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Yukon Zinc AR 05 - Yukon Zinc Corporation

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Wolverine Project Development<br />

The Finlayson District is Canada's newest volcanogenic<br />

massive sulphide (VMS) district and is centrally located in<br />

southern <strong>Yukon</strong>. The District has the potential to become a<br />

major new mining camp supplying base and precious metals.<br />

Initial exploration in the mid 1990's resulted in discovery of<br />

three significant zinc-lead-copper-silver-gold deposits.<br />

The predecessors to <strong>Yukon</strong> <strong>Zinc</strong> acquired a large claim<br />

holding in the Finlayson District following the discovery by<br />

Cominco Ltd. in 1994 of the Kudz Ze Kayah deposit.<br />

Following the discovered of the exceptionally silver-rich<br />

Wolverine deposit in the fall of 1995 the Wolverine Joint<br />

Venture acquired a very large claim holding in the District.<br />

Exploration by Expatriate led to discovery of the Ice copper<br />

deposit in 1996 and Cominco discovered the GP4F deposit in<br />

1997.<br />

Expatriate acquired a 60% joint venture interest in the<br />

Wolverine deposit from Boliden Westmin (Canada) Limited in<br />

the spring of 1999 and acquired Atna's joint venture interest in<br />

2004 giving <strong>Yukon</strong> <strong>Zinc</strong> a 100% interest in the Wolverine Joint<br />

Venture lands. <strong>Yukon</strong> <strong>Zinc</strong> now owns a 100% interest in 178<br />

square kilometers of the former Wolverine Joint Venture<br />

claims and an additional 517 square kilometres in the<br />

surrounding lands covering much of the favourable<br />

stratigraphy in the Finlayson District.<br />

Exploration continued at low levels in 20<strong>05</strong> as the focus shifted<br />

to development activities. Resumption of exploration is<br />

planned for 2007.<br />

WOLVERINE BELT<br />

The discovery of Wolverine in fall of 1995 spawned the<br />

<strong>Yukon</strong>'s largest ever staking rush and the initial exploration<br />

fever resulted in discovery of several new areas of<br />

mineralization that remain largely untested.<br />

The mid-Paleozoic volcanic and sedimentary rocks hold the<br />

promise of hosting large tonnages of high-grade massive<br />

sulphides. Similar volcanogenic massive sulphide districts<br />

have been very productive in Canada and abroad and have<br />

enjoyed long histories of discovery and development.<br />

The Wolverine deposit is a classic volcanogenic massive<br />

sulphide (VMS) deposit hosted in felsic volcanic and<br />

argillaceous sedimentary rocks of probable mid-Paleozoic<br />

age. The favourable strata are exposed over a strike length of<br />

more than 20 kilometers on the Wolverine property with<br />

multiple occurrences of mineralization. Stratigraphic drilling<br />

has defined several target areas warranting additional drilling.<br />

WOLVERINE DEPOSIT<br />

The Wolverine deposit consists of massive sulphides that<br />

occur in two tabular semi-continuous lenses. Drilling from<br />

1995 to 1997 defined a resource in all categories (Westmin<br />

Resources Ltd., 1998) of 6,237,000 tonnes grading 12.66%<br />

zinc, 1.55% lead, 1.33% copper, 371 g/t silver and 1.76 g/t<br />

gold. In early 2006, a new resource estimate was prepared<br />

PAGE 4<br />

YUKON ZINC 20<strong>05</strong> ANNUAL REPORT

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