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Mexico

Picachos Project

NWT Uranium Corp. negotiated an option to earn 70% interest in the 19,000 acre (7,700 hectare) silver-gold Picachos project in Durango, Mexico.

Soil geochemical surveys and chip-channel sampling conducted in 2005 at Picachos significantly expanded the property's potential and defined epithermal precious metal districts on four adjacent areas: Los Cochis, Guadalupe, El Toro and El Pino.

Further exploration, including drilling, in 2007 at the Los Cochis area has revealed the potential for a near-surface, bulk tonnage polymetallic (silver-lead-zinc) area that would be amenable to open-pit mining.

The property represents NWT Uranium's first initiative into the emerging Latin American gold region, an area in which PricewaterhouseCoopers recently said a significant portion of the world's exploration dollars are being spent. This investment is supported by industry confidence in the traditionally under-explored, higher quality assets available in this area of the world.

Mexico 2004 - AWW at portal of Las Chivas Mine (adit flooded), Los Cochis area 52 KB, approx. 11 seconds at 56.6Kbps

Mexico 2004 - El Pino Area from Espinaza del Diablo viewpoint 32 KB, approx. 7 seconds at 56.6Kbps

Mexico 2004 - General view of Sierra Madre Mountains near Mazatlan 19 KB, approx. 5 seconds at 56.6Kbps

Picachos

Location of the Picachos project in the Mexican State of Durango 25 KB, approx. 6 seconds at 56.6Kbps

The Picachos project area consists of a total of approximately 19,000 acres (7,700 hectares). The area includes the Picachos claim with 10,370 acres (4,200 hectares), the Camargo claim at 6,350 acres (2,570 hectares) and Camargo-2 with 2,390 acres (970 hectares).

A Conceptual Study of the Picachos silver-gold area conducted by Watts, Griffis and McOuat (WGM) in 2004 reported that the eastern portion of the Picachos claim hosts a major north-northwest trending shear zone measuring at least 2.5 miles (four kilometers) in length. This zone controls epithermal mineralization at the El Pino prospect and may be related to gold-porphyry stock at depth. WGM further explained that even at relatively low elevations, the silver-gold ratios are quite high and it is possible that the near surface mineralization at El Pino and El Toro represents the upper part of a largely unseen (or buried) mineralized system.

For the purposes of the report, WGM examined various deposits in Durango State within the Sierra Madre region that are believed to offer comparable geology to Northwestern's Picachos area. The property is located within the gold-silver district spanning 994 miles (1,600 kilometers) from near the northern U.S. border to the Pachuca deposit just north of Mexico City.

Picachos Map 161 KB, approx. 31 seconds at 56.6Kbps

Most of the regional deposits and mineralization on the property are hosted within a Late Eocene volcanic complex, specifically within caldera structures. Mineralization is of the low sulphidation epithermal type occurring in structurally controlled veins and brecciated zones within hydrothermally altered tuffs and ignimbrites. The previous operator, Camargo, had sampled 10 historical mineralized areas, many consisting of multiple showings of silver-gold and silver-lead-zinc-copper-(gold) mineralization. Based on the results of more than 190 soil, stream and rock samples reported by Camargo and 10 characterization samples collected by WGM from six of these sites, WGM is of the opinion that the Picachos area has the potential to host an economically significant silver-gold deposit.

Gold and silver mineralization is widespread in the Picachos property as indicated by numerous old mine workings (an area of more than 50 square kilometers) and geochemical rock sampling by Camargo which reportedly gave average metal values in the caldera structure of 0.9 grams of gold per tonne (g/t) and 98 g/t silver and a silver-gold ratio in the order of 200:1 to 275:1. Research by Clarke and Titley (1988) in the Tayoltita mine area about 25 miles (40 kilometers) north from Picachos, in the same geological setting indicated that the higher silver-gold ratios were characteristic of the top of the epithermal boiling zone and showed that the silver-gold ratios at Tayoltita were considerable lower indicating the possibility that the mineralization at Picachos was near the top of the epithermal zone. Sampling by Camargo of the Breccia Madre in the upper stope at El Pino mine gave an average grade of 462 g/t silver 2.6 g/t gold across 5.2 meters. Sampling by WGM, in the same upper stope, gave 722 g/t silver and 2.78 g/t gold over 2 meters. At the El Toro mine, some 800 meters lower in elevation and approximately 5 kilometers to the southwest, sampling by Camargo returned 761 g/t silver and 1.8 g/t gold across 1.8 meters. A WGM sample in the same area over 1.5 meters returned 250 g/t silver and 0.39 g/t gold.

Picachos Property 18 KB, approx. 4 seconds at 56.6Kbps

WGM postulates, based on the known mineralization on the property, and based on other regional producers whose deposits range from 1.2-97 million tonnes, that the Picachos property has an exploration target with the potential to host a deposit in the order of 10 to 20 million tonnes with metal grades in the order of 200 to 500 g/t silver and 1.0 to 3.0 g/t gold. The potential quantity and grade is conceptual in nature. There has not been sufficient exploration on the property to define a mineral resource and that it is uncertain if further exploration will result in discovery of a mineral resource on the property.

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This page was created on Tue Sep 7, 2010 at 5:34:23 AM Pacific Time.