Compression (that acts to decrease an objects volume by squashing it together), Tension (which acts to increase an objects volume by pulling it apart) and a bonus Shear which acts in opposite directions on opposite sides of an object to make the two halves slide past each other.
Tension and compression because compression occurs when forces act to squeeze an object.Tension occurs when forces act to stretch an object.
weather ,seismic ,volcanic
Two types of stress are compressional and tensional stress. Shear stress also plays a significant role in deformations in the Earth's crust at transform and strike slip faults.
Tensional forces and compressional forces.
The three main types of stress in a rock are shearing, tension, and compression.
folds-bending of the rocks without breaking faults-fracture of rocks with displacement joints-fracture of rocks wihtout displacement joints affect the resistance of rocks and making it subscitible to weathering
weather ,seismic ,volcanic
Two types of stress are compressional and tensional stress. Shear stress also plays a significant role in deformations in the Earth's crust at transform and strike slip faults.
Two types of stress are compressional and tensional stress. Shear stress also plays a significant role in deformations in the Earth's crust at transform and strike slip faults.
Two types of stress are compressional and tensional stress. Shear stress also plays a significant role in deformations in the Earth's crust at transform and strike slip faults.
Weathering is when it rains and has a vary amount of wind and different types of weather. Erosion is when he rocks deform to different shapes. So it has a HUGE Impact because it changes the look of the rock.
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
Tensional forces and compressional forces.
residual deposits and sedimentary deposits
In the rock cycle, rocks change into differant types of rocks over time. For example, igneous rocks might break into sediments that form sedimentary rocks.
In the rock cycle, rocks change into differant types of rocks over time. For example, igneous rocks might break into sediments that form sedimentary rocks.
cracks == In addition to cracks: faulting, metamorphism to new rock types, earthquakes, tilting, and folding.
The three main types of stress in a rock are shearing, tension, and compression.