New Zealand Government Publishes Its Critical Minerals List - Naming Gold and Antimony. RUA GOLD Provides Exploration Update on the Reefton Project's Extensive Antimony Potential

New Zealand Government Publishes Its Critical Minerals List - Naming Gold and Antimony. RUA GOLD Provides Exploration Update on the Reefton Project's Extensive Antimony Potential

Rua Gold Inc. (TSXV: RUA) (OTCQB: NZAUF) (WKN: A40QYC) ("Rua Gold" or the "Company") executives attended the launch event for the Minerals Strategy for New Zealand to 2040 and Critical Minerals List event hosted by New Zealand Petroleum and Minerals in Waihi on January 31, 2025. Honorable Shane Jones, Resource Minster for New Zealand, presented the critical minerals list that included both gold and antimony.

Furthermore, Rua Gold is pleased to provide an update from the exploration campaign underway at the Reefton Project on the South Island of New Zealand with significant added potential of antimony within the project.

Highlights:

  • Rua Gold is sitting on the vast majority of New Zealand's antimony inventory.
  • Byproduct credit that antimony brings the potential to add considerable economic value to the Reefton Project and New Zealand's strategic mineral inventory.
  • Antimony spot price increased 250% in 2024 and has held at all time high levels of over US$40,000 ton.
  • Auld Creek already has an antimony resource, and the Company is focused on expanding this in 2025. The resource is restricted to two of the four known shoots. Soil geochemistry indicates the potential for discovery of additional mineralised shoots over a strike length of 2.5km.
  • Drilling of Auld Creek commenced in December 2024, holes ACDD024, ACDD025 intersected 4-5m of strong stibnite (antimony sulphide) mineralization. Assays pending in the lab.
  • Rock chips have been found in several areas across the Reefton District with grades with up to 40.3% antimony (and gold grades up to 74.3g/t).
  • It is common for high grade gold and stibnite (antinomy ore mineral) to be co-located and the stibnite it is often used as a pathfinder for gold.

Robert Eckford, CEO of Rua Gold commented: "Having New Zealand's largest known antimony presence on our property is extremely encouraging, especially with it trading at all time high's and with it being announced on New Zealand's first ever critical minerals list.

We commenced drilling on Auld Creek antimony-gold prospect which already has an antimony resource. Rock chips across the other projects on the property increase our confidence this gold-antimony occurrence is consistent across the Reefton Goldfield. We are focused on expanding the Auld Creek resource and we will have assay results from the latest holes coming out in February.

This all comes on the back of the government's launch event for the Minerals Strategy for New Zealand to 2040 and Critical Minerals List, where both gold and antimony in Reefton Goldfield was called out as being one of the key focus points of the critical minerals strategy for New Zealand."

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Figure 1: Overview of the Reefton Goldfield.

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GLOBAL SUPPLY AND VALUE OF ANTIMONY

Antimony, is a critical metalloid primarily sourced from the mineral, stibnite. It is highly valuable and increasing in demand due to its versatility and has essential applications across renewable energy, liquid battery metals, defence and technological sectors.

Due to its limited supply, predominantly controlled by China, Russia & Tajikistan, antimony is considered a strategic material essential for supply chain security, particularly during periods of geopolitical instability. This was heightened in August 2024, when China announced export controls on processed antimony products. In response to these controls, nations have accelerated their efforts to secure alternative sources of antimony to mitigate the risk of significant supply chain vulnerabilities.

The US, EU, UK, Japan, Canada and Australia all designate antimony as a critical mineral. On January 31, 2025, New Zealand also announced their Critical Mineral List which included antimony.

Reflecting heightened demand, the price of antimony has reached new highs, currently trading over US$40,000 per tonne, a significant increase from US$11,350 per tonne at the start of 2024. This market shift has intensified interest in the strategic antimony potential held by Rua Gold.

