Basin Analysis. Stra-graphy

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

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

Sedimentary Basin Analysis http://eqsun.geo.arizona.edu/geo5xx/geos517/ Sedimentary basins can be classified based on the type of plate motions (divergent, convergent), type of the lithosphere, distance

TYPES OF SEDIMENTARY BASINS, MECHANISM OF BASIN FORMATION & PETROLEUM HABITAT BY S. K.BISWAS

TYPES OF SEDIMENTARY BASINS, MECHANISM OF BASIN FORMATION & PETROLEUM HABITAT BY S. K.BISWAS BASIN DEFINITION, CHARACTERISTICS & CLASSIFICATION A sedimentary basin is a structurally morphotectonic depression

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,

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. 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,

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

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

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

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 >>>

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.

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

Plate Tectonics. Theory of Plate Tectonics. What is Plate Tectonics. Plate Tectonics Plate Boundaries Causes of Plate Tectonics

Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics Plate Tectonics What is Plate Tectonics The Earth s crust and upper mantle are broken into sections called plates Plates

Plate Boundaries & Resulting Landforms

Plate Boundaries & Resulting Landforms Divergent Plate Boundaries (plates being pulled apart) Type: oceanic plates Description: rising magma gently lifts the crust creating a ridge. The flow of convection

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

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

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

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

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

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

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

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

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

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

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

Crustal Activity. Plate Tectonics - Plates - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones

Name: Date: Period: Tectonics The Physical Setting: Earth Science CLASS NOTES Tectonics - s - Lithosphere - Asthenosphere - Earth s surface consists of a major plates and some minor ones The plates are

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

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

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,

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

Plate Boundaries. Presented by Kesler Science

Presented by Kesler Science Essential Questions: 1. What is plate tectonics? 2. What are the three types of plate boundaries? 3. What crustal features are formed at plate boundaries? Quick Action INB Template

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

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

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

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

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

Plate Tectonics GEOL 101 Lecture 22 How Are Mountains Built?

Plate Tectonics GEOL 101 Lecture 22 How Are Mountains Built? The Grand Tetons, Wyoming First a Brief Review of Sea Floor Spreading Prop: Test 3 Invitations Break-Up of a Continent and Origin of an Ocean

Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6

Topics Laramide Orogeny: Late Cretaceous to Early Eocene Reading: GSA DNAG volume 3, Ch. 6 Late Cretaceous to early Eocene New patterns developed 5 main regions Tectonic interpretations Post-Laramide events

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

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

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

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)

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)

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

Chapter. Graphics by Tasa Graphic Arts. Inc.

Earth Chapter Plate Science 9 Tectonics Graphics by Tasa Graphic Arts. Inc. 1 I. Earth s surface is made up of lithospheric plates. A. Lithospheric plates are composed of the crust and part of the upper

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

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

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

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates.

Plates & Boundaries The earth's continents are constantly moving due to the motions of the tectonic plates. As you can see, some of the plates contain continents and others are mostly under the ocean.

Unit 1: Earth as a System. Section 1: Plate Tectonics and the Rock Cycle

Unit 1: Earth as a System Section 1: Plate Tectonics and the Rock Cycle Earth s Realms Earth is divided into 4 major realms: Atmosphere gases surrounding earth Hydrosphere - earth s supply of water Lithosphere

PLATE TECTONICS REVIEW GAME!!!!

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

Geology of the Hawaiian Islands

Geology of the Hawaiian Islands Class 3 20 January 2004 Any Questions? IMPORTANT Big Island Field Trip We need a firm commitment PLUS $164 payment for airfare BEFORE January 29th Plate Tectonics Fundamental

Plate Tectonics: The New Paradigm

Earth s major plates Plate Tectonics: The New Paradigm Associated with Earth's strong, rigid outer layer: Known as the lithosphere Consists of uppermost mantle and overlying crust Overlies a weaker region

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

Mountains form along convergent plate boundaries. Typically (usually) if you look at a mountain range, you know that it is at a plate boundary (active continental margin) or has been some time in the past

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

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

The Lithosphere and the Tectonic System. The Structure of the Earth. Temperature 3000º ºC. Mantle

The Lithosphere and the Tectonic System Objectives: Understand the structure of the planet Earth Review the geologic timescale as a point of reference for the history of the Earth Examine the major relief

Learning Objectives (LO)! Lecture 11: Plate Tectonics II! No Homework!! ** Chapter 3 **! What we ll learn today:!

Learning Objectives (LO)! Lecture 11: Plate Tectonics II! No Homework!! ** Chapter 3 **! What we ll learn today:! 1. List the three types of tectonic plate boundaries! 2. Describe the processes occurring

7 Sedimentation and tectonics at a mid- Ordovician to Silurian active margin

80 Mountain Building in Scotland 7 Sedimentation and tectonics at a mid- Ordovician to Silurian active margin 7.1 Introduction In mid-ordovician to Silurian times, the Grampian mountains underwent exhumation,

Contractional Tectonics: Convergence and Collision

Contractional Tectonics: Convergence and Collision Processes in Structural Geology & Tectonics Ben van der Pluijm WW Norton+Authors, unless noted otherwise 4/12/2017 5:21 PM We Discuss Contractional Tectonics

Theory of Continental Drift

Plate Tectonics Theory of Continental Drift Alfred Wegener suggested that continents had once been part of a supercontinent named Pangaea, that later broke up. The pieces moved apart over millions of years

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

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.

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

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

PLATE TECTONICS Alfred Wegener thought that the landmasses fit together like a jigsaw puzzle. He called the land mass Pangaea. Meaning all land Continental Drift Wegener theory first coining the word -

Sir Francis Bacon, 1620, noted that the continental coasts on opposites sides of the Atlantic fit together like puzzle pieces.

