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Internal Forces Shaping the Earth

Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

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Page 1: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

Internal Forces Shaping the Earth

Page 2: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

Tectonic PlatesMagma is like a

conveyer belt (see right):

Heated magma moves up towards the crust, cools and goes downward.

Riding above this system are tectonic plates.

They are large moving pieces that form the earth’s crust.

Page 3: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes
Page 4: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

FaultsWhen two plates meet,

folding/cracking of the rock can happen.

Sometimes rock is not flexible and will crack under the pressure of plate movement.

This fracture in the earth’s crust is called a fault.

Page 5: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

EarthquakesWhat is an earthquake?A violent movement of transitioning plates.

Seismograph: Device used to measure an earthquake.

Focus: Below Ground – Where it Starts

Epicenter: Above Ground – Where we feel it.

Page 6: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

Earthquake DamageHaiti – January 2010

Page 7: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

Types of Earthquake DamageLandslidesDisplacement of landFires (broken gas

lines)Collapsed buildingsTsunamis (see

right):Can travel from

epicenter at 450 mph.

Can produce waves of 50 to 100 feet – or higher.

Page 8: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

VolcanoesMagma, gases and water

from the crust or mantle collect underground.

They eventually pour out of a crack in the earth’s surface.

Magma that reaches the earth’s surface is called lava.

To the right:Mt. St. Helen’s – May 1980

Washington

Page 9: Internal Forces Shaping the Earth. Tectonic Plates Magma is like a conveyer belt (see right): Heated magma moves up towards the crust, cools and goes

The Ring of Fire