A continental plate is a large section of the Earth's crust that forms the continents. These plates are part of the larger theory of plate tectonics, which explains how the Earth's surface is divided into several pieces that move and interact. Continental plates are generally thicker and less dense than oceanic plates, allowing them to rise above sea level and create landmasses. The movement of continental plates can lead to geological events such as earthquakes and the formation of mountains. For example, the collision of the Indian Plate with the Eurasian Plate created the Himalayas. Understanding continental plates helps scientists study the Earth's history and predict future geological changes.