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.)
-----------------------------------------------------------------------------------------------------------
Learn more about monitoring the weather while inthe field here.
No comments:
Post a Comment