The bending and tilting of the Earth's crust in response to stress is called deformation. When the stress exceeds the strength of the rock, it may break, leading to the formation of faults or fractures in the Earth's crust.
The land that stretches thousands of miles below the ocean is known as the oceanic crust. It is composed of basaltic rock and is part of Earth's tectonic plates. This crust is constantly moving and being created at mid-ocean ridges while being destroyed at subduction zones.
The crust stretches and gets thinner so the pressure decreases on the mantle rocks below this causes part of the mantle to melt
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.
The Earth's crust is on the exterior, not the interior; that is why it is called the crust. It is on the outside. It is made mostly of rock, of various kinds. The rock of the crust is on average less dense than the rock of the mantle, which lies beneath the crust.
Tensional stress force pulls on the crust and stretches rock. This type of stress occurs where tectonic plates are moving away from each other.
Tensional stress pulls crust apart and stretches rock, causing it to deform and eventually break along fault lines. This type of stress commonly occurs at divergent plate boundaries where tectonic plates are moving away from each other.
The stress force that pulls on the crust and thins rock in the middle is called tension. Tensional stress occurs when two plates move away from each other, creating faults where rocks are pulled apart and thinned in the middle. This process is often associated with the formation of rift valleys and mid-ocean ridges.
Tensile stress.
Tensile force / stress.
Tensile stress is the force that pulls rock apart, causing it to break or fracture. This type of stress occurs when rocks are stretched in opposite directions, leading to the formation of cracks or faults in the rock.
When stress squeezes an object it is compression. When stress stretches an object it is called tension. The process by which the shape of a rock changes because of stress is called deformation.
Stress forces squeeze or pull the rock in the Earth's crust.
because when it acts on the surface it stretches the rock to make craters or " dents" on the crust.
because when it acts on the surface it stretches the rock to make craters or " dents" on the crust.
Tension or tensile stress is what you described in the question.
The bending and tilting of the Earth's crust in response to stress is called deformation. When the stress exceeds the strength of the rock, it may break, leading to the formation of faults or fractures in the Earth's crust.