TDG Gold Corp. announced the results of the 2023 Lithic Drainage Sampling ("LDS") survey conducted over TDG's 42 square kilometre Baker Complex, and also Greater Shasta-Newberry, covering multiple defined exploration target areas including the historical Baker A- and B-Veins and Shasta deposit that were mined intermittently between 1986-2012. TDG's 2021-2023 exploration work is the first property-wide, systematic program focused on the copper-gold-molybdenum ("Cu-Au-Mo") porphyry potential across the Baker Complex. Modern assay results from historical drillcore at the Baker B-Vein published by TDG in July to September 2023 demonstrate the presence of broad intervals up to 100 metres ("m") of Cu, Au and silver ("Ag") mineralization from near surface that was not previously mined. In August 2023, TDG undertook a specialist geochemical survey collecting lithic drainage samples from the network of creeks and gullies across the Baker Complex and Greater Shasta-Newberry. The results indicate loci of higher Cu-Au-Mo against a background of elevated Cu across extensive portions of the Baker Complex. Higher Au-Ag concentrations are dominant in areas where Au-Ag epithermal mineralization is already known to exist, which helps to validate the LDS survey approach. The maps above and below show consistently elevated Cu, Au, Ag and Mo concentrations across the Baker Complex and Greater Shasta-Newberry. The top quartile of assay results for Cu-Au-Mo appears to be concentrated into two, large footprint areas: (i) the broader area around the historical Baker mine, which was explored for its gold-silver potential, and (ii) Saunders, which has historically seen minimal exploration and evaluation for its mineral potential. Figure 4 presents areas1 with elevated tellurium ("Te") concentrations, and Te is an element commonly associated with mineralized intrusions, such as porphyry Cu-Au-Mo systems. Maps for lead ("Pb") and zinc ("Zn") display broadly similar distribution patterns. This multi-element coincident data strongly supports the concept that Baker represents a large-scale mineralized system, as does the data for Saunders. Integration is ongoing of the LDS results with the regional-scale silt geochemical samples and modern geophysics. TDG's aim is to define prioritized, drill- ready targets within the Baker Complex to help focus and inform potential joint venture discussions. Baker Mine Area The Baker mine area is marked by a distinctive 15 sq.km circular, dome-like physiographic feature. Within and around this dome-like landscape feature, extensive gossans indicative of a high sulphide endowment and widespread porphyry alteration coincide with multiple geochemical and geophysical anomalies. Historical drilling undertaken at Baker was shallow and focused on Au-Ag epithermal mineralization. Saunders The Saunders target area1 covers ~10 sq.km and has never been drill tested. It comprises multiple historical prospects with minimal exploration. The LDS survey results indicate the presence of the highest stream sediment pathfinder element anomalies across the whole Baker Complex. Cu and Mo
concentrations within the Saunders area are in the top 5% of all the samples collected in the 2023 survey. LDS sampling results from Greater Shasta indicate highly anomalous Au and Ag from drainages, particularly where the Shasta mineral resource2 has already been defined. Elevated Au- Ag in the vicinity of a defined Mineral Resource Estimate (news release May 01, 2023) provides support for the LDS technique as a prospecting method. Other highlights include the Cody Lee and Fisher target areas1 which have had limited, but successful historical drilling and are open in all directions (news releases Apr. 03 and Apr. 06, 2023). The LDS survey has also highlighted the potential to expand the mineralized footprint at Newberry which has never been drill tested. Sample Collection and Analytical Method TDG's 2023 LDS survey utilized the `Barakso Pan' method: a specialized device that collects single-phase fluvial lithic sediment (silt) whilst eliminating most variability due to seasonality or organic chemical components. Samples collected using this approach are consistent between sites and are near- homogeneous in form. Samples for the 2023 Lithic Drainage Sampling program were managed via rigorous chain of custody, through sample collection, processing, and delivery to the ALS Global laboratory in either North Vancouver or Kamloops, B.C. The samples were logged and collected across the Baker-Shasta and Bot properties by geologists and technicians at sample sites determined to be appropriate for reflecting local sediment sources where practical and possible. Samples selected for sampling were then placed sealed kraft bags, then in security-sealed rice bags before being delivered directly by TDG staff from the Baker Mine site, to Bandstra Transportation Systems in Prince George, ultimately to the ALS Global facility in North Vancouver or Kamloops, B.C. Samples were prepared and analyzed following procedures: PREP-41A for sample preparation and ME-MS41L for super trace (low detection limit) analysis featuring Au, Ag, Cu.