Monocline
A force that acts on rock to change its shape or volume called stress. Tension is the stress that sketched rock so that is becomes thinner in the middle.
The force that acts on rock to change its shape or volume is called stress. Stress can be caused by factors such as tectonic plate movement, pressure from surrounding rocks, or even human activities like mining. This stress can lead to the deformation or fracturing of rocks over time.
The term for the amount of force per unit area that acts on rock is called stress. Stress is a measure of the internal forces within a rock mass that result from the applied forces acting on it.
stress
Folded mountains are formed when rock layers are bend under stress.
Fold mountains are formed by vertical pressure when tectonic plates collide and force rock layers to bend and uplift, creating ridges and peaks. Examples include the Himalayas and the Alps.
A vertical intrusion is called a "dike." Dikes are geological formations that occur when magma pushes through existing rock layers and solidifies, creating a vertical wall of igneous rock. They are typically formed in a variety of environments, often associated with volcanic activity.
When a fault is not vertical, a hanging wall and footwall are formed. The hanging wall is the block of rock above the fault plane, while the footwall is the block of rock below the fault plane. These terms help geologists describe the displacement and movement along the fault.
Stacks are formed from erosion. They are created when a sea arch collapses due to the continual action of waves eroding away the rock, leaving behind a tall vertical column of rock isolated from the shore.
Folded mountains are formed when rock layers are bend under stress.
when magma is squeezed into horizontals craks are called sill
The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.