Deformation of the Crust

Size: px
Start display at page:

Download "Deformation of the Crust"

Transcription

1 Deformation of the Crust Review Choose the best response. Write the letter of that choice in the space provided. 1. The state of balance between the thickness of the crust and the depth at which it rides on the asthenosphere is called a. stress. b. isostasy. c. strain. d. shearing. 2. The increasing weight of mountains causes the crust to a. sink. b. fold. c. rise. d. fracture. 3. The force that changes the shape and volume of rocks is a. footwall. b. isostasy. c. rising. d. stress. 4. The type of stress that squeezes rock together is a. compression. b. tension. c. shearing. d. faulting. 5. The type of stress that pulls rocks apart, making them thinner, is a. folding. b. compression. c. tension. d. isostasy. 6. Shearing a. bends, twists, or breaks rocks. b. squeezes rock together. c. causes rock to melt. d. pulls rock apart. 7. High pressure and high temperature will cause rocks to a. fracture. b. adjust. c. plateau. d. deform. 8. Upcurved folds in rock are called a. anticlines. b. monoclines. c. fractures. d. synclines. 9. Downcurved folds in rock are called a. fractures. b. monoclines. c. anticlines. d. synclines. 10. Folds in which both limbs remain horizontal are called a. monoclines. b. fractures. c. synclines. d. anticlines. Study Guide 17

2 Choose the best response. Write the letter of that choice in the space provided. 11. When no movement occurs along the sides of a break in a rock structure, the break is called a a. normal fault. b. fracture. c. fold. d. hanging wall. 12. When a fault is not vertical, the rock above the fault plane makes up the a. tension. b. footwall. c. hanging wall. d. compression. 13. A nearly vertical fault in which the rock on either side of the fault plane moves horizontally is called a a. normal fault. b. reverse fault. c. strike-slip fault. d. thrust fault. 14. The largest mountain systems are part of still larger systems called a. continental margins. b. ranges. c. belts. d. synclines. 15. Mount St. Helens in Washington State is an example of a a. folded mountain. b. volcanic mountain. c. fault-block mountain. d. dome mountain. Critical Thinking 1. Suppose glaciers, which are vast fields of slow-moving ice, were to cover much of the earth s surface once again. What would you expect to happen to those parts of the continents that were covered by ice? Explain. 18 Study Guide

3 2. When the Indian plate collided with the Eurasian plate, producing the Himalaya Mountains, which type of stress most likely occurred? Which type of stress is most likely occurring along the Mid-Atlantic Ridge? Which type of stress would you expect to find along the San Andreas Fault? Use your knowledge of stress and plate tectonics to explain your answers. 3. If the force that is causing a rock to be slightly deformed begins to ease, what might happen to the rock? What would happen if the force causing the deformation became greater? 4. Why do you suppose dome mountains do not become volcanic mountains? Study Guide 19

4 Application 1. Suppose that a new highway is being planned. This proposed road would intersect a transform boundary. What would happen to the highway if a strike-slip fault existed along the boundary? Why? 2. A geologist discovers that part of a mountain range along the west coast of the United States contains the fossil remains of animals that do not match any other fossils from North America. What is the most likely explanation for this phenomenon? 3. Construct a concept map that illustrates the relationship between crustal deformation and types of mountains. 20 Study Guide

