The Causes of Earthquakes
Loretta F. Kasper, Ph.D.
History of Earthquake Study
Questions
about the causes and the nature of earthquakes have occupied the minds of
people since ancient times. Earthquakes
have been
attributed
to a
variety of things from subterranean winds to fires deep within the earth. However scientific theories about the causes
of earthquakes are relatively recent.
In
1859, the Irish engineer Robert Mallet proposed that earthquakes occurred by a
sudden flexing and constraint of the elastic materials forming a portion of the
earth's crust or by the crust giving way and becoming fractured. In the 1870's, the English geologist John
Milne devised a forerunner of today's earthquake recording devise, the
seismograph.
The
modern seismograph was invented by the Russian seismologist Prince Boris
Golitzyn in the early 20th century.
This device used a magnetic pendulum suspended between the poles of an
electromagnet.
Theories
About the Cause of Earthquakes
There
are two major theories which have been advanced to explain the cause of
earthquakes. The first theory states
that the snapping back of distorted
and ruptured rocks is the cause of earthquakes. This means that the rocks within the earth break apart, release
seismic waves, and then "snap back" much like a rubber band does when
we stretch and then release it.
Seismic
waves have an extremely complex nature.
The sudden force that generates them is not an actual blow, but a snap
of billions of tons of bedrock as they are twisted and strained out of shape by
an accumulation of geological
forces built up over many, many years.
The bedrock ruptures along a fault and then snaps back, relieving the
stress. This "snapping back"
causes the earthquake. This phenomenon,
called "elastic rebound,"
was first described by Harry Fielding Reid, the man who led the investigation
into the San Francisco earthquake of 1906.
The
second theory regarding the cause of earthquakes is based on the science of
plate tectonics. This theory proposes
that earthquakes result from stresses set up by movement in the major and minor
plates that make up the crust of the earth.
This theory describes the earth as being divided into many different
pieces, much like a jigsaw puzzle.
These tectonic earthquakes are very destructive and cause the most
devastation.
Earthquakes
can also be caused by volcanic activity, as in Hawaii, or even by human
activity. When people fill new
reservoirs or detonate atomic explosives underground or pump fluids deep into
the earth through wells, they can sometimes induce earthquakes.
Plate
Tectonics
Plate
tectonics is the study of the movement of the earth's plates. Plate tectonics is an important area of
study because plate movements generate a large proportion of all earthquakes. When plates glide along each other sideways, it is called a strike-slip fault. When the plates snag, pressure builds until
one lurches forward, producing an earthquake.
The San Andreas fault in California is an example of a strike-slip
fault.
When
one plate pushes over another, it is called a thrust fault. It too
will rupture if the plates lock, but its presence may be unknown until
then. The Davis fault below Los Angeles
is an example of a thrust fault. The
rupture of an unknown thrust fault running east-west in the San Fernando Valley
appears to be the cause of the 6.6 magnitude Northridge earthquake that struck
near Los Angeles in January, 1994.
Earth Waves
The interior of the earth, called the
earth's crust, is known to us by studying the records of earth waves. Earth waves carry away some of the energy
released when earth materials rupture.
Waves are generated through the earth as a consequence of a rupture of
the cracks in the earth or a constantly expanding wave front.
There
are two major types of earth waves: body waves and surface waves. Body waves travel through the interior of
the earth. Surface waves travel along
the surface. There are three sets of
earth waves--P, S, and L waves--evident in earthquakes.
P
or primary waves go through anything: gas, liquid, or solid. The wave particles move in a push-pull, or
compressional wave. These waves move
out from the quake's origin and alternately compress and stretch the material
they travel through.
S,
or shake or shear, waves go through solids only, and are responsible for the
breaking of solids. The particles move
at right angles to the direction of the waves advance. They produce a ripple effect, an up-and-down
and side-to-side oscillation
like the snapping of a rope.
L
waves are surface waves that travel along the surface to the recording station
from the area directly about the focus of the earthquake. These waves are more complex. One type, known as Love waves, whips back
and forth horizontally. The second
type, called Rayleigh waves, moves along like an ocean breaker, rotating the
rock and soil in an elliptical pattern.
All
waves travel at a constant velocity
through different materials. We can
measure the velocity of the waves to determine the type of material they travel
through. As waves pass through
different materials there is a change in their velocity. This change is called a seismic discontinuity.
Time-distance
graphs are the bases for analyzing the history and speed of earth waves. Travel times are governed by the materials
through which waves have traveled.
Locating earthquakes requires data from several stations. Earthquake prediction may be possible
primarily by observing and interpreting preceding, or precursor, events, including crustal movements, tilt of the earth's
surface, and changes in fluid pressure and in electrical and magnetic fields.
The
Structure of the Earth
The
earth is made up of three layers, crust, mantle, and core. The earth's crust is separated from the
mantle at a discontinuity called the Mohorovic, or the Moho, or the M
discontinuity. The crust of the
continental U.S. varies between 20-60 km in thickness. The crust under the oceans averages about 5
km in thickness. The mantle extends to 2900 km in depth. The lithosphere contains the crust and the
upper, colder part of the mantle. The
asthenosphere extends downward from its border with the lithosphere to about
500 km. The core is thought to have a
liquid outer zone and a solid center; the outer zone behaves as a liquid in not
allowing S waves to penetrate.
Vocabulary
Directions:
Using the context of the reading passage, write a definition for the
following words.
1.
attributed
2.
distorted
3.
accumulation
4.
induce
5.
strike-slip fault
6.
thrust fault
7.
oscillation
8.
velocity
9.
discontinuity
10.
precursor
Comprehension Questions
Directions:
Using your own words and the material provided in the reading passage,
write an answer to the following questions.
1. How were earthquakes explained in ancient
times?
2. Who was Robert Mallet?
3. Who was responsible for inventing the
seismograph?
4.
What is the elastic-rebound hypothesis for the cause of earthquakes? Which
scientist proposed the elastic-rebound hypothesis?
5. What is a second theory about the cause of
earthquakes based on?
6. Why are tectonic earthquakes so dangerous?
7. In addition to elastic-rebound and plate
tectonics, what other types of activity can cause earthquakes?
8. Plate movements generate a ______________of
all earthquakes.
9. Describe an earthquake in a strike-slip
fault.
10. Describe an earthquake in a thrust fault.
11. What are the principal earthquake
waves? How are they similar? How do they differ from one another?
12. What are some of the principal kinds of
earthquake precursors?
13.
What does a seismic
discontinuity tell us about the structure of the earth?
14. What have earthquake studies taught us about the structure of the earth's interior? Make a sketch to show the various parts of the earth.