When two tectonic plates slide past one another, a transform fault occurs, which can lead to significant geological activity. The friction between the plates can cause stress to build up, eventually resulting in earthquakes when the stress is released. Unlike converging or diverging plates, sliding plates do not typically create or destroy crust, but their movement can result in deformation of the rocks along the fault line. Examples of this include the San Andreas Fault in California.
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Plates slide past each other at transform boundaries. These boundaries occur when two plates slide horizontally in opposite directions parallel to each other. The movement can be either in the same direction but at different speeds, or in opposite directions.
Tectonic Plates move by trying to push past each other and by trying to slide past each other.
Where 2 plates slide past each other in a horizontal motion that boundary is called a Transform Boundary, or a fault.
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Transform Boundary
At convergent boundaries, plates do not slide past each other. Instead, they move towards each other and collide or subduct under one another. This collision or subduction process is what characterizes convergent plate boundaries.