tension (Dip-Slip Normal fault)
Tensional stress causes rocks to pull apart. This type of stress occurs when rocks are being pulled in opposite directions, leading to the stretching and extension of the rock mass. Over time, this can lead to the formation of faults and fractures in the rocks.
A divergent boundary causes tensional stress, where tectonic plates are moving away from each other. This stress results in the stretching and thinning of the Earth's crust, leading to the formation of new crust through volcanic activity and seafloor spreading.
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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.
A convergent boundary causes compressional stress.
compression
Compressional Stress
Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.
Tension
The strain that causes a material to pull apart is known as tensile strain. It occurs when a material is subjected to tensile stress, leading to elongation or stretching. This type of strain is significant in engineering and materials science, as it helps determine a material's ability to withstand forces without failing.
its the circulation of the rock and when it pushes together
Compressive stress causes folding mountains to form. This stress occurs when tectonic plates collide or converge, leading to the deformation and folding of rock layers, ultimately creating mountain ranges.