Explore the dynamic earth and ocean off Canada's Pacific coast

 

Plate tectonics and GPS lesson plans:

Grade 10: The Earth Moves Under Our Feet (click here for PDF version)

Grade 7: Where in the World Are We Going? (click here for PDF version)

Overview Students use near real-time data to demonstrate that tectonic plates are moving and to calculate the velocity and direction of crustal deformation at different locations.

Duration:

Two fifty minute classes or one class plus homework.

Objectives:
Students will…

  • Visualize the movement of the Juan de Fuca, Pacific and North American plates relative to each other, using images and animations
  • Identify features connected to plate movement and geologic situation in British Columbia and adjacent ocean.
  • Utilize near real-time data, graphing and formula for line to calculate average yearly velocity and direction
  • Graph resulting vectors for Victoria and Seattle and discuss implications of findings

Vocabulary:

 

 

 

(With help from Clague et al, 2006, At Risk: Earthquakes and Tsunamis on the West Coast.)
Continental crust The crust under continents (up to 60 km. thick). Rock is rich in silicon and aluminum (granitic) and is less dense than oceanic crust.
Continental shelf – Submerged shallow (<200m) fringe around continent which is part of continental plate.
Continental slope – The slope leading from the shelf to the abyss.
Crust – The outermost layer of the Earth.
Divergent boundary (oceanic) – Site of spreading found at sub-sea ridge where two plates are created from magma and move in opposite directions, for example Juan de Fuca and Pacific move east and west from Juan de Fuca Ridge.
Earthquakes – A sudden release of energy from strain built up in the Earth’s crust, usually located near plate boundaries.
Juan de Fuca plate – The oceanic plate in the deep ocean off of southwestern British Columbia, Washington and Oregon states and the northern part of California.
Juan de Fuca Ridge – The active volcanic section of the mid-ocean ridge that separates the Juan de Fuca and Pacific plates
North American plate – One of the large continental plates, that forms the crust of the Earth.
Oceanic crust – Crust on ocean floor (up to 8km. thick). Rock rich in silicon and magnesium and much more dense than continental crust.
Pacific Plate – One of the large oceanic plates that forms the crust of the Earth.
Plate tectonics – Generally accepted theory that the Earth’s crust is made up of crustal plates of different sizes that “float” on a plastic upper mantle and move more or less independently of one another. Dynamic earthquake activity is associated with the boundaries of these plates. Oceanic plates are pushed from the rear by seafloor spreading and pulled by subduction under the continent.
Subduction zone –The over-lapping part of the crust where one plate (such as a dense oceanic plate) descends at an angle under another plate (such as a lighter continental plate).
Tsunamis – Series of waves made by a major disturbance on the ocean floor such as a submarine earthquake, landslide, volcanic eruption or by impact from outer space. Trench – A long narrow deep area of the ocean floor where flexing oceanic plates slide down and under a lighter, less dense plate. 
Sub-sea ridge – An underwater divergence boundary where new plate material is pushed out as magma and cools in long fractures on the sea floor. See Juan de Fuca  Ridge.


British Columbia PLO’s: Science 10

Processes of Science
- A7 Demonstrate competence in the use of technologies specific to investigative procedures and research
Earth and Space Science
- D4 Analyze the processes and features associated with plate tectonics
- D5 Demonstrate knowledge of evidence that supports plate tectonic theory
Physical Science
- C6 explain the relationship of displacement and time interval to velocity for objects in motion
Principles of Math 10
- Examine the nature of relations with an emphasis on functions
- Represent data, using linear function models


Background:

  • See OceanLink SOLE web-pages under Dynamic Earth: Geology – Plate tectonics.
  • The PowerPoint presentation which is downloadable, has more background information specific to British Columbia’s geologic situation and pertinent to completing the worksheet.

Materials:

  • PowerPoint presentation
  • Animations* (see below) that model locked and slipping components of subduction including strain over time, distance over time and episodic tremor and slip (available on OceanLink SOLE web-pages)
  • Worksheet (available on OceanLink SOLE web-pages), pencils, calculators.

Procedure:

  1. Download the PowerPoint presentation on Tectonic plates (13 mb) and show to the class.
  2. Download and use the Grade 10 worksheet* with instructions to understand how the first calculation of average annual velocity was made for Eastward movement at the Albert Head GPS station in Victoria. Complete other three calculations in data table for Northward movement in Victoria and both directions in Seattle. Using the easting and northing magnitudes determine the velocity vector for each city and complete the discussion questions either in class or as homework.

Discussion:

  • See discussion questions on worksheet.

Extension Activities and Resources:

*This work is partially based on materials provided by the UNAVCO Education and Outreach Program with support from the National Science Foundation and NASA under NSF Cooperative Agreement No. EAR-0735156 and EAR-0453975

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