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Carolina Rush Intersects 61 m @ 1.7 g/t Au and 0.3% Cu including 10.6 m @ 4.4 g/t Au and 1% Cu at Brewer

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Toronto, Ontario--(Newsfile Corp. - October 21, 2024) - Carolina Rush Corporation (TSXV: RUSH) (OTCQB: PUCCF) ("Carolina Rush," "Rush" or the "Company") is pleased to report results from its recently completed core drilling program at the Brewer Gold and Copper Project in South Carolina. Analytical results have been received for holes 33 and 34, targeting the Tanyard Breccia Zone located south of the former mine (see Table 1, Figure 1 and Figure 2).

Carolina Rush President and CEO Layton Croft stated: “Hole 34 delivered the second-best results among the 15 holes reported thus far in the Tanyard Zone, and ranks in the top five on a grade-times-thickness basis (GxT) across all 34 Brewer holes reported to date. This strengthens the significance of the Tanyard as a promising new mineralized zone and adds to Brewer’s overall large-scale gold copper target with considerable upsides.”

Table 1. Composited Assay Results for hole B23C-033 & B24C-034

BHID

From (m)

To (m)

Interval* (m)

Au (g/t)

Cu (%)

B24C-033

No significant values

B24C-034

106.20

167.20

61.00

1.65

0.28

Incl.

121.70

167.20

45.50

2.06

0.35

Incl.

143.50

154.10

10.60

4.36

0.95

Incl.

145.65

151.00

5.35

6.92

1.20

 

*Reported intervals are drilled width and do not represent true width.

Drill hole B24C-033 was a vertical exploration hole drilled to a depth 155 meters and collared approximately 180 meters southwest of hole 34. The hole was designed to drill through the Tanyard sedimentary sequence to test an underlying chargeability anomaly. While no significant gold-copper mineralization was encountered, anomalous pathfinder elements and favorable alteration (e.g. quartz-pyrophyllite) were identified.

Drill hole B24C-034 was drilled to a depth of 223 meters with an azimuth of 120° and a -50° inclination. This was the first hole testing the Tanyard Breccia at this orientation and intersected mineralization at an elevation approximately 25 meters above B23C-021 (62.5 m @ 8.5 g/t Au). Mineralization is hosted within a silicified polylithic breccia that includes zones of strong sulfide replacement. These replacement bodies correlate with increased copper grades, with individual samples returning >2% copper. In addition, gold-telluride mineralization occurs in strongly oxidized quartz veins cutting the sulfide breccia with individual samples returning >15 g/t Au. Refer to Table 1 for a detailed breakdown of the mineralized interval.

Figure 1. Example of mineralization encountered in drill hole B24C-034

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