How about you look up - Subduction, when one plate slides beneath another at a convergent boundary.
Continental plates can tilt due to tectonic forces, mantle convection, and subduction-related movements. This tilting often occurs over millions of years and can lead to significant geological changes. For example, studies suggest that the Australian continent has been tilting northeastward since the Late Cretaceous, influenced by mantle-driven and subduction-driven forces.
