Which type of boundary is responsible for the creation of new oceanic crust?

Divergent boundaries are the areas where tectonic plates move apart from each other, resulting in the formation of new oceanic crust. At these boundaries, magma from the mantle rises to fill the space created by the diverging plates. As this magma cools and solidifies, it forms new crust at the ocean floor, which is often seen at mid-ocean ridges. This process continuously replenishes the oceanic crust and contributes to the overall structure of ocean basins.

Transform boundaries, on the other hand, involve plates sliding past one another without generating new crust. Convergent boundaries occur when plates collide, leading to one plate being subducted beneath another, often resulting in the destruction of crust rather than the creation of new. Static boundaries are not commonly recognized in the tectonic plate framework, as they suggest no movement or interaction between the plates. Thus, the formation of new oceanic crust is specifically associated with divergent boundaries.