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Revised Final Environmental Study Report (24 MB) - Gold Canyon ...

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<strong>Gold</strong> <strong>Canyon</strong> Resources Inc.<br />

Springpole <strong>Gold</strong> Access Corridor Project<br />

<strong>Final</strong> <strong>Environmental</strong> <strong>Study</strong> <strong>Report</strong><br />

4.4 Ground Water<br />

The hydrogeology of the region is predominantly controlled by the exposed bedrock or the overlying<br />

cover of native clay soil. Shallow ground water flow is assumed to be similar to surface drainage,<br />

primarily originating at the heights of land and flowing radially downslope.<br />

4.5 Soils<br />

Soils for the Project area are described in several Ontario Geological Survey publications and<br />

Northern Ontario Engineering Terrain studies.<br />

<br />

<br />

Based on Ministry of Northern Development and Mines Quaternary Geology of Ontario,<br />

West Central Sheet, Map 2554 (Scale 1:1,000,000), subsurface conditions in the region<br />

consist of undifferentiated till of predominantly sand to silty sand.<br />

Based on Ministry of Northern Development and Mines Bedrock Geology of Ontario,<br />

West Central Sheet, Map 2542 (Scale 1:1,000,000), bedrock geology at the site consists<br />

of mafic metavolcanic and metasedimentary rocks and minor iron formation.<br />

There is generally low to moderate relief in the vicinity of the Springpole <strong>Gold</strong> Project, with generally<br />

dry uplands and poorly-drained lowland valleys with thick accumulations of organic soils. In this<br />

region, soils are predominately grey wooded and podsols on well-drained sites as well as peats and<br />

gleysols in poorly-drained areas.<br />

4.6 Terrestrial Plant and Animal Life<br />

The Property is part of the Lac Seul Upland, which extends eastward from Lake Winnipeg in<br />

Manitoba to the Albany River in northwestern Ontario. Forest composition in the Property is typical of<br />

the Lac Seul Upland. Predominant tree species are trembling aspen, black spruce, with some white<br />

birch, balsam fir, and white spruce. Understory ground cover species composition and abundance is<br />

typical of mesic mixedwood boreal sites, and lacks microhabitats likely to harbor rare vascular plant<br />

species. A variety of common, early successional, graminoids and herbaceous ground cover plants<br />

are prevalent on areas of the Property where mature timber has been removed or where the canopy<br />

is open and the ground is exposed to light. Natural re-vegetation and succession has been observed<br />

to be rapid at the Property in areas of historical exploration.<br />

DST has been conducting baseline environmental work at the Springpole <strong>Gold</strong> Project area since<br />

2011. Draft factual reports have been prepared and engagement with the Aboriginal communities is<br />

anticipated prior to finalizing these reports.<br />

With respect the proposed Project, DST has prepared a biological constraints report to compare the<br />

effects associated with the two (2) corridor alternatives. A draft of this report is provided in Appendix<br />

4. A supplemental letter report from DST is provided in Appendix 5 to present the results of a winter<br />

2013 aerial survey. During this aerial survey no caribou were observed in the vicinity of the Project.<br />

Commencing in 2012, supplemental field studies have been conducted with input from MNR to<br />

ensure adherence to the provincial Endangered Species Act. If any habitat use by SAR is identified<br />

during 2012 field surveys, MNR will be consulted to identify any required mitigation measures. If<br />

required, mitigation measures that may be employed may include, but are not limited to, those that<br />

are listed in the bullets below.<br />

July 2013 Page 40

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