SlideShare une entreprise Scribd logo
1  sur  7
Télécharger pour lire hors ligne
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page1
Vocabulary
 Plate tectonics (511) – Earth’s surface is made of rigid slabs of rock, or plates, that move
with respect to each other
 Lithosphere (512) – the cold and rigid outermost rock layer
 Divergent plate boundary (513) – forms where two plates separate
 Transform plate boundary (513) – Forms where two plates slide past each other
 Convergent Plate Boundary (513) – form where two plates collide
 Subduction (513) – A process in which the denser plate sinks below the more buoyant
plate
 Convection (516) – the circulation of material caused by differences in temperature
 Ridge Push (517) – the forces that causes rising mantle material at mid-ocean ridges that
creates the potential for plates to move away from the ridges
 Slab Pull (517) – As a slab sinks, it pulls on the rest of the plate with this force
The Plate Tectonic Theory
 Earth’s crust is constantly being __________________ and destroyed
 The ______________________ of plate tectonics states that Earth’s surface is made of rigid
slabs of rock, or plates, that move with respect to each other
 Each plate moves over Earth’s hot and ______________________________ mantle
o The term _________________________ describes the forces that shape Earth’s
surface and the resulting rock structures
o Plate tectonics is used to explain ______________________and volcanic eruptions
Tectonic Plates
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page2
Tectonic Plates
 The Pacific Plate is the ______________________ plate
 The Juan de Fuca is one of the ________________________
 The boundaries that run through oceans mark the positions of the
____________________________ ridges
 Earth’s outermost layers are cold and rigid compared to the layers in Earth’s interior. It is
called the__________________________________________.
o It is made up of the crust and the solid, uppermost _______________________.
o It is ____________ below ocean ridges and __________________ below continents
o The tectonic plates are just large pieces of the ________________________.
 Just ___________________ the lithosphere is called the asthenosphere.
o This layer is so hot that it behaves like a _____________________ material
o This enables to lithosphere to ___________________
Plate Boundaries
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page3
Divergent Plate Boundaries
 Mid-ocean ridges are located along _______________________ plate boundaries.
 A divergent plate boundary forms where two plates __________________
 When the seafloor spreads at a mid-ocean ridge, lava erupts, cools, and forms new
__________________ crust.
 Divergent plate boundaries can also exist in the ______________________of a continent
o They pull continents apart and form rift ______________________
o The East African Rift is an example.
Transform Plate Boundaries
 A transform plate boundary forms where two plates _________________past each other.
o The San Andrews Fault in California is a well known example.
o As the plates move past each other, they can get stuck and _____________moving,
o ________________________builds up where the plates are stuck.
o Eventually the stress is too great and the rocks _________________
o The resulting rapid energy release is an________________________.
San Andreas Fault
Convergent Plant Boundaries
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page4
 Convergent plate boundaries form where two plates ______________________
 The ________________________ plate sinks below the more buoyant plate in a process
called subduction
o The area where a denser plate descends into Earth is called a
________________________ zone.
 When an oceanic plate and continental plate collide the denser oceanic plate subducts
under the edge of the _______________________.
o This creates a deep ocean trench
o A line of ______________________ forms above the subducting plate on the edge
of the continent
 This process can also happen with two oceanic plates.
o Typically the older, denser plate will subduct beneath the _____________________
plate.
o This creates a deep ocean trench and a line of volcanoes called an ______________
arc
 When two continental plates collide, neither plate is subducted.
o Instead rock is uplifted and create mountains like the Himalayas
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page5
Evidence for Plate Tectonics
 Continents move apart or come together at speeds of a few _______________ per years
 Today scientists use a network of ______________________ called the Global Positioning
System (GPS) to measure the movement of the plates
 The theory of plate tectonics explains why earthquakes and volcanoes occur in certain
___________________.
 All types of plate boundaries can result in _________________________ due to the rapid
release of energy
 Diverging and _______________________ plates result in volcanoes
 __________________________ form when two continental plates converge
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page6
Plate Motion
 Convection Currents
o Convection is the ________________________of material caused by differences in
temperature and density
 For example, the upstairs floors of most houses often warmer than the
lower floor
 This is because warm air ________________ while denser, cold air sinks.
 Tectonic plate activity is related to convection in the__________________ .
o ________________________________ elements heat Earth’s interior.
o When materials such as solid rock are heated, they expand and become less
______________.
o Hot mantle material rises upward and comes in contact with Earth’s ____________.
o Thermal energy is _________________________ to the surface
o As the mantle__________________ , it becomes denser and then sinks, forming a
convection current
 These currents in the ____________________________ act like a conveyor belt moving
the lithosphere.
Forces causing plate motion
o Scientists are still _______________ about which force has the greatest influence.
Basal Drag
o This is when convection currents in the asthenosphere move or drag the
_______________________ much like how walking sidewalks at the airport move
people.
Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page7
Ridge Push
o Recall that mid-ocean ridges have greater _____________________ than the
surrounding seafloor.
o Because they are higher, ___________________ pulls the surrounding rock down
and away from the ridge
o Rising mantle material at mid-ocean ridges creates the _____________________
for plates to move away from the ridge with a force called ridge push.
 This moves the lithosphere _______________ from the mid-ocean ridge.
Slab Pull
o When plates converge, the _________________ plate will sink into the mantel
along a subduction zone
o This plate is called a____________________. It is usually old and cold which makes
it denser.
o As a slab sinks, it ____________ on the rest of the plate with a force called slab pull.
A Theory in Progress
 Plate tectonics has become the ________________________ theory of geology
 It explains the connection between continental drift and the __________________ and
destruction of crust along plate boundaries.
o `It also helps to explain the occurrence of earthquakes, volcanoes, and mountains
Unanswered Questions
 Several questions remain unanswered:
o Why is Earth the only ______________ in the solar system that has plate tectonic
activity?
o Why do some earthquakes and volcanoes occur far away from plate boundaries?
 Part of the answer has to do with plate thickness. The other part is
the scientists are still learning how active the mantle really is.
o What forces _________________________ plate motion?

