tectonic jeopardy!

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Tectonic Jeopardy!

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Tectonic Jeopardy!. Tectonic Jeopardy!. How do scientists know about Earth’s interior?. By measuring seismic waves from earthquakes. Back to Menu. Starting at the surface, what are the layers of the Earth, in order?. Crust Mantle Outer Core Inner Core. Back to Menu. - PowerPoint PPT Presentation

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Page 1: Tectonic Jeopardy!

Tectonic Jeopardy!

Page 2: Tectonic Jeopardy!

Tectonic Jeopardy!Earth’s Layers

Heat Transfer

Continental Drift

Sea-Floor Spreading

Plate Tectonics

10 10 10 10 10

20 20 20 20 20

30 30 30 30 30

40 40 40 40 40

50 50 50 50 50

Page 3: Tectonic Jeopardy!

How do scientists know about Earth’s interior?

Page 4: Tectonic Jeopardy!

By measuring seismic waves from earthquakes.

Back to Menu

Page 5: Tectonic Jeopardy!

Starting at the surface, what are the layers of the

Earth, in order?

Page 6: Tectonic Jeopardy!

1. Crust2. Mantle3. Outer Core4. Inner Core

Back to Menu

Page 7: Tectonic Jeopardy!

Ocean crust is made of _______.

Continental crust is made of _______.

Which is more dense?

Page 8: Tectonic Jeopardy!

Basalt & Granite. Basalt / Ocean crust is

more dense.

Back to Menu

Page 9: Tectonic Jeopardy!

Describe the Mantle. Talk about its thickness

and state of matter.

Page 10: Tectonic Jeopardy!

The Mantle is the layer of molten material beneath the crust. It has a plastic-like state of matter and is the thickest of Earth’s layers.

Back to Menu

Page 11: Tectonic Jeopardy!

What causes Earth’s magnetic field, and why is

this field important?

Page 12: Tectonic Jeopardy!

The spinning and churning of Earth’s liquid iron outer core. The magnetic field protects us

from the Sun’s solar winds.

Final Jeopardy

Back to Menu

Page 13: Tectonic Jeopardy!

Define heat.

Page 14: Tectonic Jeopardy!

The energy transferred from a hotter object to a colder one.

Back to Menu

Page 15: Tectonic Jeopardy!

True or False: there are 4 types of heat transfer.

Name them!

Page 16: Tectonic Jeopardy!

False. There are 3 types of heat transfer: Conduction, Radiation, & Convection.

Back to Menu

Page 17: Tectonic Jeopardy!

Define Radiation heat transfer. Give two examples.

Page 18: Tectonic Jeopardy!

Radiation is heat transfer through space (do not touch directly).

Examples: the Sun & camp fire.

Back to Menu

Page 19: Tectonic Jeopardy!

If the formula for Density is Mass divided by Volume, how can heat

change an object’s density?

Page 20: Tectonic Jeopardy!

Heat = Energy. Giving an object Energy lets the particles move

faster & further away from each other, increasing Volume and

decreasing Density.

Back to Menu

Page 21: Tectonic Jeopardy!

Describe the entire process pictured below in 5 steps,

starting with the stove.

Page 22: Tectonic Jeopardy!

1. Pot is heated by stove - Conduction2. Water is heated by pot - Conduction3. Heated water spreads out (energy),

+Volume & -Density so it rises.4. Spreads out at top of pot, bumps into

other particles, -Energy.5. Less energy means -Volume,

+Density, water sinks.Back to Menu

Final Jeopardy

Page 23: Tectonic Jeopardy!

Which scientist proposed the theory of Continental Drift?

a) Harry Hessb) J. Tuzo Wilsonc) Alfred Wegenerd) Mr. Antonello

Page 24: Tectonic Jeopardy!

a) Harry Hess – Sea-Floor Spreadingb) J. Tuzo Wilson – Plate Tectonicsc) Alfred Wegener – Continental Driftd) Mr. Antonello – Theory of

Awesomeness

Back to Menu

Page 25: Tectonic Jeopardy!

How many pieces of evidence for Continental Drift does the photo below contain? What are they?

Page 26: Tectonic Jeopardy!

Three pieces of evidence. A) The continents fit like puzzle pieces. B)

Mesosaurus fossils were found on both continents. C) Africa & S. America have

the same folded mountains.

Back to Menu

Page 27: Tectonic Jeopardy!

What is Wegener’s Theory of Continental Drift and

why was it rejected?

