How do continents move (how does continental drift work?)?
The Earth’s crust is constantly moving, both vertically and horizontally, at rates of up to several inches a year. A widely-held theory that explains these movements is called “plate tectonics.” It was developed in the mid 1960s by geophysicists. The term “plate” refers to large rigid blocks of the Earth’s surface which appear to move as a unit. These plates may include both oceans and continents. When the plates move, the continents and ocean floor above them move as well. Continential Drift occurs when the continents change position in relation to each other. While plate tectonics is a relativily new idea, scientists have been gathering data in support of the Continental Drift theory for a very long time. In 1912, Alfred Wegener and Frank Taylor first proposed the theory that 200 million years ago the Earth had only one giant continent, from which today’s continents broke apart and drifted into their current locations. Wegener used the fit of the continents, the distribution of fossi
