Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,

Slides:



Advertisements
Similar presentations
DO NOW Take out last night’s homework – Continental Drift vs. Sea-Floor Spreading handout Turn to your neighbor and share your answers with your neighbor.
Advertisements

Plate Tectonics Review
EQ: What is the theory of plate tectonics?
The Theory of Plate Tectonics - Boundaries, Stresses, and Faults
Chapter 7: Plate Tectonics
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Plate Tectonics. Types of Plate Boundaries Divergent Convergent Transform.
Plate Boundaries  According to the Plate tectonic theory, three boundaries exist at the edges of each tectonic plate. 1) Divergent Boundary (Ridge) 2)
Plate Tectonics Objective(s): SWBAT describe the layers of the Earth. SWBAT describe the plate tectonics theory including, how plate tectonics operating.
8.2Types of plate boundaries
1.3 Notes Plates Move Apart.
Plate Tectonics: What changes the positions of the continents over time? DIVERGENT BOUNDARIES.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
PLATE TECTONICS Why the Earth is Like It Is. Earth Layers Earth is made up of 5 layers: 1.Inner Core 2.Outer Core 3.Mantle 4.Asthenosphere (Lower and.
April 17 Plate Tectonics Allen.
Ch. 4.2 The Theory of Plate Tectonics
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Essential Questions How does the movement of Earth’s tectonic plates result in many geologic features? What are the three types of plate boundaries and.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
What type of boundary is represented here?
Plate Tectonics Causes of Plate Tectonics Plate Boundaries.
Chapter 9 Plate Tectonics.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Plate Tectonics Evolution of the Earth.
Continental Drift Theory Plate Tectonics How the crust.
Chapter 7 Section 1: Continental Drift Section 2 : Sea Floor Spreading
Obj: What is the Theory of Plate Tectonics? Copy the following questions in your notebook: TABLE 1 (7)- What is a mid ocean ridge? TABLE 2 (8)-What is.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Plate tectonics volcanoes EEn Explain how plate tectonics, and volcanoes impact the lithosphere. I. Plate Tectonics Chapter 9, Section 2 A. Actions.
Our Amazing Planet. Planet Earth Earth’s Layers Crust Earth’s thin outermost layer. – Continental Crust (land) - thick low density rock (granite). –
 The theory of plate tectonics explains the formation, movements, and subduction of the earth’s plates. ◦ What is a plate?  A section of lithosphere.
EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens 
Plate Tectonics.
Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)
Plate Tectonics, Continental Drift, Faults and Folds Chapter 7 Sections 1-4.
Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Plate Boundary Volcanism Reference: Tarbuck and Lutgens Pages Volcanoes are associated with two of the three types of plate boundaries, these.
Plate Tectonics The theory of plate tectonics is based on the theory that plate tectonics explain the formation, movement, and subduction of Earth’s plates.
Theory of Plate Tectonics
Plate Boundary Volcanism Reference: Pages & 557 Volcanoes are associated with two of the three types of plate boundaries, these being convergent.
Intro Objective 10/5/11 Describe the three types of tectonic plate boundaries. What do you think forms when two tectonic plates collide? What about when.
Plate Boundaries Earth’s crust plus the upper mantle forms the lithosphere. Earth’s lithosphere is broken in a number of different pieces. How these pieces.
The Problem with Continental Drift While Wegener was able to find evidence of continental drift, there were 2 major problems with his ideas: – Wegener.
THEORY OF PLATE TECTONICS CHAPTER 10 SECTION 3 PAGE By: Brielle, Rachel, and Alec.
Which plate boundary is represented?. Convergent Boundary.
Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,
Plate Tectonic Recap and Review Convergent Boundary Possibilities Ocean crust meets continental crust Ocean crust meets ocean crust continental crust.
Divergent Boundaries (aka constructive boundaries) Rising convection currents force 2 plates apart Release of pressure on asthenosphere causes it to.
UNIT SIX: Earth’s Structure  Chapter 18 Earth’s History and Rocks  Chapter 19 Changing Earth  Chapter 20 Earthquakes and Volcanoes.
Continental Drift Theory The hypothesis that Earth’s continents move on Earth’s surface. Wegner proposed this theory Sea Floor Spreading a process in which.
Types of Plate Boundaries After completing this section, students will identify that the Earth is made of geologic plates (Standard PI-041) and investigate.
Theory of Plate Tectonics Chapter 10.3 pg SPI
PLATE TECTONICS Why the Earth is Like It Is What Did The Earth Look Like In The Past?
Plate Tectonics. Continental Drift _________ proposed the theory that the crustal plates are moving over the mantle. This was supported by fossil and.
Plate Tectonics. Plate Boundaries Causes of Plate Tectonics.
WHAT IS THE THEORY OF PLATE TECTONICS?  EARTH’S LITHOSPHERE, IS COMPOSED OF CRUST AND THE UPPER MANTLE.  Two types of crust: Continental and Oceanic.
 Lithosphere is broken into huge plates and float on the asthenosphere. How Plates Move.
Theory of Plate Tectonics. How do we know the plates exist?  Earthquake and Volcano Zones  Ocean floor features (Trenches and Mid-Oceanic ridges)
Chapter 9 Plate Boundaries.
Plate Tectonics Chapter 9. Theory of Plate Tectonics Plate Tectonics Plate Boundaries Causes of Plate Tectonics.
Catalyst TURN PROJECTS IN UP FRONT On a sticky note, summarize the Theory of Continental Drift.
Plate Movement Chapter 17 Section 3. Plate Tectonics Theory that describes how tectonic plates move and shape Earth’s surface –They move in different.
Plate Tectonics The crust in motion.
The Theory of Plate Tectonics - Boundaries, Stresses, and Faults
9-3 Theory of Plate Tectonics
The Theory of Plate Tectonics - Boundaries, Stresses, and Faults
The Theory of Plate Tectonics - Boundaries, Stresses, and Faults
The Theory of Plate Tectonics - Boundaries, Stresses, and Faults
Presentation transcript:

