Earth Science Chapter 11 Section 1 Review
|
|
- Madeline George
- 7 years ago
- Views:
Transcription
1 Name: Class: Date: Earth Science Chapter 11 Section 1 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Which of the following is NOT a major factor that influences the strength of a rock? a. time c. age of rock b. rock type d. temperature 2. All changes in the original shape and/or size of a rock body are called. a. faulting c. folding b. deformation d. stress 3. Under which of the following conditions do rocks exhibit ductile deformation? a. low temperature c. low confining pressure b. being near the Earth s surface d. high confining pressure 4. Which of the following combinations should favor folding rather than faulting? a. high temperature and low confining pressure b. low confining pressure and low temperature c. high confining pressure and low temperature d. high temperature and high confining pressure 5. As heat and pressure increase, ductile deformation. a. stops occurring c. becomes more likely b. becomes less likely d. is replaced by elastic deformation 6. Once the elastic limit of rock is surpassed, which of the following may occur? a. The rock may fracture. b. The rock may undergo ductile deformation. c. The rock may flow. d. all of the above 7. Which of the following is NOT a form of rock deformation? a. elastic deformation c. erosional deformation b. ductile deformation d. brittle deformation 8. Deformation in which the object returns to its original shape and size after the stress is removed is called. a. elastic deformation c. brittle deformation b. ductile deformation d. strain deformation 9. Brittle deformation is generally seen in. a. rocks with strong internal molecular bonds b. gypsum and shale c. rocks far below Earth s surface d. limestone and schist 2
2 Name: 10. The type of deformation in which the object permanently changes size and shape without fracturing is called. a. brittle deformation c. elastic deformation b. ductile deformation d. stress deformation 11. A material that undergoes tensional stress tends to. a. shorten c. become distorted b. stretch d. become less dense 12. Which of the following is NOT a type of stress seen in rocks? a. shear stress c. compressional stress b. tensional stress d. transitional stress 13. Folding is usually the result of. a. tensional stresses c. faulting b. shear stresses d. compressional stresses 14. Tensional stresses commonly cause which of the following? a. strike-slip faults c. thrust faults b. reverse faults d. normal faults 15. Compressional stresses can result in the formation of. a. rift valleys c. thrust faults b. horsts and grabens d. normal faults 16. What type of stresses have the rocks undergone to form the structures in Figure 11-1? a. shear stresses c. tensional stresses b. compressional stresses d. none of the above 17. What type of faults are shown in Figure 11-1? a. strike-slip faults c. reverse faults b. normal faults d. thrust faults 2
3 Name: 18. A fault in which the hanging wall moves down relative to the footwall is a. a. normal fault c. thrust fault b. reverse fault d. strike-slip fault 19. Faults in which movement is mainly horizontal and parallel to the trend of the fault surface are called. a. reverse faults c. strike-slip faults b. thrust faults d. normal faults 20. According to Figure 11-2, what type of structure does diagram A represent? a. normal fault c. dome b. syncline d. basin 21. According to Figure 11-2, what type of structure does diagram B represent? a. dome c. anticline b. basin d. horst 22. In diagram A of Figure 11-2, where would the oldest rock layers be located? a. at C b. at D c. between C and D d. The answer cannot be determined. 23. In diagram B of Figure 11-2, where would the oldest rock layers be located? a. at E b. at F c. between E and F d. The answer cannot be determined. 3
