Earthquake zones are areas on Earth where seismic activity is more likely to occur. These zones are often located along tectonic plate boundaries, where the Earth's plates interact. The movement of these plates can cause stress to build up, leading to earthquakes when the stress is released. Regions such as the Ring of Fire, which encircles the Pacific Ocean, are particularly prone to earthquakes. Other notable earthquake zones include the Himalayan region and the San Andreas Fault in California. Understanding these zones helps in assessing risks and preparing for potential seismic events.