The Layers of the Earth © Copyright 2006.  M. J. Krech. All rights reserved.

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The Layers of the Earth © Copyright 2006.  M. J. Krech. All rights reserved.

The Four Main Layers The four main layers are the 1.___________________ 2.___________________ 3. ___________________ 4. ____________________

Describe the temperature change that takes place as the depth inside Earth increases. Rock near the surface would be cool About 20 meters down the rock gets warmer For every 40 meters that descends a temperature increases 1°Celsius.

The force pushing on a surface or area is known as _______. Pressure

Figure 4: Comparing & Contrasting – How is the water in the swimming pool similar to Earth’s interior? How is it different? The deeper the water in the pool, the greater the pressure, just as pressure is greater the deeper you go beneath the surface of Earth The water in the pool does not have layers

Why does the pressure increase as you go deeper into Earth? The pressure increases as you go deeper inside the earth because amount and weight of the rock increases

The Crust The Earth's Crust is the layer that you walk on and is like the skin of an apple. It is very thin in comparison to the other three layers. The crust is only about 3-5 miles (8 kilometers) thick under the oceans which is called the oceanic crust and about 25 miles (32 kilometers) thick under the continents which is called the continental crust.

And what type of crust would you like with your Earth? There are two types of crust Baker 7th grade science 2003-2004

The Crust The crust is composed of two main rocks. The continental crust is mostly granite. The oceanic crust is basalt. Basalt is much denser than the granite. Because of this the less dense continents ride on the denser oceanic plates.

Figure 5: Comparing & Contrasting-Which rock looks as if it’s made up of one material? of Several materials? The basalt looks like it’s made of one material The granite looks like it’s made of several materials.

The Mantle The Mantle is the largest layer of the Earth.

The Lithosphere The crust and the upper layer of the mantle together make up a zone of rigid, brittle rock called the Lithosphere. The Greek prefix litho means “stone.”

The Lithospheric Plates The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, semi-rigid asthenosphere. The Greek prefix astheno means “weak”

The middle mantle is composed of very hot dense rock that flows like asphalt under a heavy weight. It isn’t really weak. The movement of the middle mantle (asthenosphere) is the reason that the crustal plates of the Earth move.

Convection Currents The middle mantle flows" because of convection currents. Convection currents are caused by the very hot material at the deepest part of the mantle rising, then cooling and sinking again --repeating this cycle over and over again.

Convection Currents The next time you heat anything like soup or water in a pan you can watch the convection currents move in the liquid. When the convection currents flow in the asthenosphere they also move the crust. The crust gets a free ride with these currents, like the cork in this illustration. Safety Caution: Don’t get your face too close to the boiling water!

The Outer Core The outer core of the Earth is like a ball of very hot metals. The outer core is so hot that the metals in it are all in the liquid state. The outer core is composed of the melted metals of nickel and iron.

The Inner Core The inner core of the Earth has temperatures and pressures so great that the metals are squeezed together and are not able to move about like a liquid, but are forced to vibrate in place like a solid.