SEISMIC SLINKY
A Slinky makes a handy model of earthquake waves. See for
yourself which waves may send you rocking and rolling, and which
ones may bounce you out of your chair.
Before this activity, you may want to read about waves
in the earth. You can also see illustrations of the
motion of P and S waves and the
motion of Rayleigh and Love waves.
What do I need? • A Slinky (two if you have
them) • A partner
Assembly Stretch the Slinky 6 feet (2 meters)
or more between your partner and yourself. Or, tie one end of the
Slinky to a chair or other solid object 6 feet away.
What do I do? 1. Pull the Slinky toward you a
bit and then push it away. Notice that a wave travels along the
Slinky from you to your partner.
Photo: Lily Rodriguez
|
The vibrating parts of the Slinky move back and forth in the same
direction as the wave is traveling. This type of wave is called a
longitudinal wave, or a compression wave, and it’s a model for
seismic primary waves, or P waves. They’re known as primary waves
because they’re the fastest of the earthquake waves, arriving first
at distant points.
2. Shake one end of the Slinky up and down. Notice that a
different type of wave travels along the Slinky.
This time, sections of the Slinky move up and down, perpendicular
to the direction in which the wave is traveling. This type of wave
is called a transverse wave. It provides a model for S waves, the
secondary seismic
waves that travel through solid rock. (S waves can’t travel
through liquid or gas.) More specifically, this models SV waves—S
waves in which the vibratory motion is vertical.
Photo: Lily Rodriguez
|
You can also shake the Slinky from side to side. In this case,
sections of the Slinky will move horizontally—but, as above, the
movement of the Slinky is at right angles to the direction of the
progressing wave. S waves that behave in this manner are called
horizontal S waves or SH waves.
S waves and P waves are known as body waves. They transmit energy
through the earth in all directions from the earthquake’s
focus—the place underground where the temblor began.
Photo: Lily Rodriguez
|
3. Push and pull the Slinky at the same time that you move it up
and down; your hand should move in a circle.
This circular-motion wave models an earthquake wave called a
Rayleigh wave. Rayleigh waves transmit energy from the
epicenter—the point on the surface that’s above the
focus—along the earth’s surface.
4. Hold two Slinkys, one above the other. Move them both from
side to side at the same time—but move the top Slinky further in
each direction than the bottom Slinky. This is a model of a Love
wave. Like the S wave, a Love wave is a transverse wave, but like
the Rayleigh wave, it’s confined to the earth’s surface. The bottom
Slinky illustrates that the energy of a surface wave quickly
diminishes with depth.
What's going on? An earthquake begins when
stress on large blocks of rock becomes greater than the strength of
the rock. The rock fractures, releasing vast amounts of energy. This
energy is carried outward in all directions by various seismic
waves, some of which can reach the opposite side of the earth in
about twenty minutes. The further the waves travel from the focus of
the earthquake, the weaker they become.
P waves push and pull the underground rocks, causing structures
on the surface to move back and forth. SH waves move the rocks
beneath the earth’s surface from side to side, giving buildings on
the surface a good shaking, often with very damaging effects. With
SV waves, the shaking is in a vertical direction—which sometimes can
be enough to launch you out of your seat.
Surface waves are long, slow waves. Love waves shake things from
side to side. The slowest seismic waves, Rayleigh waves, are rolling
waves that make you feel as if you’re struggling to keep your
balance on a ship in the open ocean. |