The theory that Earth's surface is composed of several rock plates that fit together like the pieces of a puzzle is called plate tectonics.
The theory that describes how Earth's surface is made up of several rock plates that fit together is called plate tectonics. Plate tectonics is the scientific concept that explains the movement and interaction of these large rock plates, which make up the Earth's outer layer or lithosphere. These plates are constantly shifting and moving, causing various geological phenomena such as earthquakes, volcanic activity, mountain formation, and the creation of oceanic trenches. The theory of plate tectonics is supported by evidence from seismic activity, the distribution of earthquakes and volcanoes, the shape of continents, and the study of oceanic ridges and trenches. It is an important principle in understanding the dynamic nature of our planet.
