December 21, Chapter 11 mountain building E.notebook. Feb 19 8:19 AM. Feb 19 9:28 AM
|
|
|
- Jeffery Foster
- 5 years ago
- Views:
Transcription
1 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 There are two kinds of continental margins (boundary between oceanic and continental crust) 1. Margins that are found on plate boundaries (active continental margins) Appalachian Mountains = used to be at a convergent boundary Himalaya Mountains = on a current convergent boundary 2. Margins that are found within a plate (passive) Both contribute to the building of mountains but in different ways. Passive margins only add accumulated sediment built up on the edge of a continent over hundreds, thousands, or millions of years and won't contribute to creating a mountain until the boundary becomes active Feb 19 8:19 AM Feb 19 9:22 AM Jan 10 11:27 AM Jan 10 11:29 AM Stress is the force that deforms rocks. Mountains form when rocks are permanently deformed from stress. There are three primary kinds of stress. 1. Tension (pulling) this will make a rock thinner and longer Tensional stress creates normal faults. Normal faults occur when the hanging wall falls down in relation to the foot wall Jan 10 11:35 AM Feb 19 9:28 AM 1
2 Normal fault Jan 10 1:17 PM Feb 19 10:00 AM Feb 19 9:59 AM Jan 10 1:15 PM Normal fault Jan 10 1:15 PM Feb 19 8:28 AM 2
3 Tensional stress cause this rock to create several successive normal faults The hanging wall is the dark basalt on the left (west). The footwall is the sandstone on the right (east). Feb 19 8:26 AM Feb 19 8:27 AM Compressional stress: Rock layers are being squeezed making them shorter and thicker Normal faulting Compressional stress can create reverse faults and folds Feb 19 8:28 AM Feb 19 9:48 AM Compression can make a type of reverse fault called a thrust fault if the fault plain is 45 degrees or less from the horizontal plane Feb 19 10:00 AM Feb 19 9:55 AM 3
4 Chapter 11 mountain building E.notebook Reverse fault Fault plane Feb 19 8:29 AM Feb 19 8:30 AM Reverse fault and folding This thrust (reverse fault) is approximately horizontal...you can see the anticline in the hanging wall and the syncline in the footwall Feb 19 8:31 AM Feb 19 9:55 AM Reverse fault Chief mountain is a good example of how faulting can create peaks. The hanging wall is the prominent peak. The footwall is the dark shale covered in vegetation Feb 19 8:32 AM Feb 19 8:31 AM 4
5 Compression can cause folding of rock if it is deep in the ground (warmer) or the rock is ductile. Folds can also occur if the stress is exerted slowly over a very long period of time Parts of a fold 1. Anticline 2. Syncline 3. Limb 4. Dip 5. Strike Feb 19 12:21 PM Feb 19 12:16 PM Feb 19 9:49 AM Feb 19 9:58 AM Feb 19 9:49 AM Feb 19 9:58 AM 5
6 Feb 19 9:50 AM Feb 19 9:51 AM Feb 19 9:52 AM Feb 19 9:53 AM Feb 19 8:34 AM Feb 19 8:35 AM 6
7 Chapter 11 mountain building E.notebook Upright folds Feb 19 8:35 AM Feb 19 8:36 AM Chevron folds Feb 19 8:36 AM Feb 19 8:37 AM Ptygmatic folds Disharmonic folds Feb 19 8:37 AM Feb 19 8:37 AM 7
8 Chapter 11 mountain building E.notebook Joints are cracks in rocks that have no movement along the plain of the crack. Joints can be caused by several factors Rebound of rock that has been compressed 2. swelling or shrinking of rock layers Feb 19 8:38 AM Feb 19 12:32 PM Exfoliation joints Feb 19 8:39 AM Feb 19 8:39 AM Exfoliation joints Jointing Feb 19 8:39 AM Feb 19 8:40 AM 8
9 Joints filled in with minerals Joints filled in with minerals Feb 19 8:40 AM Feb 19 8:40 AM Sheer stress: Involves stress moving in opposite directions away from each other, with little up or down movement Sheer stress creates strike slip faults Feb 19 9:48 AM Feb 19 9:55 AM Strike slip fault Feb 19 10:00 AM Feb 19 8:33 AM 9
10 Chapter 11 mountain building E.notebook FOLDED TYPES OF MOUNTAINS 1. Folded 2. Volcanic 3. Dome 4. Fault Block 5. Horsts and Grabens Caused by continental collision Folded mountains have characteristic anticlines and synclines Evidence of some volcanic activity is typical, and this occurs when the oceanic basin is being subducted under the continent before the collision of the two converging continents occurs. Sediment that has build up on the passive continental margin is also pushed up during collision to adds to the material forming the folded mountains Examples of folded mountains are the Himalayan and the Appalachian mountains Jan 13 11:13 AM Jan 13 11:15 AM Jan 13 11:28 AM Jan 13 11:30 AM DOME Dome mountains can occur from uplifting forces in the ground or from plutonic activity (like a laccolith) pushing up overlying flat layers * plutonic dome * tectonic dome Dome mountains are nearly circular folded mountains but do not form in belts. instead they are individual and isolated Examples of dome mountains are the Adirondack mountains of NY and the Black Hills in SD Jan 13 11:30 AM Jan 13 11:35 AM 10
