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strike-slip
fault mountains
Moving together
This occurs when plates are pushed in opposite directions along a horizontal plane.
There is local tectonic activity but the surface appears to be a single crustal plate, with little large-scale horizontal motion of plates as found on the Earth.
Horizontal shearing at tectonic plate boundaries results in a special type of strike slip fault known as a transform fault.
strike-slip
This occurs when plates are pushed in opposite directions along a horizontal plane.
The three types of stress in plates are tensile stress (stretching), compressive stress (compressing), and shear stress (sliding or tearing). These stresses can cause deformation or failure in the material if they exceed its strength.
When an Earthquake is shearing two plates from transform boundaries are sliding past one another. For example when I rub my hands past one another that is kind of like what is happening when shearing occurs.
fault mountains
Manuel Stein has written: 'Postbuckling response of long thick plates loaded in compression including higher order transverse shearing effects' -- subject(s): Aluminum Plates, Buckling, Buckling (Mechanics), Compression testing, Flexibility, Loads (Forces), Materials, Metal plates, Plates (Engineering), Plates, Aluminum, Shear (Mechanics), Shearing, Stress functions, Thick plates 'A solution procedure for behavior of thick plates on a nonlinear foundation and postbuckling behavior of long plates' -- subject(s): Mathematical models, Plates (Engineering), Structural engineering, Strength of materials
At transform boundaries, the plates move horizontal in relation to each other.
At transform boundaries, the plates move horizontal in relation to each other.
The plates are shifting all the time.
A table top is horizontal, otherwise, the plates would slide off. Any surface, drawn line, or object, classed as being level is also horizontal.
tectonic plates.