The mineral deposits at Dome Mountain are structure-controlled orogenic (mesothermal) quartzcarbonate-sulphide veins with associated gold and silver mineralization. Controlling structures are east-west and northwest southeast trending brittle fault zones that dip moderately to steeply south and southwest. The host rocks are Lower to Middle Jurassic subaerial volcanic flows, pyroclastic, and related volcanoclastic rocks.

The most significant gold mineralization on the Dome Mountain Project is contained within five zones of the past-producing Boulder Vein System (listed in order of importance):

- Boulder Main Vein: This zone has a strike ranging from 090° to 100° and dips ranging from 45° to 70° south. The vein has been defined over a strike length of 440 metres from section 652,900 UTME to 653,340 UTME and a down-dip extent of more than 180 metres starting at the surface. The mineralized zone within the vein has a shallow easterly plunge with an average horizontal width of 2.3 metres, ranging from 1.6 to 10.5 metres. The majority of the 43,900 tonnes of past production came from this zone.

- Argillite Vein: The Argillite Vein is a splay off the Boulder Main Vein. It strikes at 120° and dips to the southwest at angles ranging from 35° to 50° and it appears to flatten along strike to the southeast. The zone is somewhat discontinuous over the defined strike length of 240 metres and a maximum down-dip extent of 90 metres. The vein has an average vertical thickness of 3.2 metres, ranging from 2.1 to 3.8 metres.

- Boulder Footwall Vein: This zone is sub parallel to the Boulder Main Vein and is located at the east end of the Boulder Vein System. It has been defined by drilling over a strike length of 140 metres from 653,300 UTME to 653,440 UTME and over a down-dip extent of approximately 200 metres. The zone has an average horizontal width of 1.9 metres, ranging from 1.6 to 3.8 metres. The zone is open down plunge to the east and down-dip. Minor past production came from this zone.

- Boulder West Hangingwall Vein: This vein is also sub-parallel to the Boulder Main Vein. It is a somewhat discontinuous vein with an overall strike length of 100 metres located between 652,960 UTME and 653,060 UTME and a defined down-dip extent of approximately 100 metres. It has an average horizontal width of about 2.4 metres, ranging from 1.8 to 3.8 metres.

-Boulder East Hangingwall Vein: This is a thin and somewhat discontinuous vein that occurs over a strike length of about 50 metres at the east end of and sub-parallel to the Boulder Main Vein.

In additional to the past producing Boulder Vein System , gold mineralization at the Dome Mountain Project is present at twelve separate locations: Free Gold, Forks, 9800, Ptarmigan, Elk, Eagle, Gem, Raven, Hawk, Chance, Hoopes, Jane Cabin, and Pioneer. The Free Gold and Forks zones are classified as past-producers by the BC Government Minfile database while the others are listed as either as prospects or showings. The Cabin Vein is considered to be the westward extension of the Boulder Vein.

The veins occur in a roughly northwest southeast 12 kilometre trend from southeast of Dome Mountain to Mt. McKendrick. This trend may reflect the presence of a deep seated structure. A modest amount of diamond drilling has been conducted on the various veins but to date no minerals resources have been defined.

Several orogenic (mesothermal) quartz carbonate-sulphide veins with economic potential have been identified within the area of the Dome Mountain Project. During the period from 1991 to 1993, Timmins Nickel Inc. mined 43,900 tonnes at an average grade of 12.0 grams per tonne gold from the Boulder Main Vein. Underground mining was conducted by shrinkage stope methods accessed from trackless drift developments on the 1290 and 1370 levels.

The most recent metallurgical testing was initiated by Eagle Peak Resources Inc. in 2009. The work is being conducted by PRA Metallurgical Division (PRA) of Inspectorate America Corp. in Richmond, BC under the direction of Matt Bolu, P.Eng. The purpose of the testing was to investigate the recovery of gold and silver by flotation, cyanide leaching and heap leaching at the pre-feasibility level.

Approximately 1000 kg of sample was taken in equal amounts from the broken muck in six underground drawpoints. The sample was collected under the direction of Daryl Hanson of IGS and shipped to PRA for preparation, analysis and testing. The material from each drawpoint was assayed separately and then combined in equal amounts to form a master composite sample. The head grade of the master composite was 13.3 g/t gold and 61.7 g/t silver.

Four flotation tests were conducted at a nominal primary grind size 80% passing (P80) of 105 mm using conventional reagents such as potassi ........