Photo Gallery

Lewis Ponds

  • IMG_202507_05
    Field work at Lewis Ponds 2025
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    Field work at Lewis Ponds 2025
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    Field work at Lewis Ponds 2025
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    Field work at Lewis Ponds 2025
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    Field work at Lewis Ponds 2025
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    Field work at Lewis Ponds 2025
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    Selected diamond drill core interval 228.52-232.09m from the high-grade core of Spicer’s Lode in GLPDD006 with assay intervals returning: 228.95m-229.95m (GRD10725) = 24g/t AuEq; 222.95m-230.8m (GRD10726) = 12.54g/t AuEq and 230.8m–231.70m (GRD10727) = 6.59g/t AuEq.
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    Diamond drill core from GLPDD007 showing massive sulphide mineralisation grading into semi-massive sulphides with pyrite (yellow) and sphalerite (red) with galena and chalcopyrite. Associated sample interval GRD11022 (157.6-158.15m) returned 13.69g/t AuEq.
  • IMG_202412_0501
    Diamond drill core from GLPDD006 showing massive to semi-massive sulphides with banded pyrite (yellow) and sphalerite (red) with galena and chalcopyrite. This interval returned in sample GRD10725 (228.95-229.95m) 10.85g/t Au + 18.67% combined Lead-Zinc.
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    Diamond drill rig on site and drilling at Lewis Ponds
  • IMG_202202_EL5583_MS
    Massive Sulphides - Lewis Ponds (EL5583)
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    Quartz Blow - Ophir Mine Workings Lewis Ponds EL5583
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    Ferruginous Outcrop - Ophir Mine Workings Lewis Ponds EL5583
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    Ferruginous Outcrop - Ophir Mine Workings Lewis Ponds EL5583
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    Lewis Ponds
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    Drilling at Lewis Ponds
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    Lewis Ponds: Sulphide rich sinter? S vergences show upward facing west limb of syncline
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    Lewis Ponds: Main vertical shaft at Tom’s mine. S vergences show upward facing west limb of syncline
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    Historic workings around Tom’s Lode with timber frames still visible. Note the oxidised sulphide zones showing up as rusty dark orange colours. Light coloured material is sulphide rich sinter scree.
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    Historic timbered shafts at Lewis Ponds
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    Historic timbered shafts at Lewis Ponds
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    Historic workings around Tom’s Lode with timber frames still visible. Note the oxidised sulphide zones showing up as rusty dark orange colours. Light coloured material is sulphide rich sinter scree.
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    Lewis Ponds: S vergences show upward facing west limb of syncline
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    Old workings that have naturally revegetated, demonstrating that modern day mining, incorporating best practice rehabilitation, will be able to enhance the post mining environment
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    Historic drill core stockpiled at Lewis Ponds
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    Historic collapsed working at Lewis ponds
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    The tree lined entrance track to the historic Lewis Ponds mine site

Narraburra

  • GNBDD022
    GNBDD022 - 4m @ 2354ppm TREO from 52m, inc 2m @ 4494ppm from 52m
  • GNBDD011
    GNBDD011 - 3m @ 3481ppm from 31m
  • 202509-Narraburra-Testwork
    Narraburra metallurgical testwork
  • 202306-Narraburra
    Narraburra
  • 202305-Narraburra-site
    Narraburra site
  • 202207-Narraburra-Drilling-07
    Drilling at Narraburra, July 2022
  • 202207-Narraburra-Drilling-04
    Drilling at Narraburra, July 2022
  • 202207-Narraburra-Drilling-01
    Drilling at Narraburra, July 2022
  • 2022-Narraburra-site
    Narraburra site
  • 2022-Narraburra
    Narraburra site

Yeoval

  • GYDD001-f
    GYDD001 core
  • GYDD001-e
    GYDD001 core
  • GYDD001-d
    GYDD001 core
  • GYDD001-c
    GYDD001 core
  • GYDD001-b
    GYDD001 core
  • GYDD001-a
    GYDD001 core
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    Possible old sinter sample from historic mining and smelting
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    Gossanous outcrop on the edge of a low rise. These filed indicators reinforce the prospectivity of this project for hosting base and precious metals.

Copper Hill East

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    Native Copper - Copper Hill East (EL8556)
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    Copper Hill East - Native Cu
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    Breccia at the entrance to the property on which we did soil sampling in the west of the Copper Hill East tenement. Sample results were positive for anomalous copper.
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    Breccia at the entrance to the property on which we did soil sampling in the west of the Copper Hill East tenement. Sample results were positive for anomalous copper.
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    Landscape with occasional outcrop and stacked rocks from land clearing. Some of these rock stacks contain altered and gossanous porphyry.
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    Proximal alteration found on surface. A target of all mineral exploration. Note the box work gossans and narrow quartz veins. Sulphide bearing fluids have altered the host rock and surface weathering has caused the biscuity texture and rusty, orange colours. To locate such an alteration zone on the first visit to an area, highlights the prospectivity of the project.
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    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks
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    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks
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    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks

Mt Aubrey

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    Drilling at Mt Aubrey, February 2020
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    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
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    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
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    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
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    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
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    Mt Aubrey. Altered felsic pyroclastic flow. Note iron alteration, a sign of sulphides and potentially ore bearing fluids having passed through the rocks.
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    Mt Aubrey. Altered felsic pyroclastic flow. Note iron alteration, a sign of sulphides and potentially ore bearing fluids having passed through the rocks.
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    Old mine stockpile from the Mt Aubrey open pit gold mine, that completed mining in 1991. Obvious epithermal vein textures and alteration present in mainly felsic host rocks.
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    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
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    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
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    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
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    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration. Also shows a subvertical fault zone, running up the photo. The fault is a potential conduit for mineralised fluids and a good indicator of project prospectivity.