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Concept 2: Contour maps and topographic maps

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Topographic Maps: contour maps that use a coordinate system, map scale and key and symbols to indicate landforms and manmade structures. a. – PowerPoint PPT presentation

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Title: Concept 2: Contour maps and topographic maps


1
Concept 2 Contour maps and topographic maps
  • Read dont write this part..
  • Big Idea From NYS Standards for Earth Science
  • Key Idea 2
  • Many of the phenomena that we observe on Earth
    involve interactions among components of air,
    water, and land.
  • 2.1q Topographic maps represent landforms through
    the use of contour lines that are isolines
    connecting points of equal elevation. Gradients
    and profiles can be determined from changes in
    elevation over a given distance.

2
Field Maps
  • 1. Field maps are localized maps that show one
    aspect of the area using isolines and symbols.
  • (In Earth Science, field maps are used to show
    elevation, weather variables, pollutants,
    earthquake intensity, etc.)

3
2. Map keys and symbols
  • a. A map scale is used to measure distance on
    the map.
  • b.     A map legend or key identifies the meaning
    of symbols on a map.
  • c.    Relief indicates the change on the map from
    greatest to least field value.

4
3. Contour Maps field maps that show elevation.
  • a.     Contour maps use contour lines (isolines)
    to indicate landscape changes.
  • b.     The contour interval between the isolines
    must always be constant, and is usually measured
    in feet or meters.
  • c.     Contour lines spaced far apart indicate
    flat land. Those close together indicate steep
    ground.

5
continued
  • d.     Closed loops indicate hills. Long closed
    loops indicate ridges.
  • e.     The maximum possible elevation inside a
    closed loop is one less than whatever another
    contour line would be.
  • f.        Depressions (or basins) are shown using
    hachure lines. The first hachure line has the
    same value as the last contour line.

6
  • g.     The direction a river flows can be
    interpreted two ways on a contour map
  •     i.      The contour lines make a v shape
    that points uphill.
  •   ii.      elevation indicates which way is
    downhill
  • h.      Sea level always has an elevation of 0.
    Elevations below sea level are indicated by
    negative numbers. http//www.visualentities.com/co
    ntour.htm

http//www.sir-ray.com/Topographic20Map20Lab.htm

7
4. Finding gradient see p. 1ESRT
  • a.     On a contour map, the gradient indicates
    the change in elevation (y value) over the
    distance (x value).
  • b.     Units are very important in gradient
    problems.
  • For contour maps, the gradient units will usually
    be meters/kilometers (m/km) or feet/miles (ft/mi)

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5. profile maps use the contour lines of a flat
map to show a side view of a cross-section
  • a.     The steps to making a profile require
    visuals and practice
  • http//user.gs.rmit.edu.au/caa/topo/contours.htm
  • http//rst.gsfc.nasa.gov/Sect11/Sect11_2.html
  • Vertical exaggeration refers to how much the
    elevation has been exaggerated on the y axis to
    make the change visible over horizontal distance

10
  • 6. Topographic Maps contour maps that use a
    coordinate system, map scale and key and symbols
    to indicate landforms and manmade structures.

11
  • a.     Technology has greatly improved
    topographic maps.
  • b.     In the United States, the United States
    Geologic Survey (USGS) has made USGS Quadrant
    maps of the entire country.
  • c.     The USGS Quadrant maps use coordinate
    systems, including latitude and longitude, to
    indicate the map location in the world.
  • d.     Symbols used on these maps are
    standardized to show vegetation, types of
    structures, roads, etc.
  • e.     Topographic maps are used for planning and
    to track problems and changes.
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