The force that pulls apart the crust is called tensional or extensional tectonic stress, which occurs at divergent plate boundaries where tectonic plates move away from each other. This pulling force can lead to the formation of rift valleys and mid-ocean ridges.
Tensile stress.
The force that pulls an object apart is called tension. Tension occurs when a material is stretched or pulled in opposite directions, causing it to become elongated.
The force that pulls things forward is called "thrust."
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.
gravity is a force that pulls object toward each other
Tension stretches or pulls apart the crust.
tension
When there is a divergent boundary, regardless if the plates are ocean-ocean or continental-continental, tensional stress pulls on the crust. Rocks have weaker tensional strength than compressive strength, so they are easier to pull apart.
it may be gravity
tension
Tensile stress.
the type of stress that pulls the crust is called TENSION.
Stress that acts to pull materials (including rocks of the crust) apart is known as tensile stress.
Generally materials that fly apart are being pushed rather than pulled. We could devise a mechanism that pulls materials apart - for example, if we attach two hooks and pull them on winches in opposite directions. In that case we would describe the force as mechanical in nature. But it is more likely that things get pushed apart by their own internal pressure.
The force that pulls an object apart is called tension. Tension occurs when a material is stretched or pulled in opposite directions, causing it to become elongated.
the type of stress that pulls the crust is called TENSION.
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.