LOOKING INTO THE EARTH An introduction to geological geophysics

Size: px
Start display at page:

Download "LOOKING INTO THE EARTH An introduction to geological geophysics"

Transcription

1 LOOKING INTO THE EARTH An introduction to geological geophysics Alan E. Mussett Department of Earth Sciences, Liverpool University, UK M. Aftab Khan Department of Geology, Leicester University, UK Illustrations by Sue Button m w 'j It ;!; CAMBRIDGE UNIVERSITY PRESS

2 Contents Preface: Turning a Magician into an Expert Acknowledgements xvii xix Chapter 1 Introducing Geophysics and This Book What is geophysics? The Earth through geophysical spectacles: The relation of geophysics to geology What this book covers and how it is structured 2 Summary 3 Further reading 4 Parti GEOPHYSICAL METHODS SUBPART 1.1 Data Acquisition and Processing 7 Chapter 2 Data Acquisition and Reduction: Carrying out a Geophysical Survey Data acquisition: Taking measurements Data reduction Signal and noise Modelling Geological interpretation Displaying the results 10 Summary 11 Further reading 12 Problems 12 Chapter 3 Data Processing: Getting More Information from the Data Fourier analysis Wavelength Harmonic analysis Fourier analysis of a profile, Fourier analysis in 2D: Gridded data Why a harmonic series? 16

3 vi Contents 3.2 Digital filtering Simple filters Aliasing Designing a simple filter Filtering in 2D: Gridded data Using filters to enhance various types of features Summing up: Fourier analysis and filtering 21 Summary 22 Further reading 22 Problems 22 SUBPART 1.2 Seismology 24 Chapter 4 Global Seismology and Seismic Waves Waves, pulses, and rays Detecting seismic waves: Seismometers and geophones The Earth is concentrically layered Spherical symmetry of the Earth's interior Concentric layering Finding the path of a ray through the Earth Refraction: Snell's law Tracing rays through the Earth: The ray parameter, p Ray tracing and the Earth's velocity-depth structure Seismic features of the Earth Core and mantle Longitudinal and transverse waves The mantle-core difference Other seismological features of the Earth Attenuation Ray paths in the Earth Seismic tomography 39 Summary 39 Further reading 40 Problems 40 Chapter 5 Earthquakes and Seismotectonics What is an earthquake? Locating an earthquake Fault-plane solutions and stresses Fault-plane solutions The earthquake stress field and the double-couple mechanism Rupture dimensions and displacements Measures of earthquake size Intensity: Severity of an earthquake at a locality Seismic moment: Size of the earthquake at source Seismotectonics: Deducing tectonic processes Qualitative seismotectonics Quantitative seismotectonics: Seismic and aseismic faulting Surface waves Magnitude: Another measure of earthquake strength 57

4 Contents vii 5.9 Energies of earthquakes Earthquake damage and its mitigation Causes of damage Mitigating the damage caused by earthquakes 62 Summary 62 Further reading 63 Problems 63 Chapter 6 Refraction Seismology Critical refraction and head waves Huygens's wavelets Head waves The time-distance (t-x) diagram Multiple layers Dipping interfaces Seismic velocities in rocks Hidden layers' Hidden layer proper Low-velocity layer Carrying out a seismic-refraction survey Undulating interfaces and delay times Delay times The plus-minus method Ray tracing and synthetic seismograms Detecting offsets in interfaces Fan shooting: Simple seismic tomography \ 81 Summary 81 Further reading 82 Problems 82 Chapter 7 Reflection Seismology Seismic-reflection sections and their limitations Velocity determination using normal moveout, NMO Stacking Dipping reflectors and migration Faulted reflectors: Diffraction Multiple reflections Carrying out a reflection survey Data acquisition Common-depth-point (CDP) stacking Data display Vibroseis: A nonimpulsive source What is a reflector? Strengths of reflected and transmitted pulses Vertical resolution: The least separation at which interfaces can be distinguished Synthetic reflection seismograms Three-dimensional (3D) surveying 99

5 viii Contents 7.10 Reflection seismology and the search for hydrocarbons The formation of hydrocarbon traps The recognition of hydrocarbon traps Sequence stratigraphy Shallow-reflection seismic surveys 103 Summary 104 Further reading 105 Problems 105 SUBPART 1.3 Gravity 107 Chapter 8 Gravity on a Small Scale Newton's Law of Gravitation The mass of the Earth Densities of rocks Gravity units Gravity anomalies of some bodies Measuring gravity: Gravimeters Data reduction Instrumental effects and other corrections Residual and regional anomalies Planning and carrying out a gravity survey Modelling and interpretation The inversion problem Depth rules Modelling Total excess mass Microgravity surveys 122 Summary 122 Further reading 123 Problems 123 Chapter 9 Large-Scale Gravity and Isostasy Isostasy The concept of isostasy: Floating blocks Gravity and isostatic equilibrium Simple isostatic calculations Airy and Pratt models of isostasy Isostasy with regional compensation The isostatic anomaly The evidence for isostasy Isostatic rebound and the viscosity of the asthenosphere How the mantle is both solid and liquid: Solid-state creep What is the lithosphere? Forces on the lithosphere The shape of the Earth Seeing the ocean floor in the ocean surface The large-scale shape of the Earth 136 Summary 137