Plate Tectonics Sir Francis Bacon, 1620, noted that the continental coasts on opposites sides of the Atlantic fit together like puzzle pieces. Could North and South America once have been joined to Europe

Introduction To Plate Tectonics Evolution. (Continents, Ocean Basins, Mountains and Continental Margins)

Introduction To Plate Tectonics Evolution (Continents, Ocean Basins, Mountains and Continental Margins) Geo 386 (Arabian Shield Course) Dr. Bassam A. A. Abuamarah Mohanna G E O 3 8 6 A R A B I A N G E

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

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

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

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

SEDIMENTARY BASINS BASIN TYPES ACCORDING TO TECTONIC. by Prof. Dr. Abbas Mansour

SEDIMENTARY BASINS BASIN TYPES ACCORDING TO TECTONIC by Prof. Dr. Abbas Mansour B. Convergent plate margins 10. STABLE CONTINENTAL INTERIOR BASIN E.g. Lake Eyre Basin Intracratonic (= within stable continental

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

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.

GCSE Geology Plate Tectonics: Features and Processes

GCSE Geology Plate Tectonics: Features and Processes A) DIVERGENT BOUNDARIES: 1. O-O Divergence, Example: The Mid-Atlantic Ridge, Iceland The North American and Eurasian Plates are moving away from each

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

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

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

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

Chapter 8-1 Plate Tectonics 1. Brainstorm the type of evidence that would indicate a climate change and how this evidence supports the theory of continental drift. Tropical fossils in cold regions Evidence

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

UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA

UNIT 3 GEOLOGY VOCABULARY FLASHCARDS THESE KEY VOCABULARY WORDS AND PHRASES APPEAR ON THE UNIT 3 CBA A map that shows Earth s Topographic Map surface topography, which is Earth s shape and features Contour

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

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

Sedimentary Basins. Gerhard Einsele. Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Hong Kong Barcelona Budapest

Gerhard Einsele Sedimentary Basins Evolution, Facies, and Sediment Budget With 269 Figures Springer-Verlag Berlin Heidelberg New York London Paris Tokyo Hong Kong Barcelona Budapest Contents Part I Types

Layer Composition Thickness State of Matter

Unit 4.2 Test Review Earth and Its Layers 1. Label the layers of the earth. oceanic crust continental crust lithosphere asthenosphere mantle outer core inner core 2. Complete the Following Table about

NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2

NAME HOMEWORK ASSIGNMENT #4 MATERIAL COVERS CHAPTERS 19, 20, 21, & 2 Assignment is due the beginning of the class period on December 14, 2004. Mark answers on a scantron sheet, which will be provided.

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

What Are Tectonic Plates?

Plate Tectonics The theory that the Earth s outermost layer is fragmented into a dozen or more large and small plates that move relative to one another as they ride on top of hotter, more mobile material.

Lecture 4.1 Continental Drift

Plate Tectonics Chapter 4 California Science Content Standards Covered: Big Ideas 3A: Students know the features of the ocean floor that provide evidence of plate tectonics Mid Ocean Ridges (ex. Mid Atlantic

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

Plate Tectonics Tutoiral. Questions. Teacher: Mrs. Zimmerman. Plate Tectonics and Mountains Practice Test

Teacher: Mrs. Zimmerman Print Close Plate Tectonics and Mountains Practice Test Plate Tectonics Tutoiral URL: http://www.hartrao.ac.za/geodesy/tectonics.html Questions 1. Fossils of organisms that lived

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

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

Notebook 7a and 7b Objective (left-side): Students will be able to explain the theory of plate tectonics and be able to make predictions about plate interactions. Mapping Reflection 1. What is Wegener

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

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

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

Sequence Stratigraphy. Historical Perspective

Sequence Stratigraphy Historical Perspective Sequence Stratigraphy Sequence Stratigraphy is the subdivision of sedimentary basin fills into genetic packages bounded by unconformities and their correlative

Plate Tectonics. Goal 2.1

Plate Tectonics Goal 2.1 Lesson 1 Plate Tectonics: An Overview Think About It Look at the map below. Which two continents look like they d fit together? Focus Question How do Earth s tectonic plates cause

Earth s Continents and Seafloors. GEOL100 Physical Geology Ray Rector - Instructor

Earth s Continents and Seafloors GEOL100 Physical Geology Ray Rector - Instructor OCEAN BASINS and CONTINENTAL PLATFORMS Key Concepts I. Earth s rocky surface covered by of two types of crust Dense, thin,

Continental Drift. Wegener theory that the crustal plates are moving and once were a super continent called Pangaea.

PLATE TECTONICS WHAT IS TECTONICS? Tectonism is the faulting or folding or other deformation of the outer layer of a planet. It happens very slowly, on the scale of millions of years. Tectonic activity

83% 25 of 30 Correct. Dynamic Earth Assessment Test Results. Name: Marc Sto. Domingo Date: October 2, 2013

Dynamic Earth Assessment Test Results Name: Marc Sto. Domingo Date: October 2, 2013 83% 25 of 30 Correct Review the questions and your answers below. The answer you selected is highlighted in red, the

Plate tectonics - 3. Homework 1: Due Monday. Hot Spots Magnetic Reversals Isostasy Continental Tectonics. EESC 2200 The Solid Earth System.

2500 EESC 2200 The Solid Earth System Plate tectonics - 3 17 Sep 08 Hot Spots Magnetic Reversals Isostasy Continental Tectonics Depth (m) 6000 0 9 36 100 155 Homework 1: Due Monday Review: Fracture zone

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

Earth Science ENR Plate Boundaries Notes

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