earth’s interior notes - weebly

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Earth’s Interior Notes

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Page 1: Earth’s Interior Notes - Weebly

Earth’s Interior Notes

Page 2: Earth’s Interior Notes - Weebly

The Four Layers

• Crust

• Mantle

• Outer Core

• Inner Core

• Based on

different

densities

Page 3: Earth’s Interior Notes - Weebly

Layer Composition Thickness State of matter

Crust Continental – Granite

Oceanic – Basalt

(lowest density)

Continental- 25 miles

Oceanic – 3-5 miles

(Thinnest Layer)

Solid rocks

Mantle Magma (liquid metals

with chunks of rocks)

Largest Layer

1,800 miles

solid rocks &

Liquid

Outer Core Nickel & Iron 1,400 miles Liquid

Inner Core Mostly Iron

(highest density)

760 miles Solid

Page 4: Earth’s Interior Notes - Weebly

The Crust

The Earth's Crust is

like the skin of an

apple.

Continental crusts are

thicker than oceanic

crusts

Page 5: Earth’s Interior Notes - Weebly

The Mantle

The Mantle is the largest

layer of the Earth.

The movement of the middle mantle (asthenosphere) is the reason that the crustal plates of the Earth move.

Page 6: Earth’s Interior Notes - Weebly

The Outer Core

The 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.

Page 7: Earth’s Interior Notes - Weebly

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, so its solid.

Composed of iron

and nickel.

Page 8: Earth’s Interior Notes - Weebly

The Lithosphere

• Crust and upper mantle

• Rigid, brittle rock

• Moves together in plate tectonics

Page 9: Earth’s Interior Notes - Weebly

The Asthenosphere

• layer of middle mantle where

convection happens.

•Semi-rigid.

•Lithosphere Plates move due the

convection in the Asthenoshpere.

Page 10: Earth’s Interior Notes - Weebly

The Lithospheric Plates

The crust of the Earth is broken into many pieces called

plates. The plates "float" on the asthenosphere.

Page 11: Earth’s Interior Notes - Weebly

•Source of Earth’s interior heat started with the kinetic

energy of the collisions of metal, rock and ice fragments

converted into heat energy as the fragments impacted

with the growing Earth.

•As the Earth become compact, the gravitational energy

was converted into heat.

•The third source of heat is the decay of radioactive

elements that change to more stable forms, releasing heat

in the process. Radioactivity is one of the main sources of

heat inside the Earth.

Page 12: Earth’s Interior Notes - Weebly

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.

Page 13: Earth’s Interior Notes - Weebly

Convection• Occurs because of difference of

temperatures of the materials.

• Occurs because heated material becomes

Less dense and rises

• While materials cooling down become more

dense and sink.

**** Will

See this again in

Oceans and

Atmosphere

Page 14: Earth’s Interior Notes - Weebly

Moho Boundary

• Separates the crust from the upper mantle.

Page 15: Earth’s Interior Notes - Weebly

Moho, or Mohorovičić

discontinuity, boundary

between the Earth’s crust

and its mantle. The Moho

lies at a depth of about 22

mi (35 km) below

continents and about 4.5 mi

(7 km) beneath the oceanic

crust. Modern instruments

have determined that the

velocity of seismic waves

increases rapidly at this

boundary. The Moho was

named for Andrija

Mohorovičić.

Page 16: Earth’s Interior Notes - Weebly
Page 17: Earth’s Interior Notes - Weebly

Seismic Waves• waves of energy that travel through

the Earth, and are a result of an

earthquake, explosion, or a volcano.

• We know about the layers of the

Earth because of theses waves.

Page 18: Earth’s Interior Notes - Weebly

2 types of waves:

1. P-wave - primary

wave, can travel

through liquids

and solids

2. S-wave - secondary

wave, Can only travel

through liquids

Page 19: Earth’s Interior Notes - Weebly
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Page 21: Earth’s Interior Notes - Weebly

Main regions of Earth’s

interior:

1. Inner Core

2. Outer Core

3. Mantle

4. Crust

5. Magnetosphere

Page 22: Earth’s Interior Notes - Weebly

MAGNETOSPHERE

Region around Earth that

is influenced by Earth’s

magnetic field

Page 23: Earth’s Interior Notes - Weebly

- Rapid Rotation

- Metal (electrical conductor)

• magnetic field generation requires:

- Liquid Core

Page 24: Earth’s Interior Notes - Weebly

Will a compass lead you directly

to the geographic North Pole???

Page 25: Earth’s Interior Notes - Weebly

Magnetic Variation

A compass does not point directly to

the north pole but to the magnetic

north pole. This difference is called

magnetic variation.

Page 26: Earth’s Interior Notes - Weebly

Van Allen Belts

Two regions surrounding Earth

that capture high-energy

charged particles

**Particles originate in solar wind and

flares

Page 27: Earth’s Interior Notes - Weebly

a) outer belt - contains mostly

lighter electrons

b) inner belt contains

heavier protons

Page 28: Earth’s Interior Notes - Weebly

Charged particles then

collide with air molecules,

get excited, then…

Produce spectacular light show

called Auroras “Northern

Lights”

Page 29: Earth’s Interior Notes - Weebly

“Northern Lights”

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