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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 Earth Systems 3209 Unit: 4 The Forces Within Earth Reference: Chapters 4,

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Copyright © 2014 All rights reserved, Government of Newfoundland and Labrador

Earth Systems 3209

Unit: 4The 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.

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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 526-539Figure 19.17, pg. 528

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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

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Ocean Ocean Crust

Moho Magma Continental 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.

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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 532 - 33

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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 532 - 33

Rift Valley

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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 532 - 33

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Evolution of Rift Valley into a Divergent Plate Boundary

Text Reference:Pages 532 - 33

D) As both continue, the landmasses on both sides of the ridge continue to move apart from one another.

Examples: East African Rift Valley

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Sample Problem

Using a labelled diagram, briefly describe whathappens 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.

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Plate Boundaries - SUMMARY

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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

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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

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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

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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

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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.