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stress that pushes a mass of rock in two opposite directions is called shearing
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What is the stress that pushes a mass of rock in two opposite directions called?
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.
Stress that pushes a mass of rock in two opposite directions is called?
Have a lot of fun.
What type of stress pushes rock in opposite directions?
Shearing
What is stress that pushes rock in opposit directions?
Stress that pushes rock in diffrent directions is called tension. Not shearing
What is the stress that pushes masses of rock in opposite directions in a sideways movement?
shearing
What movement does shearing stress do?
it pushes rock in to different directions
What force pushes on rocks from different not opposite directions?
Shearing is the force that pushes rocks from different but not opposite directions. Secondary waves, S waves are all names for the shearing.
Stress that pushes rock in opposite derection?
Compression stress pushes rock in the opposite direction, causing it to be squeezed and compacted. This type of stress often leads to the folding and faulting of rocks as they respond to the pressure by deforming and moving.
What is stres that pushes masses of rock in opposite directions in a sideways movement?
shearing
What forces push on rocks from not different but opposite directions?
Shearing is the force that pushes rocks from different but not opposite directions. Secondary waves, S waves are all names for the shearing.
What kind of stress pushes rock in two different directions?
Shear stress pushes rocks in two different directions, causing them to slide or deform along parallel planes. This type of stress is common along fault lines where tectonic plates are moving past each other.
What is stress that pushes mass of rock in opposite directions?
Tensile stress is the result of a force acting over a cross sectional area that pulls material apart. This occurs in normal faults, rift valleys and at divergent plate boundaries.
