Renaissance Gold Inc.


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Nevada / Utah Properties


Status: Available for Joint Venture

Target: The Arabia District contains numerous occurrences of mesothermal high-grade, poly-metallic, gold and silver-rich deposits in a fractured intrusive and metasedimentary rock. Targets include replacement deposits, fissure veins, sheeted veins and vein stockwork in granodiorite intrusions at or proximal to contact zones beneath impermeable metasedimentary caprock.

Location: The Arabia Project is in the Arabia Mining District in the foothills of the Trinity Mountains, 20 kilometers (12 miles) north of Lovelock, Nevada.

Ownership: The property consists of unpatented mining claims administered by the BLM and owned 100% by Renaissance. Also, the property includes 7 patented claims owned by Renaissance and 8 patented claims held by Renaissance under lease agreements.

History: Mining in the Arabia District dates back to discovery in 1859. Nevada's first smelter was built nearby at Oreana to treat ore from the Arabia district and began production in 1867. The principal mines in the area include the West Workings, Montezuma, Electric and Jersey. These mines are all located along veins with some having strike lengths in excess of 330 meters (1083 feet) mined by traditional underground stoping methods. Production for the district is estimated to be about 1 million historical dollars. Antimony was the most valuable commodity produced from the district followed by silver, lead, and gold with minor copper.

Geology: Within the 4 kilometer (2.5 mile) long Arabia District, granodiorite stocks intrude the overlying metasediments of slate, quartzose and calcareous slate to meta-carbonates. The metasediments are seen to form an effective caprock to the intrusions and to ore. Mineralization and alteration tends to follow faulting oriented both north to south and east to west within the district. Favorable carbonate stratigraphy in the metasediment package creates potential replacement targets along faults and marginal to intrusions. After the mineralizing hydrothermal event, erosion exposed parts of the granodiorite intrusions. Tertiary latite and latite tuff then flowed into the area as cover-rock followed by more erosion. Younger Tertiary sediments and tuffs fill in low areas peripheral to the district.

Looking easterly to deposits in the Humboldt Range.

Historic Electric Vein assays at the 150 foot level.