Whether you are in your home, a school classroom, a high-rise or other type of
building, it is important to know how to protect yourself during an earthquake.
Practice what to do during an earthquake with your family members so you can
react automatically when the shaking starts.
If you are indoors, follow these steps:
Duck
-- Duck or drop down to the floor.
Cover
-- Take cover under a sturdy desk, table or other furniture. If that is not
possible, seek cover against an interior wall and protect your head and neck
with your arms. Avoid danger spots near windows, hanging objects, mirrors or
tall furniture.
Hold
-- If you take cover under a sturdy piece of furniture, hold on to it and be
prepared to move with it. HOLD the position until the ground stops shaking and
it is safe to move.
If you are outside when the shaking starts, get into an open area away from
trees, buildings, walls and power lines. If driving, stop safely as soon as
possible. Do not stop under overpasses or bridges. Turn off the engine and turn
on the radio. Stay inside your vehicle below window level until the shaking
stops. Do not get out of your vehicle if downed power lines have fallen across
it.
Earthquake Hazards
There are two primary "hot spots" for earthquakes in the central United States
that will impact Illinois, specifically in the south and southeastern parts of
the state.
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New Madrid Seismic Zone lies within the central Mississippi Valley, from
Cairo, Illinois, through southeastern Missouri, western Kentucky, western
Tennessee and northeast Arkansas. The epicenter of the zone is located just
west and northwest of Memphis, Tennessee.
Historically, this area has been the site of some of the largest earthquakes in
North America. Between 1811 and 1812, four catastrophic earthquakes with
magnitude estimates greater than 7.0 occurred during a three-month period.
Hundreds, if not thousands, of aftershocks followed over a period of several
years.
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Wabash Valley Seismic Zone, in southeastern Illinois
and southwestern Indiana, is capable of producing ‘New Madrid’ size earthquake
events. The epicenter of the zone is located between Mt. Vernon, Illinois, and
West Franklin, Indiana (in Posey County).
Since the discovery of this seismic zone, earthquake awareness and preparedness
have increased. Geologists in Indiana and Illinois have found liquefaction
sites and sand dikes that show evidence of prehistoric earthquakes in the
region.
Measuring the Earthquake
There are two ways to describe the size of an earthquake: magnitude and
intensity. Magnitude measures the energy released at the earthquake’s source
and is determined from seismograph measurements. Intensity measures the
strength of shaking produced by the earthquake at a particular site. This
table
compares the two earthquake characteristics.
It is important to note that as the magnitude measurement increases by one whole
number, the size of the earthquake increases by a factor of 10. Therefore, a
magnitude 6.0 earthquake is 10 times larger than a 5.0, and a 7.0 earthquake is
100 times larger than a 5.0.
For Additional Information
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