Torq Resources Inc. announced drill results from the first two drill holes at the Cerro del Medio target in the Company's inaugural drill program at the Santa Cecilia gold - copper porphyry project located in the Maricunga belt in northern Chile. The project is located approximately 100 kilometres (km) east of the city of Copiapo and is immediately adjacent to the Norte Abierto project held by Newmont and Barrick, which is comprised of the Caspiche and Cerro Casale gold - copper porphyry deposits. The Santa Cecilia project hosts a 10 square kilometre hydrothermal alteration system that extends across the property boundary to host Norte Abierto's Caspiche deposit, which is held in a 50/50 joint venture by Newmont and Barrick.

Santa Cecilia is host to a cluster of porphyry targets that are mineralized either on surface or at shallow depths across approximately 4 km of length with very limited or no drill testing, providing the Company the opportunity to find one or more large-scale porphyry deposits at or near surface. At the Cerro del Medio target area, Torq drilled two holes approximately 700 m apart for a total of 2,059 m. Both drill holes were targeting a north - northeast trending structural corridor with the objective of intersecting the high-grade causative intrusion(s) responsible for the observed wall rock mineralization from the 2012 drill holes, CDM-12-003 and CDM-12-002. Torq's drill holes were targeting porphyry mineralization underlying areas of stockwork veining, brecciation and outcropping diorite porphyries along with conductive and magnetic anomalies.

Drill Hole 23SC-DDH-002 was drilled to cross a prominent northeast trending structural corridor, zones of local stockwork veining and an associated gold-in-soils geochemical anomaly. It intercepted 557 m of 0.38 g/t Au, 0.23% Cu and 56 ppm Mo, bottoming in mineralization and successfully extending the porphyry-style mineralization in wall rock by 170 m southeast and 500 m vertically, upward from the 2012 historical intercept, CDM-12-003. The intercept accomplished two goals for the Company; a significant increase in grade and confirmation of porphyry style mineralization at higher elevations that remain open upward, downward and laterally.

Importantly, the increased grade observed within wall rock mineralization provides a clear vector toward the south and east and suggests the existence of a potentially higher-grade causative intrusion that has not yet been found. The upper part of the drill hole, from surface to 520 m, is characterized by dacitic volcanic tuffs and phreatomagmatic breccia bodies with strong argillic and sericite alteration. The entire interval averages 0.1 g/t Au; however, from 460 m - 520 m there is a 60 m interval averaging 0.47 g/t Au and 0.11% Cu in an intensely clay and silica altered pumice tuff characterized by disseminated pyrite, fine quartz veining and trace hypogene chalcocite and covellite.

The lower part of the drill hole, from 520 m - 999 m is characterized by multiphase dioritic to dacitic porphyry dykes intruding into primarily andesitic wall rock. This section of the drill hole is characterized by porphyry-style stock work veining and associated gold - copper mineralization. The porphyry dykes intersected to-date represent an increase in volume from historical drilling and at this stage, are interpreted to be pre-mineral or intra-mineral in nature.

Drill Hole 23SC-DDH-001 was drilled to cross a prominent northeast trending structural corridor, zones of local stockwork veining and an associated gold-in-soils geochemical anomaly. It intercepted 476.3 m of 0.23 g/t Au, 0.22% Cu and 93 ppm Mo, bottoming in mineralization and successfully extending the porphyry-style mineralization in wall rock by 300 me east from the 2012 historical intercept, CDM-12-003. The porphyry mineralization is primarily hosted in potassically altered andesitic and sandstone basement units.

No causative intrusion was encountered in this drill hole, although three phases of porphyry dykes were intercepted, demonstrating a multi-phase porphyry system. The upper part of the drill hole, from surface to 430 m, is characterized by late dioritic porphyry dykes and a large polymictic phreatomagmatic breccia that contains mineralized clasts of dacitic and dioritic porphyries. The average gold grade within this breccia body is approximately 0.1 g/t Au, but where mineralized clasts are abundant, gold grades increase with values of up to 0.5 g/t Au.

The presence of the mineralized porphyritic clasts suggest that higher grade mineralization may be present to the east and at depth. From 430 m - 490 m, hypogene covellite and chalcocite are observed staining pyrite veins and fractures, indicating the transition from epithermal to porphyry environments. The lower part of the drill hole, from 490 m - 1,060.3 m, is characterized by porphyry-style mineralization.

The gold - copper mineralization is hosted in pre-mineral to intra-mineral porphyry dykes and andesitic wall rock that is characterized by well-developed stockwork veining. Alteration in the lower part of the drill hole is characterized as potassic with abundant biotite that is weakly to moderately overprinted by sericite-chlorite alteration. The characteristics of the stockwork veining in the wall rock that forms the bulk of the intercept is similar in nature to that observed in the 2012 historical drill hole, CDM-12-003.

With Torq's first two drill holes completed at Santa Cecilia having demonstrated higher grades within the system, the Company's technical team is completing detailed geological logging and modeling of the porphyry system to refine additional drill targets at Cerro del Medio with the objective of intersecting the higher-grade causative intrusion. The Company plans to resume its phase 1 drill program in Fourth Quarter of this year, with an additional 10,000 m - 12,000 m of drilling that would focus on the Cerro del Medio target while also testing its Pircas Norte and Gemelos Norte porphyry targets further to the east, where there is outcropping porphyry mineralization adjacent to the Caspiche deposit.