There are seven major tectonic plates on Earth. These plates are: the African Plate, the North American Plate, the Eurasian Plate, the South American Plate, the Indo-Australian Plate, the Pacific Plate, and the Antarctic Plate.
Each of these plates has its own unique characteristics and plays a significant role in the geological processes that shape our planet. The movement and interaction of these tectonic plates can cause earthquakes, volcanic eruptions, and the formation of mountain ranges. Understanding the dynamics of these plates is crucial for comprehending the Earth’s geological history and predicting its future changes.