5 they hung their lamps. Footwall referred to the rock they walked on. Interested students may wish to research the origins of other terms. Pages 88 89: Discussion (Extension) To extend students scientific vocabulary, you may wish to point out that the geologic term for mountain building is orogeny (oro-, from the Greek word oros, meaning mountain, and -geny, from the Greek word gignesthai, meaning act of being born ). Pages 90 91: Science & Technology You may wish to tell students that the word laser is an acronym for light amplification by stimulated emission of radiation. Explain to students that lasers are used to measure the distance to Lageos satellites because laser light has special properties. One property of laser light is that it does not spread out as quickly as ordinary light does. The diameter of a typical laser beam grows by only 1 m for every 1,000 m that the light travels. Page 93: EarthBeat You may wish to point out to students that the Mediterranean Sea is a remnant of the Tethys Sea, which covered most of the Eastern Hemisphere during the Mesozoic Era. Small-Scale Investigation Folds and Fractures (p. 87) Science Process Skills: observing, identifying cause-and-effect relationships Answers to Analysis and Conclusions 1. The dowel bends but regains its original shape when the books are removed. The putty bends, but it does not regain its original shape. The dowel represents rock that is deformed temporarily by stress but regains its shape when the stress is removed. The putty represents rock that permanently folds as a result of stress. 2. Both the dowel and the putty fracture. 3. Two influential factors are the physical properties of material and type of stress. Rocks deep within the earth s crust are made more pliable by the high temperatures. Cooler temperatures at the earth s surface make rock brittle. Rocks deformed by slow, gentle stress may regain their original shape when the stress is removed. Quick, strong stress usually fractures rock. Review Answers to Review 1. b 5. c 9. d 13. c 2. a 6. a 10. a 14. c 3. d 7. d 11. b 15. b 4. a 8. a 12. c Answers to Critical Thinking 1. The continents would sink because the increase in the weight of the crust would trigger an isostatic adjustment. 2. compression, because rock is being squeezed together; tension, because rock is being pulled apart; shearing, because rock is being bent, twisted, and torn apart 3. It would return to its original shape. The rock would become permanently deformed, either folding or faulting. 4. because the weight of the crust above the molten rock prevents it from breaking through Answers to Application 1. The highway would crack apart along its width, and the two sections would be displaced horizontally. 2. Part of the mountain is a terrane that was scraped off the ocean floor as oceanic crust was subducted beneath continental crust. 3. Student concept maps should represent the connections among the types of mountains formed and the process by which they are formed. In-Depth Investigation Continental Collisions (pp ) Approximate time: 1 class period Objectives: to construct a model; to demonstrate with a model how the Himalayas formed as a result of the collision of India with Eurasia Skills: observing, experimenting, constructing and interpreting models, measuring Prelab Discussion Have students describe a convergent boundary and a subduction zone. Stress the nature of the continental and oceanic lithosphere and their respective densities. Also, discuss the idea that the formation of new T44

Unit 4 Lesson 7 Mountain Building

Unit 4 Lesson 7 Mountain Building Indiana Standards 7.2.4 Explain how convection currents in the mantle cause lithospheric plates to move causing fast changes like earthquakes and volcanic eruptions, and slow changes like creation of mountains

More information

Directed Reading. Section: How Mountains Form MOUNTAIN RANGES AND SYSTEMS. Skills Worksheet

Directed Reading. Section: How Mountains Form MOUNTAIN RANGES AND SYSTEMS. Skills Worksheet Skills Worksheet Directed Reading Section: How Mountains Form 1. How high is Mount Everest? a. about 1980 km above sea level b. more than 8 km below sea level c. more than 8 km above sea level d. more

More information

Deformation of Rocks. Orientation of Deformed Rocks

Deformation of Rocks. Orientation of Deformed Rocks Deformation of Rocks Folds and faults are geologic structures caused by deformation. Structural geology is the study of the deformation of rocks and its effects. Fig. 7.1 Orientation of Deformed Rocks

More information

4 Deforming the Earth s Crust

4 Deforming the Earth s Crust CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?

More information

Chapter Review USING KEY TERMS. asthenosphere uplift continental drift. known as. tectonic plates move. object. UNDERSTANDING KEY IDEAS

Chapter Review USING KEY TERMS. asthenosphere uplift continental drift. known as. tectonic plates move. object. UNDERSTANDING KEY IDEAS Skills Worksheet Chapter Review USING KEY TERMS 1. Use the following terms in the same sentence: crust, mantle, and core. Complete each of the following sentences by choosing the correct term from the

More information

Unit 4 Lesson 3 Mountain Building. Copyright Houghton Mifflin Harcourt Publishing Company

Unit 4 Lesson 3 Mountain Building. Copyright Houghton Mifflin Harcourt Publishing Company Stressed Out How can tectonic plate motion cause deformation? The movement of tectonic plates causes stress on rock structures. Stress is the amount of force per unit area that is placed on an object.

More information

Chapter. Mountain Building

Chapter. Mountain Building Chapter Mountain Building 11.1 Rock Deformation Factors Affecting Deformation Factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock type, and

More information

4 Deforming the Earth s Crust

4 Deforming the Earth s Crust CHAPTER 7 4 Deforming the Earth s Crust SECTION Plate Tectonics BEFORE YOU READ After you read this section, you should be able to answer these questions: What happens when rock is placed under stress?

