Cross Section and Sketch Maps
Senior 6 · Geography
Cross Section and Sketch Maps
Lesson 1 of 4
25 min
Map 1 below is a topographic extract of a small area with two hills and a river. The contours already tell you which hill is higher and where the slopes are steep, but only after careful reading, because a map shows the land from directly above. A cross section turns that information on its side. Imagine cutting the ground along a straight line and looking at the cut face: that face is what a cross section draws.
Engineers draw sections to plan roads, pipelines and radio links, and geographers use them to describe relief. In the A-level examination you may be asked to draw one from a map extract, to scale, and then to label it and calculate from it. You met contours, spot heights and trigonometrical stations in S1, and grid references and scale in S2. This lesson puts them to work.
Definition
Cross section (also called a profile): a side view of the ground surface along a straight line between two points on a map, drawn to scale from the contours and spot heights that the line crosses.
The straight line on the map is the section line, named by its end points. Example: on Map 1 the section line A–B runs along northing 225, from grid reference 103225 to 159225.
Definition
Sketch section: a quick freehand drawing of the shape of the land along a line. It shows the main rises, falls and features in the right order, but does not plot every contour to an exact vertical scale.
Example: a two-minute sketch of A–B showing a long gentle climb to Hill X, a steep drop to River Z and a short climb over Hill Y.
How to read Map 1. Each grid square is 1 km by 1 km on the ground, which is 2 cm on the original 1:50 000 sheet. The contour interval is 20 m, and the 1,600 m contour is drawn thicker. Hill X rises to a trigonometrical station at 1,671 m and Hill Y to a spot height of 1,607 m. River Z flows south between two 1,520 m contours, and a spot height of 1,508 m marks the bridge where the road crosses it. The map is illustrative: it was drawn for this lesson and is not a real place.
Figure 2 shows the strip for A–B. Because A–B runs due east, every distance along it is simply a difference in eastings: the 1,600 m contour on the east face of Hill X is at easting 12.94, so it lies 12.94 − 10.30 = 2.64 km from A.
Figure 2: the paper strip for A–B, with every crossing ticked.
| Distance from A (km) | Height (m) | Feature |
|---|---|---|
| 0.00 | 1540 | A |
| 0.50 | 1560 | |
| 0.90 | 1580 | |
| 1.20 | 1600 | |
| 1.42 | 1620 | |
| 1.60 | 1640 | |
| 1.75 | 1660 | |
| 1.90 | 1671 | trig station, summit of Hill X |
| 2.10 | 1660 | |
| 2.32 | 1640 | |
| 2.50 | 1620 | |
| 2.64 | 1600 | |
| 2.76 | 1580 | |
| 2.86 | 1560 | |
| 2.95 | 1540 | |
| 3.15 | 1520 | |
| 3.70 | 1508 | spot height at the bridge, River Z |
| 4.25 | 1520 | |
| 4.40 | 1540 | |
| 4.56 | 1560 | |
| 4.71 | 1580 | |
| 4.86 | 1600 | |
| 5.00 | 1607 | spot height, summit of Hill Y |
| 5.17 | 1600 | |
| 5.32 | 1580 | |
| 5.46 | 1560 | |
| 5.60 | 1540 | B |
Worked example 1: from the strip to the base line
Problem. On the strip, the 1,620 m contour on the east side of Hill X is 2.50 km from A. How far from the left end of the base line do you plot it, if the base line is drawn at the map's scale of 1:50 000?
Solution. At 1:50 000, 1 cm on paper represents 50 000 cm, which is 0.5 km. So
The whole base line is long. If you lay the strip itself on the base line, you need no calculation at all: that is why the strip method is used.
Worked example 2: choosing the vertical scale
Problem. The heights along A–B run from 1,508 m (the river) to 1,671 m (the trig station). The answer booklet leaves a box 4 cm high. Choose a vertical scale.
Solution.
The summit of Hill X is then plotted above the base line. Figure 3 uses this scale. The next lesson shows why this makes the land look 10 times steeper than it really is.
Worked example 3: the valley floor and the hilltop
Problem. Between 3.15 km and 4.25 km from A the section crosses no contour at all. How should the ground be drawn there?
Solution. The land on both sides is at 1,520 m, and no 1,500 m contour appears between them. So the ground there is below 1,520 m but above 1,500 m. The spot height of 1,508 m at the bridge fixes the lowest point. Draw the curve dipping gently from 1,520 m down to 1,508 m at the river and back up to 1,520 m. In the same way, the summit of Hill X lies inside the 1,660 m contour, so the curve rises above 1,660 m to the trig station's 1,671 m. Never draw a flat top at 1,660 m or a flat floor at 1,520 m.
Figure 3: the accurate cross section A–B.
Compare Figure 3 with Map 1. On the west face of Hill X the contours are far apart low down and close together near the top, so the slope steepens as you climb. On the east face the opposite happens: the contours crowd together just above the river, so the slope is gentle near the summit and steep near the valley.
Definition
Concave, convex and uniform slopes
A sketch section is drawn when a question asks for "a sketch section" or when you need a quick picture of the relief to support an answer. Use only the heights of the main features: the ends, the summits and the valley floors. Plot these roughly in their correct order and at about the right heights, then join them with a curve that shows the character of each slope (concave, convex, steep or gentle). Label the main features and give a title. Leave out the vertical scale, or write "not to scale".
| Accurate cross section | Sketch section | |
|---|---|---|
| Points plotted | Every contour crossing, summit and spot height | Main features only |
| Scales | Horizontal and vertical scales stated; vertical exaggeration given | Not to scale, or approximate |
| Tools | Paper strip, graph paper, sharp pencil | Freehand |
| Use | Measurements: gradient, intervisibility, heights | A quick picture of the relief |
Warning
Common mistakes
Tip
Exam technique. Before ticking the strip, write the value of every thick contour along the line on the map itself. Then, if two contours sit close together, you can tell whether the next one is higher or lower by counting from the nearest thick contour. A river between two equal contours is always lower than both of them.
Earth Science Classroom: "Topo Maps – How To Draw A Cross Sectional Profile". Watch how the edge of a strip of paper is used to carry each contour crossing from the map to the graph, then compare it with the seven steps above. The method works the same way whatever the units of the contours.
Practice
Practice (use Map 1, Figure 2 and Figure 3)
Summary
Sources and credits
Written by Ganzaa. Map 1, the paper strip, the cross section and all exercises were drawn and written by Ganzaa for this lesson; the map shows an invented area.
Video: "Topo Maps – How To Draw A Cross Sectional Profile", Earth Science Classroom, embedded from YouTube.