Copper Road Resources Inc. announced results of the spring/summer diamond drilling campaign at the Tribag Mine Zone located on its 21,000-hectare Copper Road Project, approximately 80 km. north-west of Sault Ste. Marie, Ontario, Canada.

Breton Breccia mineralization established from this drill program is hosted in an intensely altered polymictic breccia. The dominant alteration assemblage related to mineralization is sericite-chlorite and carbonate. Chalcopyrite and pyrite content appears to increase with increasing alteration intensity.

These drilling results have demonstrated the presence of broad zones of near surface copper mineralization at the Breton Breccia. The program also confirmed the lateral continuity of copper zones outside of the historical assay models. Drillhole TR22-001 was drilled to test the northern extension of the Breton Breccia.

The hole intersected a short interval of 8.54 meters at 0.26 % Cu and 1.07 g/t Ag from 215 m to 223.54 m. Drillhole TR22-002 tested the southwestern area of the mineralized breccia. It intersected 52 meters at 0.26 % Cu and 3.51 g/t Ag from 21 m to 73 m, including 14 meters at 0.42 % Cu and 4.49 g/t Ag. Drillhole TR22-003 was drilled towards the northwestern fringe of the mineralized breccia.

It returned grades of 0.29 % Cu and 3.19 g/t Ag over 60 meters from 16 m to 76 m, including an interval of 17 meters at 0.41 % Cu and 6.15 g/t Ag. Drillhole TR22-004 tested the southeastern edge of the Breton Breccia mineralization. It intersected several zones of copper mineralization at depth with best results of 0.26 % Cu and 1.17 g/t Ag over 24 meters from 166 m to 190 m, including a 1-meter interval containing 2.40 % Cu and 10.40 g/t Ag.

Drillhole TR22-005 tested the southwestern part of the mineralization and was intended to drill into the heart of the breccia. This drill encountered historical underground workings and was aborted at approximately 200 meters in depth. This hole was not sampled.

Drillhole TR22-006 is a re-drill of hole TR22-005. This hole's location was offset 12 meters to the southwest. This hole intersected a shallow and very wide mineralized zone containing 0.32 % Cu and 2.99 g/t Ag over 100.39 meters from 18 m to 118.39 m, including higher grade intervals of 0.58 % Cu and 4.39 g/t Ag over 30 meters and 1.02 % Cu and 8.39 g/t Ag over 7 meters.

This drillhole encountered an obstruction at 205 meters and the hole, which bottomed in mineralization, was terminated. The Company plans to investigate alternative drilling options to optimize drill hole locations at the Breton Breccia to avoid future drill bit obstructions. East Breccia mineralization is characterized by a chlorite-epidote±sericite-carbonate altered polymictic breccia containing pyrite- pyrrhotite-chalcopyrite mineralization.

Mineralization extends to metavolcanic and felsic rocks. High copper mineralization appears to be associated with increasing silver, molybdenum, and rhenium content. At depth, in a metavolcanic host, there is evidence of a structurally controlled higher-grade copper-silver-molybdenum-rhenium zone.

Drilling results have established the presence of near surface copper mineralization with accompanying anomalous silver, molybdenum and rhenium content. It also indicates the potential for higher-grade mineralization related to a feeder structure at depth. Drillhole TR22-007 tested the northwest extension of the East Breccia mineralization.

It intersected a broad zone of copper mineralization at 0.22 % Cu and 2.94 g/t Ag over 66 meters from 69 m to 135 m, including a 13-meter interval containing 0.30 % Cu and 4.07 g/t Ag from 83 m to 96 m. Drillhole TR22-008 was also drilled to test northwest extension of the East Breccia mineralization. It intersected near surface copper mineralization with best results of 0.27 % Cu and 4.84 g/t Ag over 48.6 meters from 34 m to 82.6 m, including higher grade intervals of 0.46% Cu and 9.97 g/t Ag over 14.80 m from 45 m to 59.80 m and 0.93 % Cu and 13.75 g/t Ag over 3 m from 47 m to 50 m. At depth, the hole also intersected, better grade copper mineralization of 0.60 % Cu and 6.83 g/t Ag with significant amounts of Molybdenum (Mo) and Rhenium (Re) over 9 m from 330 m to 339 m. This interval includes a higher-grade zone of 1.07 % Cu, 11.30 g/t Ag, 0.57 % Mo, and 2.09 g/t Re over 2.22 m from 333.78 m to 336 m.