The rotator theory is a scientific explanation for how the Earth's continents have moved over time. It suggests that the Earth's crust is divided into large plates that slowly move and shift due to convection currents in the mantle.
The rotator theory suggests that the Earth's crust is broken into several large plates that float on the underlying mantle. These plates are constantly moving and colliding with one another, causing changes in the Earth's surface over time.
The rotator theory helps us understand how the Earth has changed over millions of years and how the continents have shifted and formed. It also helps us predict future changes in the Earth's surface and how they may impact our planet.
There is a wealth of evidence that supports the rotator theory, including the matching shapes of coastlines on different continents, similarities in rock formations and fossils found on different continents, and the presence of similar mountain ranges on different continents.
The rotator theory involves complex geological processes and can be difficult to visualize and understand. It also requires a basic understanding of plate tectonics and geology. However, with the help of visual aids and explanations, it can be easier to grasp and appreciate the significance of this theory.