Geology                     Natural Science 1003

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Ed Wehling
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NATS 1003
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Topic 2   Plate Tectonics

 

Primary Goals

  • Understand how plate tectonics is the fundamental, underlying, global force of Earth's geology
  • Understand what plate boundaries are like
  • Explain the geological evidence that supports plate tectonics

 

Topics

2.1  Plates  

  • Terms: Lithosphere, asthenosphere, plate (tectonic plate)

2.2  Plate boundaries  

  • Terms: Divergent plate boundary; convergent plate boundary; transform plate boundary

2.3  Evidence that plates move today  

  • Explanation: How do satellites tell us that the plates are moving today?

2.4  Evidence that plates moved in the past

  • 2.4.A  Explanation: Similarity of rock sequences on different continents today

           Term: rock layer sequence

  • 2.4.B  Explanation: Similarity of mountain ranges on different continents today

           Term: deformational style

  • 2.4.C  Explanation: Apparent motion of glaciers in the southern hemisphere in the past

  • 2.4.D  Explanation: Fossils in the southern hemisphere

  • 2.4.E  Explanation: Magnetic pole wandering   D2L explanation

  • 2.4.F  Explanation: Hot spot movement

  • 2.4.G  Pangaea

2.5  Divergent plate boundaries  

  • 2.5.A  Story: What happens at a divergent plate boundary?

  • 2.5.B  Explanation: What geologic activity occurs at a divergent plate boundary?

  • Explanation: How do mountains form at a divergent plate boundary?

  • 2.5.C  Question: Where do divergent plate boundaries exist?

  • 2.5.D  Story: Idealized development of a divergent plate boundary

2.6  Evidence that plates move apart at a divergent plate boundary  

  • Reminder: Satellites

  • 2.6.A  Explanation: Age of rocks

  • 2.6.B  Explanation: Pattern of magnetic polarity in rock

  • 2.6.C  Explanation: Depth of ocean sediments

  • 2.6.D  Explanation: Heat flow data

2.7  Convergent plate boundaries

  • Explanation: Different convergent boundaries exist depending on what type of crust is coming together

2.8  Subduction zones  

  • Analytical: How can you tell which crust will subduct below the other?

  • Explanation: What geologic activity occurs at a subduction zone?

2.9  What evidence do we have that subduction zones exist?  

  • 2.9.A  Explanation: Earthquake depths

  • 2.9.B  Explanation: Deep temps

2.10  Continent-continent convergent boundaries

  • Explanation: What geologic activity occurs at continent-continent convergent plate boundaries?

2.11  Transform plate boundaries  

  • Explanation: Transform boundaries at divergent plate boundaries

  • Explanation: What geologic activity occurs at transform plate boundaries?

2.12  Why do plates move?  

  • Explanation: Subducting plates drag lithosphere

  • Explanation: Newly formed plates push away lithosphere

  • Explanation: Gravity at divergent boundaries moves lithosphere

  • Explanation: Asthenosphere may carry lithosphere along

 

Topic Resources for students

Entire topic

2.4  Evidence that plates moved in the past

  • Animations of continental drift from U. of California
  • Hot spot animation from Houghton Mifflin
  • another hot spot animation from Norton
  • Continent movement video (a bit slow) 6 min

2.6  Evidence that plates move apart at a divergent plate boundary

  • Divergent boundary animation from Houghton Mifflin
  • another animation from the San Diego Supercomputer Center
  • Animation of formation of ocean crust
  • Animation of divergent boundary on continent
  • Animation of magnetic polarity at div boundary
  • Recent crack in East Africa rift valley

2.8  Subduction zones

2.10  Continent-continent convergent boundaries

  • Indian plate movement animation

Links for further interest

2.1  Plates

  • History of the development of Plate Tectonics theory from a South African perspective (interesting side note)

2.4  Evidence that plates moved in the past

  • PaleoMap project (great site)
  • Discussion of the formation of Hawaii from the U of Hawaii

 


©2000-2019     D. Edward Wehling                   Comments should go to ed.wehling@anokaramsey.edu

The views and opinions expressed on this page are strictly those of the page author.  The contents of this page have not been reviewed or approved by Anoka-Ramsey Community College.