6 Contents ix Further reading 137 Problems 138 SUBPART I.4 Magnetism 139 Chapter 10 Palaeomagnetism and Mineral Magnetism The Earth's magnetic field, present and past Magnets and magnetic fields The Earth's magnetic field at present The Earth's magnetic field in the past Palaeomagnetism Measuring a palaeomagnetic direction Palaeopoles, palaeolatitudes, and rotations Apparent polar wander (APW) paths and relative continental movements The magnetism of rocks The atomic nature of magnetisation Magnetic domains Curie and blocking temperatures Thermal remanent magnetisation (TRM) Magnetic minerals Mechanisms that magnetise rocks at ambient temperature Testing when the remanence was acquired Laboratory tests Field tests Magnetostratigraphy The magnetic polarity timescale Magnetic polarity stratigraphy Magnetic stratigraphy utilising secular variation and excursions Mineral magnetism Magnetic fabric: Susceptibility anisotropy 158 Summary 159 Further reading 160 Problems 160 Chapter 11 Magnetic Surveying Magnetic surveying Anomaly of a buried magnet Magnetometers Data acquisition Data reduction Anomalies of some simply shaped bodies Magnetic poles and fields The field of a dipole Anomaly of a dipole, or small body Anomaly of a sphere Anomaly of a vertical sheet Depth of the body Remanent and induced magnetisation 172

7 x Contents 11.5 Computer modelling More advanced processing of data Reduction to the pole Pseudogravity Upward and downward continuation Magnetic gradiometry The Blairgowrie magnetic anomaly: A case study 176 Summary 178 Further reading 179 Problems 179 SUBPART 1.5 Electrical 181 Chapter 12 Resistivity Methods Basic electrical quantities Resistivity surveying Resistivities of rocks and minerals How electricity flows through rocks The need for four electrodes Vertical electric sounding, VES: Measuring layered structures The basic concept Refraction of current paths Apparent resistivity Carrying out a Wenner VES survey Modelling the data Other electrode arrays Limitations of vertical electrical sounding Resistivity profiling: Detecting lateral variations Introduction Some arrays for profiling Electrical imaging Designing and interpreting a resistivity survey Choosing a resistivity array Geological interpretation 199 Summary 199 Further reading 200 Problems 200 Chapter 13 Induced Polarisation and Self-Potential Induced polarization, IP What induced polarization is Carrying out an IP survey Data reduction and display Self-potential, SP What self-potential is SP surveying 206 Summary 208 Further reading 209 Problems 209

8 Contents xi Chapter 14 Electromagnetic Methods Basic concepts Electromagnetic induction Factors that affect the signal Some e-m systems Moving transmitter-plus-receiver system (Slingram) Turam system Transient electromagnetic, TEM, systems The basic concept The INPUT system Electromagnetic waves Wavelengths Absorption and attenuation of e-m waves VLF (very-low-frequency) method Basic concepts Carrying out a VLF survey Phase Magnetotelluric, MT, surveying: Looking into the deep crust and mantle Basic concepts Carrying out an MT survey Ground-penetrating radar, GPR How ground-penetrating radar works Velocity, reflection, penetration, and resolution Data reduction Uses of GPR surveys 230 Summary 230 Further reading 231 Problems 231 SUBPART 1.6 Radioactivity 233 Chapter 15 The Ages of Rocks and Minerals: Radiometric Dating The atomic clock The uranium-lead (U-Pb) dating method Assumptions of the Basic Dating Equation The potassium-argon (K-Ar) dating method The conventional K-Ar method The argon-argon (Ar-Ar) method The rubidium-strontium (Rb-Sr) dating method The samarium-neodymium (Sm-Nd) dating method The lead-lead (Pb-Pb) dating method Theory of the method The 'age of the Earth' Fission-track (FT) dating What event is being dated? Diffusion Closure temperature Cooling histories 249

9 xii Contents Two dates from a single rock, using the Rb-Sr method Two dates from a single rock, using the U-Pb discordia method Dating palaeomagnetism of slowly cooled regions Dating sedimentary rocks The geological time scale Dating young rocks Uranium-series disequilibrium methods Carbon-14 ( 14 C) and other dating methods using cosmogenic isotopes Why so many radiometric dating methods? 256 Summary 257 Further reading 258 Problems 258 Chapter 16 Radioactive Surveying Radioactive racjiations y ray surveys Measurement: The y ray spectrometer Carrying out a y ray survey Geological mapping Radon monitoring 266 Summary 267 Further reading 267 Problems 268 SUBPART I.7 Geothermics 269 Chapter 17 Geothermics: Heat and Temperature in the Earth Basic ideas in geothermics Introduction Temperature and heat How heat travels: Conduction and convection A Convection and conduction within the Earth Heat flow and temperature Measurement of heat flux Oceanic lithosphere Continental lithosphere and radioactivity Effects of changes to the lithosphere Thermal capacity Filling of a sedimentary basin Overthrusting and underthrusting Crustal thickening and orogenies Global heat flow and geothermal energy Global heat flow Sources of the Earth's heat '.4.3 Geothermal energy The effect of surface temperature changes: A record of past climates 281

