The earth moves in mysterious ways
It’s a hot Sunday afternoon at the local swimming pool. Where else would you be but in the cool water? At the other end of the pool, an adventurous swimmer leaps from the high dive, curls into a fetal position, and hits the water, cannon-ball style, with a big sploosh.
When the earth shakes, sandy or muddy soils can flow like liquid. These fissures occurred along the Pajaro River near Watsonville in northern California during the 1989 Loma Prieta earthquake.
Those of you lolling in the previously calm waters will notice waves sloshing toward you—and in all other directions from the diver, too. With all due respect to the jumper, the landing is a good metaphor for an earthquake. When the rocks along either side of a fault shift past each other, they send out energy in waves, much like the cannon-baller's sploosh rippled out. And like those waves that go through the pool, the waves of energy caused by the rupture pass through the earth and we feel them as an
An earthquake generates several different
kinds of waves, each characterized by its speed and direction. You can get
an idea of how these waves travel by picturing a Slinky (or better yet, making
waves with your own Slinky, as described in our activity, Seismic Slinky). Waves
that emanate from the site of the quake inside the earth are called body waves.
The first of these are known as P waves, for primary or pressure. They are fast,
traveling through rock at over 225 miles per hour (360 km/hr) and through water
at about one-third that speed, pushing, pulling, and compressing the earth in
the direction of their travel. Imagine that you have your Slinky on its side
on a table. With one person holding each end, push your end forward and pull
back. You’re exerting horizontal force on the Slinky, and you can see
it traveling horizontally as parts of the Slinky compress together or spread apart. This is how P waves travel through the earth, moving it back
An earthquake also causes secondary or shear waves, called S waves. These travel
at about half the speed of P waves, but can be much more destructive. S waves
move the earth perpendicularly to the direction the wave is traveling. Picking
up the Slinky again, move it left and right, rather than forward and back. You’ll
see that as the motion travels down the Slinky, it goes left to right, rather
than forward and back. Now move the end of the Slinky up and down, watch the
S waves travel, and imagine how a building would fare sitting atop the action.
P and S waves may seem
like shaky business, but the waves that really do damage are the ones that occur
when the energy of the quake reaches the surface of the earth. Rayleigh waves
churn over and under like rolling ocean waves; Love waves shake the earth from side to side. Love and Rayleigh waves, named after their discovers, are the ones often responsible for
making buildings collapse. Imagine yourself trying to remain standing while the earth was going through such contortions! To make matters worse, these waves can travel at
different speeds through different types of rock, bouncing back or changing
direction. In places with certain rock compositions, this bouncing will amplify the waves, which will then cause more damage.
Now, imagine a building sitting on ground that is going through all these motions
at once. You can see how an earthquake could devastate a city. That leaves architects
and engineers with quite a challenge when they have to consider
withstand the Big One