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it pushes rock in to different directions

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What is the stress that pushes masses of rock in opposite directions in a sideways movement?

shearing


What is the ratio of modulus of rigidity?

shearing stress to shearing strain


Three types of stress that occer in earths crust?

Compression Stress Tension Stress Shearing Stress


Compression tension and shearing are three types of?

stress


What is shearing on earth's crust?

Shearing on Earth's crust occurs when two tectonic plates slide past each other horizontally. This movement creates stress along the plate boundary, leading to the formation of fault lines and earthquakes. Shearing is one of the three main types of plate boundary interaction, along with convergent and divergent movements.


List the three types of stress that occur in earth's crust?

the 3 kinds of stress are compression,tension, and shearing


What is the difference between shear stress and bearing stress?

Sear stress are forces applied in opposition, producing a shearing or tearing force. Bearing stress is a load placed in one direction, such as the weight of a building bearing on the foundation.


What type of boundary produces shearing stress?

Transform Boundary


What type of stress pushes rock in opposite directions?

Shearing


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.


What type of stress force that produces a strike-slip fault is?

shearing


Shearing results when forces within the earth are pulled in opposite horizontal directions?

Shearing in the Earth's crust occurs when forces cause rocks to move horizontally in opposite directions along a fault line. This movement results in a strain that generates earthquakes as the rocks rupture along the fault. Shearing is a type of stress that can lead to faulting and seismic activity.