Photo Gallery

Narraburra

  • GNBDD022
    GNBDD022 - 4m @ 2354ppm TREO from 52m, inc 2m @ 4494ppm from 52m
  • GNBDD011
    GNBDD011 - 3m @ 3481ppm from 31m
  • 20230524-Narraburra-site
    Narraburra site
  • 202306-Narraburra
    Narraburra
  • 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
  • 2019_IMG_1370
    Possible old sinter sample from historic mining and smelting
  • 2019_IMG_1367
    Gossanous outcrop on the edge of a low rise. These filed indicators reinforce the prospectivity of this project for hosting base and precious metals.

Lewis Ponds

  • IMG_202202_EL5583_MS
    Massive Sulphides - Lewis Ponds (EL5583)
  • IMG_202202_EL5583_03
    Quartz Blow - Ophir Mine Workings Lewis Ponds EL5583
  • IMG_202202_EL5583_02
    Ferruginous Outcrop - Ophir Mine Workings Lewis Ponds EL5583
  • IMG_202202_EL5583_01
    Ferruginous Outcrop - Ophir Mine Workings Lewis Ponds EL5583
  • IMG_201906_261455
    Lewis Ponds
  • IMG_4379
    Drilling at Lewis Ponds
  • IMG_2521
    Lewis Ponds: Sulphide rich sinter? S vergences show upward facing west limb of syncline
  • IMG_2519
    Lewis Ponds: Main vertical shaft at Tom’s mine. S vergences show upward facing west limb of syncline
  • IMG_1435
    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.
  • IMG_1434
    Historic timbered shafts at Lewis Ponds
  • IMG_1433
    Historic timbered shafts at Lewis Ponds
  • IMG_1432
    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.
  • IMG_1430
    Lewis Ponds: S vergences show upward facing west limb of syncline
  • IMG_1426
    Old workings that have naturally revegetated, demonstrating that modern day mining, incorporating best practice rehabilitation, will be able to enhance the post mining environment
  • IMG_1417
    Historic drill core stockpiled at Lewis Ponds
  • IMG_1416
    Historic collapsed working at Lewis ponds
  • IMG_1415
    The tree lined entrance track to the historic Lewis Ponds mine site

Copper Hill East

  • IMG_202202_Cu
    Native Copper - Copper Hill East (EL8556)
  • IMG_202006_Cu
    Copper Hill East - Native Cu
  • IMG_2514
    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.
  • IMG_2513
    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.
  • IMG_1385
    Landscape with occasional outcrop and stacked rocks from land clearing. Some of these rock stacks contain altered and gossanous porphyry.
  • IMG_1384
    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.
  • IMG_1380
    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks
  • IMG_1379
    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks
  • IMG_1378
    Conglomerate outcrop on project edge, containing clasts of the target porphyry rocks

Gundagai

  • IMG_202202_SHN_CS_02
    Chalcopyrite-pyrrhotite in quartz vein - Surprise Hill North, Gundagai South (EL8061)
  • IMG_202202_SHN_CS_01
    Pyrrhotite in quartz vein - Core from Surprise Hill North, Gundagai South
  • IMG_202202_SHN_03
    Surprise Hill North - Looking NE
  • IMG_202202_SHN_02
    Surprise Hill North - Looking SE
  • IMG_202202_SHN_01
    Surprise Hill North - Looking SE
  • IMG_202202_Mantons
    View from Bongongalong Hill across Mantons Prospect and GNRC008
  • IMG_202202_MTP_03
    Quartz Veins in Serpentinite - Mt Parnassus Gundagai
  • IMG_202202_MTP_02
    Quartz Veins in Serpentinite - Mt Parnassus Gundagai
  • IMG_202202_MTP_01
    Mt Parnassus, Gundagai
  • IMG_202202_EL8586_CS_02
    Gold in Quartz - Emu Workings, Gundagai North (EL8586)
  • IMG_202202_EL8586_CS_01
    Galena-Pyrite in quartz vein - Bongongalong Hill, Gundagai North (EL8586)
  • IMG_202202_EL8061_02
    Gundagai South - EL8061 Big Ben Drilling
  • IMG_202202_EL8061_01
    Gundagai South - EL8061 Big Ben Drilling
  • IMG_201907_03
    Sample of free gold found at Gundagai North – Emu Workings
  • IMG_201907_02
    Sample of free gold found at Gundagai North – Emu Workings
  • IMG_201907_01
    Sample of free gold found at Gundagai North – Emu Workings. The scale can be determined by the field of view, which is 6.5mm.
  • IMG_2850
    Gundagai

Mt Aubrey

  • IMG_202002
    Drilling at Mt Aubrey, February 2020
  • IMG_201907_24004
    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
  • IMG_201907_24003
    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
  • IMG_201907_24002
    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
  • IMG_201907_24001
    Mt Aubrey. MAD04 diamond hole. Sulphides in brecchiated vein.
  • IMG_2510
    Mt Aubrey. Altered felsic pyroclastic flow. Note iron alteration, a sign of sulphides and potentially ore bearing fluids having passed through the rocks.
  • IMG_2508
    Mt Aubrey. Altered felsic pyroclastic flow. Note iron alteration, a sign of sulphides and potentially ore bearing fluids having passed through the rocks.
  • IMG_2502
    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.
  • IMG_1361
    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
  • IMG_1360
    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
  • IMG_1359
    Altered felsic pyroclastic flow. Note variable clast size and orientation. Zones of strongest alteration highlighted by rusty coloured, iron alteration.
  • IMG_1358
    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.