No
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No, transform faults do not make mountains. Transform faults occur where tectonic plates slide past each other horizontally. Mountains are typically formed by the convergence of tectonic plates, where one plate is forced beneath the other, or by volcanic activity.
A transform fault does not typically form mountains. Transform faults are characterized by horizontal motion and sliding past each other, so they do not promote vertical displacement that creates mountains like convergent or divergent boundaries do.
Fault block mountains go up and down, but at transform boundaries plates slide past each other horizontally.
Transform faults occur when two tectonic plates slide past each other horizontally. These faults are found in mid-ocean ridges where plates are moving apart. The movement along transform faults can result in earthquakes.
Strike-slip faults are common at transform boundaries because the plates are sliding past each other horizontally in opposite directions. This movement creates shear stress along the faults, leading to the formation of strike-slip faults. The San Andreas Fault in California is a well-known example of a transform boundary with a prominent strike-slip fault.
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