FREE BOOKS

Author's List




PREV.   NEXT  
|<   595   596   597   598   599   600   601   602   603   604   605   606   607   608   609   610   611   612   613   614   615   616   617   618   619  
620   621   622   623   624   625   626   627   628   629   630   631   632   633   634   635   636   637   638   639   640   641   642   643   644   >>   >|  
depending on whether its reference number is greater or smaller than that of the outer contour. A hilltop is shown when the closed contour is higher than the contour next to it; a depression is shown when the closed contour is lower than the one next to it. If the student will first examine the drainage system, as shown by the courses of the streams on the map, he can readily locate all the valleys, as the streams must flow through valleys. Knowing the valleys, the ridges or hills can easily be placed, even without reference to the numbers on the contours. =For example:= On the Elementary Map, Woods Creek flows north and York Creek flows south. They rise very close to each other, and the ground between the points at which they rise must be higher ground, sloping north on one side and south on the other, as the streams flow north and south, respectively (see the ridge running west from Twin Hills). The course of Sandy Creek indicates a long valley, extending almost the entire length of the map. Meadow Creek follows another valley, and Deep Run another. When these streams happen to join other streams, the valleys must open into each other. =1867. Map Distances (or horizontal equivalents).= The horizontal distance between contours on a map (called map distance, or M. D.; or horizontal equivalents or H. E.) is inversely proportional to the slope of the ground represented--that it to say, the greater the slope of the ground, the less is the horizontal distance between the contours; the less the slope of the ground represented, the greater is the horizontal distance between the contours. [Illustration: Fig. 10] +-----------+--------+--------------+ | Slope | Rise | Horizontal | | (degrees) | (feet) | Distance | | | | (inches) | +-----------+--------+--------------+ | 1 deg. | 1 | 688 | | 2 deg. | 1 | 688/2 = 344 | | 3 deg. | 1 | 688/3 = 229 | | 4 deg. | 1 | 688/4 = 172 | | 5 deg. | 1 | 688/5 = 138 | +-----------+--------+--------------+ It is a fact that 688 inches horizontally on a 1 degree slope gives a vertical rise of one foot; 1376 inches, two feet, 2064 inches, three feet, etc., from which we see that on a slope of 1 degree, 688 inches multiplied by vertical rises of 1 foot, 2 feet, 3 feet, etc., gives us the corresponding horizontal distance in inches. For example, if the
PREV.   NEXT  
|<   595   596   597   598   599   600   601   602   603   604   605   606   607   608   609   610   611   612   613   614   615   616   617   618   619  
620   621   622   623   624   625   626   627   628   629   630   631   632   633   634   635   636   637   638   639   640   641   642   643   644   >>   >|  



Top keywords:
inches
 

horizontal

 

streams

 

ground

 

distance

 

valleys

 
contour
 

contours

 

greater

 

represented


closed
 

reference

 

vertical

 
higher
 
equivalents
 
valley
 

degree

 
happen
 

inversely

 

proportional


Distances

 

called

 

Horizontal

 

horizontally

 

Distance

 
Illustration
 

degrees

 
multiplied
 

sloping

 

readily


locate

 

courses

 

drainage

 

system

 
easily
 

Knowing

 
ridges
 

examine

 

smaller

 

number


depending

 

hilltop

 

student

 
depression
 

numbers

 
extending
 
Meadow
 

length

 
entire
 
running