Physics Tool

Wave Diagram Generator for Transverse & Longitudinal Waves

Create a labeled wave diagram in seconds. Show crest, trough, wavelength, amplitude, rest position, frequency, and period for transverse waves — or compression and rarefaction for longitudinal waves — then download your diagram, free.

Crest, trough, wavelength & amplitude labeledTransverse and longitudinal wave types

Wave Diagram Generator

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Wave Diagram Examples

Labeled transverse and longitudinal wave diagrams for physics

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Labeled Transverse Wave

All key parts in one diagram — crest, trough, wavelength, amplitude, and equilibrium line clearly labeled.

transverselabeledcrest

Transverse vs Longitudinal Wave

Transverse oscillation is perpendicular to wave travel; longitudinal oscillation is parallel — shown side by side.

transverselongitudinalcomparison

Parts of a Wave

Every part of a wave labeled on one diagram — ideal for notes, posters, and revision.

partsreferencelabeled

Wavelength and Amplitude

Wavelength is one full cycle; amplitude is the displacement from rest — both measured and labeled.

wavelengthamplitudemeasurement

Longitudinal Wave: Compression & Rarefaction

Compression (dense) and rarefaction (spread) regions labeled on a longitudinal wave with wavelength marked.

longitudinalcompressionrarefaction

Blank Wave Worksheet

Leader lines, no labels — print and hand out for students to identify crest, trough, amplitude, and wavelength.

worksheetblankunlabeled

What is a wave diagram?

A wave diagram is a labeled drawing that shows the shape and key measurements of a wave. For a transverse wave it is a sinusoidal curve with annotations pointing to the crest, trough, wavelength, amplitude, and rest (equilibrium) position. For a longitudinal wave it is a coiled spring or series of dots showing alternating compressions and rarefactions, with the wavelength spanning one complete compression-rarefaction pair. Wave diagrams appear in every introductory physics course because they connect the visual pattern of a wave to the quantities — wavelength, amplitude, frequency, and period — that appear in equations.

Parts of a wave: crest, trough, wavelength, amplitude, and rest position

  • Crest: the highest point of a transverse wave — the peak of the sinusoidal curve.
  • Trough: the lowest point of a transverse wave — the valley of the sinusoidal curve.
  • Wavelength (λ): the distance from one crest to the next (or trough to trough, or any two identical points one full cycle apart). Measured in metres.
  • Amplitude (A): the maximum displacement of the medium from the rest position — the vertical distance from the equilibrium line to the crest. Larger amplitude means more energy.
  • Rest position (equilibrium line): the undisturbed position of the medium, drawn as a horizontal dashed line through the middle of the wave.
  • Frequency (f): the number of complete waves that pass a point per second. Measured in hertz (Hz). Related to period by f = 1/T.
  • Period (T): the time for one complete wave cycle. Measured in seconds. Related to frequency by T = 1/f.

Transverse waves vs longitudinal waves

In a transverse wave the particles of the medium oscillate perpendicular to the direction the wave travels — like a rope shaken up and down while the wave moves along the rope. Light and water surface waves are transverse. In a longitudinal wave the particles oscillate parallel to the wave's direction of travel — like the coils of a spring being pushed and pulled along its length. Sound is a longitudinal wave. Both types share the same wave-speed formula v = fλ, but their diagrams look very different: a transverse wave is drawn as a sinusoidal curve, while a longitudinal wave is shown as alternating compressions and rarefactions.

Compression and rarefaction in longitudinal waves

  • Compression: a region where the particles of the medium are pushed together — the coils of a spring are densely packed. This is the equivalent of a crest in a transverse wave.
  • Rarefaction: a region where the particles are spread apart — the coils are widely spaced. This is the equivalent of a trough in a transverse wave.
  • One full wavelength of a longitudinal wave spans exactly one compression and one rarefaction.
  • Sound waves in air are longitudinal: the speaker cone pushes air molecules together (compression) then pulls them apart (rarefaction), and the wave carries that pressure pattern outward.

The wave equation: v = fλ

The wave equation v = fλ links wave speed (v, in m/s), frequency (f, in Hz), and wavelength (λ, in m). Since period T = 1/f, you can also write it as v = λ/T. If you know any two of the three quantities you can find the third. For example, sound travels at about 340 m/s in air; if the frequency is 340 Hz the wavelength is 1 m. A wave diagram makes these relationships visual: wavelength is the length of one cycle, and frequency tells you how many of those cycles pass a fixed point every second.

Labeled vs blank wave diagrams for worksheets

Teachers often need two versions of the same diagram: a fully labeled one for notes and slides, and an unlabeled version with empty leader lines for students to fill in as a quiz or homework. With this generator you can describe a labeled wave for your lesson and then ask for a printer-friendly, black-and-white blank version of the same layout — no redrawing required. You can also adjust complexity, for instance asking for a simple single-wave diagram for middle school or a multi-wave comparison poster for A-level physics.

Frequently Asked Questions