Why do geological processes that occur at convergent boundaries expanding?

Geological processes at convergent boundaries are expanding due to the ongoing interactions between tectonic plates, where one plate is forced beneath another in a process called subduction. This subduction leads to the formation of deep ocean trenches, volcanic arcs, and mountain ranges, contributing to the dynamic nature of the Earth's crust. As these processes continue over time, they can create new geological features and reshape existing ones, increasing their extent and complexity. Moreover, the release of energy from these interactions can trigger earthquakes, further contributing to geological changes.