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Earthquake Preparedness Information |
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Asst Coordinator |
If you are indoors, follow these steps: Drop -- 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.
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.
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.
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). 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. 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 |
» County EMA (main page) » County EMA (main page)
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