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

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Vegetati<strong>on</strong><br />

Vegetati<strong>on</strong> mapping of <strong>the</strong> general Pine Point area was first undertaken in 1977 by BC<br />

Research using black and white aerial photographs and fieldwork. Mapping of <strong>the</strong> area was<br />

carried out again using aerial photographs taken in June 1979 by Beak C<strong>on</strong>sultants Ltd. The<br />

plant communities identified from <strong>the</strong>se studies were: jack pine, aspen, mixed jack pine/black<br />

spruce, white spruce, black spruce, shrub, fen, muskeg and burn, for a total of nine distinct<br />

types.<br />

In September 2005, EBA collected new baseline vegetati<strong>on</strong> and ecosystem data for <strong>the</strong><br />

proposed Tamerlane Pilot Project Regi<strong>on</strong>al Study area located immediately to <strong>the</strong> west of <strong>the</strong><br />

current area of interest.<br />

Eight naturally vegetated ecosystem units were classified within <strong>the</strong> Pine Point Regi<strong>on</strong>al Study<br />

Area. The most comm<strong>on</strong> ecosystem was <strong>the</strong> upland, Labrador Tea – Mesic ecosite (28.3 %).<br />

The Shrubby and Treed fens, characteristic of lowland landforms, were sec<strong>on</strong>d and third in area<br />

(24.6 % and 24.3 %) (EBA 2005a).<br />

Based <strong>on</strong> <strong>the</strong> informati<strong>on</strong> <str<strong>on</strong>g>report</str<strong>on</strong>g>ed in EBA 2005a and our understanding that <strong>the</strong> area of interest<br />

to <strong>the</strong> north of <strong>the</strong> former Pine Point Mine c<strong>on</strong>sists primarily of lowland landforms draining<br />

towards Great Slave Lake, wetland ecosystems dominate <strong>the</strong> land in this area.<br />

The main wetland ecosystems present in <strong>the</strong> area of interest include Graminoid, Shrubby and<br />

Treed Fen ecosites. The fens are generally restricted to areas of poorly drained organic soils.<br />

Soils tend to be rich in nutrients. Stand compositi<strong>on</strong> in <strong>the</strong> regi<strong>on</strong> varies due to <strong>the</strong> fire regime.<br />

Early successi<strong>on</strong>al stands are dominated by an open canopy of bog birch, while mature stands<br />

have a closed canopy of black spruce and larch.<br />

The limited upland landforms in <strong>the</strong> area of interest include Bearberry Pj, Canada Buffalo –<br />

Green Alder, Labrador Tea – Mesic, and Labrador Tea – Subhygric ecosites. They are<br />

dominated by jack pine, aspen and paper birch in seral communities, and black and white<br />

spruce in climax communities. Immediately after fire, <strong>the</strong> communities are dominated by fast<br />

growing deciduous seral species such as paper birch and alder (Alnus species). The slower<br />

growing jack pine becomes <strong>the</strong> dominant species a few years after fire.<br />

To c<strong>on</strong>firm that <strong>the</strong> vegetati<strong>on</strong> cover present in <strong>the</strong> area of interest is as described herein, it is<br />

recommended that an appropriate field study be undertaken during <strong>the</strong> early summer of 2010.<br />

This study could be undertaken in c<strong>on</strong>juncti<strong>on</strong> with an equally necessary wildlife and wildlife<br />

habitat study.<br />

Technical Report 43-101 – March 13, 2011 Page 18-103<br />

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

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