10 Contents xiii Summary 282 Further reading 283 Problems 283 SUBPART 1.8 Subsurface Geophysics 285 Chapter 18 Well Logging and Other Subsurface Geophysics Introduction Drilling and its effects on the formations Sources of information from a borehole: Logs Geophysical well logging in the oil industry The most commonly used logs The measurement of strata dip, borehole inclination, and diameter The self-potential log Resistivity logs Radioactivity logs The sonic log The temperature log Cross plots Geophysical logging outside the oil industry Mineral exploration Magnetic logs The IP-resistivity log Other well-logging applications Other subsurface geophysics 303 Summary \ 303 Further reading 304 Problems 305 Part II EXAMPLES OF APPLICATIONS Chapter 19 Which Geophysical Methods to Use? Introduction Does the problem have geophysical expression? Is the variation lateral or vertical? Is the signal detectable? Will the result be clear enough to be useful? Is a survey practicable? 311 Problems 311 Chapter 20 Global Tectonics The basic concept of plate tectonics Divergent, or constructive, margins Ocean-floor magnetic anomalies The shape of spreading ridges Conservative margins 317

11 xiv Contents 20.4 Convergent, or destructive, margins Ocean-ocean convergent margins and subduction zones Ocean-continent convergent margins Continent-continent convergent margins The geometry of plate tectonics Poles of rotation Triple junctions and plate evolution The globe according to plate tectonics Continental positions in the past Crust formation at ridges What moves the plates? Forces on plates The hot-spot frame of reference: Plate velocities Deducing the dominant drive forces Plate tectonics and mantle convection 340 Summary 341 Further Reading 343 Problems 343 Chapter 21 Is the Kenya Rift a New Plate Margin? A Regional Geophysical Study Introduction: The East African Rift System Morphology and geology of the Kenya Rift Gravity studies Seismic surveys The seismicity of Kenya Teleseismic studies Seismic refraction and wide-angle reflection surveys Combined seismic and gravity models Heat flow studies Electrical conductivity Summary 360 Further reading 360 Chapter 22 Hydrocarbon Exploration Introduction: Energy sources and the demand for hydrocarbons The origin and accumulation of hydrocarbons Where sedimentary basins form Exploration for petroleum The West Sole gas field of the southern North Sea: A case study The Forties oil field of the northern North Sea: A case study Discovery and initial development of the field Further development of the Forties field The future 376 Further reading 377

12 Contents xv Chapter 23 Exploration for Metalliferous Ores Introduction: Metalliferous and other ore deposits The formation of ores and their geophysical properties Where ores form Exploration for orebodies The Elura Orebody, New South Wales, Australia: A case study Background and reconnaissance surveys Initial surveys of the Elura orebody Evaluation of the deposit Assessment of geophysical surveying methods 388 Further reading 388 Chapter 24 Volcanoes Introduction: Types of eruption and damage Methods for investigating volcanoes and monitoring activity The eruption of Redoubt Volcano, Alaska: A case study Background The eruption Monitoring of activity Etna lava eruptions : A case study Background Deformation and microgravity The eruption 396 Further reading 398 Chapter 25 The Chicxulub Structure and the K/T Mass Extinction Introduction Impacts and craters The Chicxulub structure Background The structure of Chicxulub Ages of the Chicxulub structure and ejecta The Manson Crater Giant eruptions 25.5 Conclusions to date Further reading Chapter 26 Hydrogeology and Contaminated Land 26.1 Introduction 26.2 Aquifers 26.3 Geophysical methods useful in hydrogeology 26.4 GPR surveying of the water table, the Netherlands: An example Background Offsets of the water table Structural control of aquifers in East Anglia, England: A case study Introduction Geophysical surveys

13 xvi Contents Chapter 27 Chapter Saline contamination of the Crag aquifer, East Anglia: A case study Background Geophysical surveys Landfill sites and contaminated ground Introduction Investigation of a landfill in northern England: A case study Landfill monitoring: A case study 418 Further reading Location of Cavities and Voids 27.1 Introduction 27.2 Possible geophysical techniques for locating cavities Seismic methods Electrical methods Magnetic methods Gravity methods Fracturing around cavities Collapses in buried karstic terrain, Kuwait: A case study Background Gravity survey Land reclamation, south Wales: A case study Background Gravity survey 427 Further reading Archaeological Site Surveying 28.1 Site surveying 28.2 Archaeological features and their geophysical expression Ditches, pits, and postholes Foundations Furnaces, fireplaces, and kilns Geophysical methods useful for archaeological surveying Magnetic and susceptibility surveys Resistivity surveys Ground-penetrating radar (GPR) Other techniques Display of data A possible Roman villa: A case study Background Geophysical surveys Hudson's Bay Company fur trade post: A case study Background Geophysical surveys 436 Further reading Appendix A List of Symbols and Abbreviations Appendix B Answers to Problems Bibliography Figure Sources Index

INTRODUCTION TO APPLIED GEOPHYSICS

INTRODUCTION TO APPLIED GEOPHYSICS INTRODUCTION TO APPLIED GEOPHYSICS EXPLORING THE SHALL0W SUBSURFACE H. Robert Burger Anne F. Sheehan Craig H.Jones VERSITY OF COLORADO VERSITY OF COLORADO W. W. NORTON & COMPANY NEW YORK LONDON Contents

More information

An Introduction to Geophysical Exploration

An Introduction to Geophysical Exploration An Introduction to Geophysical Exploration Philip Kearey Department of Earth Sciences University of Bristol Michael Brooks Ty Newydd, City Near Cowbridge Vale of Glamorgan Ian Hill Department of Geology

More information

3. Magnetic Methods / 62

3. Magnetic Methods / 62 Contents Preface to the Second Edition / xv Excerpts from Preface to the FirstEdition / xvii Mathematical Conventions / xix 1. Introduction / 1 Reference / 5 2. Gravity Methods / 6 2. I. Introduction /

More information

Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.

Global Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth. Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.

