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Pierre River Mine Project

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WATER AENV SIRS 15 – 43<br />

Section 12.1<br />

Response 33c The data to support the position presented in the May 2009 <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong>,<br />

Supplemental Information, Volume 2, SIR 306b, that the sinkholes do not<br />

exacerbate or attenuate effects of the project, were described in SIR 306a. These<br />

data included:<br />

Reference<br />

• local geology and hydrogeology (Section 5.4.3 and Figures 29, 32 to 38 of<br />

the Hydrogeology ESR, WorleyParsons Komex, 2007)<br />

• groundwater levels in shallow and deeper Quaternary deposits (Figures 37<br />

and 38; WorleyParsons Komex, 2007)<br />

• bathymetry data for Sinkhole Lakes 1 and 2 (EIA, Section 8.4.5.2, pp 8-77)<br />

• water chemistry for Sinkhole Lakes 1 and 2<br />

• groundwater chemistry for Quaternary deposits, McMurray Formation, Basal<br />

aquifer and Devonian Formation (Table 11, WorleyParsons Komex, 2007)<br />

• major ion characterization for Sinkhole Lake, Basal aquifer and Devonian<br />

Formation waters (Figure 306-1, May 2009 <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong>, Supplemental<br />

Information, Volume 2)<br />

Based on these data, the following conclusions were reached:<br />

• the shallow groundwater flow direction is not altered by the sinkholes<br />

• the hydrochemical signature of the sinkhole lakes is calcium-bicarbonate<br />

(Ca-HCO3) type, indicative of freshwater<br />

• the hydrochemical signature of the basal aquifer near the sinkholes is<br />

sodium-bicarbonate-chloride (Na- HCO3-Cl) type, indicative of an older,<br />

deeper, regional groundwater flow system<br />

• the difference in hydrochemical signatures indicates a lack of hydraulic<br />

connection between the sinkholes and deeper deposits<br />

WorleyParsons Komex. 2007. Hydrogeology Environmental Setting Report for<br />

the Jackpine <strong>Mine</strong> Expansion and <strong>Pierre</strong> <strong>River</strong> <strong>Mine</strong> <strong>Project</strong>. Prepared<br />

for Shell Canada Limited, Calgary, AB. Submitted December 2007.<br />

Request 33d In Shell’s discussion of Karst, a reference is made to Figure 8.4-6 in Volume 5 of<br />

the EIA, the Terrestrial Section. Figure 8.4-6 illustrates the locations of three<br />

sinkholes, while Figure 8.4-7 shows there to be four. Clarify this discrepancy.<br />

Response 33d Figure 8.4-7 is based on the surficial geology map by Bayrock (1971) and shows<br />

four sinkhole locations near the border of the Eymundson ESA and a fifth<br />

12-48 Shell Canada Limited April 2010<br />

CR029

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