Contenu connexe

Tendances (9)

1
11
1
 
OLM Science6_7
OLM Science6_7OLM Science6_7
OLM Science6_7
 
Stress in the earth’s crust
Stress in the earth’s crustStress in the earth’s crust
Stress in the earth’s crust
 
How rocks behave under different types of stress
How rocks behave under different types of stressHow rocks behave under different types of stress
How rocks behave under different types of stress
 
3.1 crust deformation
3.1 crust deformation3.1 crust deformation
3.1 crust deformation
 
Butler_masters_thesis_proposal_final
Butler_masters_thesis_proposal_finalButler_masters_thesis_proposal_final
Butler_masters_thesis_proposal_final
 
Isostasy- Engineering Geology
Isostasy- Engineering GeologyIsostasy- Engineering Geology
Isostasy- Engineering Geology
 
Crustal Deformation and Orogeny
Crustal Deformation and OrogenyCrustal Deformation and Orogeny
Crustal Deformation and Orogeny
 
Project Report on Soil Liquefaction
Project Report on Soil LiquefactionProject Report on Soil Liquefaction
Project Report on Soil Liquefaction
 

Similaire à Chapter 14.3: The Theory of Plate Tectonics

Mountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notesMountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notes
harvey09
 
Shaky ground
Shaky groundShaky ground
Shaky ground
matcol
 
C2c Does The Earth Move
C2c Does The Earth MoveC2c Does The Earth Move
C2c Does The Earth Move
M F Ebden
 
L2 plate boundaries ap
L2 plate boundaries apL2 plate boundaries ap
L2 plate boundaries ap
SHS Geog
 
Earth Science. Geosphere, Plate Tectonic Notes
Earth Science. Geosphere, Plate Tectonic NotesEarth Science. Geosphere, Plate Tectonic Notes
Earth Science. Geosphere, Plate Tectonic Notes
Mrs. Henley
 

Similaire à Chapter 14.3: The Theory of Plate Tectonics (20)