More information

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY

COMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic

More information

An Introduction to Applied and Environmental Geophysics

An Introduction to Applied and Environmental Geophysics An to Applied and Environmental Geophysics 2nd Edition John M. Reynolds Reynolds International Ltd Preface to the 2 na Edition Acknowledgements 1 1.1 1.2 1.3 1.4 1.5 What are 'applied' and 'environmental'

More information

Physics of the Earth

Physics of the Earth Physics of the Earth Fourth edition Frank D Stacey CSIRO Exploration and Mining, Brisbane, Australia Paul M Davis Department of Earth and Space Sciences, University of California, Los Angeles, USA CAMBRIDGE

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

What Forces Drive Plate Tectonics?

What Forces Drive Plate Tectonics? What Forces Drive Plate Tectonics? The tectonic plates are moving, but with varying rates and directions. What hypotheses have been proposed to explain the plate motion? Convection Cells in the Mantle

More information

LIGO sees binary neutron star merger on August 17, 2017

LIGO sees binary neutron star merger on August 17, 2017 LIGO sees binary neutron star merger on August 17, 2017 Laser Interferometer Gravitational-Wave Observatory (LIGO) Laser Interferometer Gravitational-Wave Observatory (LIGO) Multi-Messenger Astronomy This

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

Marine Science and Oceanography

Marine Science and Oceanography Marine Science and Oceanography Marine geology- study of the ocean floor Physical oceanography- study of waves, currents, and tides Marine biology study of nature and distribution of marine organisms Chemical

More information

Topic 12 Review Book Earth s Dynamic Crust and Interior

Topic 12 Review Book Earth s Dynamic Crust and Interior Topic 12 Review Book Earth s Dynamic Crust and Interior Define the Vocabulary 1. asthenosphere 2. continental crust 3. Convection current 4. Convergent plate boundary 5. Divergent plate boundary 6. earthquake

More information

PHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION)

PHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION) Chapter 2: Plate Tectonics Chapter Summary: Plate tectonics is a theory that suggests Earth's surface is divided into several large plates that change position and size. Intense geologic activity occurs

More information

Mineral Element Compound Atom Crystal. Silicate Nonsilicate Inorganic Luster Streak. Cleavage Fracture Hardness Density Reclamation

Mineral Element Compound Atom Crystal. Silicate Nonsilicate Inorganic Luster Streak. Cleavage Fracture Hardness Density Reclamation 6 th Grade Science Midterm Study Guide Due February 5 th * Midterm Date: February 9th (Tuesday) * Midterm will consist of 50 multiple choice questions (about 10 per chapter) YOU MUST DEFINE THE KEY TERMS

More information

Plate Tectonics Practice Test

Plate Tectonics Practice Test Plate Tectonics Practice Test 1. What is the main idea Alfred Wegner proposed in the Theory of Continental Drift that he published in 1915? a. The continents float on a liquid layer that allows them to

More information

A Petroleum Geologist's Guide to Seismic Reflection

A Petroleum Geologist's Guide to Seismic Reflection A Petroleum Geologist's Guide to Seismic Reflection William Ashcroft WILEY-BLACKWELL A John Wiley & Sons, Ltd., Publication Contents Preface Acknowledgements xi xiii Part I Basic topics and 2D interpretation

More information

Chapter 7 Plate Tectonics

Chapter 7 Plate Tectonics Chapter 7 Plate Tectonics Earthquakes Earthquake = vibration of the Earth produced by the rapid release of energy. Seismic Waves Focus = the place within the Earth where the rock breaks, producing an earthquake.

More information

Dynamic Crust Practice

Dynamic Crust Practice 1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides

More information

Department of Geophysics Faculty of Earth Sciences King Abdulaziz University

Department of Geophysics Faculty of Earth Sciences King Abdulaziz University Department of Geophysics Faculty of Earth Sciences King Abdulaziz University Dr. Mansour A. Al-Garni Office: room 233/Buld. 27 OR Dept. chair office/buld. 55 Introduction to Geophysics EGP 211 Time: 10-10:55

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

Earth s Interior HW Packet HW #1 Plate Tectonics (pages )

Earth s Interior HW Packet HW #1 Plate Tectonics (pages ) Name Earth s Interior HW Packet HW #1 Plate Tectonics (pages 676 683) 1. Is the following sentence true or false? According to the theory of plate tectonics, Earth s plates move about quickly on top of

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

Continental Drift and Plate Tectonics

Continental Drift and Plate Tectonics Continental Drift and Plate Tectonics Continental Drift Wegener s continental drift hypothesis stated that the continents had once been joined to form a single supercontinent. Wegener proposed that the

More information

ENV-5004B/ENVK5005B. Figure 6. Student Registration No. ENV-5004B/ENVK5005B Version 2

ENV-5004B/ENVK5005B. Figure 6. Student Registration No. ENV-5004B/ENVK5005B Version 2 ENV-5004B/ENVK5005B Figure 6 Student Registration No UNIVERSITY OF EAST ANGLIA School of Environmental Sciences Main Series UG Examination 014-15 SOLID EARTH GEOPHYSICS SOLID EARTH GEOPHYSICS WITH FIELDCOURSE

More information

Plate Tectonics. I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move

Plate Tectonics. I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move Plate Tectonics I. The Discovery of Plate Tectonics II. A Mosaic of Plates III. Types of Plate Boundaries IV. How Plates Move I. The Discovery of Plate Tectonics A. Continental Drift (Alfred Wegener) Proposed

More information

Theory of Plate Tectonics

Theory of Plate Tectonics Plate Tectonics Theory of Plate Tectonics Lithosphere is made of sections called plates that move around called continental drift Plates move because they float on the asthenosphere Most plates consist

More information

Yanbu University College. General Studies Department. PHSC001 Course. Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions

Yanbu University College. General Studies Department. PHSC001 Course. Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions Yanbu University College General Studies Department PHSC001 Course Chapter9 (Basic Geology: Earthquakes and volcanoes ) Worksheet Solutions Phsc001 worksheet9 solutions, yuc Page 1-6 Chapter 9 worksheet

More information

A) B) C) D) 4. Which diagram below best represents the pattern of magnetic orientation in the seafloor on the west (left) side of the ocean ridge?