11 Jan 13 11:43 AM Jan 13 11:45 AM Volcanic Volcanic mountains tend to form on continental crust near a subduction boundary Andes Mountains are an example on the western side (oceanic material is subducting below the South American continent) of South America Jan 13 12:52 PM Jan 13 11:45 AM FAULT BLOCK Tensional stress on rocks produce normal faults which can result in the formation of fault block mountains The tension responsible for the formation of fault block mountains comes from uplift Examples of fault block mountains are the Sierra Nevada range in California and the Wasatch Range in Utah Jan 13 11:48 AM Jan 13 11:52 AM 11
12 Jan 13 11:53 AM Jan 13 11:55 AM HORSTS AND GRABENS Caused by tensional stress and normal faulting Caused from the stretching of tectonic plates. Examples are the great rift valley in Africa (where the continent is being ripped apart) and the Basin and range province in NV Jan 13 11:56 AM Feb 19 9:54 AM Jan 13 1:20 PM Jan 13 1:22 PM 12
13 Feb 19 9:54 AM 13
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,
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
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
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,
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
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
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
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
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.
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
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
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
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
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
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.
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
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?
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,
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
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
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
Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms.
Chapter 10 Section 10.1 The Nature of Volcanic Eruptions This section discusses volcanic eruptions, types of volcanoes, and other volcanic landforms. Reading Strategy Previewing Before you read the section,
Convergent plate boundary.
Crustal Deformation Convergent plate boundary http://my.execpc.com/~acmelasr/mountains/geogramsnf.html Plate Tectonic Settings and Magma Where plates CONVERGE, water is driven off the subducting plate,
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 >>>
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
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
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # Main Idea:
Chapter 10: Volcanoes and Other Igneous Activity Section 1: The Nature of Volcanic Eruptions I. Factors Affecting Eruptions Group # A. Viscosity Group # B. Dissolved Gases Group # II. Volcanic Material
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.
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
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
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
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
FINAL EXAM Crustal Deformation CONVERGE DIVERGENT PLATES MANTLE PLUMES FLUX BASALTIC GRANITIC
Crustal Deformation Reading: Chapter 10 Pages 283-294 FINAL EXAM 8 to 10 AM, THURSDAY DEC. 6 HERE: Natural Science 101 BRING A SCAN TRON TURN IN YOUR REVIEW QUESTIONS BEFORE THE TEST, PICK UP WHEN YOU
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
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
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
Folding. Faulting. Volcanoes
Folding Faulting Volcanoes Most major global mountain ranges were formed by the collision of continental (tectonic) plates Fold mountains are actually formed by crust which have been uplifted and folded
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?
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
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
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
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
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
Deformation of the Crust
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
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
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education
Copyright McGraw-Hill Education. All rights reserved. No reproduction or distribution without the prior written consent of McGraw-Hill Education Tibetan Plateau and Himalaya -southern Asia 11.00.a VE 10X
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
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
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
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.
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
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,
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?