Dynamic Earth Note Packet
Dynamic Earth Note PacketDynamic Earth Note Packet
Dynamic Earth Note Packet
 
The theroy of plate tectonic directed reading a
The theroy of plate tectonic directed reading a The theroy of plate tectonic directed reading a
The theroy of plate tectonic directed reading a
 
Dynamic Earth
Dynamic EarthDynamic Earth
Dynamic Earth
 
Dynamic earth np1
Dynamic earth np1Dynamic earth np1
Dynamic earth np1
 
Mountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notesMountains%2c earthquakes%2c volcanoes notes
Mountains%2c earthquakes%2c volcanoes notes
 
COT PLATE TECTONIC.pptx
COT PLATE TECTONIC.pptxCOT PLATE TECTONIC.pptx
COT PLATE TECTONIC.pptx
 
Plate Tectonics
Plate TectonicsPlate Tectonics
Plate Tectonics
 
Science 10 1st Quarter Quiz 2.pdf
Science 10 1st Quarter Quiz 2.pdfScience 10 1st Quarter Quiz 2.pdf
Science 10 1st Quarter Quiz 2.pdf
 
Shaky ground
Shaky groundShaky ground
Shaky ground
 
C2c Does The Earth Move
C2c Does The Earth MoveC2c Does The Earth Move
C2c Does The Earth Move
 
Outline: Chapter 15.1: Earthquakes
Outline: Chapter 15.1: EarthquakesOutline: Chapter 15.1: Earthquakes
Outline: Chapter 15.1: Earthquakes
 
Pangaea
PangaeaPangaea
Pangaea
 
Chapter 11.2
Chapter 11.2Chapter 11.2
Chapter 11.2
 
Earthquake Srevised Sci8
Earthquake Srevised Sci8Earthquake Srevised Sci8
Earthquake Srevised Sci8
 
L2 plate boundaries ap
L2 plate boundaries apL2 plate boundaries ap
L2 plate boundaries ap
 
2-TYPES OF PLATE BOUNDAREIS.pptx
2-TYPES OF PLATE BOUNDAREIS.pptx2-TYPES OF PLATE BOUNDAREIS.pptx
2-TYPES OF PLATE BOUNDAREIS.pptx
 
Earth Science. Geosphere, Plate Tectonic Notes
Earth Science. Geosphere, Plate Tectonic NotesEarth Science. Geosphere, Plate Tectonic Notes
Earth Science. Geosphere, Plate Tectonic Notes
 
ch14-140318032351-phpapp01.pdf
ch14-140318032351-phpapp01.pdfch14-140318032351-phpapp01.pdf
ch14-140318032351-phpapp01.pdf
 
Chapter 14.3: The Theory of Plate Tectonics
Chapter 14.3: The Theory of Plate TectonicsChapter 14.3: The Theory of Plate Tectonics
Chapter 14.3: The Theory of Plate Tectonics
 
Outline: Chapter 15.2: Volcanoes
Outline: Chapter 15.2: VolcanoesOutline: Chapter 15.2: Volcanoes
Outline: Chapter 15.2: Volcanoes
 

Plus de Korrnell Academy: L Class Grade 8 Science

Plus de Korrnell Academy: L Class Grade 8 Science (20)

G7 Ch5.3 - DNA and Genes
G7 Ch5.3 - DNA and GenesG7 Ch5.3 - DNA and Genes
G7 Ch5.3 - DNA and Genes
 
G7 Ch 5.1-2 - Inheritance
G7 Ch 5.1-2 - InheritanceG7 Ch 5.1-2 - Inheritance
G7 Ch 5.1-2 - Inheritance
 
G7 Ch4.2 - Asexual Reproduction
G7 Ch4.2 - Asexual ReproductionG7 Ch4.2 - Asexual Reproduction
G7 Ch4.2 - Asexual Reproduction
 
G7 Ch4.1 - Sexual Reproduction and Meiosis
G7 Ch4.1 - Sexual Reproduction and MeiosisG7 Ch4.1 - Sexual Reproduction and Meiosis
G7 Ch4.1 - Sexual Reproduction and Meiosis
 
