The earth has changed alot since it existed. For alot of years the earth has been in slow but constant motion. Some forces that change the earth such as wind and water happen on the earth's surface. The other forces that change the earth are volcanic eruptions and earthquakes. Those originate deep in the earth's interior.
The earth is composed of three layers. The inner core is thelayer at the center of the planet. The inner core is very very hot but it is also solid. It is about 4,000 miles below the surface of the earth. Some Scientist believe that the inner core is made of nickel and iron under enormous pressure.
After the inner core is a liquid outer core. The outer core is about 1,400 miles thick. There is band of melted iron and nickel that begins about 1,800 miles below the surface of the earth. The temperatures can go up to 8,500 degrees in the outer core.
The next layer of the earth is the mantle. The mantle is a thick layer of hot dense rock. The mantle is made of silicon, aluminium, iron, magnesium, oxygen, and other elements. The temperature of this layer continuously changes. 80% of the heat is generated from the earth's interior. The outer layer is the crust. It is a rocky shell forming the earth's surface. This layer is very thin and it ranges about 2 miles thick under oceans to about 25 miles thick under mountains. The crust is parted into more than a dozen great slabs of rock called plates that rest on a partially melted layer in the upper mantle.
About 500 million years ago the earth did not look the way it does today. Scientists have a theory that a long time ago all the continents where joined together to form one big continent. That continent was called Pangea. Pangea is the name of the continent that was supously formed by all of the continents we have today a long time ago. The Scientists think the earth was all joined together and then over the years slowly drifted apart. This theory is called the continental drift.
Many scientists say that plates that move slowly around the globe have made earth's largest features. Plate movement is so small that a plate can move about 4 inches in a year. Imagine how many years it took to separate all of the continents! That is probably why we don't feel it. Some plates may crash into eachother while moving, they can also pull apart, or grind and slide past eachother. Plates are contstantly changing the way our planet earth looks. Plates push up against eachother to create volcanoes and even earthquakes. When plates spread apart, magma, wich is another name for molten rock is pushed up from the mantle and ridges are formed. Once the plates bump against one another, one may slide under another forming a trench.

Scientists refer to these changes as plate teconics. Scientists predict that the plate tectonics have been shaping the earth for 2.5 ro 4 billion years. We dont really know what it is that causes plate tectonics but they predict it can be the heat rising from the earth's core.
There is two forces of change, Internal forces of change, and extrernal forces of change. Internal forces of change can include, colliding and spreading plates, Folds and faults, earthquakes, and volcanic eruptions. External forces of change include the weathering, wind erosion, glacial erosion, and water erosion.