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What fault would create landforms through shearing stress?

A strike-slip fault would create landforms through shearing stress. In a strike-slip fault, two blocks of rock slide past each other horizontally, causing a horizontal shearing stress that can result in landforms such as fault scarps or offset river channels.


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

shearing


Are faults caused by stress?

Yes, a strike-slip fault is caused by shearing.


What stress causes a slip-strike fault?

The stress that causes strike-slip faults is produced by a shearing force and so is called shear stress.


What type of fault has shearing?

A strike-slip fault


What is the ratio of modulus of rigidity?

shearing stress to shearing strain


What type of fault is produced from shearing?

The deformation of a material so that its layers move laterally over each other. In geology, shearing bends, twists, and draws out rocks along a fault or thrust plane. Such shearing is sometimes accompanied by shattering or crushing of the rock near the fault. A shearing force acts parallel to a plane rather than perpendicularly. Shear stress is the force or forces applied tangentially to the surface of a body and causing bending, twisting, or drawing out of that body.


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.


What type of fault is caused by shearing San Andres fault in California?

A transverse fault


What fault is caused by shearing forces?

Transform or Strike Slip Fault


Which fault is most likely to occur with shearing?

Strike-slip fault


What force causes a strike slip fault?

Strike-slip faults are caused by horizontal shear stress along the fault plane, which results in horizontal movement of the rocks on either side of the fault. The movement can be either left-lateral (sinistral) or right-lateral (dextral), depending on the direction of the shear stress.