More information

KEY CHAPTER 12 TAKE-HOME QUIZ INTERNAL STRUCTURES AND PROCESSES Score Part B = / 55 PART B

KEY CHAPTER 12 TAKE-HOME QUIZ INTERNAL STRUCTURES AND PROCESSES Score Part B = / 55 PART B GEOLOGY 12 KEY CHAPTER 12 TAKE-HOME QUIZ INTERNAL STRUCTURES AND PROCESSES Score Part B = / 55 PART B CHAPTER 12 Isostacy and Structural Geology 1. Using the terms below, label the following diagrams and

More information

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building

Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,

More information

Essentials of Geology, 11e

Essentials of Geology, 11e Essentials of Geology, 11e Crustal Deformation and Mountain Building Chapter 17 Instructor Jennifer Barson Spokane Falls Community College Geology 101 Stanley Hatfield Southwestern Illinois College Jennifer

More information

Mountains and Mountain Building: Chapter 11

Mountains and Mountain Building: Chapter 11 Mountains and Mountain Building: Chapter 11 Objectives: 1)Explain how some of Earth s major mountain belts formed 2) Compare and contrast active and passive continental margins 3) Explain how compression,

More information

1. occurs when the oceanic crust slides under the continental crust.

1. occurs when the oceanic crust slides under the continental crust. 1. occurs when the oceanic crust slides under the continental crust. 2. What type of stress is shown? 3. Where two plates slide past one another is called a boundary. 4. What type of stress is shown? 5.

More information

Answers: Internal Processes and Structures (Isostasy)

Answers: Internal Processes and Structures (Isostasy) Answers: Internal Processes and Structures (Isostasy) 1. Analyse the adjustment of the crust to changes in loads associated with volcanism, mountain building, erosion, and glaciation by using the concept

More information

11.1 Rock Deformation

11.1 Rock Deformation Tarbuck Lutgens Mountain Building 11.1 Rock Deformation Factors Affecting Deformation Factors that influence the strength of a rock and how it will deform include temperature, confining pressure, rock

More information

Forces in Earth s Crust

Forces in Earth s Crust Forces in Earth s Crust This section explains how stresses in Earth s crust cause breaks, or faults, in the crust. The section also explains how faults and folds in Earth s crust form mountains. Use Target

More information

Mohorovicic discontinuity separates the crust and the upper mantle.

Mohorovicic discontinuity separates the crust and the upper mantle. Structure of the Earth Chapter 7 The Earth is divided into 3 Main Layers 1. Crust outermost layer 1% of the Earth s mass thickness varies: 5 100 km two types: oceanic denser continental Mohorovicic discontinuity

More information

Earth s Changing Surface

Earth s Changing Surface Earth s Changing Surface Tectonics What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the statement or

More information

Plate Tectonic Vocabulary Chapter 10 Pages

Plate Tectonic Vocabulary Chapter 10 Pages Name: Period: Plate Tectonic Vocabulary Chapter 10 Pages 239-260 Vocabulary Word What is this? What are some examples? What does it look like? (draw a picture or diagram) Continental drift Mid-ocean ridge

More information

Chapter 16. Mountain Building. Mountain Building. Mountains and Plate Tectonics. what s the connection?

Chapter 16. Mountain Building. Mountain Building. Mountains and Plate Tectonics. what s the connection? Chapter 16 Mountains and Plate Tectonics what s the connection? Mountain Building Most crustal deformation occurs along plate margins. S.2 Active Margin Passive Margin Mountain Building Factors Affecting

More information

Lecture Outlines PowerPoint. Chapter 10 Earth Science, 12e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 10 Earth Science, 12e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 10 Earth Science, 12e Tarbuck/Lutgens 2009 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information

Forces in Earth s Crust

Forces in Earth s Crust Forces in Earth s Crust (pages 180 186) Types of Stress (page 181) Key Concept: Tension, compression, and shearing work over millions of years to change the shape and volume of rock. When Earth s plates

More information

Earthquakes. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

Earthquakes. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left. Earthquakes Chapter Test A Multiple Choice Write the letter of the correct answer on the line at the left. 1. Stress that pushes a mass of rock in two opposite directions is called a. shearing. b. tension.

More information

RESTLESS EARTH - CHAPTER 4

RESTLESS EARTH - CHAPTER 4 RESTLESS EARTH - CHAPTER 4 continental crust - Composition is similar to granite and forms the continents and the areas of shallow seabed. oceanic crust - Composition similar to basalt. It is thinner,

More information

Ch. 9 Review. Pgs #1-31 Write Questions and Answers

Ch. 9 Review. Pgs #1-31 Write Questions and Answers Ch. 9 Review Pgs. 356-357 #1-31 Write Questions and Answers 356-357 #1-5 Answers 1. The layer of the upper mantle that can flow is the: A - Asthenosphere 2. Most scientists rejected Wegener s theory of

More information

Outcome C&D Study Guide

Outcome C&D Study Guide Name: Class: Outcome C&D Study Guide Identify the layers of Earth s interior Lithosphere the upper most layer of the earth that includes the crust and the hard outer mantle. It is fractured into tectonic

More information

Crustal Deformation. Earth Systems 3209

Crustal Deformation. Earth Systems 3209 Crustal Deformation Earth Systems 3209 Crustal Deformation pg. 415 Refers to all changes in the original form and/or size of a rock body. May also produce changes in the location and orientation of rocks.

