Convergent boundaries occur where two tectonic plates move toward each other. This interaction can lead to one plate being forced beneath another in a process called subduction. As a result, these boundaries are often associated with geological features like mountain ranges, deep ocean trenches, and increased seismic activity. At convergent boundaries, the collision of plates can create intense pressure, leading to earthquakes and volcanic activity. For example, the Himalayas formed when the Indian Plate collided with the Eurasian Plate. Understanding these boundaries is crucial for assessing geological hazards and the Earth's dynamic processes.