Page 28: Tectonic Jeopardy!

The continents were once a supercontinent called Pangea, and are slowly moving, even

now. Wegener had no evidence to explain what caused the

continents to move.

Back to Menu

Page 29: Tectonic Jeopardy!

While researching in Antarctica, you discover the fossil remains

of the tropical plant Glossopteris. This plant is native to Australia. What 2 things does this tell you

about Antarctica?

Page 30: Tectonic Jeopardy!

•Antarctica and Australia were at one time connected (since the plant can not migrate across an ocean).

•Antarctica once had a tropical climate.

Back to Menu

Page 31: Tectonic Jeopardy!

What do the reversing magnetic stripes on the ocean floor reveal?

Use this information to explain the difference between “magnetic” North and “geographic” North.

Page 32: Tectonic Jeopardy!

Stripes tell us that magnetic poles reverse every 300,000 years.

Geographic North is always at 90⁰ North. Magnetic North is where the

magnetic field originates.

Back to Menu

Final Jeopardy

Page 33: Tectonic Jeopardy!

Why is the theory of Sea-Floor Spreading important?

Page 34: Tectonic Jeopardy!

It provides the final piece of evidence – the mechanism –

for Continental Drift.

Har

ry H

ess

Back to Menu

Page 35: Tectonic Jeopardy!

Describe the Mid-Ocean Ridge and why it’s important.

Page 36: Tectonic Jeopardy!

Underwater mountain range where magma cools to form

new crust. Stretches across all the oceans of the world,

driving sea floor spreading.Back to Menu

Page 37: Tectonic Jeopardy!

Where is old crust destroyed and what is it called when the crust sinks

back underneath, into the mantle?

Page 38: Tectonic Jeopardy!

The crust is destroyed at deep-sea Trenches in a process

known as Subduction.

Back to Menu

Page 39: Tectonic Jeopardy!

Studying the crust at the Mid-Ocean ridge reveals 3 pieces

of evidence for Sea-floor Spreading. What are they?

Page 40: Tectonic Jeopardy!

1. Formation of “pillow” basalts2. Reversing magnetic stripes3. Relative age dating of core

samples

Back to Menu

Page 41: Tectonic Jeopardy!

Describe the process of Sea-floor Spreading and why it

is like a conveyor belt.

Page 42: Tectonic Jeopardy!

1. Magma rises at the Mid-Ocean Ridge2. Entering the ocean, magma cools into Basalt3. New magma rises and cools, spreading the

rock out4. Old crust subducts under less dense crust

and melts5. The cycle repeats!

Back to Menu

Final Jeopardy

Page 43: Tectonic Jeopardy!

Plate Tectonics states that plates in Earth’s lithosphere move by

floating on the mantle. What are the 2 types of plates?

Page 44: Tectonic Jeopardy!

Back to Menu

Plates can be classified as either Continental or Oceanic crust.

Page 45: Tectonic Jeopardy!

Plate Tectonics combines the theories of Alfred Wegener & Harry Hess with a method of heat transfer.

Name the theories and method.

Page 46: Tectonic Jeopardy!

Back to Menu

Continental Drift & Sea-Floor Spreading and the heat transfer method of

Convection.

Page 47: Tectonic Jeopardy!

Describe the 3 types of boundaries symbolized by

the following motions.

Page 48: Tectonic Jeopardy!

Convergent (moving towards each other), Divergent

(moving away), and Transform boundaries (sliding past one

another).Back to Menu

Page 49: Tectonic Jeopardy!

Locate & name the types of plate boundaries (and crust) in the picture below. What features are at these locations, & what is the missing

boundary?

Page 50: Tectonic Jeopardy!

1) Convergent: Oceanic/Oceanic crust Subduction zone

2) Divergent: Mid-Ocean Ridge3) Transform Boundary (not shown)

1

2

Back to Menu

Page 51: Tectonic Jeopardy!

The Purple line on the map represents the Mid-Ocean Ridge. What type of features do you think exist along the Ring of Fire and what causes them?

Page 52: Tectonic Jeopardy!

The Ring of Fire marks the location of volcanic island arcs as a result of Subduction

of ocean crust at deep-sea trenches.

Back to Menu

Final Jeopardy

Page 53: Tectonic Jeopardy!

You have 60 seconds to name as many plates as you can.

Spelling counts!603010

Page 54: Tectonic Jeopardy!

STOP

Page 55: Tectonic Jeopardy!

Back to Menu