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Unit 1: Earths Dimensions

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The Earth is called an oblate spheriod. It is flattened at the poles and bulged at the equator ... The Oblate Spheroid. The difference is small. We can not see ... – PowerPoint PPT presentation

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Title: Unit 1: Earths Dimensions


1
Unit 1 Earths Dimensions
  • Topic Change and Earths Shape
  • Objectives
  • 1. Differences between cyclic and non-cyclic
    changes
  • 2. Introduce evidence for Earths Shape

2
Objective 1
  • Graphs that show patterns illustrate a cyclic
    change

3
Cyclic changes
  • Day and night?
  • Yes
  • Seasons
  • Yes
  • Earthquakes
  • No

4
Objective 1
  • A BOUNDARY between the affected parts of the
    environment that causes an exchange of energy is
    called an
  • INTERFACE
  • Examples
  • layers of the atmosphere
  • weather fronts

5
Cyclic and the environment
  • If the change is cyclic, then it is said to be
    predictable!!!
  • Examples
  • The end of school?
  • Yes
  • Tornadoes
  • No

6
How did they prove the Earth to be round?
  • Ships appearing to sink as it travels over the
    horizon
  • Polaris (North Star) changes altitude directly
    with you latitude
  • Eclipses of the Earths shadow on the moon
  • Satellite Imagery

7
Ships appear to sink
8
Polaris Changes in Altitude
90º
9
Locating Polaris
10
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11
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12
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13
Is the Earth Perfectly round?
  • The Earth is called an oblate spheriod
  • It is flattened at the poles and bulged at the
    equator
  • How does weight determine that the Earth is not
    perfectly round?

14
Weight!!!
  • We are further from the center of the Earth at
    the equator
  • This means we weigh LESS!!!
  • We are closer at the poles
  • We weigh MORE!!!!

15
  • At the Poles we are closer to the center
    stronger gravity more weight

Center of Earth center of gravity
16
The Oblate Spheroid
  • The difference is small
  • We can not see it with the naked eye
  • It still appears like a sphere
  • Be careful on multiple choice
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