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Earth’s Layers S6E5.a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition.

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Presentation on theme: "Earth’s Layers S6E5.a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition."— Presentation transcript:

1 Earth’s Layers S6E5.a. Compare and contrast the Earth’s crust, mantle, and core including temperature, density, and composition.

2 We Have 2 ways of Dividing Earth’s Layers:

3 Earth is divided into 3 compositional layers:
1. Crust 2. Mantle 3. Core

4 CRUST: Location: outermost layer Temperature: 0°C to 1,000°C Thickness: 5km to 100 km Composition: Oxygen Silicon Aluminum

5 2 TYPES OF CRUST: Oceanic crust is very thin & dense. Continental crust is thick but less dense.

6

7 MANTLE: Location: below the crust. Temperature: 1,000°C to 3,700°C Thickness: 2,900 km Composition: Contains most of Earth’s mass Solid and molten rock

8 CORE: Location: Earth’s center Temperature: 3,700°C - 7,000°C Thickness: 3,500 km Composition: mostly iron, some nickel Divided into 2 layers: Outer Core Inner Core

9 Earth is divided into 5 physical layers:
1. Lithosphere 2. Asthenosphere 3. Mesosphere 4. Outer Core 5. Inner Core

10 LITHOSPHERE: This is the “crunchy” layer of the Earth. Location: crust and upper mantle Thickness: kilometers Lithosphere = tectonic plates

11 ASTHENOSPHERE: Location: the middle mantle, below the lithosphere Soft – can bend like plastic Lithosphere floats on this layer (like jello) Thickness: 250 km

12 MESOSPHERE: Location: the strong, lower part of the mantle Thickness: 2,550 kilometers

13 Outer Core: Thickness: 2,300 km
Composition: liquid iron (with some nickel) Thickness: 2,300 km

14 Inner Core: Composition: solid iron and a little nickel. Thickness: 1,220 km thick. Solid because of increased pressure.

15 Lithosphere Asthenosphere Mesosphere CRUST MANTLE OUTER CORE
INNER CORE

16 Density, Pressure, and Temperature
Moving towards the center of the earth: Density increases Pressure increases Temperature increases

17 How do we know there are layers of the earth?
Earthquakes emit different kinds of seismic waves that can travel through different substances and at different speeds Scientists used these waves to determine the layers based on the speed and movement of the layers!

18 The MOHO The Moho is the boundary where the crust meets the mantle It was discovered in 1909 by Andrija Mohorovicic It was discovered because at this point density changes and seismic waves change direction

19 The MOHO

20 Why does Earth have a magnetic field?

21 Why does Earth have a magnetic field?
Earth’s magnetic field is a result of the movement of iron in the Earth’s liquid inner core.

22 In Review: What are the 3 main layers of the Earth? Crust, Mantle, Core Which layer is the least dense? Crust Which core layer is solid iron and nickel? Inner core What is the name given to the “crunchy” layer of the crust and uppermost part of the mantle? Lithosphere 5. The motion in this layer is the reason Earth has a magnetic field. Outer core


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