A) B) C) D) 4. Which diagram below best represents the pattern of magnetic orientation in the seafloor on the west (left) side of the ocean ridge? 1. Crustal formation, which may cause the widening of an ocean, is most likely occurring at the boundary between the A) African Plate and the Eurasian Plate B) Pacific Plate and the Philippine Plate C)

More information

GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli

GENERAL GEOLOGY Fall Chapter 18: The Sea Floor. Partial Examination IV Study Guide Dr. Glen S. Mattioli GENERAL GEOLOGY 1113-005 Fall 2008 Partial Examination IV Study Guide Dr. Glen S. Mattioli Note that these are NOT questions, but rather are a list of topics that we have covered either in class or are

More information

Practice Questions: Plate Tectonics

Practice Questions: Plate Tectonics Practice Questions: Plate Tectonics 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which type of plate boundary is shown? A) divergent

More information

Core. Crust. Mesosphere. Asthenosphere. Mantle. Inner core. Lithosphere. Outer core

Core. Crust. Mesosphere. Asthenosphere. Mantle. Inner core. Lithosphere. Outer core Potter Name: Date: Hour: Score: /21 Learning Check 4.1 LT 4.1 Earth s Interior: I can draw and interpret models of the interior of the earth. Draw the following models (put the words in the right order)

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

Essentials of Oceanography Eleventh Edition

Essentials of Oceanography Eleventh Edition Chapter Chapter 1 2 Clickers Lecture Essentials of Oceanography Eleventh Edition Plate Tectonics and the Ocean Floor Alan P. Trujillo Harold V. Thurman Chapter Overview Much evidence supports plate tectonics

More information

Topic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by:

Topic 5: The Dynamic Crust (workbook p ) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: Topic 5: The Dynamic Crust (workbook p. 65-85) Evidence that Earth s crust has shifted and changed in both the past and the present is shown by: --sedimentary horizontal rock layers (strata) are found

More information

TAKE HOME EXAM 8R - Geology

TAKE HOME EXAM 8R - Geology Name Period Date TAKE HOME EXAM 8R - Geology PART 1 - Multiple Choice 1. A volcanic cone made up of alternating layers of lava and rock particles is a cone. a. cinder b. lava c. shield d. composite 2.

More information

Gravitational constraints

Gravitational constraints Gravitational constraints Reading: Fowler p172 187 Gravity anomalies Free-air anomaly: g F = g g( λ ) + δg obs F Corrected for expected variations due to the spheroid elevation above the spheroid Bouguer

More information

Before Plate Tectonics: Theory of Continental Drift

Before Plate Tectonics: Theory of Continental Drift Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.

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

OCN 201 Seafloor Spreading and Plate Tectonics. Question

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

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

Alfred Wegener gave us Continental Drift. Fifty years later...

Alfred Wegener gave us Continental Drift. Fifty years later... CHAPTER 2 Plate Tectonics and the Ocean Floor Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later... Words Chapter Overview Much evidence supports plate tectonics

More information

Prentice Hall EARTH SCIENCE

Prentice Hall EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined

More information

Prentice Hall EARTH SCIENCE

Prentice Hall EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined

More information

Plate Tectonics. A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism

Plate Tectonics. A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism Plate Tectonics A. Continental Drift Theory 1. Early development 2. Alfred Wegener s mechanism B. Seafloor Spreading 1. Earthquakes and volcanoes 2. Seafloor maps and dates 3. Continental drift revisited

More information

6. In the diagram below, letters A and B represent locations near the edge of a continent.

6. In the diagram below, letters A and B represent locations near the edge of a continent. 1. Base your answer to the following question on the cross section below and on your knowledge of Earth science. The cross section represents the distance and age of ocean-floor bedrock found on both sides

More information

Benjamin N. Cardozo Dynamic Planet Test

Benjamin N. Cardozo Dynamic Planet Test Names: Score: /83 Benjamin N. Cardozo Dynamic Planet Test - Labeling Questions are worth 1 Point Each (1 point per labeled/identified item) - Multiple Choice Questions are worth 2 Points Each - Short Answer

More information

CONTENTS PREFACE. VII 1. INTRODUCTION VARIOUS TOPICS IN SEISMOLOGY TECTONICS PERTAINING TO EQ PREDICTION 5

CONTENTS PREFACE. VII 1. INTRODUCTION VARIOUS TOPICS IN SEISMOLOGY TECTONICS PERTAINING TO EQ PREDICTION 5 CONTENTS PREFACE. VII 1. INTRODUCTION.... 1 2. VARIOUS TOPICS IN SEISMOLOGY TECTONICS PERTAINING TO EQ PREDICTION 5 2.1. Spatial distribution of strong EQs. 5 2.1.1. Mapping of major seismic fracture zones

