The bending of rock is known as rock deformation, which occurs when rocks are subjected to stress (pressure). This stress can cause rocks to change shape and ultimately deform, leading to the formation of folds or faults in the Earth's crust. Rock deformation is a key process in the field of structural geology, helping to understand how rocks respond to tectonic forces.
Stress changes the shape or breaks (fractures) rocks whereas bending leads to folding
Folding is the bending of rock layers due to stress.
The force that causes rock layers to crumple and fold is mainly tectonic forces, such as compression. When two tectonic plates collide or move toward each other, the rocks in between experience intense pressure, leading to deformation and folding of the rock layers.
"Folding" is the term that describes the bending of rock layers due to stress.There are different types of Folds and these include:Anticlinal Folds: This is when the rock layers have an upward-arching folds.Synclinal Folds: This is when the rock layers have a downward, trough-like folds.Monoclinal Folds: This is when both rock layers ends are horizontal.
Folding
The bending of rock is known as rock deformation, which occurs when rocks are subjected to stress (pressure). This stress can cause rocks to change shape and ultimately deform, leading to the formation of folds or faults in the Earth's crust. Rock deformation is a key process in the field of structural geology, helping to understand how rocks respond to tectonic forces.
It is called Folding
elastic limit
elastic limit
Folding.
Stress changes the shape or breaks (fractures) rocks whereas bending leads to folding
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The bending of rock layers due to stress
injury
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