More information

Chapter 4 Section 3, 4. Deforming the Earth s Crust

Chapter 4 Section 3, 4. Deforming the Earth s Crust Chapter 4 Section 3, 4 Deforming the Earth s Crust Deformation The process by which the shape of a rock changes because of stress Stress The amount of force per unit area on a given material Compression

More information

Continental Drift to Plate Tectonics: From Hypothesis to Theory

Continental Drift to Plate Tectonics: From Hypothesis to Theory Continental Drift to Plate Tectonics: From Hypothesis to Theory 1 Key Understandings Internal structure of the earth/structure of the crust. Difference between continental drift & plate tectonics. Evidence

More information

UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS

UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS UNIT 10 MOUNTAIN BUILDING AND EVOLUTION OF CONTINENTS ROCK DEFORMATION Tectonic forces exert different types of stress on rocks in different geologic environments. STRESS The first, called confining stress

More information

Name Class Date. In the space provided, write the letter of the definition that best matches the term or phrase.

Name Class Date. In the space provided, write the letter of the definition that best matches the term or phrase. Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition

More information

Section 2: How Mountains Form

Section 2: How Mountains Form Section 2: How Mountains Form Preview Objectives Mountain Ranges and Systems Plate Tectonics and Mountains Types of Mountains Objectives Identify the types of plate collisions that form mountains. Identify

More information

Section 3 Deforming Earth s Crust

Section 3 Deforming Earth s Crust Section 3 Deforming Earth s Crust Key Concept Tectonic plate motions deform Earth s crust. Deformation causes rock layers to bend and break and causes mountains to form. What You Will Learn Stress is placed

More information

In the space provided, write the letter of the definition that best matches the term or phrase.

In the space provided, write the letter of the definition that best matches the term or phrase. Skills Worksheet Directed Reading Section: The Changing Continents 1. What is the result of slow movements of tectonic plates? RESHAPING EARTH S CRUST In the space provided, write the letter of the definition

More information

Instructor s Manual Chapter 10. Deformation, Mountain Building, and the Continents

Instructor s Manual Chapter 10. Deformation, Mountain Building, and the Continents Chapter 10 Table of Contents Chapter Outline Learning Outcomes Chapter Summary Lecture Suggestions Enrichment Topics Common Misconceptions Consider This Key Terms Internet Sites, Videos, Software, and

More information

Refer to the map on page 173 to answer the following questions.

Refer to the map on page 173 to answer the following questions. Chapter 8-1 Plate Tectonics 1. Brainstorm the type of evidence that would indicate a climate change and how this evidence supports the theory of continental drift. Tropical fossils in cold regions Evidence

More information

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE

Directed Reading. Section: The Theory of Plate Tectonics. to the development of plate tectonics, developed? HOW CONTINENTS MOVE Skills Worksheet Directed Reading Section: The Theory of Plate Tectonics 1. The theory that explains why and how continents move is called. 2. By what time period was evidence supporting continental drift,

More information

Chapter 7 Plate Tectonics. Plate tectonics accounts for important features of Earth s surface and major geologic events.

Chapter 7 Plate Tectonics. Plate tectonics accounts for important features of Earth s surface and major geologic events. Chapter 7 Plate Tectonics Plate tectonics accounts for important features of Earth s surface and major geologic events. 7-2 Alfred Wegener s Hypothesis of Continental Drift (1915) He noticed that the continents

More information

Learning Objectives (LO) What we ll learn today:!

Learning Objectives (LO) What we ll learn today:! Learning Objectives (LO) Lecture 13: Mountain Building Read: Chapter 10 Homework #11 due Tuesday 12pm What we ll learn today:! 1. Define the types of stress that are present in the crust! 2. Define the

More information

Mountains are then built by deforming crust: Deformation & Mountain Building. Mountains form where stresses are high!

