Layers of the Earth Learning Objectives



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Bog'liq
Shavkatov Shaxboz Shavkatovich


Lithosphere. Soil degradation. Industrial household waste and their processing.
Prepared by: Shavkatov Sh. Sh.

Layers of the Earth

Learning Objectives

  • I can describe the structure of the Earth’s interior.
  • I can relate the structure of the Earth’s interior to plate tectonics.
  • I can explain the convection currents that power plate movement.

Essential Question: How are layers of the Earth different from one another?

Standard:

S6E5a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition.

The Earth is made up of 3 main layers:

Crust

Mantle

Core

Think of the layers of the Earth like the layers of a cake.

Use the Layers of the Earth Foldable to take notes

Crust


Ocean
Land
Oceanic Crust
Continental Crust

The Earth’s crust is like the skin of an apple.

Crust

  • Thinnest layer of the Earth
  • Made up of large amounts of silicon and aluminum
  • Composed of plates on which the continents and oceans rest. These “ride” over molten mantle.
  • Crust is part of the lithosphere.
  • Two types of Crust: Oceanic and Continental

Ocean
Land
Oceanic Crust
Continental Crust
Oceanic Crust
Continental Crust

Continental vs. Oceanic Crust


Category

Continental

Oceanic

Rock Type

Granite

Basalt

Thickness

5 – 70km (Thicker)

3 – 8 km (Thinner)

State

Solid

Solid

Crust Age

4 billion years old or Older

180 million years old or Younger

Density

Less Dense

More Dense

Element Composition

Oxygen, Sodium, Silicon, Aluminum, Potassium

Iron, Magnesium, Calcium


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