CRUSTAL DEFORMATION. Chapter 10
CRUSTAL DEFORMATION and dgeologic Structures t Chapter 10 Deformation Df Deformation involves: Stress the amount of force applied to a given area. Types of Stress: Confining Stress stress applied equally
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
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
Use a highlighter to mark the most important parts, or the parts. you want to remember in the background information.
P a g e 1 Name A Fault Model Purpose: To explore the types of faults and how they affect the geosphere Background Information: A fault is an area of stress in the earth where broken rocks slide past each
6.1 Geological Stresses
www.ck12.org Chapter 6. Geological Activity from Plate Tectonics Processes 6.1 Geological Stresses Define the types of geological stress and describe their affect on various types of rock under a range
Mountain Building. Mountain Building
Mountain Building Mountain building has occurred during the recent geologic past American Cordillera the western margin of the Americas from Cape Horn to Alaska Includes the Andes and Rocky Mountains Alpine
Study the architecture and processes responsible for deformation of Earth s crust. Folding and Faulting
Crustal Deformation AKA Structural geology (adapted from Brunkel, 2012) Study the architecture and processes responsible for deformation of Earth s crust. Folding and Faulting How Rocks Deform: 4 Controls
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
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
Evolution of Continents Chapter 20
Evolution of Continents Chapter 20 Does not contain complete lecture notes. Mountain belts Orogenesis the processes that collectively produce a mountain belt Includes folding, thrust faulting, metamorphism,
Plate Tectonics - Demonstration
Name: Reference: Prof. Larry Braile - Educational Resources Copyright 2000. L. Braile. Permission granted for reproduction for non-commercial uses. http://web.ics.purdue.edu/~braile/indexlinks/educ.htm
Folding/Faulting: Topographic Expression of Folded Strata
Folding/Faulting: Topographic Expression of Folded Strata Mountains: Orogenesis and Deformation Folding Faulting Joints & Fractures Domes and Basins Horst and Graben Rift Valleys US Examples: Sierra Nevada
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,
Continental Landscapes
Continental Landscapes Landscape influenced by tectonics, climate & differential weathering Most landforms developed within the last 2 million years System moves toward an equilibrium Continental Landscapes
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
Do NOT open the test until instructed to do so.
Raw Score: Rank: School: Team Number: Names: Boyceville Invitational, December 2, 2017 Dynamic Planet Plate Tectonics and Geographical Impacts Do NOT open the test until instructed to do so. 2011 Tohoku
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
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.
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
Evidence from the Surface. Chapter 02. Continental Drift. Fossil Evidence for Pangaea. Seafloor Spreading. Seafloor Spreading 1/31/2012
Evidence from the Surface Surface landforms Continental shelf and slope Abyssal Plane Mid-oceanic ridge Oceanic Trenches Chapter 02 Continental Drift Continental Drift - a hypothesis that the continents
OCN 201 Seafloor Spreading and Plate Tectonics. Question
OCN 201 Seafloor Spreading and Plate Tectonics Question What was wrong from Wegener s theory of continental drift? A. The continents were once all connected in a single supercontinent B. The continents
Captain s Tryouts 2017
Captain s Tryouts 2017 Dynamic Planet Test Written by: Araneesh Pratap (Chattahoochee High School) Name: Date: Answer all questions on the answer sheet. Point values are given next to each question or
Lecture 6 Folds, Faults and Deformation Dr. Shwan Omar
Fold: A fold is a bend or wrinkle of rock layers or foliation; folds form as a sequence of ductile deformation. Folding is the processes by which crustal forces deform an area of crust so that layers of
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
Chapter 8. Foundations of Geology
Chapter 8 Foundations of Geology Structure of the Earth The earth can be divided into three parts: Crust Mantle Core The Earth s Crust The crust is the part of the earth we are most familiar with It is
Lecture # 6. Geological Structures
