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INVESTIGATING PLATE MOVEMENT AND FAULTS

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Title: INVESTIGATING PLATE MOVEMENT AND FAULTS


1
LESSON 15
  • INVESTIGATING PLATE MOVEMENT AND FAULTS

2
INTRODUCTION
  • What does the word model mean to you?
  • Miniature version
  • Used for study
  • Somethings too large to view

3
OBJECTIVES
  • Describe what a model is and distinguish models
    from real objects or events. Use models to
    simulate the movement of lithospheric plates as
    they collide, separate, and slide past one
    another.
  • Use a globe and a map to find evidence of plate
    movement and to identify landforms that result
    from plate movement.

4
  • Classify materials as either brittle or ductile.
  • Investigate the effects of applying a force to a
    model of a fault.

5
GETTING STARTED
  • Look at the wall map called This Dynamic
    Planet.
  • How is this map different from others you have
    seen?
  • How is it the same?

6
  • Look at student Sheet 14.1.
  • What patterns do you notice in the location of
    volcanoes and earthquakes?
  • Look at the plates shown on the map. Is there
    any relationship between the locations of
    earthquakes and volcanoes on the earth and the
    boundaries, or outer edges, of plates?
  • What ideas do you have to explain this
    relationship?

7
Lets view the CD-ROM, The Theory of Plate
Tectonics
  • Record the following in your notebooks
  • A. How do plates move?
  • B. How does plate movement cause earthquakes,
    volcanoes, mountains, and trenches?

8
MODELS
  • A. How are the map and computer images used in
    this lesson like the real earth? How are they
    different?
  • The map and computer images are models of the
    earth.
  • B. What are some examples of models?
  • Globe, map, tornado in a bottle
  • C. Write a working definition for the word
    model.
  • A representation of an object or event that is
    too large, too small or complicated to be viewed
    or studied.
  • Lets look at the models well use for this
    lesson.

9
Inquiry 15.1Using a Simple Model of Plate
Movement
  • Look at the blue and green foam pads used in this
    activity and record their properties.
  • Density, appearance, thickness, weight, and
    size.

10
Predict
  • How would each pad respond if we did the
    following
  • Pulled on the pad from opposite ends
  • Pushed on the pad at opposite ends
  • Slid two pads past one another
  • Collided two pads by pushing them together

11
Test and Record
  • As each foam pad is demonstrated, record in your
    notebook what happens. Use a table to record your
    observations.
  • pull push slide collide

12
REFLECTIONS 15.1
  • A. How did the pads behave when pulled from
    opposite ends?
  • The pads were stretched thin. The blue pad was
    more stretchy.
  • B. How did the pads behave when compressed?
  • The pads foldedresembling mountains

13
  • C. If oceanic plates are colder, denser, and
    thinner than continental plates are, which pad do
    you think represented oceanic plates? Which pad
    represented continental plates?
  • The thin, blue, dense pads represented oceanic
    plates. The thick green pads represented
    continental plates.
  • D. How did the density of the pads affect the
    way they behaved when you made them collide?
  • The dense blue pads always moved beneath the less
    dense green pads.

14
  • E. When do colliding plates on the earth form
    mountains?
  • Mountains form when two continental plates of a
    similar density collide.
  • F. When do colliding plates form trenches?
  • Trenches form when a dense oceanic plate collides
    with a less dense continental plate.
  • G. Why would a more dense oceanic plate slide
    under a less dense continental plate?
  • Something more dense usually moves beneath
    something less dense.

15
  • H. Can plates ever move without forming new
    land? If so, when?
  • No new land forms when plates slide past one
    another.
  • I. How do you think colliding plates on the
    earth cause earthquakes?
  • Colliding plates either bend or fracture the
    land earthquakes can form when rock fractures.

16
Read pgs. 174, 175
  • Colliding, Sliding, and Separating Plates

17
INQUIRY 15.2Using the Moving Plates Model
  • Turn to page 176 in your Catastrophic Events book
    and follow the procedure listed as its
    demonstrated for you.

18
REFLECTIONS 15.2
  • A. How do you think the Moving Plates Model shows
    what happens on the earth when two plates
    separate?
  • It shows the form they took as they moved.
  • B. What causes the ocean floor to separate and
    grow?
  • Newly melted rock rises and pushes aside the old
    rock.

19
  • C. Think about what happened to the black belt as
    it reached the edges of the models lid. What
    landform is created when the ocean floor sinks
    back into the earth?
  • A trench forms
  • D. What patterns did you observe in the shapes
    of Africa and South America?
  • They fit together like puzzle pieces.

20
  • E. How did the shapes of these continents
    compare with the shape of the Mid-Atlantic Ridge?
  • The MAR has the same shape as the coastlines of
    these continents, which border the Atlantic.
    This is because the continents broke apart as the
    ridge formed.
  • F. What landform is created when plates separate?
    Give an example.
  • A ridge forms. Ex The Mid-Atlantic Ridge.

21
  • G. What landform is created when two continental
    plates collide? Give an example.
  • A mountain forms. Ex The Appalachian Mountains
    (North Amer)

22
INQUIRY 15.3Investigating Faults With Models
  • Turn to page 179, 181 in your Catastrophic Events
    book and follow the procedure listed on these
    pages.

23
REFLECTIONS 15.3
  • A. How did the amount of friction along the
    fault affect the amount of force needed to
    rupture the fault? Use data to support your
    answer.
  • The greater the friction, the more force is
    needed to rupture the fault. The hooks and loops
    of the Velcro act like protrusions that connect
    the rock across the rock.

24
  • B. Under what conditions did the blocks rupture
    more abruptly?
  • The greater the force applied to the block, the
    more abrupt the rupture.
  • C. Under what conditions did the block slip
    (more slowly) but not rupture?
  • When two strips of loop Velcro are side by side,
    the friction along the fault was at its lowest.
    When resistance along a fault is low, blocks of
    rock can slip without faulting.

25
  • D. Think about what happened with the masking
    tape. Is there any sign on the earths surface
    that the earth is moving slowly beneath the
    crust?
  • Wrinkles in a sidewalk or on a road are signs
    that pressure is building up along a fault. This
    is called creep.
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