Canadian Gold and Base Metal Exploration
TSX-V: KG

Title Holder:
Klondike Gold
KG Ownership:
100%
Acquisition Method:
Takeover
Underlying Royalties:
5%
Land:
1,341 ha
Claims:
239 claims leased
Location:
48 km SSE of Dawson City at Indian River
600125 E 7062600 N, UTM ZONE 7N (NAD 83)
Mineral Targets:
Gold (Placer)
Qualified Person:
N/A
Indian River

Asset Considerations

The Indian River property, including McKinnon Creek, is a 7 kilometer long by 2 kilometer wide property that hosts one of the largest unmined White Channel Gravel-hosted placer gold resources in the region. The property is owned 100% by Klondike Gold Corp. through the acquisition of Klondike Star Mineral Corp. (now a subsidiary of Klondike Gold Corp) completed July 2014 and the acquisition of 46799 Yukon Inc. 50% interest completed September 2014. An underlying 5% gross production royalty is payable to 19651 Yukon Inc.

In 2014 Klondike Gold Corp. entered into a lease agreement with Todd Hoffman’s Jerusalem Mining LLC (“Jerusalem Mining”)(operating as “316 Mining”) whereby Klondike Gold assigned to 316 Mining the rights and permits to placer mine on the McKinnon Creek property, Yukon. Under the terms of the lease agreement Klondike Gold will receive a 20% production royalty from 316 Mining (including the 5% payable to 19651 Yukon Inc.) subject to a minimum annual payment of 100 ounces of raw gold or cash equivalent. The lease agreement is renewable annually for three years subject to annual approval by both parties.

Property Geology

The Indian River valley is located south of Dawson City and forms the southern boundary of the “Klondike Gold Fields”. Bedrock is Jurassic age Klondike schist dated at +/- 260 Ma. Gold-bearing White Channel Gravel is Pliocene age and was deposited in the Indian River Valley between 5 Ma and 2.6 Ma in a braided river environment. The lower portion of White Channel Gravel at Indian River is a clast-supported cobble-size gravel comprised of predominantly angular to sub-round quartz clasts plus other Klondike schist lithologies. The highest gold concentrations consistently occur in this subunit. The upper portion of White Channel Gravel is oxidized, matrix-supported sand and gravel. Stacked channelized scours on 10-30 meter scale occur, with coarser material in the bottom of the scour. Locally high concentrations of gold can occur in these scours.

Work Completed

Approximately 50% of the property has been tested by 550 auger drill holes between 2005 and 2014 to locate and delineate White Channel Gravel ‘pay streaks’. Gold was recovered from nearly 100% of the holes in the main target area. Drill results indicate gold-bearing gravels extend over a distance of more than three km (1.9 miles) and remain open for expansion to the east and south.

Test mining beginning at the north-eastern claim boundary began in 2012. A total of 120 ounces of gold was reported as recovered that year. Mining continued in 2013 with a total of 210 ounces of gold reported as recovered. This operation was terminated in late 2013 and Klondike Gold repurchased full ownership and control. In 2014, 316 Mining produced 1,350 ounces of gold from the area mined in 2012. In 2015, 316 Mining opened a new cut where mining recovered 3,000 ounces of gold from upper gravels out of a 4,500 ounce projected resource. 316 Mining terminated the lease in May 2016. A gold-bearing stockpile remains, and testing in September 2016 determined appreciable gold remains in the lowest gravels within the “mined” cut. The fineness of the gold assays at 82%.

As of January 2017, this placer project is for sale.

Photo Gallery - McKinnon Creek Placer Mine

IMG_1062

KG Director Tour 2015


DSC01137

Dave Debriefing Peter on the Progress



P1010010

Going Over the Drill Maps


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First Clean Out of 2014