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What is a wave?

Far from shore a gull rides up and down as each wave passes, yet it does not travel with the wave.

A disturbance that travels

Drop a stone into a still pond and rings spread out across the surface. Pluck a guitar string and it blurs into a shimmer. Shout across a field and someone hears you a moment later. All three are waves. OpenStax College Physics gives a short definition: a wave is a disturbance that propagates, or moves away from the place where it was created. In the pond the disturbance is the shape of the water surface. In the air it is a change in pressure. On the string it is a sideways bend.

The important word is disturbance. The pattern moves, but the material mostly stays where it was. A gull sitting on the open sea goes up as a crest arrives and down as a trough passes, and after the wave has gone by it is roughly where it started. OpenStax notes that in water waves far from shore, the water particles move in small circles and stay in one area while the energy moves on. If a wave pushes you in deep water, what you feel is the energy, not a stream of water rushing past.

The parts of a simple wave. The orange dot marks a crest (a high point), the purple dot a trough (a low point). The wavelength λ is the distance between two neighbouring crests. The amplitude A is the height of a crest above the flat line.

Crest, trough, wavelength and amplitude

A simple repeating wave has high points called crests and low points called troughs. The distance from one crest to the next, measured along the direction the wave travels, is the wavelength, written with the Greek letter λ (lambda). The amplitude is how far the medium moves away from its resting position, so it is the height of a crest above the flat line, or half the distance from crest to trough. OpenStax points out that the amplitude is completely independent of how fast the wave travels. A big wave and a small wave on the same rope move at the same speed.

Two directions of shaking

Waves come in two basic kinds, sorted by the direction of the shaking compared with the direction of travel. In a transverse wave the medium moves at right angles to the direction the wave goes. Flick one end of a rope tied to a post and a hump runs along it while each bit of rope moves up and down. Waves on the strings of musical instruments are transverse, and so are light and other electromagnetic waves. In a longitudinal wave the medium moves back and forth along the direction of travel. Push and pull one end of a long spring and you see bunched-up regions, called compressions, run along it.

T: a transverse wave on a rope. The red arrow shows one piece of rope moving up and down while the wave moves right. L: a longitudinal wave in a spring. The coils move left and right, along the direction of travel, and bunch into compressions.

Sound in air and in water is longitudinal. A fluid has almost no stiffness against being bent sideways, so the only disturbance it can pass along is squeezing and stretching. Solids can carry both kinds. Water waves on the sea are a mix of the two, which is why the water particles trace circles. Earthquakes send both kinds through the ground: compressional P-waves that travel at 4 to 7 km/s and shear S-waves at 2 to 5 km/s, according to OpenStax. Seismographs record the P-wave first, and the gap before the S-wave arrives tells how far away the earthquake was.

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Top: a rope carrying a transverse wave. Bottom: a spring carrying a longitudinal wave with the same wavelength and frequency. Watch the red bead and the red coil: neither travels along with the wave.

Waves that need no medium

Water waves, sound and earthquake waves are mechanical waves: they need some material to travel through. Sound cannot cross empty space because there is nothing to squeeze. Light, radio and the other electromagnetic waves are different. They are made of changing electric and magnetic fields and travel through a vacuum, which is how sunlight reaches us across 150 million kilometres of space. OpenStax warns about a common mix-up here: a radio carries sound to you, but the radio waves themselves are electromagnetic, not sound.

