Properties

Golden Goliath has Acquired Four Rare Earth Element Properties in Quebec, Canada.

  • Property Summary

    Early stage Rare Earth Element prospects with excellent geological potential.  Located near the Manicouagan impact crater.  Recent and active forestry provides good road access.

    Next steps for the summer of 2023:

    • Geological mapping.
    • Prospecting.
    • Radiometric survey.
    • Heavy mineral Geochem sampling.
  • Victory 21 Property

    • 100% held by Golden Goliath.
    • 18 map claims, 10 pending claims over 1200ha.
    • Located in Central Quebec, stable modern mining jurisdiction.
    • Access from highway 389, nearby accommodations.
    • Multiple clearcuts and roads across property.
    • Early stage Rare Earth Element prospect with excellent geological potential.
    • Significant values:
      • 814 ppm Ce
      • 446 ppm La
      • 298 ppm Nd
      • 86 ppm Pr
      • 173 ppm Rb
      • 156 ppm Th
      • 385 ppm V
      • 617 ppm Zr

    Key targets will be the paragneiss and quartz monzonite components within the Plus-Value Complex.

     

     

  • Citadell Property

    • 100% held by Golden Goliath.
    • 24 map claims.
    • Located in Central Quebec, stable modern mining jurisdiction.
    • Access from highway 389,  nearby accommodations.
    • 2022: Property within active logging area. Multiple clearcuts and roads across property.
    • Caotibi Plutonic Suite.
    • Within Mangerite.

    • Stars are location of anomalous lake sediment samples.
    • Within circular geophysics anomaly.

     

     

  • Bedard Property

    • 100% held by Golden Goliath.
    • 22 map claims.
    • Located in Central Quebec, stable modern mining jurisdiction.
    • Access from highway 389,  nearby accommodations at Manic Cinq.
    • 2022: Property within recent logging area. Multiple clearcuts and roads across property.
    • Plus-Value complex
      • within Mangerite
      • Gneiss and Paragneiss
      • Gabbro Norite
      • Granite
      • Felsic Intrusive
      • Calc silicate

    • Rock Samples with anomalous rare earth elements:
      • 4,041 ppm Ba
      • 312 ppm Ce
      • 13.9 ppm Hf
      • 10.3 ppm Dy
      • 38.6 ppm Nb
      • 172.2 ppm Nd
      • 41.1 ppm Pr
      • 133 ppm Rb
      • 27.5 ppm Sm
      • 1,586 ppm Sr
      • 176 ppm V
      • 46.7 ppm Y
      • 890.5 ppm Zr

     

    • Circular mag feature corresponding with the Plus-Value Complex
    • Anomalous rock samples correspond to northern rim of anomaly

    Ernest Property

    • Option to acquire 100% held by Golden Goliath.
    • 34 map claims.
    • Located in Central Quebec, stable modern mining jurisdiction.
    • Access from highway 389,  nearby accommodations at Manic Cinq.
    • 2022: Property within recent logging area. Multiple clearcuts and roads across property.
    • MRN geologists collected four rock samples of granitic pegmatite within the Mesoproterozoic Canyon Complex.  
    • Anomalous results included; 2605 ppm Cerium, 1466 ppm Lanthanum, 965 ppm Neodymium, 274 ppm Praseodymium, 543 ppm Thorium, 1628 ppm Strontium, and 1722 ppm Zirconium.
    • Lake Sediment Survey returned 117.8ppm Ce, 65.6 ppm La, and 65.7 Sr.

     

    • Key target will be rheologically-controlled pegmatite dykes between gabbronoritic and mangeritic units of the Mezoproterozoic Canyon Complex.

     

     

  • Ernest Property

    • Option to acquire 100% held by Golden Goliath.
    • 34 map claims.
    • Located in Central Quebec, stable modern mining jurisdiction.
    • Access from highway 389,  nearby accommodations at Manic Cinq.
    • 2022: Property within recent logging area. Multiple clearcuts and roads across property.
    • MRN geologists collected four rock samples of granitic pegmatite within the Mesoproterozoic Canyon Complex.  
    • Anomalous results included; 2605 ppm Cerium, 1466 ppm Lanthanum, 965 ppm Neodymium, 274 ppm Praseodymium, 543 ppm Thorium, 1628 ppm Strontium, and 1722 ppm Zirconium.
    • Lake Sediment Survey returned 117.8ppm Ce, 65.6 ppm La, and 65.7 Sr.

     

    • Key target will be rheologically-controlled pegmatite dykes between gabbronoritic and mangeritic units of the Mezoproterozoic Canyon Complex.