4 Name: Completion Complete each statement. 24. The general term that refers to all changes in the original shape and/or size of a rock body is. 25. is the force per unit area acting on a solid. 26. When a rock is permanently altered by folding or flowing, it is said to have undergone deformation. 27. Forces that pull apart rocks or Earth s crust are called stresses. 28. A distortion in rock with no change in volume is caused by stress. 29. Troughs or downfolds in rock layers are called. 30. A(n) is a fracture in rock along which no appreciable movement has occurred. 31. A low-angle fault in which the hanging wall moves up relative to the footwall is called a(n) fault. 4
5 Name: Short Answer 32. List the factors that influence the strength of a rock and affect how it will deform. 33. What is the change in shape or volume of a body of rock as a result of stress called? 34. Briefly explain the difference between elastic deformation, ductile deformation, and brittle deformation. 35. List the three types of stresses. 36. Describe anticlines and synclines. 5
6 Name: Essay 37. Briefly describe the relative movements and dominant stresses involved in the four major types of faults. 6
7 Earth Science Chapter 11 Section 1 Review Answer Section MULTIPLE CHOICE 1. ANS: C PTS: 1 DIF: L1 OBJ: ANS: B PTS: 1 DIF: L1 OBJ: ANS: D PTS: 1 DIF: L2 OBJ: ANS: D PTS: 1 DIF: L2 OBJ: ANS: C PTS: 1 DIF: L2 OBJ: ANS: D PTS: 1 DIF: L1 OBJ: ANS: C PTS: 1 DIF: L1 OBJ: ANS: A PTS: 1 DIF: L1 OBJ: ANS: A PTS: 1 DIF: L2 OBJ: ANS: B PTS: 1 DIF: L2 OBJ: ANS: B PTS: 1 DIF: L1 OBJ: ANS: D PTS: 1 DIF: L1 OBJ: ANS: D PTS: 1 DIF: L2 OBJ: ANS: D PTS: 1 DIF: L2 OBJ: ANS: C PTS: 1 DIF: L2 OBJ: ANS: C PTS: 1 DIF: L2 OBJ: ANS: B PTS: 1 DIF: L2 OBJ: ANS: A PTS: 1 DIF: L1 OBJ: ANS: C PTS: 1 DIF: L1 OBJ: ANS: C PTS: 1 DIF: L1 OBJ: ANS: B PTS: 1 DIF: L1 OBJ: ANS: A PTS: 1 DIF: L2 OBJ: ANS: B PTS: 1 DIF: L2 OBJ: 11.4 COMPLETION 24. ANS: deformation PTS: 1 DIF: L1 OBJ: ANS: Stress PTS: 1 DIF: L1 OBJ: ANS: ductile PTS: 1 DIF: L1 OBJ: ANS: tensional PTS: 1 DIF: L1 OBJ: ANS: shear PTS: 1 DIF: L2 OBJ:
8 29. ANS: synclines PTS: 1 DIF: L1 OBJ: ANS: joint PTS: 1 DIF: L1 OBJ: ANS: thrust PTS: 1 DIF: L2 OBJ: 11.4 SHORT ANSWER 32. ANS: temperature, confining pressure, time, and rock type PTS: 1 DIF: L1 OBJ: ANS: strain PTS: 1 DIF: L1 OBJ: ANS: In elastic deformation, once the stresses are removed, the deformed body returns to its original shape and size; in ductile deformation, the body undergoes a permanent change in shape and/or size without fracturing; in brittle deformation, the body breaks or fractures once its strength is exceeded. PTS: 1 DIF: L2 OBJ: ANS: tensional stress, compressional stress, and shear stress PTS: 1 DIF: L1 OBJ: ANS: Anticlines are formed from the upfolding or arching of rock layers; synclines are downfolds or troughs. PTS: 1 DIF: L1 OBJ:
9 ESSAY 37. ANS: Normal faults are relatively high-angle faults in which the hanging wall moves down relative to the footwall. Normal faults result from tensional stresses and result in the stretching or extension of the crust. Reverse faults are relatively high-angle faults in which the hanging wall moves up relative to the footwall. These faults are caused by compressional stresses and result in the thickening and shortening of rocks or the crust. Thrust faults are low-angle reverse faults with the hanging wall moving up relative to the footwall. Because of their low angle, most of the movement in a thrust fault is in a horizontal direction. Thrust faults are caused by compressional stresses and result in thickening and shortening of the crust. In strike-slip faults, the movement is mainly in a horizontal direction and parallel to the trend, or strike, of the fault. Strike-slip faults are commonly caused by shear stresses. PTS: 1 DIF: L2 OBJ:
Questions & Answers Proposed for Exam #3
Questions & Answers Proposed for Exam #3 GE50 Introduction to Physical Geology (Geology for Engineers) Missouri University of Science and Technology Fall Semester 2007, Leslie Gertsch (GertschL@mst.edu)
More informationLaboratory #8: Structural Geology Thinking in 3D
Name: Lab day: Tuesday Wednesday Thursday ENVG /SC 10110-20110L Planet Earth Laboratory Laboratory #8: Structural Geology Thinking in 3D http://www.nd.edu/~cneal/physicalgeo/lab-structural/index.html Readings:
More informationDip is the vertical angle perpendicular to strike between the imaginary horizontal plane and the inclined planar geological feature.
