Quebec, Canada

• Property area totals over 100 Square Kilometers
• Property close in proximity to Superior Diamonds, Contact Diamonds and Aurizon Mines
• Easy access to the property via logging roads, close to major highways & towns

The Temiscamingue property is located approximately 40 kilometres east of the town of Ville Marie and 100 kilometeres south of Rouyn Noranda, halfway between the Elliott Lake Uranium camp in Ontario and the Abitibi Gold Belt, within the Grenville Province Front. The project is accessible via logging roads.

Government regional stream sediment survey have identified many anomalies in the area. Property is strategically located between the claims of Superior Diamonds (adjacent to the north) where new kimberlites have recently been discovered and the property of Aurizon Mines (adjacent to the south) which has reported as much as 100 grams of gold per ton during till sampling with the objective of identifying the gold dispersion trains previously outlined. Ivany Mining has acquired a 100% undivided interest of 24928.68 acres in this mineral rich Temiscamingue region.

Regional Geology

The Superior Province is the largest Archean craton in the world, half of which is located in Québec. This craton is a highly prospective region for kimberlite exploration, meeting all four criteria for hosting economic grades of diamond-bearing kimberlite: 1) the presence of an Archean craton; 2) the refractive, relatively cool and low-density peridotitic root of the craton has been insulated against reheating and excessive tectonic reworking; 3) the presence of major tectonic structures; and 4) association of diamonds with other intrusive rocks. Four kimberlite fields have been identified in Québec, the Temiscamingue Field being one of these.

Local Geology

The Property over thrusts 2 geological structural provinces, intruded by granite-granodiorite-mafic and ultramafic rocks all faulted and sheared. Fault sets and lineaments intersect the Structural Thrust Front.

It is on the Central-median ridge of the “Temiscamingue Lake Rift” and on the strike of many Diamond Kimberlite occurrences.
Stream sediment geochemistry points to strong anomalies for Nickel, Uranium, and Rare Earths Elements along with good gold potential and many circular shape magnetic anomalies to be tested for their Kimberlitic potential.