Mountains are then built by deforming crust: Deformation & Mountain Building. Mountains form where stresses are high! Deformation & Mountain Building Where are mountains located? Deformation and Folding Mountain building Mountains form where stresses are high! Mountains form at all three types of plate boundaries where

More information

Geologic Structures. Changes in the shape and/or orientation of rocks in response to applied stress

Geologic Structures. Changes in the shape and/or orientation of rocks in response to applied stress Geologic Structures Changes in the shape and/or orientation of rocks in response to applied stress Figure 15.19 Can be as big as a breadbox Or much bigger than a breadbox Three basic types Fractures >>>

More information

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017

ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth

More information

December 21, Chapter 11 mountain building E.notebook. Feb 19 8:19 AM. Feb 19 9:28 AM

December 21, Chapter 11 mountain building E.notebook. Feb 19 8:19 AM. Feb 19 9:28 AM Mountains form along convergent plate boundaries. Typically (usually) if you look at a mountain range, you know that it is at a plate boundary (active continental margin) or has been some time in the past

More information

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

FORCES ON EARTH UNIT 3.2. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. FORCES ON EARTH UNIT 3.2 An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. USE THESE NOTES: OUR HOME PLANET EARTH: What do you know about our planet? SO.HOW

More information

Earth s Dynamic Surface

Earth s Dynamic Surface Earth s Dynamic Surface Shaping Earth s Surface What do you think? Read the two statements below and decide whether you agree or disagree with them. Place an A in the Before column if you agree with the

More information

Forces That Shape Earth. How do continents move? What forces can change rocks? How does plate motion affect the rock cycle?

Forces That Shape Earth. How do continents move? What forces can change rocks? How does plate motion affect the rock cycle? Forces That Shape Earth How do continents move? What forces can change rocks? How does plate motion affect the rock cycle? Plate Motion Mountain ranges are produced by plate tectonics. The theory of plate

More information

FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth.

FORCES ON EARTH. An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. FORCES ON EARTH An investigation into how Newton s Laws of Motion are applied to the tectonic activity on Earth. GEOLOGY Geologists scientists who study the forces that make and shape the Earth Geologists

More information

PLATE TECTONICS REVIEW GAME!!!!

PLATE TECTONICS REVIEW GAME!!!! PLATE TECTONICS REVIEW GAME!!!! Name the four layers of the earth - crust - mantle - outer core - inner core Which part of Earth s structure contains tectonic plates? LITHOSPHERE Name one reason why the

More information

Directed Reading. Section: Continental Drift. years ago? WEGENER S HYPOTHESIS

Directed Reading. Section: Continental Drift. years ago? WEGENER S HYPOTHESIS Skills Worksheet Directed Reading Section: Continental Drift 1. Who obtained new information about the continents and their coastlines 400 years ago? 2. What did people notice when they studied new world

More information

Continental Drift. & Plate Tectonics

Continental Drift. & Plate Tectonics Continental Drift & Plate Tectonics Alfred Wegener, a German scientist, proposed the hypothesis of CONTINENTAL DRIFT, in 1912. Hypothesis stated: All Earth s continents were once a single landmass (Pangaea)

More information

Boundaries, Stresses, and Faults OH MY! How do geologic events change and shape Earth s surface?

Boundaries, Stresses, and Faults OH MY! How do geologic events change and shape Earth s surface? Boundaries, Stresses, and Faults OH MY! How do geologic events change and shape Earth s surface? Remember The Lithosphere is made of The CRUST + The Upper Rigid Mantle Plates may be called by different

More information

USU 1360 TECTONICS / PROCESSES

USU 1360 TECTONICS / PROCESSES USU 1360 TECTONICS / PROCESSES Observe the world map and each enlargement Pacific Northwest Tibet South America Japan 03.00.a1 South Atlantic Arabian Peninsula Observe features near the Pacific Northwest

More information

The Theory of Plate Tectonics

The Theory of Plate Tectonics Plate Tectonics Objectives Describe how plates move. Explain the features of plate tectonics. Describe the types of plate boundaries and the features that can form and events that can occur at each. The

More information

Earth Movement and Resultant Landforms

Earth Movement and Resultant Landforms Earth Movement and Resultant Landforms Structure of the Earth Lithosphere : earth s crust Asthenosphere : upper mantle zone where material is near its melting point & acts almost like liquid (appprox.

More information

Lecture Outline Friday March 2 thru Wednesday March 7, 2018

Lecture Outline Friday March 2 thru Wednesday March 7, 2018 Lecture Outline Friday March 2 thru Wednesday March 7, 2018 Questions? Lecture Exam Friday March 9, 2018 Same time, Same room Bring Pencils and WSU ID 50 question Multiple Choice, Computer Graded Interlude

More information

Crustal Deformation Earth - Chapter Pearson Education, Inc.