Geological Visualization Tools and Structural Geology Geologists use several visualization tools to understand rock outcrop relationships, regional patterns and subsurface geology in 3D and 4D. Geological
More informationLABORATORY TWO GEOLOGIC STRUCTURES
EARTH AND ENVIRONMENT THROUGH TIME LABORATORY- EES 1005 LABORATORY TWO GEOLOGIC STRUCTURES Introduction Structural geology is the study of the ways in which rocks or sediments are arranged and deformed
More informationUSING RELATIVE DATING AND UNCONFORMITIES TO DETERMINE SEQUENCES OF EVENTS
EARTH AND ENVIRONMENT THROUGH TIME LABORATORY- EES 1005 LABORATORY THREE USING RELATIVE DATING AND UNCONFORMITIES TO DETERMINE SEQUENCES OF EVENTS Introduction In order to interpret Earth history from
More informationLocation and Distance on Earth (Chapter 22 part 1)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: Location and Distance on Earth (Chapter 22 part 1) For this assignment you will require: a calculator, protractor, and a metric ruler, and an
More informationGEOLOGIC MAPS. PURPOSE: To be able to understand, visualize, and analyze geologic maps
GEOLOGIC MAPS PURPOSE: To be able to understand, visualize, and analyze geologic maps Geologic maps show the distribution of the various igneous, sedimentary, and metamorphic rocks at Earth s surface in
More informationYasuhiro Yamada a, *, Ken McClay b
Journal of Structural Geology 25 (2003) 1331 1336 www.elsevier.com/locate/jsg Application of geometric models to inverted listric fault systems in sandbox experiments. Paper 2: insights for possible along
More informationPore pressure. Ordinary space
Fault Mechanics Laboratory Pore pressure scale Lowers normal stress, moves stress circle to left Doesn Doesn t change shear Deviatoric stress not affected This example: failure will be by tensile cracks
More informationTYPES OF ROCKS & THE ROCK CYCLE
Visit http://www.learner.org/interactives/rockcycle/index.html to complete the following questions and activities. TYPES OF ROCKS: 1. Click on TYPES OF ROCKS. Read the information on the webpage and answer
More informationPlate Tectonics Web-Quest
Plate Tectonics Web-Quest Part I: Earth s Structure. Use the following link to find these answers: http://www.learner.org/interactives/dynamicearth/structure.html 1. Label the layers of Earth in the diagram
More informationEarth Science Chapter 14 Section 2 Review
Name: Class: Date: Earth Science Chapter 14 Section Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Which of the following is NOT one of the three
More informationCHAPTER 6 THE TERRESTRIAL PLANETS
CHAPTER 6 THE TERRESTRIAL PLANETS MULTIPLE CHOICE 1. Which of the following is NOT one of the four stages in the development of a terrestrial planet? 2. That Earth, evidence that Earth differentiated.
