Earth s structure
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Earth’s Structure. The layers of Earth. Earth is divided into 3 layers based on chemical composition. Core: Dense metallic center, made up of mainly metal iron. Mantle: Liquid middle layer made up of silicon, oxygen and magnesium.

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Earth’s Structure

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Earth s structure

Earth’s Structure


The layers of earth

The layers of Earth

  • Earth is divided into 3 layers based on chemical composition.

  • Core: Dense metallic center, made up of mainly metal iron.

  • Mantle: Liquid middle layer made up of silicon, oxygen and magnesium.

  • Crust: The solid outer layer made up of silicon, oxygen and aluminum.


Continental and oceanic crust

There are two types of crust:

Continental: is thicker

Oceanic: is thinner and heavier.

Compared to the other layers, both types of crust are rocky, thin and fractured.

Continental and Oceanic Crust


The physical structure of earth

Earth is divided into five layers based on physical properties.

Lithosphere

Asthenosphere

Mesosphere

Outer core

Inner core

The Physical Structure of Earth


Lithosphere

Lithosphere

  • Lithosphere:

    cool rigid layer, made up of the crust and upper layer of the mantle.

    Lithosphere is divided into pieces called tectonic plates.


Asthenosphere

Asthenosphere

2. Asthenosphere

  • Below the lithosphere.

  • Made up of slow flowing solid rock.

  • The moving rock allows for tectonic plates to move.


Physical structure cont

3.Mesosphere: Slow flowing layer beneath the Asthenosphere

4.Outer core: Layer of liquid Iron and Nickel.

5.Inner core: Solid iron and nickel, temperature is estimated to be between 4000ºC to 5000ºC

Physical Structure cont.


Mapping earth s interior

How can we know so much about Earth’s interior if no one has ever drilled through the crust?

Earthquakes produce seismic waves, and travel thru materials at different speeds.

Scientists use these waves to determine the density of each of Earth's layers

Mapping Earth’s Interior


Continental drift

In the 1900’s,Scientist Alfred Wagner, viewed the continents as puzzle pieces.

Had a hypothesis that our continents used to be one large continent.

He named his hypothesis the Continental Drift Theory.

Continental Drift


Evidence for continental drift

Evidence for Continental Drift

  • Fossils of same plant can be found on continents that are far from each other.

  • Location of mountain ranges with similar rocks show a pattern.


The breakup of pangaea

A single continent Pangaea (many thousands of years ago).

Split into two continents – Laurasia and Gondwana (thousands of years ago).

Split into today's continents.

Continents sometimes collided, forming mountain ranges and volcanoes.

The Breakup of Pangaea


Sea floor spreading

Sea-Floor Spreading.

  • When Wagner introduced his hypothesis, many scientists did not accept it because the strength needed to move Earth’s crust seemed impossible.

  • In the 1960’s Scientist studying the ocean floor discovered identical patterns of magnetism on both sides of the mid ocean ridge.

  • This was proof that continental drift was possible.


Sea floor spreading cont

Sea-Floor Spreading cont.

  • At a mid-ocean ridge, magma rises through fractures in the sea floor.

  • As the magma cools it forms new sea floor.

  • As this continues to happen, new floor is made and older floor is pushed away from the fracture.

  • Sea-floor spreading was proven to cause continents to move.


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