1 Lecture # 6 Geological Structures ( Folds, Faults and Joints) Instructor: Dr. Attaullah Shah Department of Civil Engineering Swedish College of Engineering and Technology-Wah Cantt. 2 The wavy undulations
Crustal Deformation. (Building Earth s Surface, Part 1) Science 330 Summer Mapping geologic structures
Crustal Deformation (Building Earth s Surface, Part 1) Science 330 Summer 2005 Mapping geologic structures When conducting a study of a region, a geologist identifies and describes the dominant rock structures
Structural Geology and Geology Maps Lab
Structural Geology and Geology Maps Lab Mesa College Geology 101 Lab Ray Rector: Instructor Structural Geology Lab Pre-Lab Resources Pre-Lab Internet Links 1) Fundamentals of Structural Geology 2) Visualizing
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
Topic 12: Dynamic Earth Pracatice
Name: Topic 12: Dynamic Earth Pracatice 1. Earth s outer core is best inferred to be A) liquid, with an average density of approximately 4 g/cm 3 B) liquid, with an average density of approximately 11
Tectonics is a study of the major structural features of the Earth s crust or a broad structure of a region. Tecto- means building
TECTONICS AND TECTONIC STRUCTURES Tectonics is a study of the major structural features of the Earth s crust or a broad structure of a region. Tecto- means building The plate theory Different stages are
GEOLOGIC MAPS PART II
EARTH AND ENVIRONMENT THROUGH TIME LABORATORY - EES 1005 LABORATORY FIVE GEOLOGIC MAPS PART II Introduction Geologic maps of orogenic belts are much more complex than maps of the stable interior. Just
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
Earth Dynamics. Landforms at Plate Boundaries
Earth Dynamics CHAPTER 8 LESSON 2 Landforms at Boundaries 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
Tectonics. Planets, Moons & Rings 9/11/13 movements of the planet s crust
Tectonics Planets, Moons & Rings 9/11/13 movements of the planet s crust Planetary History Planets formed HOT Denser materials fall to center Planet cools by conduction, convection, radiation to space
GEOLOGY MEDIA SUITE Chapter 13
UNDERSTANDING EARTH, SIXTH EDITION GROTZINGER JORDAN GEOLOGY MEDIA SUITE Chapter 13 Earthquakes 2010 W.H. Freeman and Company Three different types of seismic waves are recorded by seismographs Key Figure
GEOL 110. Sedimentary Layering. Geologic Structures (faults, joints, folds), Unconformities, Karst. Sedimentary Layering 9/23/17. Geologic Structures
GEOL 110 Sedimentary Layering Geologic Structures (faults, joints, folds), Unconformities, Karst Layering = horizontal, continuous banding produced during sediment deposition Sedimentary Layering Geologic
Layers of the Earth Date: SWABT: Identify and describe the layers of the Earth and their characteristics
Layers of the Earth SWABT: Identify and describe the layers of the Earth and their characteristics CRUST Composition: Thickness: State of Matter: : Mostly Basalt : Mostly Granite : Crust and Upper Mantle
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)
Lecture 9 faults, folds and mountain building
Lecture 9 faults, folds and mountain building Rock deformation Deformation = all changes in size, shape, orientation, or position of a rock mass Structural geology is the study of rock deformation Deformation
Geology of Landscapes Chapter 6 (Building Earth s Surface Faulting and Folding)
Geology of Landscapes Chapter 6 (Building Earth s Surface Faulting and Folding) Process of _ that the earth s Stress and Strain Any solid material responds to a force in a way that depends on: pressure
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
YORK CASTLE HIGH SCHOOL CHRISTMAS TERM EXAMINATIONS GEOGRAPHY Duration 1 1 /2 HRS.
GRADE 9 YORK CASTLE HIGH SCHOOL CHRISTMAS TERM EXAMINATIONS GEOGRAPHY Duration 1 1 /2 HRS. Name: 1. Label the internal structure of the earth provided below. WRITE on the space provide. Oceanic Crust/Upper
PART 7: PLATE TECTONICS, EARTHQUAKES & VOLCANOES
PART 7: PLATE TECTONICS, EARTHQUAKES & VOLCANOES 1. Theory of Plate Tectonics: a theory born in 1968 that there are massive rock plates under the surface of the Earth called tectonic plates that are in
Faults, Fossils, Rocks and Minerals Review:
Faults, Fossils, Rocks and Minerals Review: 1. The preserved remains or traces of organisms that lived in the past are. - Fossils 2. How do Fossils form? - A dead organism becomes buried in sediment 3.
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
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