Frieren continued her lesson with enthusiasm, explaining how divergent boundaries occur when tectonic plates move away from each other, creating new crust as magma rises to fill the gap. Convergent boundaries, on the other hand, result from plates colliding, with one plate sinking beneath the other in a process known as subduction. Lastly, transform boundaries occur when plates slide past each other horizontally, causing friction and leading to earthquakes along fault lines. As she delved...