G7 ch3.1 levels of organization
G7 ch3.1   levels of organizationG7 ch3.1   levels of organization
G7 ch3.1 levels of organization
 
G7 ch2.3 2.4 - cellular transport
G7 ch2.3 2.4 - cellular transportG7 ch2.3 2.4 - cellular transport
G7 ch2.3 2.4 - cellular transport
 
G7 cell cycle
G7 cell cycleG7 cell cycle
G7 cell cycle
 
G7 ch2.3 moving cellular material
G7 ch2.3   moving cellular materialG7 ch2.3   moving cellular material
G7 ch2.3 moving cellular material
 
G7 ch2.2 the cell
G7 ch2.2   the cellG7 ch2.2   the cell
G7 ch2.2 the cell
 
G7 ch2.1 cells and life
G7 ch2.1   cells and lifeG7 ch2.1   cells and life
G7 ch2.1 cells and life
 
G7 ch1.1 characteristics of life
G7 ch1.1   characteristics of lifeG7 ch1.1   characteristics of life
G7 ch1.1 characteristics of life
 
G7 ch7.1 transport and defense
G7 ch7.1   transport and defenseG7 ch7.1   transport and defense
G7 ch7.1 transport and defense
 
G7 ch1.3 exploring life
G7 ch1.3   exploring lifeG7 ch1.3   exploring life
G7 ch1.3 exploring life
 
Stages of mitosis
Stages of mitosisStages of mitosis
Stages of mitosis
 
G9 energy processing notes
G9 energy processing notesG9 energy processing notes
G9 energy processing notes
 
G9 ch 10 meiosis
G9 ch 10   meiosisG9 ch 10   meiosis
G9 ch 10 meiosis
 
G9 ch9.2 mitosis and cytokinesis
G9 ch9.2 mitosis and cytokinesisG9 ch9.2 mitosis and cytokinesis
G9 ch9.2 mitosis and cytokinesis
 
G9 ch9.1 cell cycle
G9 ch9.1 cell cycleG9 ch9.1 cell cycle
G9 ch9.1 cell cycle
 
G9 Chapter 9.1 Cell Cycle
G9 Chapter 9.1 Cell CycleG9 Chapter 9.1 Cell Cycle
G9 Chapter 9.1 Cell Cycle
 
G9 mitosis mc quiz
G9 mitosis mc quizG9 mitosis mc quiz
G9 mitosis mc quiz
 

Dernier

Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
ciinovamais
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
QucHHunhnh
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
kauryashika82
 

Dernier (20)

Activity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdfActivity 01 - Artificial Culture (1).pdf
Activity 01 - Artificial Culture (1).pdf
 
Unit-IV; Professional Sales Representative (PSR).pptx
Unit-IV; Professional Sales Representative (PSR).pptxUnit-IV; Professional Sales Representative (PSR).pptx
Unit-IV; Professional Sales Representative (PSR).pptx
 
General Principles of Intellectual Property: Concepts of Intellectual Proper...
General Principles of Intellectual Property: Concepts of Intellectual  Proper...General Principles of Intellectual Property: Concepts of Intellectual  Proper...
General Principles of Intellectual Property: Concepts of Intellectual Proper...
 
Role Of Transgenic Animal In Target Validation-1.pptx
Role Of Transgenic Animal In Target Validation-1.pptxRole Of Transgenic Animal In Target Validation-1.pptx
Role Of Transgenic Animal In Target Validation-1.pptx
 
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
Explore beautiful and ugly buildings. Mathematics helps us create beautiful d...
 