BackgroundEarthquake waves let geologists see inside the planet. Richard Dixon Oldham studied seismograph records of large earthquakes from around the world and found that waves passing through the centre of the Earth behaved as if they had crossed a liquid. Later Inge Lehmann used more precise records, partly from a network of seismographs she helped set up, and showed that the core has a solid inner part inside a liquid outer part. Nobody has drilled more than a few kilometres down; the picture of the core comes from waves.
WaveA disturbance that travels away from where it started, carrying energy
Crest and troughHighest and lowest points of a wave
Wavelength λDistance between neighbouring crests
AmplitudeLargest distance from the rest position
Transverse waveOscillation is perpendicular to travel: the medium in a rope wave, electric and magnetic fields in light
Longitudinal waveMedium moves along the travel direction (sound in air)
Mechanical waveNeeds a material medium; sound cannot cross a vacuum
  1. What does a wave carry from one place to another?
    • Energy
    • The water or air itself
    • Mass
    • Nothing at all
  2. A gull floats on the open sea as waves pass under it. How does the gull move?
    • Mostly up and down, staying near one place
    • Along with the wave toward the shore
    • Only sideways
    • It does not move
  3. A wave on a guitar string is…
    • Transverse
    • Longitudinal
    • Neither
    • Only a sound wave
  4. Sound travelling through air is…
    • Longitudinal
    • Transverse
    • Electromagnetic
    • A mix that needs no air
  5. Which of these can travel through the vacuum of space?
    • Radio waves
    • Sound
    • Water waves
    • Earthquake S-waves
  6. A wave on a rope measures 60 cm from the top of a crest to the bottom of a trough. What is its amplitude?
  7. You make bigger waves on the same rope without changing how tight it is. Their speed…
    • Stays the same
    • Doubles
    • Halves
    • Drops to zero
  8. In an earthquake, which wave reaches a distant seismograph first?
    • The P-wave (compressional)
    • The S-wave (shear)
    • They always arrive together
    • Neither reaches it
  9. Made-up example: P-waves travel at 6 km/s and S-waves at 3.5 km/s. The S-wave arrives 20 s after the P-wave. How far away was the earthquake?
Key points
  • A wave is a travelling disturbance; it carries energy, not the medium.
  • Wavelength λ: crest to crest. Amplitude: rest position to crest.
  • Transverse: shaking at right angles (rope, light). Longitudinal: along the travel (sound in air).
  • Mechanical waves need a medium; electromagnetic waves do not.
Sources for this course (11)
  • OpenStax College Physics 2e (openstax.org/books/college-physics-2e): 16.9 Waves (disturbance that propagates, gull example λ 10.0 m, T 5.00 s, v = 2.00 m/s, transverse and longitudinal, amplitude independent of speed)
  • 16.10 Superposition and Interference (constructive, destructive, standing waves, f1 = v/2L, beats fB = |f1 − f2|, 256 Hz fork with 2 beats -> 254 or 258 Hz)
  • 17.2 Speed of Sound (Table 17.1: air 331 m/s at 0 °C, helium 965, fresh water 1480, sea water 1540, steel 5960, vulcanized rubber 54; v = 331 m/s × √(T/273 K); 343 m/s at 20 °C; audible range 20 to 20 000 Hz; P-waves 4 to 7 km/s, S-waves 2 to 5 km/s; Oldham and Lehmann)
  • 17.3 Sound Intensity (I0 = 10⁻¹² W/m², Table 17.2, factor 10 = 10 dB, factor 2 = 3 dB, 85 dB for 8 h footnote, bel named for Bell)
  • 17.5 Sound Interference and Resonance (noise-cancelling headphones 30 dB or more, closed tube λ = 4L and f_n = n v/4L with n odd, open tube f_n = n v/2L, 128 Hz tube at 22 °C = 0.672 m, ninth harmonic 1.15 kHz, trumpet vs clarinet overtones)
  • 24.1 (Maxwell; Hertz from 1887)
  • 24.3 The Electromagnetic Spectrum (c = fλ, Table 24.1, three rules of thumb, AM 540 to 1600 kHz, FM 88 to 108 MHz, microwave oven 2.45 GHz, visible 400 to 750 nm, UV 400 to about 10 nm, UV-A 320 to 400, UV-B 290 to 320, UV-C 220 to 290 nm, 99% of surface UV is UV-A, X-rays below 0.01 nm)
  • 27.3 Young's Double Slit (1801, d sin θ = mλ, 0.0100 mm and 633 nm example)
  • NASA science.nasa.gov/ems (Introduction, Visible Light: 380 to 700 nm; atmospheric windows)
  • NIST, c = 299 792 458 m/s exact (nist.gov/si-redefinition/meter)
  • ISO 16:1975 (A = 440 Hz, iso.org/standard/3601.html).

Checked: 2026-10-17