tABle 8.3. commonly Used Isarithms




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Judith A. Tyner. Principles of map design. New York. „The Guilford Press”, 2010

tABle 8.3. commonly Used Isarithms
Isobars
Lines of equal barometric pressure
Isobaths
Lines of equal water depth
Isochrones
Lines of equal minimum travel time from a point
Isogones
Lines of equal earth magnetism (declination)
Isohyets
Lines of equal precipitation
Isohypses
Lines of equal land elevation (more commonly called “contour lines”)
Isotherms
Lines of equal temperature


172 sYMBOLizaTiOn 
the isarithms. Evenly spaced lines represent an even rate, closely spaced lines repre-
sent a steep gradient, and widely spaced lines represent a gentle gradient.
The population map in Figure 8.35, while similar in appearance to the rainfall 
map, is an isoplethic map. The isopleth does not permit the estimation of population 
at any point because the control points represent values for areas, not actual points. 
That is, the values describe population per square mile, not numbers of people at spe-
cific points. This map does, however, permit the reader to note patterns and general 
gradients. In the same way that rate of change can be determined from an isometric 
map, areas of rapid or gradual change can be found on isoplethic maps.
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fIgURe 8.33. 
Formation of isarithms.
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