Food Chain and Food Web (Ecosystem) EVS, B. Pharmacy 1st Year, Sem-II
Food Chain and Food Web (Ecosystem) EVS, B. Pharmacy 1st Year, Sem-IIFood Chain and Food Web (Ecosystem) EVS, B. Pharmacy 1st Year, Sem-II
Food Chain and Food Web (Ecosystem) EVS, B. Pharmacy 1st Year, Sem-II
 
Energy Resources. ( B. Pharmacy, 1st Year, Sem-II) Natural Resources
Energy Resources. ( B. Pharmacy, 1st Year, Sem-II) Natural ResourcesEnergy Resources. ( B. Pharmacy, 1st Year, Sem-II) Natural Resources
Energy Resources. ( B. Pharmacy, 1st Year, Sem-II) Natural Resources
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdf
 
Unit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptxUnit-IV- Pharma. Marketing Channels.pptx
Unit-IV- Pharma. Marketing Channels.pptx
 
Class 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdfClass 11th Physics NEET formula sheet pdf
Class 11th Physics NEET formula sheet pdf
 
2024-NATIONAL-LEARNING-CAMP-AND-OTHER.pptx
2024-NATIONAL-LEARNING-CAMP-AND-OTHER.pptx2024-NATIONAL-LEARNING-CAMP-AND-OTHER.pptx
2024-NATIONAL-LEARNING-CAMP-AND-OTHER.pptx
 
Mehran University Newsletter Vol-X, Issue-I, 2024
Mehran University Newsletter Vol-X, Issue-I, 2024Mehran University Newsletter Vol-X, Issue-I, 2024
Mehran University Newsletter Vol-X, Issue-I, 2024
 
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
 
1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
 
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
 
Sociology 101 Demonstration of Learning Exhibit
Sociology 101 Demonstration of Learning ExhibitSociology 101 Demonstration of Learning Exhibit
Sociology 101 Demonstration of Learning Exhibit
 
Mixin Classes in Odoo 17 How to Extend Models Using Mixin Classes
Mixin Classes in Odoo 17  How to Extend Models Using Mixin ClassesMixin Classes in Odoo 17  How to Extend Models Using Mixin Classes
Mixin Classes in Odoo 17 How to Extend Models Using Mixin Classes
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in DelhiRussian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
Russian Escort Service in Delhi 11k Hotel Foreigner Russian Call Girls in Delhi
 
psychiatric nursing HISTORY COLLECTION .docx
psychiatric  nursing HISTORY  COLLECTION  .docxpsychiatric  nursing HISTORY  COLLECTION  .docx
psychiatric nursing HISTORY COLLECTION .docx
 

