In the KMZ interval, mineralization is hosted in brecciated volcaniclastic andesite in the hanging wall of a healed fault zone at 156-184 m. Alteration is potassic (magnetite-chlorite ± biotite ± actinolite) and phyllic (sericite-chlorite ± albite ± ankerite). Veins include early-, intermediate-, and late-stage types. Chalcopyrite-pyrite mineralization is vein-hosted and disseminated.

In the Kliyul North interval, mineralization is hosted in volcaniclastic andesite with an early diorite intrusion from 367-433 m. Alteration is phyllic and propylitic (epidote-chlorite ± anhydrite ± albite) overprinting relict potassic. Mineralization is vein-hosted and disseminated pyrite > chalcopyrite. KLI-22-046 (azimuth 360°, inclination -55°) provided a 100-150 m westward step-out from mineralization in KLI-15-035 and KLI-22-042 in Kliyul North.

The drill hole was collared in KMZ and intersected the Valley Fault at 92 m after which drilling remained in Kliyul North until end-of-hole at 501.0 m. Significant intervals of mineralization include, 169.0 m of 0.55% CuEq or 0.75 g/t AuEq starting from 273 m (Kliyul North); including 59.0 m of 0.89% CuEq or 1.22 g/t AuEq starting from 371 m (Kliyul North). Mineralization is hosted in volcaniclastic andesite and an early diorite dyke and local rock-flour matrix breccia. Alteration is alternating sericite-chlorite and propylitic assemblages with local phyllic overprint.

Veins include mainly early-to-intermediate stage types. Chalcopyrite-pyrite mineralization is vein-hosted and disseminated. KLI-22-047 (azimuth 008°, inclination -55°) tested a plug-shaped chargeability-resistivity geophysical target 500 m west of KMZ along the Valley Fault Trend.

The drill hole was collared 500 m west of Lui Fault in a large step-out into Kliyul West zone. The Valley Fault zone appears to have been intersected between 329-352 m and drilling continued into Kliyul North zone to 486 m. The best mineralized interval is, 53.0 m of 0.18% CuEq or 0.25 g/t AuEq starting from 332 m (Kliyul West/Kliyul North). Weak mineralization is spatially related to the interpreted Valley Fault.

It is hosted in volcaniclastic andesite with a narrow (1.4 m) diorite dyke. Alteration is phyllic. Mineralization is fracture fill and disseminated pyrite > chalcopyrite.

Intermediate-stage pyritic veins (D vein equivalent) are also noted. KLI-22-048A (azimuth 290°, inclination -65°) tested a chargeability-resistivity geophysical target 600 m east of KMZ along the Valley Fault Trend. KLI-22-048A was a re-entry on KLI-22-048 due to a cave-in while reducing from HQ to NQ.

The drill hole was collared 500 m east of the Divide Lake Fault in a large step-out into Kliyul East zone. For logistical reasons the hole was collared above the projected Valley Fault zone and drilled into Kliyul North where it continued to 591.0 m. The best mineralized interval is, 10.0 m of 0.46% CuEq or 0.63 g/t AuEq starting from 352 m (Kliyul North). Narrow mineralization is spatially related to a foliated shear zone at 347-361 m and hosted in volcaniclastic andesite.

Alteration is chlorite-sericite overprinting relict potassic. Mineralization is disseminated and vein-hosted pyrite > chalcopyrite. Quartz-rich barren veins are also noted.

KLI-22-049 (azimuth 345°, inclination -65°) tested favorable surface alteration and trace element geochemistry as well as a transition from low to high chargeability in the East Wedge zone, a 300 m eastward step-out from KLI-22-045 in KMZ. East Wedge is a block defined by the intersection of Divide Lake Fault and Valley Fault. The drill hole was collared in KMZ about 300 m southeast of KLI-22-045 and 30 m southwest of Divide Lake Fault.

The fault zone was intersected from 37-167 m. Drilling remained in East Wedge to 468 m where it intersected Valley Fault at depth and then continued in Kliyul North to end-of-hole at 603.0 m. Significant intervals of mineralization constrained by zone boundaries include, 66.0 m of 0.41% CuEq or 0.57 g/t AuEq starting from 250 m (East Wedge); and 16.0 m of 0.63% CuEq or 0.87 g/t AuEq starting from 468 m (Kliyul North). In the East Wedge interval, mineralization is spatially related to a fault strand at 309-318 m and is hosted in volcaniclastic andesite. Alteration is chlorite-sericite and propylitic assemblages overprinting potassic.

Veins include early-, intermediate-, and late-stage types. Intermediate-stage (D type) veins are associated with the fault. Mineralization is disseminated, fracture fill and vein-hosted pyrite > chalcopyrite ± bornite.

In the Kliyul North interval, mineralization is adjacent to Valley Fault and hosted in volcaniclastic andesite. Alteration is phyllic. Veins are early- and intermediate stage.

Mineralization is disseminated, fracture fill and vein-hosted pyrite > chalcopyrite. KLI-22-050 (azimuth 048°, inclination -54°) was designed to test mineralization in Kliyul West at the top- of-hole and then continue across KMZ towards Valley Fault at depth. The drill hole was collared in Kliyul West about 110 m southwest of the Lui Fault.

The fault zone was intersected from 228-250 m. Drilling remained in KMZ to end-of-hole at 807.0 m and ended in the Valley Fault zone (starting from 800 m) without crossing completely through into Kliyul North. Significant intervals of mineralization constrained by zone boundaries include: 180.5 m of 0.33% CuEq or 0.45 g/t AuEq starting from 58 m (Kliyul West); and 204.5 m of 0.87% CuEq or 1.19 g/t AuEq starting from 239 m (KMZ). In the Kliyul West interval, mineralization is hosted in volcaniclastic andesite with a diorite dyke (14.1 m) and feldspar porphyry dyke (5.4 m), and secondary fault structures (14-19 m wide) at 103 m and 160 m. Alteration is chlorite-sericite locally overprinting potassic.

Veins include early-, intermediate-, and late- stage types. Intermediate-stage (D type) veins are associated with the fault at 103 m. Mineralization is disseminated, fracture fill and vein-hosted pyrite > chalcopyrite. In the KMZ interval, mineralization is hosted in volcaniclastic andesite with a few narrow (<4 m) diorite and hornblende porphyry dykes.

Alteration is moderate-strong potassic with patchy overprinting chlorite- sericite. Veins include early-, intermediate-, and late-stage types. Mineralization is mainly disseminated, fracture fill and vein-hosted chalcopyrite > bornite, or chalcopyrite > pyrite.