Plate Tectonics: A Unified Theory for Change of the Earth's Surface

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  • 0:07 Background on the Ground
  • 0:32 Definition of Plate Tectonics
  • 1:39 Causes of Plate Movement
  • 4:10 More Causes of Plate Movement
  • 5:21 Lesson Summary
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Lesson Transcript
Instructor: Peter Jaeger

Pete currently teaches middle school Science, college level introductory Science, and has a master's degree in Environmental Education.

After many years of trying to solve the mystery of the moving continents, enough data and evidence was collected to develop a unifying theory of how the surface of the earth changes. It's called plate tectonics.

Background on the Ground

Have you ever been babysitting and decided it would be fun to play Nerf Gun Wars with the child, only to have a misaimed dart hit a rare plate from Israel and fall on the brick fireplace hearth, breaking into many pieces? Not that I have ever done this or anything... The only good thing is that the pieces of the plate fit together nicely and allowed a stressed-out babysitter to glue it back together. But what does this have to do with the earth?

Definition of Plate Tectonics

In the middle of the 20th century, just a few decades ago, a new theory about the earth and how it changed was proposed, and the mystery of drifting continents was solved. Geologists, scientists who study the earth, now had an all-encompassing theory to tie all of its observations and data together. This new theory of large-scale change on the earth is known as plate tectonics.

Plate tectonics is the theory that the surface of the earth is broken into larger pieces of crust called plates that ride along on a softer layer of the earth, known as the asthenosphere, which is the upper part of the mantle.

A diagram of the plates moving along the surface of the earth
Plate Tectonics Diagram

Each plate's thickness depends on the type of crust it is made of and the location of the plate. Continental plates can be up to 150 km thick, whereas oceanic plates usually average about 5-10 km thick. Also, plate boundaries are not the same as continental boundaries, as the edges of the plates can be underwater. For example, the North American plate extends from the middle of the Atlantic Ocean to the west coast of North America.

Causes of Plate Movement

So, the big question that remains is: how do the continents move? The answer is related to the layers of the earth and how they interact with each other. So, first, we need to understand how the properties determine the layers of the earth. Let's use an apple as an example. An apple has 3 main layers to it - the peel, the fruit, and the core.

The crust, or lithosphere, is the hard outer layer of the earth and would be the peel of our apple. This is the part where we reside and about which we have the most data.

The mantle is the middle layer of the earth, consisting mostly of oxygen, silicon, magnesium, and iron. This would be represented by the fruit of the apple between the peel and the core.

The core is the center of the earth that is represented by the core of the apple. The earth's core consists of two parts - a solid center about 1200 km thick, surrounded by a liquid layer consisting of iron and nickel that is about 2300 km thick.

The main theory of plate movement states that heat from the core causes convection cells in the mantle that move the plates as they ride on the mantle. The main source of heat that drives this process is thought to be the radioactive decay of uranium and other elements that give up their energy as heat as they break down. All this heat softens the rock enough that it will begin to flow. But how does this happen? When you put a pot of water on the stove to boil, the water nearest the stove heats up faster than the water on the surface of the pot.

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