Rift zones are areas where tectonic plates are moving apart, leading to geological activity. These zones are often characterized by volcanic activity, earthquakes, and the formation of new crust. They typically occur at divergent boundaries, where the Earth's lithosphere is being pulled apart. One of the most famous rift zones is the East African Rift, which stretches from Ethiopia to Mozambique. This region is notable for its unique landscapes, including rift valleys and volcanic mountains. Rift zones play a crucial role in understanding plate tectonics and the dynamic processes shaping our planet.