More information

PSc 201 Chapter 3 Homework. Critical Thinking Questions

PSc 201 Chapter 3 Homework. Critical Thinking Questions PSc 201 Chapter 3 Homework Critical Thinking Questions 1. (adapted from text) Seawater is denser than fresh water. A ship moving from the Atlantic Ocean into the Great Lakes goes from seawater to fresh

More information

Introduction to Oceanography. Chapter 2: Plate Tectonics Overview

Introduction to Oceanography. Chapter 2: Plate Tectonics Overview Introduction to Oceanography Chapter 2: Plate Tectonics Overview Much evidence supports plate tectonics theory. The plate tectonics model describes features and processes on Earth. Plate tectonic science

More information

Chapter 20. Plate Tectonics

Chapter 20. Plate Tectonics Chapter 20 Plate Tectonics Early Evidence (Wegener) The geometric fit of the continents. The similarity in rock age groups between adjoining regions. The similarity in Paleozoic fossils between adjoining

More information

Static Corrections for Seismic Reflection Surveys

Static Corrections for Seismic Reflection Surveys Static Corrections for Seismic Reflection Surveys MIKE COX Volume Editors: Series Editor: Eugene F. Scherrer Roland Chen Eugene F. Scherrer Society of Exploration Geophysicists Tulsa, Oklahoma Contents

More information

Principles of Applied Geophysics

Principles of Applied Geophysics Principles of Applied Geophysics Fifth edition D.S. Parasnis Professor emeritus of Applied Geophysics Department of Applied Geophysics, University ofluled, Lulea, Sweden Fellow of the Royal Swedish Academy

More information

Earthquakes. Earthquakes are caused by a sudden release of energy

Earthquakes. Earthquakes are caused by a sudden release of energy Earthquakes Earthquakes are caused by a sudden release of energy The amount of energy released determines the magnitude of the earthquake Seismic waves carry the energy away from its origin Fig. 18.1 Origin

More information

Physical Geology, 15/e

Physical Geology, 15/e Lecture Outlines Physical Geology, 15/e Plummer, Carlson & Hammersley Plate Tectonics: The Unifying Theory Physical Geology 15/e, Chapter 19 Plate Tectonics Plate Tectonics Earth s surface is composed

More information

Elements of 3D Seismology Second Edition

Elements of 3D Seismology Second Edition Elements of 3D Seismology Second Edition Copyright c 1993-2003 All rights reserved Christopher L. Liner Department of Geosciences University of Tulsa August 14, 2003 For David and Samantha And to the memory

More information

Plate Tectonics on a Plane. Observations related to plate tectonics " " Plate tectonic theory types of plate boundaries!

Plate Tectonics on a Plane. Observations related to plate tectonics   Plate tectonic theory types of plate boundaries! Plate Tectonics on a Plane Scripps Inst. Of Oceanography" Observations related to plate tectonics " Ocean and continent topography, hypsometry, and crustal thickness. Global seismicity, Benioff zones,

More information

Unit Topics. Topic 1: Earth s Interior Topic 2: Continental Drift Topic 3: Crustal Activity Topic 4: Crustal Boundaries Topic 5: Earthquakes

Unit Topics. Topic 1: Earth s Interior Topic 2: Continental Drift Topic 3: Crustal Activity Topic 4: Crustal Boundaries Topic 5: Earthquakes The Dynamic Earth Unit Topics Topic 1: Earth s Interior Topic 2: Continental Drift Topic 3: Crustal Activity Topic 4: Crustal Boundaries Topic 5: Earthquakes Topic 1: Earth s Interior Essential Question:

More information

Elastic Rebound Theory

Elastic Rebound Theory Earthquakes Elastic Rebound Theory Earthquakes occur when strain exceeds the strength of the rock and the rock fractures. The arrival of earthquakes waves is recorded by a seismograph. The amplitude of

More information

Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates

Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates Isostasy and Tectonics Lab Understanding the Nature of Mobile Floating Lithospheric Plates Crust Mantle Dynamics Introductory Geology Lab Ray Rector - Instructor Isostasy and Tectonics Laboratory Topics

More information

OCN 201: Seafloor Spreading and Plate Tectonics I

OCN 201: Seafloor Spreading and Plate Tectonics I OCN 201: Seafloor Spreading and Plate Tectonics I Revival of Continental Drift Theory Kiyoo Wadati (1935) speculated that earthquakes and volcanoes may be associated with continental drift. Hugo Benioff

More information

Important information from Chapter 1

Important information from Chapter 1 Important information from Chapter 1 Distinguish between: Natural hazard // Disaster // Catastrophe What role does human population play in these categories? Know how to read a Hazard Map, such as Figure

More information

Civilization exists by geologic consent, subject to change without notice William Durant

Civilization exists by geologic consent, subject to change without notice William Durant 89.325 Geology for Engineers Plate Tectonics Civilization exists by geologic consent, subject to change without notice William Durant Properties of the Planets Size Density Distance from sun Chemistry

More information

Lab 1: Plate Tectonics April 2, 2009

Lab 1: Plate Tectonics April 2, 2009 Name: Lab 1: Plate Tectonics April 2, 2009 Objective: Students will be introduced to the theory of plate tectonics and different styles of plate margins and interactions. Introduction The planet can be

More information

12.2 Plate Tectonics

12.2 Plate Tectonics 12.2 Plate Tectonics LAYERS OF THE EARTH Earth is over 1200 km thick and has four distinct layers. These layers are the crust, mantle (upper and lower), outer core, and inner core. Crust outer solid rock

More information

GEOLOGY CURRICULUM. Unit 1: Introduction to Geology

GEOLOGY CURRICULUM. Unit 1: Introduction to Geology Chariho Regional School District - Science Curriculum September, 2016 GEOLOGY CURRICULUM Unit 1: Introduction to Geology OVERVIEW Summary In this unit students will be introduced to the field of geology.