More informationGeological Maps 3: Faulted Strata
Geological Maps 3: Faulted Strata Brittle deformation in rocks is characterized by fractures, joints and faults. Fractures and joints can be of any size, orientation or pattern. Some joints form regular
More informationPlate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot
Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where
More informationStress Strain Relationships
Stress Strain Relationships Tensile Testing One basic ingredient in the study of the mechanics of deformable bodies is the resistive properties of materials. These properties relate the stresses to the
More informationMaterial Deformations. Academic Resource Center
Material Deformations Academic Resource Center Agenda Origin of deformations Deformations & dislocations Dislocation motion Slip systems Stresses involved with deformation Deformation by twinning Origin
More informationLANDFORMS OF THE EARTH STD VIII
LANDFORMS OF THE EARTH STD VIII 1) What do you understand by the term geomorphology? A) Geomorphology is the systematic study of the Earth s relief features. Geo means earth; morph meaning form and ology
More informationMechanical Properties of Metals Mechanical Properties refers to the behavior of material when external forces are applied
Mechanical Properties of Metals Mechanical Properties refers to the behavior of material when external forces are applied Stress and strain fracture or engineering point of view: allows to predict the
More informationRocks & Minerals. 10. Which rock type is most likely to be monomineralic? 1) rock salt 3) basalt 2) rhyolite 4) conglomerate
1. Of the Earth's more than 2,000 identified minerals, only a small number are commonly found in rocks. This fact indicates that most 1) minerals weather before they can be identified 2) minerals have
More informationES Chapter 10 Review. Name: Class: Date: Multiple Choice Identify the choice that best completes the statement or answers the question.
Name: Class: Date: ES Chapter 10 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Scientists used the pattern of alternating normal and reversed
More informationChapter Outline Dislocations and Strengthening Mechanisms
Chapter Outline Dislocations and Strengthening Mechanisms What is happening in material during plastic deformation? Dislocations and Plastic Deformation Motion of dislocations in response to stress Slip
More information4. Plate Tectonics II (p. 46-67)
4. Plate Tectonics II (p. 46-67) Seafloor Spreading In the early 1960s, samples of basaltic ocean crust were dredged up from various locations across the ocean basins. The samples were then analyzed to
More informationPROPERTIES OF MATERIALS
1 PROPERTIES OF MATERIALS 1.1 PROPERTIES OF MATERIALS Different materials possess different properties in varying degree and therefore behave in different ways under given conditions. These properties
More informationChapter Outline Dislocations and Strengthening Mechanisms
Chapter Outline Dislocations and Strengthening Mechanisms What is happening in material during plastic deformation? Dislocations and Plastic Deformation Motion of dislocations in response to stress Slip
More informationLECTURE SUMMARY September 30th 2009
LECTURE SUMMARY September 30 th 2009 Key Lecture Topics Crystal Structures in Relation to Slip Systems Resolved Shear Stress Using a Stereographic Projection to Determine the Active Slip System Slip Planes
More informationContinental Drift, Sea Floor Spreading and Plate Tectonics
Page 1 of 13 EENS 1110 Tulane University Physical Geology Prof. Stephen A. Nelson Continental Drift, Sea Floor Spreading and Plate Tectonics This page last updated on 26-Aug-2015 Plate Tectonics is a theory
More informationGlossary. continental crust: the sections of crust, the outermost layer of the earth, that include the continents
aftershock: an earthquake that follows a larger earthquake or main shock and originates in or near the rupture zone of the larger earthquake. Generally, major earthquakes are followed by a number of aftershocks
More informationRocks and Plate Tectonics
Name: Class: _ Date: _ Rocks and Plate Tectonics Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is a naturally occurring, solid mass of mineral or
More informationLayers of the Earth and Plate Tectonics
Layers of the Earth and Plate Tectonics Objectives: explain various ways the earth can be changed by natural forces define the term Geology define the terms Crust, Mantle, Outer Core and Inner Core classify
More informationObjectives. Experimentally determine the yield strength, tensile strength, and modules of elasticity and ductility of given materials.
Lab 3 Tension Test Objectives Concepts Background Experimental Procedure Report Requirements Discussion Objectives Experimentally determine the yield strength, tensile strength, and modules of elasticity
More information1. Foliation or schistose textures are easily seen in rocks consisting of. 2. Which of these tectonic settings will be hottest at 20km depth?
