Contours are the thin brown lines that snake across a
topographic (topo) map. Contour lines
connect equal points of elevation such that every point on a specific line will
be at that elevation above sea level.
Contour lines are distinct and separate from lines for roads,
coordinate systems (e.g., latitude and longitude) and trails. Man made features like roads and buildings are
black. Contour lines are brown. By adding elevation data to the map contour
lines provide a three dimensional view of the terrain. These lines provide shape and a sense of
texture.
The graphic above uses shading and electronic editing in an
attempt to gain a three dimensional view of the terrain. Compare the two maps.
Here are a few “keys to the kingdom” of reading these the brown
contour lines.
There are two primary types of contour lines, index and
intermediate lines.
The dark brown, wider lines (below) are “index lines.” The numbers adjacent correspond to altitude along
the line.
For example, if the hiker locates his position on the topo
and its right on top of the dark brown line with 5200 printed on the line, the
altitude at that point is 5200 feet.
Consider the altitude to be the height above sea level.
The faint brown lines between the index lines are “intermediate
contour” lines (see graphic above.)
Critical to intermediate lines is the specific elevation change between
the lines. This is known as the “contour
interval.” The contour interval could be 10 feet, 20 feet or 200 feet; it just
depends on the scale of the map and terrain.
To find the contour interval on a topo go to the bottom of the map or to
the map key/index. On a United States
Geologic Survey (USGS) 7.5 minute topo map it will be at the bottom center of
the map. In the graphic below, the contour
interval is circled in red.
In the small map above, look at Browns Mountain. The spacing between the intermediate contour
lines represents an elevation change of 20 feet. Notice that the index lines are spaced five
contour intervals apart or 100 feet between index lines.
Contour lines (index and intermediate) can provide a view of
slope and pitch, depressions, ridge lines and level ground; the highs and lows
of the earth’s surface.
The contour lines at Browns Mountain are close together and
represent a steep increase in elevation.
Lines close together can indicate a peak, hill, ridge line or a cliff.
The contours of the land area to the left or west of Browns
Mountain are spaced farther apart. Such
lines indicate flat ground like a meadow or plain. Lines far apart make for gentle slopes and
flat ground.
Ridges, valleys, and streams are represented by contour
lines too. A line’s shape identifies
these land features. For example, a
valley’s shape is formed by a collection of “v’s.” Tips of the v's point toward higher
elevations. Look at Alder Creek on the
map below. Note that the creek bed is in
the bottom of a valley and water flow is from higher elevation to lower.
The contour lines that shape Alder Creek have v’s that point
to higher altitude. Look closely at the
index lines and try to determine the elevation change as the creek flows north.
Contours shaped like a v or u, pointing toward lower
elevation denotes ridges. Notice the shape
of the contour lines to the right and east of Alder Creek. The v’s tips point toward lower
elevation. In fact, the v’s have become
more like expanded “u’s.”
For more information about contour lines visit www.landnavigation.org or search the
internet for the “World of Teaching – Topographic maps” (a very fine power
point presentation.)
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