Rockcliff Metals Corporation Stocks

CA$ 0Last Updated 23.03.2026

Issuer Rating

1/7
Performance

Poor

Risk

High

Recommendation

Sell

Market Cap

CA$ 12.78M

Buy
Review
Evaluation
Target price
Dynamics
Performance
Growth
Dividends
Risks
CA$ 0
Key Takeaways

Risk factor

Very high price volatility

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Data is available to registered users only

Profitability factor

Very low or no dividends

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Data is available to registered users only
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Risks

  • Default risk
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  • Volatility
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  • Selling difficulty
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  • Stress test
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  • Country risks
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  • Other risks
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About

Rockcliff Metals Corporation operates as a resource development and exploration company and near-term copper-zinc producer in Canada. It holds interests in various advance stage, copper, and zinc dominant volcanogenic massive sulphide deposits in the Snow Lake area of Manitoba. It holds a 100% interest in Tower property located in the Thompson Nickel Belt District in Manitoba; a 100% interest in the Rail; the Freebeth property; the Morgan property; and the Copperman property located in the Snow Lake District in Manitoba. The company is a principal landholder in the Flin Flon-Snow Lake greenstone belt, which is home to the Paleoproterozoic VMS district, hosting mines and deposits containing copper, zinc, gold, and silver. It holds an extensive portfolio of properties that totals approximately 4,000 square kilometers and include several undeveloped VMS deposits. The company was formerly known as Rockcliff Copper Corporation and changed its name to Rockcliff Metals Corporation in November 2017. Rockcliff Metals Corporation was founded in 2005 and is headquartered in Toronto, Canada.

Risks

  • Default risk
    Data is available to registered users only
  • Volatility
    Data is available to registered users only
  • Selling difficulty
    Data is available to registered users only
  • Stress test
    Data is available to registered users only
  • Country risks
    Data is available to registered users only
  • Other risks
    Data is available to registered users only
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