2nd Midterm Questions Metamorphic Rocks 1. Foliation or schistose textures are easily seen in rocks consisting of. a. framework silicates (quartz, feldspar) b. platy minerals (micas) c. chain-silicates
More informationFATIGUE CONSIDERATION IN DESIGN
FATIGUE CONSIDERATION IN DESIGN OBJECTIVES AND SCOPE In this module we will be discussing on design aspects related to fatigue failure, an important mode of failure in engineering components. Fatigue failure
More informationPlate Tectonics. Introduction. Boundaries between crustal plates
Plate Tectonics KEY WORDS: continental drift, seafloor spreading, plate tectonics, mid ocean ridge (MOR) system, spreading center, rise, divergent plate boundary, subduction zone, convergent plate boundary,
More informationStructural Geology Laboratory 9 (Name)
Structural Geology Laboratory 9 (Name) Geologic maps show the distribution of different types of structures and rock stratigraphic units generally on a topographic base such as a quadrangle map. Key structures
More informationThe mechanical properties of metal affected by heat treatment are:
Training Objective After watching this video and reviewing the printed material, the student/trainee will learn the basic concepts of the heat treating processes as they pertain to carbon and alloy steels.
More informationFluid Mechanics: Static s Kinematics Dynamics Fluid
Fluid Mechanics: Fluid mechanics may be defined as that branch of engineering science that deals with the behavior of fluid under the condition of rest and motion Fluid mechanics may be divided into three
More informationSedimentary Basins. Revision Material. Introduction. CE3A8 SMJ Geology for Engineers 1
CE3A8 SMJ Geology for Engineers 1 Sedimentary Basins Revision Material This handout lists the topics covered in the two lectures on sedimentary basins and provides a few key diagrams. Either of the following
More informationStep 2: Learn where the nearest divergent boundaries are located.
What happens when plates diverge? Plates spread apart, or diverge, from each other at divergent boundaries. At these boundaries new ocean crust is added to the Earth s surface and ocean basins are created.
More informationName Date Class. By studying the Vocabulary and Notes listed for each section below, you can gain a better understanding of this chapter.
CHAPTER 7 VOCABULARY & NOTES WORKSHEET Earthquakes By studying the Vocabulary and Notes listed for each section below, you can gain a better understanding of this chapter. SECTION 1 Vocabulary In your
More informationName Score /225. (Make sure you identify each key concept by identifying the section [1.1, 1.2, etc.].]
Name Score /225 Changing Earth Chapter 1 Worksheet Before reading Chapter 1 (pages 9 37). On a separate sheet of paper, make two columns. Title the first column Before I Read. Title the second column After
More informationPlate Tectonics. Plate Tectonics The unifying concept of the Earth sciences. Continental Drift
Plate Tectonics The unifying concept of the Earth sciences. The outer portion of the Earth is made up of about 20 distinct plates (~ 100 km thick), which move relative to each other This motion is what
More informationChapter Outline. Mechanical Properties of Metals How do metals respond to external loads?
Mechanical Properties of Metals How do metals respond to external loads? Stress and Strain Tension Compression Shear Torsion Elastic deformation Plastic Deformation Yield Strength Tensile Strength Ductility
More informationTECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
More information2. Fault mechanics: some basic aspects
15 2. Fault mechanics: some basic aspects The behavior of rocks in the shallow crust (fig. 7) has been extensively investigated with rock mechanics laboratory experiments. The results of experiments on
More informationMechanical Properties and Fracture Analysis of Glass. David Dutt Chromaglass, Inc.
Mechanical Properties and Fracture Analysis of Glass David Dutt Chromaglass, Inc. IES ALC Williamsburg 2006 2 IES ALC Williamsburg 2006 3 Outline The Ideal The Practical The Reality IES ALC Williamsburg
More informationLong term performance of polymers
1.0 Introduction Long term performance of polymers Polymer materials exhibit time dependent behavior. The stress and strain induced when a load is applied are a function of time. In the most general form
More information1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I.
PLATE TECTONICS ACTIVITY The purpose of this lab is to introduce the concept of plate tectonics and the formation of mountains. Students will discuss the properties of the earth s crust and plate tectonics.
More informationGeol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II 4. Which of the following statements about paleomagnetism at spreading ridges is FALSE? A. there is a clear pattern of paleomagnetic
More informationPlate Tectonics: Big Ideas. Plate Tectonics. Plate Tectonics. The unifying concept of the Earth sciences.
