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Chapter 3 Models of the Earth

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Title: Chapter 3 Models of the Earth


1
Chapter 3Models of the Earth
2
3-1 Modeling the Planet
  • A.  Maps
  • a.   Map-A flat, two-dimensional representation
    of Earths surface.
  • b. Cartographers-A mapmaker who has devised
    tools to help a map user relate two-dimensional
    images on a map with the three-dimensional world.

3
3-1 Modeling the Planet
  • B.  Map Projections
  • a.   Projections-To reduce distortion,
    cartographers draw world maps in three different
    ways.
  • b.  Mercator-Depicts the earth as if it had been
    projected onto a large cylinder and then
    unwrapped. Areas at the poles are distorted in
    this projection.

4
3-1 Modeling the Planet
  • B.  Map Projections
  • c.   Gnomonic Projection- This projection is
    made as if a sheet of paper had been laid out on
    a given point on the earths surface. This
    projection distorts landmass shapes.
  • d. Polyconic Projection- In this projection it
    is as if a cone of paper has been wrapped around
    the earth. Lines of latitude and longitude are
    curved slightly. Most landforms have their true
    shape.

5
3-1 Modeling the Planet
  • C.  Latitude and Longitude
  • a.   A grid of imaginary lines placed on the
    earth.
  • b.  The earth is divided into Hemispheres. The
    Equator is the imaginary line dividing the north
    from the south. The Prime Meridian divides east
    and west.

6
3-1 Modeling the Planet
  • c.   The equator is a latitude line that circles
    the world from east to west. Latitude is
    measured in degrees north and south.
  • d. The prime meridian is a longitude line that
    runs from north to south. It is measured in
    degrees east and west.

7
3-1 Modeling the Planet
  • D.  Map Scales
  • a.   The scale on a map tells you how the maps
    features compare in size with the earths
    surface.
  • b.  This is depicted using a ratio. Ex. one
    inch equals one mile.
  • E.  Map Orientation
  • a. Always locate north. On new maps it is
    always on top. East is on the right, west on the
    left and south on the bottom.

Compass Rose
N
E
W
S
8
3-2 Mapmaking and Technology
  • A.  How Cartographers Traditionally Worked
  • a.   The USGS created its first map in 1879.
    Its main purpose was to survey and map the West.
  • b. Plane Table Surveying was the technique
    originally used. This technique involved
    carrying a plane table to the highest vantage
    point and drawing a map of whatever features they
    could see.

9
3-2 Mapmaking and Technology
  • B.    How Technology Has Changed in Mapmaking
  • a.   The use of airplanes, cameras and radar
    advanced mapmaking tremendously. Why?
  •  
  • C.    Satellite Technology
  • a.   In 1972 NASA launched the first Landsat
    satellite into space.
  • b.  False color Image-made up of colors that
    represent images collected by the satellite.
  • c. Provide a larger view of the
    earths features

Because you could see the land from above
10
3-2 Mapmaking and Technology
  • D.    Computer Technology
  • a.   Computers are needed to process the images
    collected by satellites. Advances in computer
    technology have made it easier and faster to
    process this information.

11
3-2 Mapmaking and Technology
  • b.  Global Positioning System (GPS)-Allows people
    to determine their position, speed, and time
    anywhere in the world.
  • c.  Triangulates its position using the
    satellites in the sky.
  • d. Geographic Information Systems
    (GIS)-Combines satellite images and surveys. See
    page 52.

12
3-3 Topographic Maps
  • A.   Qualities of Topographic Maps
  • a.   Depicts the features of an area using
    contour lines and symbols.
  • b.  7.5 maps-represent 7.5 minutes of latitude
    by 7.5 minutes of longitude.
  • c. Why are these maps important?

They show us the location and elevation of
landmarks
  • http//erg.usgs.gov/isb/pubs/booklets/symbols/

13
3-3 Topographic Maps
  • A. Qualities of Topographic Maps
  • d.   Contour Lines- Narrow brown lines on
    topographic maps that indicate the landscapes
    elevation. They connect points of the same
    elevation.

14
3-3 Topographic Maps
The contour interval can be calculated by taking
the difference in the two bold lines and dividing
by 5. Ex. (800ft-700ft)/520 ft
  • e.  Contour Interval- The difference in elevation
    between two consecutive contour lines.
  • f. Contour lines that are close together
    indicate steep terrain lines that are far apart
    indicate a gentle slope.

15
3-3 Topographic Maps
  • B.   Understanding Topographic Map Symbols
  • a.   These symbols help to understand what
    features are on the map. See page 697.
  • b. Magnetic Declination- Angle by which a
    compass needle will vary from true north.

16
3-3 Topographic Maps
  • C.   Using Topographic Maps
  • a.   Shape of the land can be determined by
    making a profile from a topographic map. See
    page 57.
  • b. A map scale indicates how much land is being
    covered in a given area on the map.
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