The type of stress that causes rocks to pull apart is a tension stress. It is the major type of stress found in divergent plate boundaries.
When tension forces act on rocks, they can cause the rocks to stretch and eventually break. This type of stress can lead to the formation of faults, fractures, and rock rifts as the rocks are pulled apart. Over time, this can result in the creation of features like rift valleys or deep fractures in the Earth's crust.
Faults in Earth's crust are caused by the movement of tectonic plates. When these plates collide, slide past each other, or pull apart, the stress that builds up along the plate boundaries can lead to the formation of faults. This can result in rocks breaking and sliding along the fault plane.
Ah, that's a wonderful question, friend. The stress that pushes a mass of rock in two opposite directions is called "compressional stress." Just like when we paint, sometimes rocks feel the pressure from different directions, but they can still create something beautiful in the end.
Fault, crack, fracture, fissure, joint are all terms that could be applied to this question.In structural terms, tensile stress in the earth's crust initially creates normal faults. If the tensile stress state persists, larger scale structures such as horst and graben will develop (where graben are down thrown blocks of crust surrounded by normal faults, horsts are the upthrown crustal blocks surrounding the graben).Ultimately this may result in the formation of a rift valley and or the creation of a divergent tectonic plate boundary.
There are three main forces that drive deformation within the Earth. These forces create stress, and they act to change the shape and/or volume of a material. The following diagrams show the three main types of stress: compressional, tensional, and shear. Stress causes the build up of strain, which causes the deformation of rocks and the Earth's crust. Compressional stresses cause a rock to shorten. Tensional stresses cause a rock to elongate, or pull apart. Shearstresses causes rocks to slip past each other.
The type of stress that causes rocks to pull apart is a tension stress. It is the major type of stress found in divergent plate boundaries.
Stress that acts to pull materials (including rocks of the crust) apart is known as tensile stress.
The force that tends to pull rocks apart is called tensional stress. This stress occurs when rocks are being stretched in opposite directions, causing them to break and create faults or fractures in the Earth's crust.
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.
When tension stresses inside Earth pull rocks apart, fractures known as faults are formed. These faults can lead to earthquakes as accumulated stress is suddenly released along the fault plane.
Divergent Pull Ex.<--_-->
if you mean whene you give some one lots of tension <><><><><> Tension is stress, or voltage, to name just two. tension-is stress that streches or pull rocks apart
A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
because they are the same lengh
The stress force that causes a mass of rock to pull or twist in opposite directions is called tension. Shearing is the stress force that causes a mass of rock to pull or twist in opposite directions.
When tension forces act on rocks, they can cause the rocks to stretch and eventually break. This type of stress can lead to the formation of faults, fractures, and rock rifts as the rocks are pulled apart. Over time, this can result in the creation of features like rift valleys or deep fractures in the Earth's crust.
Stress forces affect rocks in various ways. The most common effects include cracking, breaking, shrinking or total change in their composition among others.