Crustal Deformation Earth - Chapter Pearson Education, Inc. Crustal Deformation Earth - Chapter 10 Structural Geology Structural geologists study the architecture and processes responsible for deformation of Earth s crust. A working knowledge of rock structures

More information

Chapter 10: Deformation and Mountain Building. Fig. 10.1

Chapter 10: Deformation and Mountain Building. Fig. 10.1 Chapter 10: Deformation and Mountain Building Fig. 10.1 OBJECTIVES Describe the processes of rock deformation and compare and contrast ductile and brittle behavior in rocks. Explain how strike and dip

More information

Plate Tectonics. entirely rock both and rock

Plate Tectonics. entirely rock both and rock Plate Tectonics I. Tectonics A. Tectonic Forces are forces generated from within Earth causing rock to become. B. 1. The study of the origin and arrangement of Earth surface including mountain belts, continents,

More information

* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is.

* If occurs, fossils that formed in shallow water may be found in water. Subsidence mean the crust is. Name Notes: Topic 5B Topic 5B: The Dynamic Crust A. What evidence exists that proves the Earth s Crust is and has moved? Earth Science 1. Tilted, folded or faulted strata Strata is a term that refers to.

More information

Chapter 15 Structures

Chapter 15 Structures Chapter 15 Structures Plummer/McGeary/Carlson (c) The McGraw-Hill Companies, Inc. TECTONIC FORCES AT WORK Stress & Strain Stress Strain Compressive stress Shortening strain Tensional stress stretching

More information

Shape Earth. Plate Boundaries. Building. Building

Shape Earth. Plate Boundaries. Building. Building Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Lesson 4 Chapter Wrap-Up Forces That Shape Earth Landforms at Plate Boundaries Mountain Building Continent Building How is Earth s surface shaped by plate

More information

Stress and Strain. Stress is a force per unit area. Strain is a change in size or shape in response to stress

Stress and Strain. Stress is a force per unit area. Strain is a change in size or shape in response to stress Geologic Structures Geologic structures are dynamically-produced patterns or arrangements of rock or sediment that result from, and give information about, forces within the Earth Produced as rocks change

More information

Faults, folds and mountain building

Faults, folds and mountain building Faults, folds and mountain building Mountain belts Deformation Orogens (Oro = Greek all changes for mountain, in size, shape, genesis orientation, = Greek for or formation) position of a rock mass Structural

More information

Strike-Slip Faults. ! Fault motion is parallel to the strike of the fault.

Strike-Slip Faults. ! Fault motion is parallel to the strike of the fault. Strike-Slip Faults! Fault motion is parallel to the strike of the fault.! Usually vertical, no hanging-wall/footwall blocks.! Classified by the relative sense of motion. " Right lateral opposite block

More information

1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted?

1. What is Wegener s theory of continental drift? 2. What were the 4 evidences supporting his theory? 3. Why wasn t Wegener s theory excepted? Notebook 7a and 7b Objective (left-side): Students will be able to explain the theory of plate tectonics and be able to make predictions about plate interactions. Mapping Reflection 1. What is Wegener

More information

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS

Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS Lab 7: STRUCTURAL GEOLOGY FOLDS AND FAULTS This set of labs will focus on the structures that result from deformation in earth s crust, namely folds and faults. By the end of these labs you should be able

More information

Earth Science Lesson 3 Dynamic Earth Processes (Grades 8-12 ) Instruction 3-3 Plate Boundaries

Earth Science Lesson 3 Dynamic Earth Processes (Grades 8-12 ) Instruction 3-3 Plate Boundaries As we told you in a recent Instruction, much of the Earth's lithosphere (its Crust and the top layer of its Outer Mantle) is made up of moving masses of rock called tectonic plates (tectonic means moving).

More information

Plate Tectonics. Structure of the Earth

Plate Tectonics. Structure of the Earth Plate Tectonics Structure of the Earth The Earth can be considered as being made up of a series of concentric spheres, each made up of materials that differ in terms of composition and mechanical properties.

More information

UNIT 6 PLATE TECTONICS

UNIT 6 PLATE TECTONICS UNIT 6 PLATE TECTONICS CONTINENTAL DRIFT Alfred Wegner proposed the theory that the crustal plates are moving over the mantle. He argued that today s continents once formed a single landmass, called Pangaea

More information

The Theory of Continental Drift. Continental Drift Discovery

The Theory of Continental Drift. Continental Drift Discovery The Theory of Continental Drift Continental Drift Discovery The World ALFRED WEGENER THEORY OF CONTINENTAL DRIFT Found evidence for PANGAEA and proposed the theory of continental drift. Continental Drift

More information

SAC Geography Form 2 Chapter 3: Plate Tectonics Topic 3: Plate Movement

SAC Geography Form 2 Chapter 3: Plate Tectonics Topic 3: Plate Movement What causes an earthquake? Plate movement causes pressure to build up along faults, or breaks, in the earth's crust. When the rocks cannot take any more pressure, the rock layers shift and an earthquake

More information

What Causes Rock to Deform?

