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Power Metals Corp V.PWM

Alternate Symbol(s):  PWRMF

Power Metals Corp. is a Canada-based diversified mining company. The principal business of the Company is the acquisition, exploration and evaluation of resource properties. Its exploration project includes Case Lake property. Case Lake Property is located in Steele and Case townships, 80 km east of Cochrane, NE Ontario, close to the Ontario-Quebec border. The Case Lake pegmatite swarm consists of six spodumene dykes: North, Main, South, East and Northeast Dykes on the Henry Dome and the West Joe Dyke on a new tonalite dome. The Case Lake Property is 10 km x 9.5 km in size and consists of 475 cell claims. The Case Lake pegmatite swarm occurs along a sub provincial boundary between the metasedimentary Opatica Sub province to the north and greenstone Abitibi Sub province to the south. The Company has staked the Pelletier Project consisting of approximately 337 mineral claims that account for total surface area of 7000 hectares in northeast Ontario , approximately 50 km south of Hearst .


TSXV:PWM - Post by User

Post by trader53on Feb 10, 2023 12:45am
768 Views
Post# 35278803

post from Brineboys

post from BrineboysAll the available data below bodes well for an extremely high recovery and lower end capex costs via DMS as fine grains are more expensive to separate. 1.5pct plus Li20, coarse(better) spodumene , crystal size (bigger the better)and iron content (lower the better) play pivotal roles. The iron content is expected to be fairly low as the spodumene are white and green in color. The lighter the color the lower the iron content. Crystals average 3-7 cm. In the very coarse zone... Spodumene crystals are fewer in number but may be 50 cm long and 5-7 cm in diameter. In the quartz core, grain size is in excess of 5 cm and is composed of mainly quartz with feldspar and spodumene. Spodumene crystals are up to 90 cm in length. : The spodumene in the North Dyke is very coarse-grained with blades up to 5 by 70 cm. The spodumene in the Main Dyke is abundant, very coarse-grained and green to white in colour. Tantalum mineralization is abundant in the Main Dyke and the North Dyke.
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