convergent boundary

A convergent boundary is a place where two tectonic plates in the Earth's crust move toward each other. This often occurs when one plate slides beneath the other, a process called subduction. As the plates collide, they can create mountains, earthquakes, and volcanic activity. For example, the Himalayas formed where the Indian and Eurasian plates pushed together. Convergent boundaries are significant because they shape the Earth's landscape and can lead to dramatic geological events. Understanding these boundaries helps us appreciate the dynamic nature of our planet.