Open in TheBrain

CORNUCOPIA

LOCATIONElko County, Nevada, near the town of Tuscarora
TARGET:Volcanic hosted, low-sulfidation, epithermal Ag-Au quartz veins
COMMODITY:Gold and Silver
Project Highlights

Drill

Hole

From

(ft)

To

(ft)

Length

(ft)

True Width (ft)*

Silver

oz/ton

Silver

g/t

CD-16621316964.82.4283.1
CD-1723533027.28.23282.0
Including23432018.111.92408.7
CD-17164.51738.57.71.8162.1
CD-1818917330.86.60226.1
Including5666704.238.001302.9
CD-2010010034.27.31250.5
Including45904515.413.84474.5
*True widths are approximate and based upon interpretation of the mineralizing controls as currently understood.

Drill

Hole

From

(ft)

To

(ft)

Length

(ft)

True Width (ft)*

Silver

oz/ton

Silver

g/t

CD-4016516556.41.7760.8
Including120145258.64.78163.7
CD-60303010.31.8262.3
L4S-OE019519566.71.3245.1
L5S-OE0909030.80.9934.0
L6S-OE0707023.91.1740.2
*True widths are approximate and based upon interpretation of the mineralizing controls as currently understood.
Overview

Silver Predator’s Cornucopia claims lie within the historic Cornucopia silver (gold) mining district located in Elko County, Nevada. The consolidated land position consists of one patented and 28 unpatented lode claims oriented north-northwest along the Leopard vein system. These claims cover the areas of previous mining activity and historic, non-NI 43-101 compliant silver resources, as well as the remainder of the Cornucopia mining district.

Mineral Resources

There are no current Ni 43-101 compliant resources or reserves on the Cornucopia Property.

Geology and Mineralization

The mineralization in the Cornucopia District is hosted by Tertiary volcanic rocks and is considered to be of the low-sulfidation epithermal type, similar to the Midas mine (Newmont) and the Ivanhoe property (currently under development by Great Basin Gold) located 32 miles to the southwest. Silver (gold) mineralization occurs with quartz veining, silicification and argillic alteration. High-grade silver quartz veins of the Leopard mine display crustiform to colliform banding, and multiple periods of vein and wall rock brecciation. Silver and gold occur with pyrite, acanthite, ruby silver, tetrahedrite, stephanite and electrum.

Historical Exploration

The high-grade silver-gold veins were first discovered in the Cornucopia district in 1873. The Leopard vein was by far the most productive in the district and exhibited grades as high as 400 oz/ton silver and 1 oz/ton gold. Buchanan (1981) reported historical production of 762,000 ounces of silver and 13,400 ounces of gold from 31,000 tons of ore, yielding approximate average grades of 24.6 oz/ton silver and 0.43 oz/ton gold. From 1937 to 1940, approximately 10,000 tons of mine tailings were reworked (Smith, 1976).

Current Work

Silver Predator is currently compiling all historical data and the property is available for lease or option to purchase.

MAPS

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Thomas H. Chadwick, CPG, A Consultant and Officer of the Company, is the Qualified Person as defined under National Instrument 43-101 and has reviewed and verified the information presented above