More information

Features of Tectonic Plates

Features of Tectonic Plates Features of Tectonic Plates PowerPoint 12.2 The Earth s Layers Crust Brittle Continental crust composed mainly of granite Oceanic crust composed mainly of basalt Mantle Denser than the crust Upper is molten

More information

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent

Crustal Boundaries. As they move across the asthenosphere and form plate boundaries they interact in various ways. Convergent Transform Divergent Name: Date: Period: Plate Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonic plates are constantly moving and interacting As they move across the asthenosphere and form plate boundaries

More information

Chapter Overview. Evidence for Continental Drift. Plate Tectonics. Evidence for Continental Drift. Evidence for Continental Drift 9/28/2010

Chapter Overview. Evidence for Continental Drift. Plate Tectonics. Evidence for Continental Drift. Evidence for Continental Drift 9/28/2010 Chapter Overview CHAPTER 2 Plate Tectonics and the Ocean Floor Much evidence supports plate tectonics theory. Different plate boundaries have different features. Tectonic plates continue to move today.

More information

Plate Tectonics. Essentials of Geology, 11 th edition Chapter 15

Plate Tectonics. Essentials of Geology, 11 th edition Chapter 15 1 Plate Tectonics Essentials of Geology, 11 th edition Chapter 15 2 3 4 5 6 7 8 9 10 11 12 13 14 15 Plate Tectonics: summary in haiku form Alfred Wegener gave us Continental Drift. Fifty years later...

More information

CONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence

CONTENT. A. Changes in the Crust Facts Changes Construction and Destruction. B. Continental Drift What is it? Evidence Name Earth Science Date Period TOPIC THE DYNAMIC EARTH CONTENT A. Changes in the Crust Facts Changes Construction and Destruction B. Continental Drift What is it? Evidence C. Theory of Plate Tectonics

More information

Earth. Temp. increases with depth, the thermal gradient is 25 o C/km. Pressure and density also increase with depth.

Earth. Temp. increases with depth, the thermal gradient is 25 o C/km. Pressure and density also increase with depth. Plate Tectonics Earth Earth overall average density = 5.5 g/cm 3. Temp. increases with depth, the thermal gradient is 25 o C/km. Pressure and density also increase with depth. Spheroid: with a longer major

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

PART A: Short-answer questions (50%; each worth 2%)

PART A: Short-answer questions (50%; each worth 2%) PART A: Short-answer questions (50%; each worth 2%) Your answers should be brief (just a few words) and may be written on these pages if you wish. Remember to hand these pages in with your other exam pages!

More information

12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time

12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7 Stanley C. Hatfield Southwestern Illinois College Continental drift: an idea before its time Alfred Wegener First proposed

More information

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation)

1. I can describe evidence for continental drift theory (e.g., fossil evidence, mountain belts, paleoglaciation) Science 10 Review Earth Science Vocabulary asthenosphere continental drift theory converging plates diverging plates earthquakes epicentre fault hot spot inner core lithosphere mantle mantle convection

More information

10/27/2014. Before We Begin, You Need to Understand These Terms: Earth s Structural Key Elements & the Hazards of Plate Movement

10/27/2014. Before We Begin, You Need to Understand These Terms: Earth s Structural Key Elements & the Hazards of Plate Movement Earth s Structural Key Elements & the Hazards of Plate Movement Before We Begin, You Need to Understand These Terms: Density Convection Currents AICE EM: Lithosphere Key Content 1 & 2 Density: heat rises,

More information

TEST NAME:Geology part 1 TEST ID: GRADE:06 - Sixth Grade SUBJECT:Life and Physical Sciences TEST CATEGORY: My Classroom

TEST NAME:Geology part 1 TEST ID: GRADE:06 - Sixth Grade SUBJECT:Life and Physical Sciences TEST CATEGORY: My Classroom TEST NAME:Geology part 1 TEST ID:1542715 GRADE:06 - Sixth Grade SUBJECT:Life and Physical Sciences TEST CATEGORY: My Classroom Geology part 1 Page 1 of 6 Student: Class: Date: 1. The picture below shows

More information

Origin of the Oceans II. Earth A Living Planet. Earthquakes and Volcanoes. Plate Tectonics II

Origin of the Oceans II. Earth A Living Planet. Earthquakes and Volcanoes. Plate Tectonics II Origin of the Oceans II Plate Tectonics II Earth A Living Planet Heat of formation of the planet is trapped at center, gradually escaping Center is nickel and iron Earthquakes and Volcanoes 1 Tracing the

More information

Topic 12: Dynamic Earth Pracatice

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

More information

Earth and Space Science Semester 2 Exam Review. Part 1. - Convection currents circulate in the Asthenosphere located in the Upper Mantle.

