<meta http-equiv="refresh" content="1; url=/nojavascript/"> Seismic Waves from Earthquakes | CK-12 Foundation
Dismiss
Skip Navigation
You are reading an older version of this FlexBook® textbook: CK-12 Earth Science Concepts For Middle School Go to the latest version.

Are seismic waves like ocean waves?

Yes, in some ways. Ocean waves travel at the interface between the sea surface and the atmosphere. They have all the features that all waves have. Some seismic waves also travel at an interface. Which ones?

Seismic Waves

Seismic waves are the energy from earthquakes. Seismic waves move outward in all directions away from their source. Each type of seismic wave travels at different speeds in different materials. All seismic waves travel through rock, but not all travel through liquid or gas. Geologists study seismic waves to learn about earthquakes and the Earth’s interior.

Wave Structure

Seismic waves are just one type of wave. Sound and light also travel in waves. Every wave has a high point called a crest and a low point called a trough . The height of a wave from the center line to its crest is its amplitude . The horizontal distance between waves from crest to crest (or trough to trough) is its wavelength ( Figure below ).

The energy from earthquakes travels in waves, such as the one shown in this diagram.

Types of Seismic Waves

There are two major types of seismic waves. Body waves travel through the Earth’s interior. Surface waves travel along the ground surface. In an earthquake, body waves are responsible for the sharp jolts. Surface waves are responsible for the rolling motions that do most of the damage in an earthquake.

Body Waves

Primary waves (P-waves) and secondary waves (S-waves) are the two types of body waves ( Figure below ). Body waves move at different speeds through different materials.

P-waves are faster. They travel at about 6 to 7 kilometers (about 4 miles) per second. Primary waves are so named because they are the first waves to reach a seismometer. P-waves squeeze and release rocks as they travel. The material returns to its original size and shape after the P-wave goes by. For this reason, P-waves are not the most damaging earthquake waves. P-waves travel through solids, liquids, and gases.

S-waves are slower than P-waves. They are the second waves to reach a seismometer. S-waves move up and down. They change the rock’s shape as they travel. S-waves are about half as fast as P-waves, at about 3.5 km (2 miles) per second. S-waves can only move through solids. This is because liquids and gases don’t resist changing shape.

P-waves and S-waves are the two types of body waves.

Surface Waves

Love waves and Rayleigh waves are the two types of surface waves.

Surface waves travel along the ground outward from an earthquake’s epicenter. Surface waves are the slowest of all seismic waves. They travel at 2.5 km (1.5 miles) per second. There are two types of surface waves. Love waves move side-to-side, much like a snake. Rayleigh waves produce a rolling motion as they move up and backward ( Figure above ). Surface waves cause objects to fall and rise. They also cause objects to sway back and forth. These motions cause damage to rigid structures during an earthquake.

Vocabulary

  • amplitude : Height of a wave; this can be measured from a center line to the top of the crest, or to the bottom of the trough.
  • body wave : Type of seismic wave that travels through the body of a planet; body waves include primary waves and secondary waves.
  • crest : Highest point of a wave.
  • Love wave : Surface wave that has a side-to-side motion, much like a slithering snake.
  • primary wave (P-wave) : Fastest type of body wave, capable of traveling through solids, liquids, and gases.
  • Rayleigh wave : Surface wave that has a rolling motion.
  • secondary wave (S-wave) : Slower moving, transverse body wave that can only travel through solids.
  • surface wave : Seismic wave that travels around the ground surface; the two types are Love and Rayleigh waves.
  • trough : Lowest point of a wave.
  • wavelength : Horizontal distance between two waves, as measured from crest to crest or trough to trough.

Summary

  • Body waves travel through the body of a planet. Surface waves travel along the surface.
  • There are two types of body waves: P-waves travel fastest and through solids, liquids, and gases; S-waves only travel through solids.
  • Surface waves are the slowest, but they do the most damage in an earthquake.

Practice

Use the resource below to answer the questions that follow.

  1. What are body waves?
  2. Which waves move the fastest?
  3. What are the S-waves? Describe them.
  4. What happens to body waves as they move through the Earth?
  5. What are the two types of surface waves?
  6. Describe how surface waves travel.

Review

  1. Draw a set of waves and label the parts: crest, trough, amplitude, wavelength.
  2. Compare and contrast P-waves and S-waves.
  3. Describe the motions of surface waves.

Vocabulary

amplitude

amplitude

Height of a wave; this can be measured from a center line to the top of the crest, or to the bottom of the trough.
body wave

body wave

Type of seismic wave that travels through the body of a planet; body waves include primary waves and secondary waves.
crest

crest

Highest point of a wave.
Love wave

Love wave

Surface wave that has a side-to-side motion, much like a slithering snake.
P-wave

P-wave

Primary wave; fastest type of body wave, capable of traveling through solids, liquids, and gases.
Rayleigh wave

Rayleigh wave

Surface wave that has a rolling motion.
S-wave

S-wave

Secondary wave; slower moving, transverse body wave that can only travel through solids.
surface wave

surface wave

Seismic wave that travels around the ground surface; the two types are Love and Rayleigh waves.
trough

trough

Lowest point of a wave.
wavelength

wavelength

Horizontal distance between two waves, as measured from crest to crest or trough to trough.

Image Attributions

Description

Difficulty Level:

Basic

Grades:

6 , 7

Date Created:

Jan 04, 2013

Last Modified:

Dec 15, 2014

We need you!

At the moment, we do not have exercises for Seismic Waves from Earthquakes.

Files can only be attached to the latest version of Modality

Reviews

Please wait...
Please wait...
Image Detail
Sizes: Medium | Original
 
SCI.ESC.363.L.1

Original text