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technical report on the nechalacho deposit, thor lake project ...

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ENVIRONMENTAL CONSIDERATIONS<br />

Envir<strong>on</strong>mental baseline studies were completed for <strong>the</strong> Thor Lake site by Stantec Inc. in<br />

January 2010. Based <strong>on</strong> <strong>the</strong> baseline studies and <strong>the</strong> pre-feasibility study <strong>project</strong> plan EBA<br />

Engineering C<strong>on</strong>sultants Ltd. have provided a list of potential effects and mitigati<strong>on</strong> measures.<br />

Using EBA’s list of potential effects and mitigati<strong>on</strong> measures, Aval<strong>on</strong> has since submitted a<br />

<strong>project</strong> descripti<strong>on</strong> <str<strong>on</strong>g>report</str<strong>on</strong>g> to <strong>the</strong> Mackenzie Valley Envir<strong>on</strong>mental Impact Review Board to<br />

initiate <strong>the</strong> permitting process.<br />

The observed baseline c<strong>on</strong>diti<strong>on</strong>s, possible risks and mitigati<strong>on</strong> measures are discussed below.<br />

THOR LAKE<br />

General Ecology<br />

The TLP is located within <strong>the</strong> Great Slave Upland High Boreal (HB) Ecoregi<strong>on</strong>, which is a<br />

subdivisi<strong>on</strong> of <strong>the</strong> more extensive Taiga Shield HB Ecoregi<strong>on</strong> (Ecosystem Classificati<strong>on</strong> Group<br />

2008). The landscape is dominated by subdued topography and fractured bedrock plains. Black<br />

spruce, jack pine, paper birch, and trembling aspen form disc<strong>on</strong>tinuous forested patches that<br />

are interspersed with exposed rock. Wetlands and peat plateaus comm<strong>on</strong>ly form around <strong>the</strong><br />

margins of shallow <strong>lake</strong>s, as well as in wetter depressi<strong>on</strong>s and lowlands.<br />

Lakes cover a substantial porti<strong>on</strong> of <strong>the</strong> Ecoregi<strong>on</strong> and several major rivers are also present,<br />

eventually draining into Great Slave Lake (Ecosystem Classificati<strong>on</strong> Group 2008). Lakes are<br />

characterized as transiti<strong>on</strong>al between those located within <strong>the</strong> former basin of Glacial Lake<br />

McC<strong>on</strong>nell, which are more shallow and silty, and those occupying areas at higher elevati<strong>on</strong>s,<br />

which are deeper and more clear.<br />

Hydrogeology<br />

Hydrogeological tests were c<strong>on</strong>ducted by Stantec using multipurpose holes drilled by Aval<strong>on</strong><br />

during 2008-2009. Five holes were installed as m<strong>on</strong>itoring wells, and <strong>on</strong>e hole was installed with<br />

a <strong>the</strong>rmistor. Hydrogeological parameters studied include groundwater elevati<strong>on</strong>, hydraulic<br />

c<strong>on</strong>ductivity, groundwater temperature, and hydrogeochemistry.<br />

Groundwater elevati<strong>on</strong> was observed to be 0.7 m to 4.5 m below ground surface in all <strong>the</strong> wells.<br />

A minimum <strong>the</strong>rmistor reading of -0.75°C was recorded at 14 m below ground surface, which<br />

was <strong>the</strong> maximum depth of <strong>the</strong> string. Recovery tests yielded hydraulic c<strong>on</strong>ductivity estimates<br />

ranging from 6.06 x 10 -8 m/s to 3.08 x 10 -5 m/s, while packer tests yielded estimates from 1.66 x<br />

10 -6 m/s close to surface to 2.90 x 10 -8 m/s at depth. Hydrogeochemical tests show that <strong>the</strong><br />

dominant cati<strong>on</strong>s are sodium and magnesium, and <strong>the</strong> dominant ani<strong>on</strong> is carb<strong>on</strong>ate.<br />

Technical Report 43-101 – March 13, 2011 Page 18-95<br />

Prepared by Aval<strong>on</strong> Rare Metals Inc.

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