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4, 15, 16, 19; Appendix A & B

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Plate Boundaries - Divergent Unit 4: Topic 2.5 Focus on...  describing a rift valley and explaining how it evolves into a divergent boundary.  demonstrating through a drawing the processes associated with plate divergence.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Plate Boundaries  According to the Plate tectonic theory, three boundaries exist at the edges of tectonic plates. 1)Divergent Boundary (Ridge) 2)Convergent Boundary (Trench) 3)Transform Boundary Text Reference: Pages Figure 19.17, pg. 528

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador  A divergent plate boundary is characterized by two plates moving away from one another as a result of tensional forces exerted on them by convection currents in the upper mantle (Asthenosphere).  As the plates move apart, hot molten material upwells at the boundary forcing the edges of both plates upwards, creating a Ridge.  New ocean floor is created along the length of ridges. Divergent Plate Boundary

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador OceanOcean Crust MohoMagmaContinental Crust Divergent Plate Boundary  Divergent plate boundaries are referred to as constructive margins since new oceanic crust is being formed there.  Examples include; Mid-Atlantic ridge and Mid-Indian ridge.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador A)If tensional forces, due to the motion of convection currents in the upper mantle, begin beneath continents, it can cause continents to split into two or more smaller segments. Evolution of Rift Valley into a Divergent Plate Boundary Text Reference: Pages

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador B)A spreading center is formed and a rift valley is formed as a result of the associated faulting (normal) and thinning of the crust. Eventually the thinning becomes significant enough for ocean water to move into the rift valley. Evolution of Rift Valley into a Divergent Plate Boundary Text Reference: Pages Rift Valley

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Evolution of Rift Valley into a Divergent Plate Boundary C)Ridge (Rift) volcanism and seafloor spreading begin and a divergent plate boundary is produced. Text Reference: Pages

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Evolution of Rift Valley into a Divergent Plate Boundary Text Reference: Pages D)As both continue, the landmasses on both sides of the ridge continue to move apart from one another.  Examples: East African Rift Valley

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Sample Problem  Using a labelled diagram, briefly describe what happens at a mid-ocean ridge. Diagram: Answer: Tensional forces cause the plates to move apart resulting in upwelling of molten material from the mantle to create new ocean floor.

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Plate Boundaries - SUMMARY

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Example 1: At which of the following is crust being created? (A)ridge(C)trench (B)transform fault(D)subduction zone What rock type is generated at oceanic ridges? (A)andesite(C)dunite (B)basalt(D)granite

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Example 2: Which plate boundary does tensional forces dominate resulting in tectonic plates moving apart? (A)convergent(C)transform (B)divergent(D)subduction The rocks of the Avalon Peninsula and North Africa are similar. Which tectonic process was responsible for the separation of the Avalon from Africa? (A) Convergence(B) elastic rebound (C) Rifting(D) subduction

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Your Turn... Take the time and complete the following questions... (Solutions to follow) Question: Which sequence correctly illustrates the evolution of a divergent plate boundary? (A) 1, 2, 3, 4 (B) 1, 3, 2, 4 (C) 4, 2, 1, 3 (D) 4, 2, 3, 1

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Solutions... Question: Which sequence correctly illustrates the evolution of a divergent plate boundary? (A) 1, 2, 3, 4 (B) 1, 3, 2, 4 (C) 4, 2, 1, 3 (D) 4, 2, 3, 1

Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador Summary... Overview of Points covered: At Divergent Boundaries;  Plates move apart, resulting in upwelling of molten material from the mantle to create new ocean floor.  Features called Ridges are formed.  Tensional forces cause the plates to move apart.  New oceanic crust is being formed, and these boundaries are referred to as constructive margins.  Examples include; Mid-Atlantic ridge and Mid-Indian ridge.