Plate Tectonics: Big Ideas Our understanding of Earth is continuously refined. Earth s systems are dynamic; they continually react to changing influences from geological, hydrological, physical, chemical,
More informationNancy West, Beth Pratt-Sitaula, and Shelley Olds (UNAVCO) expanded from work by Vince Cronin (Baylor University)
Nancy West, Beth Pratt-Sitaula, and Shelley Olds (UNAVCO) expanded from work by Vince Cronin (Baylor University) Earth s crust is deforming. While people who live through earthquakes know this from shaking,
More informationFIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FIRST GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIRST GRADE VOLCANOES WEEK 1. PRE: Learning the shapes of volcanoes. LAB: Experimenting with "lava." POST:
More informationWEATHERING, EROSION, AND DEPOSITION PRACTICE TEST. Which graph best shows the relative stream velocities across the stream from A to B?
NAME DATE WEATHERING, EROSION, AND DEPOSITION PRACTICE TEST 1. The diagram below shows a meandering stream. Measurements of stream velocity were taken along straight line AB. Which graph best shows the
More informationHow Did These Ocean Features and Continental Margins Form?
298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations
More informationII. Earth Science (Geology) Section (9/18/2013)
EAPS 100 Planet Earth Lecture Topics Brief Outlines II. Earth Science (Geology) Section (9/18/2013) 1. Interior of the Earth Learning objectives: Understand the structure of the Earth s interior crust,
More informationPhysics 3 Summer 1989 Lab 7 - Elasticity
Physics 3 Summer 1989 Lab 7 - Elasticity Theory All materials deform to some extent when subjected to a stress (a force per unit area). Elastic materials have internal forces which restore the size and
More information2.0 External and Internal Forces act on structures
2.0 External and Internal Forces act on structures 2.1 Measuring Forces A force is a push or pull that tends to cause an object to change its movement or shape. Magnitude, Direction, and Location The actual
More informationChapter 12 - Liquids and Solids
Chapter 12 - Liquids and Solids 12-1 Liquids I. Properties of Liquids and the Kinetic Molecular Theory A. Fluids 1. Substances that can flow and therefore take the shape of their container B. Relative
More informationEarthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel
Earthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel Jordan, Deborah and Spiegel, Samuel: Learning Research Development Center, University of Pittsburgh. Earthquakes and Plate Boundaries.
More informationEarthquakes. Earthquakes: Big Ideas. Earthquakes
Earthquakes Earthquakes: Big Ideas Humans cannot eliminate natural hazards but can engage in activities that reduce their impacts by identifying high-risk locations, improving construction methods, and
More informationLABORATORY EXPERIMENTS TESTING OF MATERIALS
LABORATORY EXPERIMENTS TESTING OF MATERIALS 1. TENSION TEST: INTRODUCTION & THEORY The tension test is the most commonly used method to evaluate the mechanical properties of metals. Its main objective
More informationMap Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface
Map Patterns and Finding the Strike and Dip from a Mapped Outcrop of a Planar Surface Topographic maps represent the complex curves of earth s surface with contour lines that represent the intersection
More informationGeorgia Performance Standards Framework for Shaky Ground 6 th Grade
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
More informationStrengthening. Mechanisms of strengthening in single-phase metals: grain-size reduction solid-solution alloying strain hardening
Strengthening The ability of a metal to deform depends on the ability of dislocations to move Restricting dislocation motion makes the material stronger Mechanisms of strengthening in single-phase metals:
More informationDescription of mechanical properties
ArcelorMittal Europe Flat Products Description of mechanical properties Introduction Mechanical properties are governed by the basic concepts of elasticity, plasticity and toughness. Elasticity is the
More information6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island
More informationStructural Integrity Analysis
Structural Integrity Analysis 1. STRESS CONCENTRATION Igor Kokcharov 1.1 STRESSES AND CONCENTRATORS 1.1.1 Stress An applied external force F causes inner forces in the carrying structure. Inner forces
More informationSolution for Homework #1
Solution for Homework #1 Chapter 2: Multiple Choice Questions (2.5, 2.6, 2.8, 2.11) 2.5 Which of the following bond types are classified as primary bonds (more than one)? (a) covalent bonding, (b) hydrogen
More informationVAPORIZATION IN MORE DETAIL. Energy needed to escape into gas phase GAS LIQUID. Kinetic energy. Average kinetic energy
30 VAPORIZATION IN MORE DETAIL GAS Energy needed to escape into gas phase LIQUID Kinetic energy Average kinetic energy - For a molecule to move from the liquid phase to the gas phase, it must acquire enough
More informationTectonic plates have different boundaries.
