Contour lines are used when maps are designed to show the physical
nature of the land. They do this by linking all points which are the same
height above sea level. The width between the contour lines indicates the
steepness of gradients or slopes in the area. The closer the lines are
together, the steeper is the slope.
On physical maps giving the height of mountains, rivers, lakes and
principal towns all areas between certain heights are generally shown in the
same colour. This is known as layer colouring. Other methods for indicating
heights include relief maps moulded in plastic to the physical feature raised
as on a model. Spot heights may be shown, but these merely-give the heights
above sea level of certain points of the map and it does not follow that the
ground rises evenly from one point to another.
Very old maps have mountains drawn on them. Later ones
have lines called hachures radiating from a central point, with longer lines to
show gentler slopes. Another system is to show the form of the land by hill
shading. But none of these methods is so effective as the use of contour lines.
On physical maps giving the height of mountains, rivers, lakes and
principal towns all areas between certain heights are generally shown in the
same colour. This is known as layer colouring.
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