Basic principles of reading maps
A map is a drawing of part of the Earth’s surface, seen from above and reduced to scale. To read a map, look at the title, the key (legend), the scale, the direction (north arrow), the grid (eastings and northings) and the symbols.
Scale
The scale shows how much the map is reduced. It can be stated as a ratio or representative fraction (RF), for example 1 : 50 000, as a statement (1 cm represents 500 m), or as a line scale. At 1 : 50 000, 1 cm on the map is 50 000 cm = 500 m on the ground.
Two towns are 7.5 cm apart on a map of scale 1 : 50 000. What is the real distance?
- Multiply by 50 000.
- Change to km.
Answer: The towns are 3.75 km apart.
Relief on topographical maps
Contour lines join points of the same height above sea level. Close lines show a steep slope, lines far apart show a gentle slope, and V-shaped contour lines pointing uphill show a valley. A spot height gives the height of one point, and a trigonometrical station is a surveyed point.
The gradient of a slope is the vertical interval divided by the horizontal distance.
Statistical maps
Statistical maps show data such as population or rainfall. Dot maps use dots, choropleth maps use colours or shades for different values, proportional symbol maps use circles of different sizes, and flow maps use lines of different widths.
Choose the scale (1 : N) and the distance on the map.
Key terms
- Scale
- The ratio between the distance on the map and on the ground.
- Contour line
- A line joining points of equal height.
- Gradient
- The steepness of a slope.
- Key
- The explanation of the symbols used on a map.
Summary
- Read the title, key, scale, direction and grid first.
- Ground distance = map distance × scale denominator.
- Contours show the height and shape of the land.
- Statistical maps use dots, shading, circles or flow lines.