temperature, confining pressure, rock type, and time
it is the movement of tectonic plates due to compression and tension which causes rock to fold and deform
Temperature, rainfall, vegetation, animal activity, type of rock being weathered.
The type of rock and climate influence how fast it will weather. If a rock is more permeable, it is more prone to deteriorating quickly because pockets of air leave a larger surface area to be damaged. The climate can break down rocks through wind and water.
time
As these isostatic adjustment occur, areas of the crust are bent up and down. This bending cause rock in that area to deform.
temperature, confining pressure, rock type, and time
The factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock type, and time.
Internal Controlling Factors: Strength: The strength of the rock determines the amount of deformation that can occur before it fractures. Different types of rocks have different strengths, so the amount of deformation that can occur will vary depending on the type of rock. 2. Temperature: The temperature of the rock determines the amount of deformation that can occur. When rocks are heated, they become more ductile and can deform more easily than when they are cold. 3. Composition: The chemical composition of the rock can also influence its ability to deform. Rocks with higher amounts of silica tend to deform more easily than rocks with lower amounts. External Controlling Factors: Pressure: The external pressure applied to the rock can influence the amount of deformation it can endure. Higher pressures tend to cause rocks to deform more easily than lower pressures. 2. Stress: The type of stress applied to the rock can also influence how much deformation it can endure. Different types of stresses can cause different amounts of deformation. 3. Time: The amount of time over which the deformation takes place can also influence the amount of deformation that can occur. Deformation can occur over
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time
rocks deform due to stress that bends the rock into different shapes and sizes.
Parent Rock (material) and Climate.
a deeply buried rock is pushed down by the weight of all material above it. Since the rock cannot move, it cannot deform.
Parent Rock (material) and Climate.
it is the movement of tectonic plates due to compression and tension which causes rock to fold and deform
The stress reduction factor is a product of the relationship between the Unconfined compressive strength of a rock and the sigma 1, or principal stress field in that area. The higher the value, the more likely the rock is to deform when placed under load.
Rate of cooling of the magma and Chemical composition of the magma.