What Causes Rock to Deform? Crustal Deformation Earth, Chapter 10 Chapter 10 Crustal Deformation What Causes Rock to Deform? Deformation is a general term that refers to all changes in the shape or position of a rock body in response

More information

Name Class Date. 1. What is the outermost layer of the Earth called?. a. core b. lithosphere c. asthenosphere d. mesosphere

Name Class Date. 1. What is the outermost layer of the Earth called?. a. core b. lithosphere c. asthenosphere d. mesosphere Name Class Date Assessment Geology Plate Tectonics MULTIPLE CHOICE Write the letter of the correct answer in the space provided. 1. What is the outermost layer of the Earth called?. a. core b. lithosphere

More information

Plate Tectonics Notes

Plate Tectonics Notes Plate Tectonics Notes Last 30 Days Earthquakes Physical Features Last 30 Days Earthquakes with Plate Boundaries Earth s Structure Earth s Layers Core: Inner Core: Center of the earth, solid ball of metal

More information

8 th Grade Campus Assessment- NSMS Plate Tectonics

8 th Grade Campus Assessment- NSMS Plate Tectonics 1. A group of students were discussing plate tectonics in their science class. All of the following statements about the tectonic plates are incorrect EXCEPT: A. The Eurasian Plate consists of the Asian

More information

Plate Tectonics Unit II: Plate Boundaries (3.5 pts)

Plate Tectonics Unit II: Plate Boundaries (3.5 pts) T. James Noyes, El Camino College Plate Tectonics Unit II: The Plate Boundaries (Topic 11A-2) page 1 Name: Section: Plate Tectonics Unit II: Plate Boundaries (3.5 pts) Plate Boundaries We will now discuss

More information

PLATE TECTONICS 11/13/ Investigations of glaciers also indicated that the land masses on Earth were once a supercontinent.

PLATE TECTONICS 11/13/ Investigations of glaciers also indicated that the land masses on Earth were once a supercontinent. PLATE TECTONICS Alfred Wegener thought that the landmasses fit together like a jigsaw puzzle. He called the land mass Pangaea. Meaning all land Continental Drift Wegener theory first coining the word -

More information

How to Build a Mountain and other Geologic Structures. But first a short review

How to Build a Mountain and other Geologic Structures. But first a short review How to Build a Mountain and other Geologic Structures But first a short review Where do we see deep earthquakes? What is happening there? What can happen at a plate boundary? 1. Plates can move apart

More information

How to Build a Mountain and other Geologic Structures. But first, questions

How to Build a Mountain and other Geologic Structures. But first, questions How to Build a Mountain and other Geologic Structures But first, questions Questions your students might ask How were Montana s mountains formed? How old are the mountains? What are the different ways

More information

How mountains are made. We will talk about valleys (erosion and weathering later)

How mountains are made. We will talk about valleys (erosion and weathering later) How mountains are made We will talk about valleys (erosion and weathering later) http://www.ilike2learn.com/ilike2learn/mountainmaps/mountainranges.html Continent-continent plate convergence Less dense,

More information

10. Paleomagnetism and Polar Wandering Curves.

10. Paleomagnetism and Polar Wandering Curves. Map of ocean floor Evidence in Support of the Theory of Plate Tectonics 10. Paleomagnetism and Polar Wandering Curves. The Earth's magnetic field behaves as if there were a bar magnet in the center of

More information

Earth Science ENR Plate Boundaries Notes

Earth Science ENR Plate Boundaries Notes Name Earth Science ENR Plate Boundaries Notes Per Tchr Plate Boundary Types: 1) Divergent Plate Boundary (Seafloor Spreading Centers) 2) Divergent Plate Boundary (Continental Rift Valley) 3) Transform

More information

Forces in the Earth s crust

Forces in the Earth s crust EARTHQUAKES Forces in the Earth s crust How does stress in the crust change Earth s surface? Where are faults usually found, and why do they form? What land features result from the forces of plate movement?

