happens. These folds form under various conditions such as stress, hydrostatic pressure, pore pressure, and temperature gradient.
Yes, stress can build up along fault lines where rocks snag and remain locked. This stress can accumulate over time until it is released in the form of an earthquake when the built-up energy exceeds the strength of the rocks holding the fault together.