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Laboratory Manual for Introductory Geology 4e

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9.3.2 Contour Lines and Elevation

Topographic maps provide several key features to help determine elevations. Two of

the easiest to use are benchmarks and index contour lines. A benchmark is an accurately

surveyed point marked on the ground by a brass plaque cemented in place.

It records the latitude, longitude, and elevation of that spot. On topographic maps,

elevations of selected points (such as hilltops, lake surfaces, and highway intersections)

are indicated with a symbol and a number, such as X 1438”

or D 561

. The latter

symbol represents the location of a benchmark.

To find the elevations of other points on the map, however, we must use the

contour lines. Take another look at Figure 9.4, but first, remember to check

for the contour interval at the bottom of the map for the difference in elevation

between adjacent contour lines. On Figure 9.4, as on most topographic

maps, every fifth contour line is darker than those around it and has its elevation

labeled. These lines are index contours, which represent elevation intervals that

are five times the contour interval (multiples of 5 3 20 in Fig. 9.4—300 feet,

400 feet, and so on). To determine the elevation of an unlabeled contour line,

determine its position relative to an index contour. For example, a contour line

immediately adjacent to the 500-foot index contour must be 480 or 520 feet—20

feet lower or higher than the index contour on a map with a contour interval

of 20 feet.

What about the elevation of points between two contour lines? All points on

one side of a contour line are at higher elevations than the line itself, and those

on the opposite side are at lower elevations—but how much higher or lower? The

contour interval in FIGURE 9.6 is 50 feet, so a point between two adjacent contour

lines must be less than 50 feet higher or lower than those lines. Estimate the

elevation by how close a point is to either contour line: a point midway between

the 500- and 550-foot contour lines would be estimated as 525 feet above sea level;

a point ¾ of the way to the 550-foot contour would be about 538 feet above sea

level, and so forth.

Point C on Figure 9.6 lies between two 500-foot contour lines, and the adjacent

contours indicate that C is near the crest of a hill. What can we say about the elevation

of the highest point on the hill? First, that it is over 500 feet, and second, that

it must be less than 550 feet, because there isn’t a 550-foot contour line. There is no

further information that would allow us to be more precise.

The elevation of Point A is between 400 and 450 feet. Because the slope of the

hill is constant between those contour lines, and A is halfway between them, the

estimated elevation of A is 425 feet above sea level.

Point B lies between 350 and 400 feet. Here, however,

the spacing of the contour lines indicates that FIGURE 9.6 Reading elevations of hills and valleys from

the slope is gentler near the 350-foot line than near

topographic maps.

the 400-foot line. The estimated elevation of B is 355

Map view

feet above sea level.

E

D

A C

Concentric contour lines may indicate either a hill (as

E

in Exercise 9.1b) or a depression. To avoid confusion, it

must be clear that concentric contour lines outlining a

B

depression indicate progressively lower elevations toward

C

A

the center rather than the higher elevations that would

E

D

indicate a hill. To show this, small marks called hachures

500

E

B 400

are added to the line, pointing toward the lower elevation

(see the innermost two lines in FIG. 9.7).

Repeat

300

200

The feature in Figure 9.7 could be a volcano with a

100

Repeat

crater at its summit. Note that the nested contour lines 0

350

300

250

200

200

250

300

350

350

400

450

500

500

450

400

350

300

9.3 READING TOPOGRAPHIC MAPS

223

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