West Lake CAG NRRB Submission REVISED ADDENDUM January 4 2018
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11) Short and Long-Term Seismic Risk<br />
Evaluation of earthquake risks at the <strong>West</strong> <strong>Lake</strong> Landfill appears deficient. The <strong>CAG</strong> is greatly<br />
concerned about the unlined landfill being in the alluvial floodplain of the Missouri River. The<br />
landfill is susceptible to liquefaction in the event of a large earthquake. Using the Modified Mercalli<br />
Intensity Scale applied to a 7.6 magnitude earthquake along the New Madrid Fault, St. Louis<br />
County would experience, “Panel walls thrown out of frames; fall of walls, monuments, chimneys;<br />
sand and mud ejected; drivers of autos disturbed. 12 ” It’s not clear to the <strong>CAG</strong> how any cap-andleave<br />
design will prevent the ejection of sand, mud, radioactive and non-radioactive contaminants of<br />
concern at the landfill. Further, the liquefaction of the alluvium will cause slumping and<br />
mobilization of the radioactive contamination into the groundwater, which will make it significantly<br />
more difficult and expensive to remove in the future.<br />
The DNR estimates the probability of a repeat of the 1811-1812 (magnitude 7.5-8.0) earthquakes is<br />
7-10%. More from the DNR:<br />
“The NMSZ [New Madrid Seismic Zone] appears to be about 30 years overdue for a<br />
magnitude 6.3 quake because the last quake of this size occurred 100 hundred years ago at<br />
Charleston, Missouri; on Oct. 31, 1895 (it was a magnitude 6.7). A magnitude 6.3 quake<br />
near Lepanto, Arkansas, on Jan. 5, 1843, was the next prior earthquake of this magnitude.<br />
About 75 percent of the estimated recurrence time for a magnitude 7.6 earthquake has<br />
elapsed since the last quake of this size occurred in 1812. 13 ”<br />
Further, in 2014 the United States Geological Survey (USGS) and various universities discovered a<br />
new seismically active zone closer to the <strong>West</strong> <strong>Lake</strong> Landfill, called the St. Genevieve Seismic<br />
Zone. The severity of impacts in the St. Louis region from a 7.6 magnitude earthquake that<br />
originates in St. Genevieve would likely be greater than a 7.6 magnitude earthquake that originates<br />
near the New Madrid fault.<br />
From the Indiana University report’s author Michael Hamburger “It’s an underappreciated zone of<br />
seismic activity that has potential implications for St. Louis and other populated areas in eastern<br />
Missouri and Southwestern Illinois,” he said. “It’s comparable to the Wabash Valley Seismic Zone<br />
in western Indiana, which is capable of producing moderate-sized earthquakes every few decades<br />
and perhaps has the potential for larger earthquakes. 14 ”<br />
12) Air Contaminates<br />
Exposure pathways focus on the inhalation of air or ingestion of soils from the landfill. The risk of<br />
inhalation from air should include smoke that can carry radionuclides as well as toxic particles and<br />
gases considering that several surface fires have occurred at the landfill since the radioactive wastes<br />
were dumped. Reported fires that the <strong>CAG</strong> is aware of include the following:<br />
− 2015: Surface fire in grass area near OU-1 Area 1<br />
− 2013: South quarry surface fire along Old Boenker Rd.<br />
12<br />
Facts About the New Madrid Seismic Zone, Missouri Department of Natural Resources. Accessed Nov. 2017.<br />
https://dnr.mo.gov/geology/geosrv/geores/techbulletin1.htm<br />
13<br />
Facts About the New Madrid Seismic Zone, Missouri Department of Natural Resources. Accessed Nov. 2017.<br />
https://dnr.mo.gov/geology/geosrv/geores/techbulletin1.htm<br />
14<br />
IU Geologists Identify New Seismic Zone Near Illinois-Missouri Border, Indiana University. Accessed Oct. 2017:<br />
http://archive.news.indiana.edu/releases/iu/2014/11/ste-geneview-seismic-zone.shtml<br />
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