Coyote Knoll is located in central Utah, approximately 85 Km south of Bingham Canyon Cu-Mo-Au Porphyry deposit and 40 km southwest of the city of Eureka. Eureka is historically associated with the Tintic Mining District, which has been a major producer of gold, silver, lead, and zinc from both epithermal and Carbonate Replacement Deposits (CRD). The Tintic District is known for its productive mining history and the potential for undiscovered porphyry systems. Access to the property is vis US highway 6 and well graded gravel roads maintained by Juab County. Rail and power lines are also within close proximity to the project. The 83 lode mining claims are located in parts of sections 33 & 34 of T11S, R6W, sections 4, 5, 6 & 9 of T11S, R7W and section  1 of T12S, R7W, Sal Lake Base and Meridian, Juab County, Utah. The two state leases are section 32 of T11S R6W and section 2 of T12S R7W, Juab County.

The Coyote Knoll project area includes Oligocene-Eocene intermediate to felsic intrusions and associated lavas. Intrusions are hosted in a Proterozoic wall-rock that appears to be dominated by quartzite and lesser limestone. Caldera-collapse ring-structures have been inferred throughout the property and may be broadly related to some of the outcropping intrusions and lavas.

The main mineralizing structure strikes east-west (070°) dipping steeply towards the NNW. This main Coyote Knoll trend host multiple fluid textures including silica flooded pebble clastic fault breccia’s commonly referred to as a pebble dyke along with jasperoid and chalcedony infilling. The two bulk samples were mined from this area targeting native silver and gold mineralization as well as silver sulphide compounds. Mapping and trenching also identified epithermal veining striking northwest-southeast associated with a low angle thrust fault and hosts anomalous silver, gold as well as epithermal pathfinder elements (Sb, As, Mo, Cu, Pb, Zn) within quartz-carbonate and jasperoid Infilling.

The geological setting at Coyote Knoll has important similarities to the Tintic mining district where epithermal precious metal mineralization is hosted within fissure veins that crosscut quartzite, dolostone and volcanic stratigraphy. In the Tintic district quartzites can trap mineralizing fluids providing a ponding effect forming base metal Carbonate Replacement Deposits (CRD) hosted in underlying limestones and dolostones as seen at the Burgin, and Tintic Standard mines. Coyote Knoll hosts similar stratigraphy and carbonate replacement mineralization remain an exploration target in areas where mineralized structures interact with dolostone and limestone units.

During the Coyote Knoll site visit (March 25-27), Triumph Gold confirmed the presence of epithermal mineralization through geological surface grab sampling along known areas of mineralization. Samples returned up to 795 g/t Ag and 1.58 g/t Au from within the historic open pit (Table 3). During this period the company also toured the underground high-grade Trixie gold mine to better understand the regional geological setting of the Tintic Mining district.