Skip to content
9 MIN LESSON · MATHEMATICS

Introduction to Graphs: Complete Concepts and Practice

Mathematics — Graph types, axes, origin, ordered coordinates, scales, plotting, line graphs, linear models, fixed charges, distance–time graphs, rates, coordinate rectangles and interpolation limits.

Big picture

A graph represents information through positions, lengths or shapes. Coordinate graphs show how values of two quantities are related. They allow us to see trends, compare observations and estimate values more quickly than a long list of numbers alone.

A bus timetable, a distance–time record and a shop's cost chart all use related ideas. Accurate reading depends on labels, units and scale. A steep-looking line can be misleading if the scales have been changed, so mathematical interpretation must follow the numbers as well as the picture.

Learning goals

  • Distinguish common statistical graphs and choose a suitable representation.

  • Identify axes, origin, coordinates and points on an axis.

  • Choose scales and plot points accurately using ordered pairs.

  • Draw and interpret line and simple linear graphs.

  • Model cost, distance, time and simple geometric relationships.

  • Distinguish interpolation from extrapolation and recognise limits of graphical evidence.

Core ideas

1. Match the graph to its purpose

A bar graph compares categories; a histogram represents grouped numerical intervals; a pie chart represents shares of a whole; a line graph shows changes across ordered values such as time. These representations answer different questions.

Question

Suitable display

Reason

Which club has most members?

Bar graph

Categories are separate

How are heights distributed in intervals?

Histogram

Measurements form adjacent classes

How is a fixed budget divided?

Pie chart

Categories are parts of one total

How does temperature change through the day?

Line graph

Time has a meaningful order

A line connecting favourite-colour categories suggests a continuity that does not exist. Conversely, a temperature record benefits from showing the order of observation rather than arranging the readings from smallest to largest.

2. Axes and origin

The horizontal axis is the x-axis and the vertical axis is the y-axis. Their intersection is the origin, written O or (0, 0). The axes provide reference directions so that points can be located consistently.

This chapter mainly uses nonnegative coordinates in the first quadrant. A full Cartesian plane extends to negative values as well. On the x-axis, the y-coordinate is zero; on the y-axis, the x-coordinate is zero. The origin belongs to both axes.

Worked example. A point 4 units right of the origin and 3 units up is (4, 3). A point 5 units right without moving up is (5, 0), on the x-axis. A point 2 units up without moving right is (0, 2), on the y-axis.

3. Coordinates are ordered pairs

An ordered pair (x, y) gives the horizontal coordinate first and vertical coordinate second. The order matters. The points (2, 5) and (5, 2) occupy different locations unless both coordinates happen to be equal.

To plot (3, 6), locate 3 on the horizontal scale, move parallel to the y-axis until the vertical reading is 6 and mark the intersection. Construction lines may be drawn lightly. Label the point if the question names it, for example A(3, 6).

Worked rectangle. Plot A(1, 1), B(5, 1), C(5, 4), D(1, 4), then join in that order. AB is horizontal with length 5 − 1 = 4 units; BC is vertical with length 4 − 1 = 3 units. The perimeter is 2(4 + 3) = 14 units, and area is 4 × 3 = 12 square units. The joining order is essential; a different order might cross the diagonals instead of tracing the boundary.

4. Choose a uniform scale

A scale states how much one division represents. Equal distances on the same axis must represent equal numerical differences. You may use different scales on the two axes if each is labelled clearly.

Worked example. To display time from 0 to 4 hours and distance from 0 to 120 km, choose 1 large division = 1 hour horizontally and 1 large division = 20 km vertically. At 2 hours and 60 km, the point lies at the second horizontal division and third vertical division: (2, 60) in the stated units.

Do not read the third vertical division as 3 km. The division number and the measured value are different. Give a title and label the axes “Time, hours” and “Distance, km”. A number with no unit can be ambiguous.

5. Plot a table and draw a line graph

A line graph connects data points in meaningful order. It need not be a single straight line. Plot the observations accurately before drawing connecting segments. Do not bend the graph merely to make it appear smooth when straight segments are requested.

Worked example. A classroom records temperature as follows:

Time

Temperature

8 a.m.

20°C

10 a.m.

24°C

Noon

28°C

2 p.m.

26°C

Use equal horizontal spacing for equal two-hour intervals. The highest observed temperature is 28°C at noon. From 8 a.m. to noon the increase is 28 − 20 = 8°C. From noon to 2 p.m. the fall is 28 − 26 = 2°C. These statements concern recorded values, not every instant between observations.

6. Linear graphs from a rule

A linear graph consists of points on a straight line representing a linear relationship. A table supplies convenient points, but the rule determines the full relationship over the chosen domain.

Worked example. A photocopy shop charges ₹3 per page with no fixed charge. Let x be pages and y be cost in rupees: y = 3x.