Chapter 14.3: The Theory of Plate Tectonics

  • 1. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page1 Vocabulary  Plate tectonics (511) – Earth’s surface is made of rigid slabs of rock, or plates, that move with respect to each other  Lithosphere (512) – the cold and rigid outermost rock layer  Divergent plate boundary (513) – forms where two plates separate  Transform plate boundary (513) – Forms where two plates slide past each other  Convergent Plate Boundary (513) – form where two plates collide  Subduction (513) – A process in which the denser plate sinks below the more buoyant plate  Convection (516) – the circulation of material caused by differences in temperature  Ridge Push (517) – the forces that causes rising mantle material at mid-ocean ridges that creates the potential for plates to move away from the ridges  Slab Pull (517) – As a slab sinks, it pulls on the rest of the plate with this force The Plate Tectonic Theory  Earth’s crust is constantly being __________________ and destroyed  The ______________________ of plate tectonics states that Earth’s surface is made of rigid slabs of rock, or plates, that move with respect to each other  Each plate moves over Earth’s hot and ______________________________ mantle o The term _________________________ describes the forces that shape Earth’s surface and the resulting rock structures o Plate tectonics is used to explain ______________________and volcanic eruptions Tectonic Plates
  • 2. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page2 Tectonic Plates  The Pacific Plate is the ______________________ plate  The Juan de Fuca is one of the ________________________  The boundaries that run through oceans mark the positions of the ____________________________ ridges  Earth’s outermost layers are cold and rigid compared to the layers in Earth’s interior. It is called the__________________________________________. o It is made up of the crust and the solid, uppermost _______________________. o It is ____________ below ocean ridges and __________________ below continents o The tectonic plates are just large pieces of the ________________________.  Just ___________________ the lithosphere is called the asthenosphere. o This layer is so hot that it behaves like a _____________________ material o This enables to lithosphere to ___________________ Plate Boundaries
  • 3. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page3 Divergent Plate Boundaries  Mid-ocean ridges are located along _______________________ plate boundaries.  A divergent plate boundary forms where two plates __________________  When the seafloor spreads at a mid-ocean ridge, lava erupts, cools, and forms new __________________ crust.  Divergent plate boundaries can also exist in the ______________________of a continent o They pull continents apart and form rift ______________________ o The East African Rift is an example. Transform Plate Boundaries  A transform plate boundary forms where two plates _________________past each other. o The San Andrews Fault in California is a well known example. o As the plates move past each other, they can get stuck and _____________moving, o ________________________builds up where the plates are stuck. o Eventually the stress is too great and the rocks _________________ o The resulting rapid energy release is an________________________. San Andreas Fault Convergent Plant Boundaries
  • 4. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page4  Convergent plate boundaries form where two plates ______________________  The ________________________ plate sinks below the more buoyant plate in a process called subduction o The area where a denser plate descends into Earth is called a ________________________ zone.  When an oceanic plate and continental plate collide the denser oceanic plate subducts under the edge of the _______________________. o This creates a deep ocean trench o A line of ______________________ forms above the subducting plate on the edge of the continent  This process can also happen with two oceanic plates. o Typically the older, denser plate will subduct beneath the _____________________ plate. o This creates a deep ocean trench and a line of volcanoes called an ______________ arc  When two continental plates collide, neither plate is subducted. o Instead rock is uplifted and create mountains like the Himalayas
  • 5. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page5 Evidence for Plate Tectonics  Continents move apart or come together at speeds of a few _______________ per years  Today scientists use a network of ______________________ called the Global Positioning System (GPS) to measure the movement of the plates  The theory of plate tectonics explains why earthquakes and volcanoes occur in certain ___________________.  All types of plate boundaries can result in _________________________ due to the rapid release of energy  Diverging and _______________________ plates result in volcanoes  __________________________ form when two continental plates converge
  • 6. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page6 Plate Motion  Convection Currents o Convection is the ________________________of material caused by differences in temperature and density  For example, the upstairs floors of most houses often warmer than the lower floor  This is because warm air ________________ while denser, cold air sinks.  Tectonic plate activity is related to convection in the__________________ . o ________________________________ elements heat Earth’s interior. o When materials such as solid rock are heated, they expand and become less ______________. o Hot mantle material rises upward and comes in contact with Earth’s ____________. o Thermal energy is _________________________ to the surface o As the mantle__________________ , it becomes denser and then sinks, forming a convection current  These currents in the ____________________________ act like a conveyor belt moving the lithosphere. Forces causing plate motion o Scientists are still _______________ about which force has the greatest influence. Basal Drag o This is when convection currents in the asthenosphere move or drag the _______________________ much like how walking sidewalks at the airport move people.
  • 7. Chapter 14 Lesson 3: The Theory of Plate Tectonics – p510-519 - page7 Ridge Push o Recall that mid-ocean ridges have greater _____________________ than the surrounding seafloor. o Because they are higher, ___________________ pulls the surrounding rock down and away from the ridge o Rising mantle material at mid-ocean ridges creates the _____________________ for plates to move away from the ridge with a force called ridge push.  This moves the lithosphere _______________ from the mid-ocean ridge. Slab Pull o When plates converge, the _________________ plate will sink into the mantel along a subduction zone o This plate is called a____________________. It is usually old and cold which makes it denser. o As a slab sinks, it ____________ on the rest of the plate with a force called slab pull. A Theory in Progress  Plate tectonics has become the ________________________ theory of geology  It explains the connection between continental drift and the __________________ and destruction of crust along plate boundaries. o `It also helps to explain the occurrence of earthquakes, volcanoes, and mountains Unanswered Questions  Several questions remain unanswered: o Why is Earth the only ______________ in the solar system that has plate tectonic activity? o Why do some earthquakes and volcanoes occur far away from plate boundaries?  Part of the answer has to do with plate thickness. The other part is the scientists are still learning how active the mantle really is. o What forces _________________________ plate motion?