KEY CONCEPT Plates move apart. BEFORE, you learned The continents join and break apart The sea floor provides evidence that tectonic plates move The theory of plate tectonics helps explain how the plates
More informationFIFTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FIFTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIFTH GRADE VOLCANOES WEEK 1. PRE: Exploring the rocks produced by volcanoes. LAB: Comparing igneous rocks.
More informationFOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types
More informationChapter 7 Earthquake Hazards Practice Exam and Study Guide
Chapter 7 Earthquake Hazards Practice Exam and Study Guide 1. Select from the following list, all of the factors that affect the intensity of ground shaking. a. The magnitude of the earthquake b. Rather
More informationStates of Matter CHAPTER 10 REVIEW SECTION 1. Name Date Class. Answer the following questions in the space provided.
CHAPTER 10 REVIEW States of Matter SECTION 1 SHORT ANSWER Answer the following questions in the space provided. 1. Identify whether the descriptions below describe an ideal gas or a real gas. ideal gas
More informationTEACHER BACKGROUND INFORMATION THERMAL ENERGY
TEACHER BACKGROUND INFORMATION THERMAL ENERGY In general, when an object performs work on another object, it does not transfer all of its energy to that object. Some of the energy is lost as heat due to
More informationName: Period: # Plate Tectonics. Journey to the center of the Earth
Plate Tectonics Journey to the center of the Earth Use pages 124 129 to answer the following questions. Exploring Inside Earth (p. 125-126) 1. What are the two main types of evidence that Geologist use
More informationInteractive Plate Tectonics
Interactive Plate Tectonics Directions: Go to the following website and complete the questions below. http://www.learner.org/interactives/dynamicearth/index.html How do scientists learn about the interior
More informationStability Assessment of Chamshir Dam Based on DEM, South West Zagros
2015 2nd International Conference on Geological and Civil Engineering IPCBEE vol. 80 (2015) (2015) IACSIT Press, Singapore DOI: 10.7763/IPCBEE. 2015. V80. 13 Stability Assessment of Chamshir Dam Based
More informationGeologic History Review
1. The climate that existed in an area during the early Paleozoic Era can best be determined by studying (1) the present climate of the area (2) recorded climate data of the area since 1700 (3) present
More informationContinental Drift. Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on:
Plate Tectonics and Continental Drift Continental Drift Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on: Similarities in shorelines
More informationGeorgia Performance Standards Framework for Science Grade 6. Unit Organizer: Geology: Inside the Earth (Approximate Time: 7 Weeks)
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
More informationPlate Tectonics: Ridges, Transform Faults and Subduction Zones
Plate Tectonics: Ridges, Transform Faults and Subduction Zones Goals of this exercise: 1. review the major physiographic features of the ocean basins 2. investigate the creation of oceanic crust at mid-ocean
More information12.510 Introduction to Seismology Spring 2008
MIT OpenCourseWare http://ocw.mit.edu 12.510 Introduction to Seismology Spring 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. 04/30/2008 Today s
More informationThe interior of the Earth is divided into layers based on chemical and physical properties.
