Scottie Resources Corp has the option to acquire a 100% interest in the 471.92 hectare Bow property (the “Bow”) located in the Golden Triangle mining district of British Columbia.
The Bow is contiguous with the Company’s 100% owned Scottie Gold property which hosts the past producing Scottie Gold mine. The Scottie Gold mine, operated from 1981 to 1985, milled vein material averaging 16.2 g/t gold, producing 95,426 ounces of gold from 183,147 tonnes of mineralization. Previous exploration work has indicated 13 different gold-bearing veins on the Bow and Scottie Gold properties.
The Bow property covers a package of Hazelton Group volcanic rocks in contact with the Summit Lake stock, part of the Texas Creek plutonic suite. This sequence of rocks exhibits similar alteration and mineralization to the former-producing Premier mine 20 kilometres south of the Bow property, and the KSM copper-gold porphyries and Brucejack gold deposits 20 kilometres north of the Bow property.
A small drill program in 1985 by Esso (1091 m) targeted the Bend vein, where drill results over a 16 m strike-length interval of the vein had an average width of 2 m, with average grades of 22.7 g/t gold and 67.5 g/t silver. This includes a 4.17 m true width interval grading 70.65 g/t gold. Drilling also tested the Blueberry vein, where a 1.59m interval was intersected - averaging 26.59 g/t gold, and 21.83 g/t silver.
Drilling in 2005 by Tenajon (535.7 m) traced the Bend vein structure over 110 m and up to 60 m down-dip. Using only the weighted averages from the 2005 drill core, the zone grades 13.3 g/t Au, 36.7 g/t Ag, 0.25% Co and 0.16% Cu across 1.64m (true width).
In late 2013, Decade Resources Ltd. (“Decade”) completed an extensive program of mapping, sampling, prospecting and trenching on the Bow property. Trenching of a 4.5 metre vein returned numerous high-grade gold results including 23 assays exceeding 500 g/t gold. Three main areas were explored, namely the Bend vein area, the Oro Grande/Blueberry vein area and an area near the south end of the Bow property. Work defined three new veins and a possible fourth along the access tunnel to the former Scottie Gold mine near its A portal. This access tunnel starts at the southwestern portion of the Bow property and was driven southwest for 2.3 kms to the Scottie Gold mine. The dumps for the broken muck from the first 500 metres of the tunnel (on the Bow property) are at the A portal. Pieces of massive pyrrhotite-pyrite mineralization are present in this dump, indicating the presence of a vein and/or veins in the first 500 metres of drifting. Fine visible gold is present in bluish quartz fragments within a matrix of massive pyrrhotite-pyrite.