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The Dynamic Earth

Layers of the earth

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Page 1: Layers of the earth

The DynamicEarth

Page 2: Layers of the earth

Earth Facts:• circumference around the poles is 40,007 km• circumference around the equator is

40,074 km• Earth is NOT a perfect sphere… it is a oblate

spheroid, a slightly flattened sphere

• Earth’s mass is approximately 6.0 x 1024 kg

• Earth’s average diameter is 12,735 km• Difference between the height of the tallest

mountains and the depth of the deepest ocean trenches is only 20 km

Page 3: Layers of the earth

Layers above the Earth• Hydrosphere: all of the water that covers the Earth

• Atmosphere: blanket of gases that surround the Earth; 78% Nitrogen; 21% Oxygen; The rest (1%) is combination of argon, carbon dioxide

helium and water

• Atmosphere is divided up into 5 regions

Page 4: Layers of the earth

Layers inside the Earth

Page 5: Layers of the earth

Layers inside the EarthCrust: The thin, solid outermost zone

of the Earth

• Makes up only 1% of Earth’s mass

• Oceanic Crust: crust under the oceans• Only 5km to 10km thick

• Continental Crust: crust that makes up thecontinents

• 15km to 80km thick• Thickest beneath high mountain ranges

Page 6: Layers of the earth

Layers inside the EarthMantle: Zone of rock nearly 2,900km thick

Makes up almost 67% of Earth’s massLayers of the Mantle:

Lithosphere: uppermost part of the mantle and the crust above it; cool and brittle. The boundary between the crust and mantle is referred to as the MOHO

Asthenosphere: solid rock with the ability to flow due to heat and pressure (plasticity)

Mesosphere: increasingly dense and solid rock layer (aka “Lower Mantle”)

Page 7: Layers of the earth

Layers inside the EarthCore: Center of the earth made up mostly

of iron

Outer core: dense liquid layer about 2,250km thick

Inner core: dense solid layer about 1,228km thick

Together the inner and outer core make up about 33.3 % of Earth’s mass

Page 8: Layers of the earth
Page 9: Layers of the earth

P and S Waves

Liquids and Solids

How Do We Know?

Seismic Wave Studies

We will talk more about seismic waves when we study Earthquakes!

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The Earth As A Magnet

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The Earth’s Gravity

Sir Isaac Newton’s Law of Gravitation: The force of attraction between two objects depends on the mass of the objects and the distance between them.

Weight: A measure of the strength of the pull of gravity on an object

Weight and Mass are NOT the same….

EUREKA !

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Page 14: Layers of the earth

The Earth is not perfectly round it is slightly wider around the Equator

So… a person standing at the Equator is farther from the center of the Earth than a person standing at the North Pole.

The person at the Equator will weigh less because he is farther from the center of the Earth.

Page 15: Layers of the earth

The Movements of the Earth

How fast is the Earth spinning?

0.5 km/sec Called: ROTATION

Time it takes for Earth to ROTATE once on it’s axis: 24 hours

How fast is the Earth revolving around the Sun?

30 km/sec Called: REVOLUTION

Time it takes for Earth to REVOLVE once around the sun: 365.24 days (1 year)

How far is the Earth from the sun when it is CLOSEST TO IT?

147,100,000km Called:Perihelion

How far is the Earth from the sun when it is FARTHEST FROM IT?

152,600,000km Called:Aphelion

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Page 17: Layers of the earth

The Earth is tilted on it’s axis

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The Reasons for the Seasons

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