Inside the Earth Composition What it is made

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Inside the Earth

Inside the Earth

Composition (What it is made of) • Crust • Mantle • Core

Composition (What it is made of) • Crust • Mantle • Core

Physical Structure of the Earth (5 Layers) • Lithosphere- rigid outer layer (crust) •

Physical Structure of the Earth (5 Layers) • Lithosphere- rigid outer layer (crust) • Asthenosphere- solid rock that flows slowly (like hot asphalt) • Mesosphere- middle layer • Outer Core- liquid layer • Inner Core- solid, very dense

The Crust • Outer layer • 5 -100 km thick • 2 types of

The Crust • Outer layer • 5 -100 km thick • 2 types of crust – Oceanic (very dense, made of basalt) – Continental (less dense, made of granite)

2 Types of Plates • Ocean plates - plates below the oceans • Continental

2 Types of Plates • Ocean plates - plates below the oceans • Continental plates - plates below the continents

Oceanic and Continental Crust

Oceanic and Continental Crust

The Mantle • Middle layer • Very thick layer

The Mantle • Middle layer • Very thick layer

The Core • Made mostly of iron • 1/3 of the earth’s mass •

The Core • Made mostly of iron • 1/3 of the earth’s mass • Very hot

Earth’s Layers • How are the earth’s layers similar to an egg? • Shell=crust

Earth’s Layers • How are the earth’s layers similar to an egg? • Shell=crust • Egg white=mantle • Yolk=core

Physical Structure of the Earth (5 Layers) • Lithosphere- rigid outer layer (crust) •

Physical Structure of the Earth (5 Layers) • Lithosphere- rigid outer layer (crust) • Asthenosphere- solid rock that flows slowly (like hot asphalt) • Mesosphere- middle layer • Outer Core- liquid layer • Inner Core- solid, very dense

What is the Lithosphere? • The crust and part of the upper mantle =

What is the Lithosphere? • The crust and part of the upper mantle = lithosphere – 100 km thick –Less dense than the material below it so it “floats”

What is the Asthenoshere? • The plastic layer below the lithosphere = asthenosphere •

What is the Asthenoshere? • The plastic layer below the lithosphere = asthenosphere • The plates of the lithosphere float on the asthenosphere

Tectonic Plates • Earth’s crust is broken into about 19 pieces • These plates

Tectonic Plates • Earth’s crust is broken into about 19 pieces • These plates move on top of the asthenosphere

Theory of Plate Tectonics Plate Boundaries Causes of Plate Tectonics

Theory of Plate Tectonics Plate Boundaries Causes of Plate Tectonics

Plate Tectonics

Plate Tectonics

What is Plate Tectonics • The Earth’s crust and upper mantle are broken into

What is Plate Tectonics • The Earth’s crust and upper mantle are broken into sections called plates • Plates move around on top of the mantle like rafts

Questions. . . • What is theory of plate tectonics? • What is the

Questions. . . • What is theory of plate tectonics? • What is the lithosphere? • What is the asthenosphere? • What is the connection between the two? • What are the two types of plates?

Plate Boundaries

Plate Boundaries

Types • Divergent – Rifting • Convergent – Sub-duction • Transform Fault Boundaries –

Types • Divergent – Rifting • Convergent – Sub-duction • Transform Fault Boundaries – (Sliding)

Divergent Boundaries • Boundary between two plates that are moving apart or rifting •

Divergent Boundaries • Boundary between two plates that are moving apart or rifting • RIFTING causes SEAFLOOR SPREADING

Divergent Plate Movement: Seafloor Spreading • the movement of two oceanic plates away from

Divergent Plate Movement: Seafloor Spreading • the movement of two oceanic plates away from each other (at a divergent plate boundary), which results in the formation of new oceanic crust (from magma that comes from within the Earth's mantle) along a a mid-ocean ridge. • Ocean floor spreading was first suggested by Harry Hess and Robert Dietz in the 1960's.

Features of Divergent Boundaries • Mid-ocean ridges • rift valleys • fissure volcanoes

Features of Divergent Boundaries • Mid-ocean ridges • rift valleys • fissure volcanoes

Convergent Boundaries • Boundaries between two plates that are colliding • There are 3

Convergent Boundaries • Boundaries between two plates that are colliding • There are 3 types…

Type 1 • Ocean plate colliding with a less dense continental plate • Subduction

Type 1 • Ocean plate colliding with a less dense continental plate • Subduction Zone: where the less dense plate slides under the more dense plate • VOLCANOES occur at subduction zones

Andes Mountains, South America

Andes Mountains, South America

Type 2 • Ocean plate colliding with another ocean plate • The less dense

Type 2 • Ocean plate colliding with another ocean plate • The less dense plate slides under the more dense plate creating a subduction zone called a TRENCH

 • Two Oceanic Plates - When two oceanic plates collide, one may be

• Two Oceanic Plates - When two oceanic plates collide, one may be pushed under the other and magma from the mantle rises, forming volcanoes in the vicinity

 • Two Oceanic Plates - When two oceanic plates collide, one may be

• Two Oceanic Plates - When two oceanic plates collide, one may be pushed under the other and magma from the mantle rises, forming volcanoes in the vicinity

Aleutian Islands, Alaska

Aleutian Islands, Alaska

Type 3 • A continental plate colliding with another continental plate • Have Collision

Type 3 • A continental plate colliding with another continental plate • Have Collision Zones: –a place where folded and thrust faulted mountains form.

 • Two Continental Plates - When two continental plates collide, mountain ranges are

• Two Continental Plates - When two continental plates collide, mountain ranges are created as the colliding crust is compressed and pushed upwards.

Transform Fault Boundaries • Boundary between two plates that are sliding past each other

Transform Fault Boundaries • Boundary between two plates that are sliding past each other • EARTHQUAKES along faults

 • When two plates move sideways against each other (at a transform plate

• When two plates move sideways against each other (at a transform plate boundary), there is a tremendous amount of friction which makes the movement jerky. • The plates slip, then stick as the friction and pressure build up to incredible levels. When the pressure is released suddenly, and the plates suddenly jerk apart, this is an earthquake.

San Andreas Fault, CA

San Andreas Fault, CA

Questions. . . • What are the types of boundaries? • What direction do

Questions. . . • What are the types of boundaries? • What direction do plates go for each? • Which boundary has a subduction zone…what occurs at a subduction zone?

Causes of Plate Tectonics

Causes of Plate Tectonics

Convection Currents • Hot magma in the Earth moves toward the surface, cools, then

Convection Currents • Hot magma in the Earth moves toward the surface, cools, then sinks again. • Creating convection currents beneath the plates that cause the plates to move.

Questions. . . • What causes plates to move? • How is a convection

Questions. . . • What causes plates to move? • How is a convection current formed?