Pages x

Cost y

0

0

2

6

4

12

6

18

Plot (0, 0), (2, 6), (4, 12), (6, 18). They lie on a straight line through the origin. For 5 pages, y = 3 × 5 = ₹15. The line illustrates the rule, but actual page counts are whole numbers; 2.5 pages may not be an available purchase.

7. A straight line need not show direct proportion

A delivery service charges ₹20 plus ₹5 per packet. The rule is y = 20 + 5x. For x = 0, 2 and 4, costs are ₹20, ₹30 and ₹40. The points lie on a straight line, but it does not pass through the origin.

The graph meets the y-axis at (0, 20), representing the fixed charge in the model. For 6 packets, y = 20 + 5 × 6 = ₹50. The cost is not directly proportional to packet count because y/x is not constant.

This distinction matters in exam statements: “Every straight-line graph shows direct proportion” is false. Direct proportion is a special linear relationship passing through the origin. Interpret a fixed-charge model only over situations where the stated charge actually applies.

8. Distance–time graphs

Place elapsed time on the horizontal axis and distance from the starting point on the vertical axis. For a journey moving steadily away from the start, the increase in distance divided by elapsed time gives speed.

Worked example. A cyclist is 0 km from the start at 0 hours, 12 km at 1 hour, 24 km at 2 hours and still 24 km at 3 hours. During the first two hours, speed = (24 − 0) ÷ (2 − 0) = 12 km/h. From hour 2 to hour 3, distance is unchanged, so the horizontal segment indicates a 1-hour stop in this simple outward-journey model.

Over the whole three hours, average speed = total distance travelled ÷ total elapsed time = 24 ÷ 3 = 8 km/h. This differs from the moving speed because the stop is included. A distance-from-start graph requires extra care for return journeys: total distance travelled is not simply the final distance from the start.

9. Read intervals and rates carefully

A larger vertical coordinate means a larger value, not automatically a larger rate. Compare the change in y over the same change in x. With identical scales, a steeper outward straight segment on a distance–time graph means faster motion.

Worked example. Traveller A covers 18 km in 2 hours, while B covers 15 km in 1 hour. A's speed = 18 ÷ 2 = 9 km/h; B's = 15 ÷ 1 = 15 km/h. A has travelled farther at the stated endpoint but B's rate is higher. Do not compare steepness visually across separate graphs with different scales.

A horizontal segment in a temperature graph means constant temperature, not that an object has stopped moving. Meaning comes from the axis labels.

10. Estimates, interpolation and extrapolation

Interpolation estimates a value between known observations. Extrapolation extends beyond them and usually needs a stronger assumption. If temperature rises linearly from 20°C at 8 a.m. to 24°C at 10 a.m., an interpolated 9 a.m. reading is 22°C. That is an estimate, not a directly recorded observation.

Extending the same line to much later times assumes the same rate continues. The later fall in the example shows why such a prediction can fail. Connecting data points does not prove that nature followed the drawn segments exactly.

For an exact model such as y = 3x, substitution gives an exact model value. For measured data, the precision of the instruments and graph limits the precision of a read-off estimate. Avoid unnecessary decimal places that the scale cannot justify.

11. Diagram description and construction checks

A clear coordinate diagram should show a horizontal x-axis, vertical y-axis, their origin, regular ticks, numerical scale and labelled points. In the rectangle example, AB and CD run parallel to the x-axis; BC and DA run parallel to the y-axis. Opposite sides share equal coordinate differences.

Before interpreting a graph, inspect whether the axis begins at zero, whether breaks are shown and whether units change. A dramatic-looking graph may reflect scale choices. A fair conclusion reports the actual increase or difference rather than relying only on visual height.

A reliable approach to questions

  1. Identify quantities, units, graph type and the question asked.

  2. Read or choose a uniform labelled scale on each axis.

  3. Keep x first and y second when forming ordered pairs.

  4. Plot accurately and join only in the appropriate order.

  5. Calculate changes or rates from numerical values, not appearance alone.

  6. Distinguish exact model values, observations and graphical estimates.

Connections that matter

  • Data handling explains which displays suit categories, intervals and shares.

  • Direct proportion produces straight lines through the origin.

  • Mensuration uses coordinate differences for simple lengths, perimeters and areas.

Common mistakes

  • Reversing coordinates: read horizontal first, then vertical.

  • Treating each division as one unit: apply the stated scale.

  • Calling every line graph straight: successive observations may form changing segments.

  • Calling a horizontal segment a stop regardless of labels: interpret the actual vertical quantity.

Revision checklist

  • I can identify axes, origin and ordered coordinates.

  • I can choose scales and plot points accurately.

  • I can distinguish line graphs from linear relationships.

  • I can interpret cost and distance–time models.

  • I can calculate a change, rate and simple coordinate area.

  • I can separate observations from interpolated or extrapolated values.

Practise this topic →

Discussion

Sign in to join the discussion.

Sign in

No comments yet. Be the first to share your thoughts.