More information

Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building

Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building Crags, Cracks, and Crumples: Crustal Deformation and Mountain Building Updated by: Rick Oches, Professor of Geology & Environmental Sciences Bentley University Waltham, Massachusetts Based on slides prepared

More information

The Structure of the Earth and Plate Tectonics

The Structure of the Earth and Plate Tectonics The Structure of the Earth and Plate Tectonics Agree or Disagree? 1. The Earth if made up of 4 different layers. 2. The crust (where we live) can be made of either less dense continental crust or the more

More information

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn

Plate Tectonics. By Destiny, Jarrek, Kaidence, and Autumn Plate Tectonics By Destiny, Jarrek, Kaidence, and Autumn .The Denali Fault and San Andreas Fault - The San Andreas Fault is a continental transform fault that extends roughly 1300 km (810 miles) through

More information

Distribution of Continents Mid-ocean Ridges Trenches. Deformation Metamorphism Volcanism Earthquakes

Distribution of Continents Mid-ocean Ridges Trenches. Deformation Metamorphism Volcanism Earthquakes Earthquakes and Plate Tectonics Global Problems in Geology Distribution of Continents Mid-ocean Ridges Trenches Orogenic Belts Deformation Metamorphism Volcanism Earthquakes Development of Continental

More information

Section 1: Continental Drift

Section 1: Continental Drift Plate Tectonics Section 1 Section 1: Continental Drift Preview Key Ideas Wegener s Hypothesis Sea-Floor Spreading Paleomagnetism Wegener Redeemed Continental Drift (Pangaea) Plate Tectonics Section 1 Key

More information

Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s

Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s Movement of the Earth s Crust: Formation of: Mountain s Plateau's and Dome s References Information taken from several places including Prentice Hall Earth Science: @ http://www.eram.k12.ny.us/education/components/docmgr/default.php?sectiondetaili

More information

The Structure of the Earth and Plate Tectonics

The Structure of the Earth and Plate Tectonics The Structure of the Earth and Plate Tectonics Structure of the Earth The Earth is made up of 4 main layers: Inner Core Outer Core Mantle Crust Crust Mantle Outer core Inner core The Crust This is where

More information

The Theory of Plate Tectonics - Boundaries, Stresses, and Faults

The Theory of Plate Tectonics - Boundaries, Stresses, and Faults The Theory of Plate Tectonics - Boundaries, Stresses, and Faults 1. What is the theory of plate tectonics? 2. What are the three types of plate boundaries? What are Plates? The Earth s crust and upper

More information

Chapter 6: Earthquakes

Chapter 6: Earthquakes Section 1 (Forces in Earth s Crust) Chapter 6: Earthquakes 8 th Grade Stress a that acts on rock to change its shape or volume Under limited stress, rock layers can bend and stretch, but return to their

More information

on the earthquake's strength. The Richter scale is a rating of an earthquake s magnitude based on the size of the

on the earthquake's strength. The Richter scale is a rating of an earthquake s magnitude based on the size of the Earthquakes and Seismic Waves An earthquake is the shaking and trembling that results from the movement of rock beneath Earth's surface. The point beneath Earth s surface where rock under stress breaks

More information

The Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and

The Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and Earth s Structure The Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and

More information

Forces in Earth s Crust

Forces in Earth s Crust Name Date Class Earthquakes Section Summary Forces in Earth s Crust Guide for Reading How does stress in the crust change Earth s surface? Where are faults usually found, and why do they form? What land

More information

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES

3. PLATE TECTONICS LAST NAME (ALL IN CAPS): FIRST NAME: PLATES LAST NAME (ALL IN CAPS): FIRST NAME: PLATES 3. PLATE TECTONICS The outer layers of the Earth are divided into the lithosphere and asthenosphere. The division is based on differences in mechanical properties

More information

The Basics The lithosphere is made up of numerous plates (14 major, 38 minor)

The Basics The lithosphere is made up of numerous plates (14 major, 38 minor) The Basics The lithosphere is made up of numerous plates (14 major, 38 minor) These plates float atop the asthenosphere, where they can move (albeit very slowly) Plate tectonics describes the formation,

More information

FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC

FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC Crustal Deformation Reading: Chapter 10 Pages 283-304 Review Questions 4, 6, 7, 10, 12, 15, 18, 20 FINAL EXAM NOON TO 2 PM, TUESDAY DEC. 5 HERE: Natural Science 101 BRING A SCAN TRON TURN IN YOUR REVIEW

More information

I. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow

I. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow I. Earth s Layers a. Crust: Earth s outside layer. Made of mostly rock. i. Continental: er; made of mostly granite, forms the continents and shallow sea beds, floats! ii. Oceanic: er; dense rock such as

More information

1.4 Notes: Plates Converge or Scrape Past Each Other Think About Tectonic Plates Push Together at Convergent Boundaries

1.4 Notes: Plates Converge or Scrape Past Each Other Think About Tectonic Plates Push Together at Convergent Boundaries 1.4 Notes: Plates Converge or Scrape Past Each Other Think About If new crust is created at divergent boundaries, why does the total amount of crust on Earth stay the same? Tectonic Plates Push Together

More information