Answer:
Tectonic plates are large pieces of the Earth's lithosphere that float on the semi-fluid asthenosphere beneath them. There are several major tectonic plates, and they are continually moving and interacting with one another, which leads to geological phenomena such as earthquakes, volcanoes, and the creation of mountain ranges. Here are some of the major tectonic plates:
- North American Plate
- South American Plate
- Pacific Plate
- Eurasian Plate
- African Plate
- Antarctic Plate
- Indo-Australian Plate
- Indian Plate
- Arabian Plate
- Philippine Sea Plate
- Cocos Plate
- Nazca Plate
- Juan de Fuca Plate
- Caribbean Plate
- Scotia Plate
- Arabian Plate
- Andean Plate
- Juan Fernandez Plate
These plates interact at their boundaries, which are classified into three main types: divergent boundaries (moving away from each other), convergent boundaries (moving towards each other), and transform boundaries (sliding past each other). The interactions at these boundaries are responsible for the dynamic nature of the Earth's crust and the geological features we observe on the surface.
Step-by-step explanation: