* Transform boundaries are primarily about horizontal movement. Unlike divergent (where new crust is created) or convergent (where crust is destroyed) boundaries, transform boundaries involve two tectonic plates sliding past each other.

* Minimal crustal creation or destruction. While there might be some localized areas of minor crustal creation or destruction due to friction and stress, the dominant process at transform boundaries is lateral movement, not the generation or destruction of crust.

* Example: The San Andreas Fault. This famous fault is a transform boundary where the Pacific Plate slides past the North American Plate. You can see evidence of this lateral movement in the offsetting of geological features along the fault zone.

Therefore, the statement that crust is neither created nor destroyed along a transform boundary is a good simplification. However, it's important to remember that there can be some localized exceptions due to the complexities of plate tectonics.