Plato Closes Agreement to Acquire Ruffle Lake Phosphate-Rare Earth Property

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Plato Gold Corp.
Plato Gold Corp.

Toronto, July 18, 2024 (GLOBE NEWSWIRE) -- Plato Gold Corp. (TSX-V: PGC) (OTCQB: NIOVF) (Frankfurt: 4Y7 or WKN: A0M2QX) (“Plato” or the “Company”) an exploration company with a portfolio of properties in Northern Ontario and Santa Cruz, Argentina, is pleased to announce that it has closed the binding agreement of purchase and sale dated July 8, 2024 (the “Agreement”) with Rudolf Wahl and Mike Dorval (the “Wahl Group”), as previously announced on July 8, 2024. The Company has acquired (the “Acquisition”) a 100% interest in forty-two (42) unpatented cell claims in Killala Lake Area Townships, Thunder Bay Mining District, in the Province of Ontario (the “Claims” or the “Ruffle Lake Property”).

Description of the Ruffle Lake Property

The Ruffle Lake Property is readily accessible via an all-weather road 35 km north from the Trans Canada Highway 17. The geology in this area is dominated by the Prairie Lake Carbonatite Complex which lies immediately south of the Ruffle Lake Property and the Company’s adjoining Good Hope Property. In general, these Carbonatite Complexes are uncommon and known to host rare earth elements and critical minerals such as niobium, phosphate and yttrium currently in demand for EV (Electric Vehicle) and other Clean Energy technology.

The emplacement of the Prairie Lake Carbonatite is related to a major rifting or structural event along the north shore of Lake Superior. The event resulted in the development of a prominent north-trending fault system which was responsible for the emplacement of several carbonatite and alkaline intrusions in addition to the Prairie Lake Complex in this area.

Carbonatite related mineralization continues to be recognized along this fault structure in ongoing exploration which includes recent work on the Ruffle Lake Property. The Wahl Group, through preliminary prospecting and sampling have uncovered two sites (Site #5 and #6) in rusty-altered carbonatite with analysis returning up to 30% P2O5, 4558 ppm yttrium and anomalous light and heavy rare earth elements. Initial scintillometer readings gathered over these areas indicate the highest values appear to correlate with much higher than background radiation. A recent (May 2024) visit to Site #6 on the property revealed an area of approximately 130 m by 500 m exhibiting a medium to high radiometric signature covering the carbonatite.

A detailed radiometric survey planned by the Company, may help to define the size and extent of carbonatite body(s) on the Ruffle Lake Property. Anomalous areas will be targeted for stripping and trenching followed by detailed mapping and sampling.