Earth and Space Science Semester 2 Exam Review. Part 1. - Convection currents circulate in the Asthenosphere located in the Upper Mantle. Earth and Space Science 2015 Semester 2 Exam Review Part 1 Convection -A form of heat transfer. - Convection currents circulate in the Asthenosphere located in the Upper Mantle. - Source of heat is from

More information

PLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence

PLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence Continental Drift PLATE TECTONICS E.B. Taylor (1910) and Alfred Wegener (1915) published on Continental Drift. Continental Drift Wegener s evidence 1. Fit of the Continents 2. Fossil Evidence 3. Rock Type

More information

Chapter 4: Plate Tectonics

Chapter 4: Plate Tectonics Chapter 4: Plate Tectonics K2 in the Himalaya, inset round submersible (beneath the submarine) that went to the Marianas Trench in 1960 http://www.nydailynews.com/news/world/james-cameron-presents-record-setting-deep-sea-expedition-article-1.1215139

More information

RAYMOND SIEVER Harvard University

RAYMOND SIEVER Harvard University E A R T H FOURTH EDITION FRANK PRESS National Academy of Sciences RAYMOND SIEVER Harvard University W. H. Freeman and Company New York Preface xiii Acknowledgments xviii PART I PROLOGUE CHAPTER 1 HISTORY

More information

Geophysics for Environmental and Geotechnical Applications

Geophysics for Environmental and Geotechnical Applications Geophysics for Environmental and Geotechnical Applications Dr. Katherine Grote University of Wisconsin Eau Claire Why Use Geophysics? Improve the quality of site characterization (higher resolution and

More information

Questions and Topics

Questions and Topics Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that

More information

Chapter 2 Plate Tectonics and the Ocean Floor

Chapter 2 Plate Tectonics and the Ocean Floor Chapter 2 Plate Tectonics and the Ocean Floor Chapter Overview Much evidence supports plate tectonics theory. The plate tectonics model describes features and processes on Earth. Plate tectonic science

More information

THE INTERNAL STRUCTURE OF THE EARTH

THE INTERNAL STRUCTURE OF THE EARTH UNIT 1 THE INTERNAL STRUCTURE OF THE EARTH 1.1.Earth s interior layers The interior of the Earth can be divided into layers according to: -Composition layers ( organized in order of increasing density

More information

Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name

Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name Geology 300, Physical Geology Spring 2019 Quiz Ch 19, Plate Tectonics Name MULTIPLE CHOICE. Choose the one alternative that best completes the statement or answers the question. 1) The portion of a fracture

More information

Chapter 2: Plate Tectonics: A Unifying Theory

Chapter 2: Plate Tectonics: A Unifying Theory Chapter 2: Plate Tectonics: A Unifying Theory Chapter Outline 2.1 Introduction 2.2 Early Ideas About Continental Drift 2.3 What Is the Evidence for Continental Drift? 2.4 Features of the Seafloor 2.5 Earth

More information

12. The diagram below shows the collision of an oceanic plate and a continental plate.

12. The diagram below shows the collision of an oceanic plate and a continental plate. Review 1. Base your answer to the following question on the cross section below, which shows the boundary between two lithospheric plates. Point X is a location in the continental lithosphere. The depth

More information

Plate Tectonics: A Scientific Revolution Unfolds

Plate Tectonics: A Scientific Revolution Unfolds Chapter 2 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Plate Tectonics: A Scientific Revolution Unfolds Tarbuck and Lutgens From Continental Drift to Plate Tectonics Prior to the

More information

Last Time. Today s s Agenda. Geophysics. Geophysics. Geophysics. MAS 603: Geological Oceanography. Lecture 21: Geophysics 1: Gravity

Last Time. Today s s Agenda. Geophysics. Geophysics. Geophysics. MAS 603: Geological Oceanography. Lecture 21: Geophysics 1: Gravity UNIVERSITY OF SOUTH ALABAMA Last Time MAS 603: Geological Oceanography Extinctions Lecture 21: 1: http://www.cartoonstock.com/newscartoons/cartoonists/for/lowres/forn441l.jpg Today s s Agenda Introduction

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

Plate Tectonics. The Theory of Plate Tectonics. The Plate Tectonics Theory. 62 Plate Tectonics Reading Essentials

Plate Tectonics. The Theory of Plate Tectonics. The Plate Tectonics Theory. 62 Plate Tectonics Reading Essentials CHAPTER 4 LESSON 3 Tectonics The Theory of Tectonics Key Concepts What is the theory of plate tectonics? What are the three types of plate boundaries? Why do tectonic plates move? What do you think? Read

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

Structure of the Earth

Structure of the Earth Structure of the Earth Compositional (Chemical) Layers Crust: Low density Moho: Density boundary between crust and mantle Mantle: Higher density High in Magnesium (Mg) and Iron (Fe) Core: High in Nickel

More information

Chapter 12 Lecture. Earth: An Introduction to Physical Geology. Eleventh Edition. Earth s Interior. Tarbuck and Lutgens Pearson Education, Inc.

Chapter 12 Lecture. Earth: An Introduction to Physical Geology. Eleventh Edition. Earth s Interior. Tarbuck and Lutgens Pearson Education, Inc. Chapter 12 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Earth s Interior Tarbuck and Lutgens Earth s Internal Structure Earth s interior can be divided into three major layers defined

More information

Earth s Interior. Theory of Tectonics. Tectonics & Landforms. Vocabulary

Earth s Interior. Theory of Tectonics. Tectonics & Landforms. Vocabulary Vocabulary Earth s Interior Theory of Tectonics Tectonics & Landforms Earthquake Volcano 100 100 100 100 100 100 200 200 200 200 200 200 300 300 300 300 300 300 400 400 400 400 400 400 500 500 500 500

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