Dynamic Earth

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    Dynamic Earth - Presentation Transcript

    1. Dynamic Earth Dr. Jennifer Wright
    2. Shake, Rattle, ‘n Roll
      • Plate Tectonics – the big picture, creation of the major geographic features of the Earth
        • Layers of the Earth
        • Plate Boundaries
        • Earthquakes
        • Volcanoes
        • Impact Craters
    3. Layers of the Earth
      • Inner core
        • Solid Fe, Ni
      • Outer core
        • Liquid Fe, Ni
        • Creates magnetic field
      • Mantle
        • Magma, convection
      • Crust
        • Thinnest, coldest layer
        • Plates!!
    4. Plate Tectonics
      • Framework for understanding most geographic features of the planet
        • Mountain ranges, volcanoes, earthquakes
        • Deepest point (Marianas Trench), Highest point (Mt. Everest) caused by plate interaction
      • 3 kinds of plate boundaries
        • Divergent
        • Convergent
        • Transform
    5. Divergent Boundaries
      • Are the result of “pulling” forces
      • Have small earthquakes
      • Create many normal faults
      • Are usually on the opposite side of the plate from a convergent boundary
    6. Convergent Boundaries
      • Collision of two plates
      • Have all the large earthquakes
      • 90% of all earthquakes happen here
      • Ocean-continent collisions = subduction
      • Explosive volcanoes
      • Reverse faults
    7. Transform Boundaries
      • Are the result of parallel and opposite forces
      • Have small to medium earthquakes earthquakes
      • Create strike-slip faults
      • Can cause streams to turn at right angles
    8. Earthquakes
      • Mostly happen on plate boundaries
        • 90% happen on convergent boundaries
      • Seismographs can record earthquakes from all over the world above 2.5-3 on magnitude scale
      • Are a release of energy as two blocks move relative to each other
      • Are measured on a logarithmic scale (multiply by 10)
    9. Volcanoes
      • Mostly created by melting of oceanic plate in the subduction zone and by hot spots in the mantle
      • Explosive volcanoes associated with dissolved gases (H 2 O) in lava
        • Ex. Mt. St. Helen’s
    10. Impact Craters
      • Far fewer visible impacts than other planetary bodies
        • Atmosphere
        • Oceans
        • Erosion/deposition
      • High velocity of impacts vaporize the meteor
      • Chesapeake Bay was created by an impact ~36 million years ago
        • Most earthquakes in the region today are due to settling from impact and glacial rebound
        • Contamination by saltwater limits the freshwater available today
    11. Classroom Activities
      • Plate Boundaries
        • Plot earthquakes on maps
        • Graph earthquakes based on depth, magnitude, and boundary type
          • Earthquakes on convergent boundaries are deeper and larger
        • For more advanced students, locate the epicenter using “Virtual Earthquake”
        • Plot volcanoes to locate plate boundaries (convergent) and hot spots (Hawaii)
      • Discuss the week’s planetary events in terms of potential human impact
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