Jefferson County - East-West Gateway Coordinating Council
Jefferson County - East-West Gateway Coordinating Council
Jefferson County - East-West Gateway Coordinating Council
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52<br />
<strong>Jefferson</strong> <strong>County</strong> – Section 2<br />
probability of a magnitude 6.0 or greater earthquake is 25-40% through the year 2053.<br />
The January estimates show a 7-10% chance of magnitudes between 7.5 and 8.0 in a 50year<br />
period through 2053.<br />
Probable Risk of Modified Mercalli Levels<br />
I-V Highly Likely<br />
VI Highly Likely<br />
VII Highly Likely<br />
VIII-XIII Likely<br />
Landslides have been categorized by the USGS based on incidence and susceptibility.<br />
These categories are found below. The probable risk of future occurrence in the St. Louis<br />
metropolitan area would be ranked as low, less than 1.5% of the area involved, with a<br />
moderate susceptibility and low incidence.<br />
Landslide Incidence<br />
Low- less than 1.5% of area involved<br />
Moderate- 1.5% to 15% of area involved<br />
High- Greater than 15% of area involved<br />
Landslide Susceptibility/Incidence<br />
Moderate susceptibility/low incidence<br />
High susceptibility/low incidence<br />
High susceptibility/moderate incidence<br />
In the USGS Map, Figure J25, susceptibility is not indicated with the same or lower<br />
incidence. Susceptibility to landsliding was defined as the probable degree of response or<br />
the rocks and soils to natural or artificial cutting or loading of slopes, or to anomalously<br />
high precipitation. High, moderate, and low susceptibility are delimited by the same<br />
percentages used in classifying the incidence of landsliding. Some generalization was<br />
necessary at the map scale and several small areas of high incidence and susceptibility were<br />
slightly exaggerated.<br />
Statement of Next Disaster’s Likely Adverse Impact on Community<br />
The next disaster’s likely adverse impact on <strong>Jefferson</strong> <strong>County</strong> could be critical in terms of<br />
amount of damage to infrastructure (utilities, communications) buildings, deaths and other<br />
cascading disasters including fire and explosions from natural gas and oil pipeline ruptures.<br />
At the time of the New Madrid earthquake in 1811-1812, St. Louis and other major cities<br />
in the central U.S. were sparsely settled and there were few man-made structures. Today,<br />
this region is home to millions of people, including the populations of large cities, such as