Plate Tectonics Lecture Notes: Slide 1. Title Slide Slide 2. The interior of the Earth is divided into layers based on chemical and physical properties. The Earth has an outer silica-rich, solid crust,
More informationEARTH SCIENCE 110 INTRODUCTION to GEOLOGY MINERALS & ROCKS LABORATORY
EARTH SCIENCE 110 INTRODUCTION to GEOLOGY DR. WOLTEMADE NAME: SECTION: MINERALS & ROCKS LABORATORY INTRODUCTION The identification of minerals and rocks is an integral part of understanding our physical
More informationModern Construction Materials Prof. Ravindra Gettu Department of Civil Engineering Indian Institute of Technology, Madras
Modern Construction Materials Prof. Ravindra Gettu Department of Civil Engineering Indian Institute of Technology, Madras Module - 2 Lecture - 2 Part 2 of 2 Review of Atomic Bonding II We will continue
More informationUnit 4 Lesson 6 Measuring Earthquake Waves. Copyright Houghton Mifflin Harcourt Publishing Company
Shake, Rattle, and Roll What happens during an earthquake? As plates of the lithosphere move, the stress on rocks at or near the edges of the plates increases. This stress causes faults to form. A fault
More informationUsing Google Earth to Explore Plate Tectonics
Using Google Earth to Explore Plate Tectonics Laurel Goodell, Department of Geosciences, Princeton University, Princeton, NJ 08544 laurel@princeton.edu Inspired by, and borrows from, the GIS-based Exploring
More information7.2.4 Seismic velocity, attenuation and rock properties
7.2.4 Seismic velocity, attenuation and rock properties Rock properties that affect seismic velocity Porosity Lithification Pressure Fluid saturation Velocity in unconsolidated near surface soils (the
More informationSECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SECOND GRADE VOLCANOES WEEK 1. PRE: Investigating the parts of a volcano. LAB: Comparing the parts of a
More informationPractice Test. 4) The planet Earth loses heat mainly by A) conduction. B) convection. C) radiation. D) all of these Answer: C
Practice Test 1) Increase the pressure in a container of oxygen gas while keeping the temperature constant and you increase the A) molecular speed. B) molecular kinetic energy. C) Choice A and choice B
More informationFluids and Solids: Fundamentals
Fluids and Solids: Fundamentals We normally recognize three states of matter: solid; liquid and gas. However, liquid and gas are both fluids: in contrast to solids they lack the ability to resist deformation.
More informationChesapeake Bay Governor School for Marine and Environmental Science
Choose the best answer and write on the answer sheet provided. 1. Which of the following is LEAST likely to be an effect of global warming? (a) Loss of fertile delta regions for agriculture (b) Change
More information1. Fluids Mechanics and Fluid Properties. 1.1 Objectives of this section. 1.2 Fluids
1. Fluids Mechanics and Fluid Properties What is fluid mechanics? As its name suggests it is the branch of applied mechanics concerned with the statics and dynamics of fluids - both liquids and gases.
More informationChapter 13 - LIQUIDS AND SOLIDS
Chapter 13 - LIQUIDS AND SOLIDS Problems to try at end of chapter: Answers in Appendix I: 1,3,5,7b,9b,15,17,23,25,29,31,33,45,49,51,53,61 13.1 Properties of Liquids 1. Liquids take the shape of their container,
More informationBiomechanics of Joints, Ligaments and Tendons.
Hippocrates (460-377 B.C.) Biomechanics of Joints, s and Tendons. Course Text: Hamill & Knutzen (some in chapter 2 and 3, but ligament and tendon mechanics is not well covered in the text) Nordin & Frankel
More informationKINETIC MOLECULAR THEORY OF MATTER
KINETIC MOLECULAR THEORY OF MATTER The kinetic-molecular theory is based on the idea that particles of matter are always in motion. The theory can be used to explain the properties of solids, liquids,
More informationSeismic Waves Practice
1. Base your answer to the following question on the diagram below, which shows models of two types of earthquake waves. Model A best represents the motion of earthquake waves called 1) P-waves (compressional
More informationExperiment: Crystal Structure Analysis in Engineering Materials
Experiment: Crystal Structure Analysis in Engineering Materials Objective The purpose of this experiment is to introduce students to the use of X-ray diffraction techniques for investigating various types
More informationUnit 8.3.1 Study Guide: Rocks, Minerals, and the Rock Cycle
Name Date Per Unit 8.3.1 Study Guide: Rocks, Minerals, and the Rock Cycle I Can Statements I Can Statements are the learning targets for each unit. By the time you take the test for this unit, you should
More information