Geography 417
California for Educators

Using the Geographic Grid

Objectives

      Students will identify and explain the geographic grid system.

      Students will use coordinates to locate positions on the earth’s surface.

      Students will find the coordinates of identified locations.

      Students will recall the basic components of the geographic grid.

The Geographic Grid

      The geographic grid is a coordinate system that is used to locate or identify place on the earth.

      Generally coordinate system employs latitude and longitude degrees as identifiers, although there are dozens of systems.

      Basis for system goes back to Eratosthenes in 247 B.C. who calculated the polar circumference.

      Formalized by Ptolemy.

      Based on the simple geometry of a the earth as a sphere.

Figure: The Geometry of the Grid System

Parallels of Latitude           Meridians of Longitude

Latitude

      The angle measured in degrees, minutes and seconds created between any location on earth and the equator

360 ° = Circle

60'   = 1 degree

60"  = 1 minute

      Maximum value is 90° north and south of the equator

      Distance between 1 ° of latitude is 111 km (69 miles)

      Reference circle is the equator (0 °)

        Newer system is based on fractions of 10, not 60.

      Places frequently referenced as ‘high’ or “low” latitudes.  We live in the ‘mid-latitudes’

Figure: Parallels of Latitude

Figure: Geometry of Latitude

Parallels of Latitude           Meridians of Longitude

Longitude

      The angle measured in degrees, minutes and seconds created between any location on earth and the Prime Meridian

      Maximum value is  180 ° (International Date Line)

      Distance between lines of longitude varies

   111 km (69 miles) at the equator and decreases towards the poles

      Reference meridian is the Prime Meridian (0 °) which runs through Greenwich, England

      Reflects the political power and England’s navigational needs.

Figure: Geometry of Longitude

Figure: Meridians of  Longitude

International Date Line

Figure: Locate any point with Lat/Long

Figure 2: Earth with Graticule

Hemispheres

      Hemispheres are the “halves” of the earth. 

      Northern hemisphere is that above the equator.

      Western hemisphere is that half which is west of the Prime Meridian and east of the International date line.

      Not to be confused with “The East” or “The North” or “The West”, which are perceptual regions.

Can you identify these?

Figure: Small Circle

Figure: Great Circle

Figure: Navigation with Great Circle

Projections

     Since the earth is spherical and maps are flat, it is impossible to map the 3D earth without creating distortions on a 2D map.

     All maps are distorted in at least 1 of 3 ways: Shape, Size or Direction.

     Can you identify the problems with each of the following projections?

Mercator Projection

Peter’s Projection

Goode Projection

Robinson Projection

Perspective is Important