Manual for Noncommissioned Officers and Privates of Cavalry of the Army: of the United States 1917. To be also used by Engineer Companies (Mounted) for Cavalry Instruction and TrainingUnited States. War Department
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Manual for Noncommissioned Officers and Privates of Cavalry of the Army: of the United States 1917. To be also used by Engineer Companies (Mounted) for Cavalry Instruction and Training
United States. War Department
United States. Army -- Handbooks, manuals, etc.
Contours also show =slopes=. It has already been explained that from
any contour to the next one above it the ground rises a fixed number
of feet, according to the vertical interval of that map. From the
scale of distances on the map the horizontal distance between any two
contours can be found. For example: On the map the horizontal distance
between D and E is 90 yards, or 270 feet. The vertical distance is 20
feet, the V. I. of the map. The slope then is 20/270 = 1/13.5 = 7-1/2%
= 4-1/2°, in all of which different ways the slope can be expressed.
[Illustration: Slope.]
On a good many contoured maps a figure like this will be found in one
of the corners:
[Illustration: Scale.]
On that particular map contours separated by the distance
[Illustration: Scale.]
on the vertical scale show a slope of 1°; if separated by the distance
[Illustration: |__2°__| ] they show a 2° slope, etc. A slope of 1° is
a rise of 1 foot in 57. To use this scale of slopes, copy it on the
edge of a piece of paper just as you did the scale of distances and
apply it directly to the map.
You will notice that where the contours lie closest the slope is
steepest; where they are farthest apart, the ground is most nearly
flat.
It has already been set forth how contours show height and slope; in
addition to this they show the shape of the ground, or GROUND FORMS.
Each single contour shows the shape at its particular level of the
hill or valley it outlines; for instance, the 880 contour about the
penitentiary shows that the hill at that level has a shape somewhat
like a horse's head. Similarly, every contour on the map gives us the
form of the ground at its particular level, and knowing these ground
forms for many levels we can form a fair conception of what the whole
surface is like.
A round contour like the letter O outlines a round ground feature; a
long, narrow one indicates a long, narrow ground feature.
Different hills and depressions have different shapes. A good many of
them have one shape at one level and another shape at another level,
all of which information will be given you by the contours on the map.
One of the ways to see how contours show the shape of the ground is to
pour half a bucket of water into a small depression in the ground. The
water's edge will be exactly level, and if the depression is
approximately round the water's edge will also be approximately round.
The outline will look something like figure 6.
Draw roughly on a piece of paper a figure of the same shape and you
will have a contour showing the shape of the bit of ground where you
poured your water.
Next, with your heel gouge out on one edge of your little pond a
small, round bay. The water will rush in and the watermark on the soil
will now be shaped something like figure 7.
Alter your drawing accordingly, and the new contour will show the new
ground shape.
Public-domain text, read in full here on John Shaqi.
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