For many years, the
Richter Scale was the most common and familiar earthquake magnitude scale, but
as recording instruments have become increasingly sophisticated, more accurate
calculations have evolved to determine magnitude. Today, the Richter Scale is
seldom used, and scientists prefer to designate any given earthquake with just
the word "magnitude," which can represent a number of different scales used in
the calculation process.
There are two
important things to remember about earthquake magnitude:
-
The size of an earthquake
increases by a factor of 10 as magnitude increases by one whole number. A
magnitude 6.0 earthquake, then, is 10 times larger than a 5.0; a magnitude 7.0
is 100 times larger, and a magnitude 8.0 is 1,000 times larger than a 5.0.
-
The amount of energy released,
however, increases by a factor of about 32. Looking at the same magnitudes, a
magnitude 6.0 earthquake releases 32 times more energy than a magnitude 5.0; a
7.0 releases about 1,000 times more energy, and a magnitude 8.0 releases about
32,000 times more energy than a 5.0. It is easy to see why magnitude 7.0 and
8.0 earthquakes cause such widespread damage and destruction.
From those numbers
it can also be observed that even though a fault may produce a lot of small
earthquakes, a larger one won't be prevented.Scientists have also
learned that the New Madrid fault system may not be the only fault system in
the Central U.S. capable of producing damaging earthquakes. The Wabash Valley
fault system in Illinois and Indiana shows evidence of large earthquakes in its
geologic history, and there may be other, as yet unidentified, faults that
could produce strong earthquakes.