High Tide Resources Reports 205.16 Metres of 32.06% Fe at Labrador West Iron Project

In This Article:

Includes 69.5 Metres of 34.52% Fe from Near Surface

TORONTO, ON / ACCESSWIRE / August 10, 2022 / High Tide Resources Corp. ("High Tide" or the "Company") (CSE:HTRC) is pleased to report assay results (Table 1) from drill hole 22LB0060 from the 2022 spring/summer drilling program at its flagship Labrador West Iron Project (the "Project" or "Property"). The Project is located 20 km northeast and adjacent to IOC/Rio Tinto's Carol Lake Mine complex in Labrador City, Newfoundland (Figure 1).

Steve Roebuck, Director, President & Interim CEO of High Tide states, "We are pleased to report a very good first drill intercept that is a desirable combination of both high-grade oxide iron over an extensive interval width. The location of this drill hole confirms the broad continuity of the iron formation in between historic and recent drill holes providing the team with a high-level of confidence as we prepare for a maiden resource later this year."

Table 1: Significant Iron Intercepts of Oxide-Dominated Iron Formation

DDH ID

Easting (NAD83 Zone 19N)

Northing (NAD83 Zone 19N)

Elevation (m)

Dip (Deg.)

From (m)

To (m)

Drill Width (m) **

Fe Total (%) *

22LB0060

650892

5895630

559

-90

4.60

209.76

205.16

32.06

including

4.60

74.10

69.50

34.53

including

74.10

150.20

76.10

28.66

including

150.20

209.76

59.56

33.53

* Significant FeT (%) values are weighted length averages with a minimum total Fe grade of 24 wt. %

** True Widths are estimated to be 80 to 90 % of drill width

A total of 2298 metres of core was drilled with iron mineralization visually identified in all seven HQ/NQ-diameter diamond dill holes (Figure 2). The 2022 drill program was designed to in-fill between recent and historical drill holes and test for depth and lateral continuity in preparation for a maiden resource later this year. Drill hole 22LB0060 was drilled to a depth of 272.0 metres intersecting 257.72 metres of Sokomon Iron Formation, including 205.16 meters of the oxide-dominated Middle Sokomon Iron Formation, before being halted in the barren quartz-rich Wishart Formation (Figure 3).

The oxide facies of the Sokomon Iron Formation are dominated by the iron oxide minerals, hematite and magnetite accompanied by quartz occurring predominantly as chert. There may be accessory carbonates (calcite or dolomite), silicates, and, rarely, manganese oxides or carbonates. Production experience in the Labrador Trough indicates that hematite and magnetite in such a lithological setting tend to be readily easily recoverable using modern beneficiation methods, and produce high purity, desirable iron concentrates.