EXPLORATION POTENTIAL

Auld Creek Focus

Rua Gold commenced drilling at Auld Creek in December 2024. It has a targeted program to drill four mineralised shoots identified from historical surface exploration work interpreted by the Rua Gold team over the past 3 months.

Auld Creek is situated between two past producing mines, Globe Progress mine, and the Crushington Group of mines which collectively produced 933,000oz at 14.0g/t Au (Barry 1993). Auld Creek has three historic adits but no commercial production from the reefs.

Rua Gold has an inferred resource indicating 700,000 tonnes at 3.1g/t Au and 1.1% Sb for 67,000oz of gold and 8,000 tonnes of antimony1 (AuEq 110,000oz2). The resource is restricted to two of the four known shoots. Soil geochemistry indicates the potential for discovery of additional mineralised shoots over a strike length of 2.5km.

Two of the four holes completed to date intersected 4-5m of strong visible stibnite (antimony sulfide) mineralization in the Fraternal-Bonanza structure. Logging and assaying are in progress.

Previous diamond drilling by Siren Gold Limited ("Siren") confirmed the presence of significant antimony, with notable drill holes including:

  • ACDDH011: 8.1m @ 2.73g/t Au and 4.33% Sb (AuEq of 11.0g/t) 80m below the surface.
  • ACDDH015: 12.4m @ 5.19g/t Au and 13.65% Sb (AuEq of 31.3g/t) 75m below the surface.

Full table of results in Table 1 in the appendix below.

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Figure 2: Extent of drilling and mapping at Auld Creek with four main reef tracks overlain on arsenic soil geochemistry.

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Other Reefton Prospects

With the increased interest in antimony over 2024, the exploration team widened its focus to include testing for stibnite (antimony) mineralization across other known targets of the Reefton Goldfield.

In the early 1900's, the Fiery Cross lode, within Capleston, reported significant antimony mineralisation associated with the gold-bearing quartz reef, but at the time, in common with many other Reefton Goldfield mines, mining this posed a problem for gold recovery and the material was discarded on the tip head. Re-sampling of this mined material from the tip head (float), and from an insitu quartz reef of the old mine at surface has returned exceptionally high results including:

  • Sample GER3721 with 23.5g/t gold and 20.6% antimony
  • Sample GER3725 with 7.53g/t gold and 16.7% antimony
  • Sample GER3726 with 52.3g/t gold and 16.0% antimony

Refer to Table 2 in the appendix below for a complete list of rock samples.

Murray Creek hosts the Golden Treasure mine, 350m south south-west of the Victoria-Inglewood mines. Gold recovery at the Golden Treasure was also hindered by the presence of stibnite. In parts of the mine where the shoot consisted of 30-40 % antimony the ore was stacked in the workings for future sale (Downey, 1928a).

Rua Gold conducted both channel samples on surface and assayed a suite of rocks from the tip head of the mine workings. This has provided firsthand evidence of the tenor of the antimony has returned exceptionally high results including:

  • GERS6027: Trench with 1m wide with 10.8g/t gold and 1.7% antimony
  • GERS6028: Trench with 1m wide with 3.66g/t gold and 3.8% antimony
  • GERS3714: Rock sample with 2.29g/t gold and 40.3% antimony
  • GERS3716: Rock sample with 6.72g/t gold and 26.9% antimony
  • GERS3720: Rock sample with 4.77g/t gold and 23.3% antimony

Refer to Table 3 and 4, respectively, in the appendix below, for a complete list of trench and rock samples.

With results from this surface exploration work, the exploration team are encouraged that the stibnite mineralization is demonstrated throughout the Reefton Goldfield and further work will form part of the surface exploration campaign in 2025.

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Figure 3: Location of known antimony locations.

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ABOUT Rua Gold

Rua Gold is an exploration company, strategically focused on New Zealand. With decades of expertise, our team has successfully taken major discoveries into producing world-class mines across multiple continents. The team is now focused on maximizing the asset potential of Rua Gold's two highly prospective high-grade gold projects.

The Company controls the Reefton Gold District as the dominant landholder in the Reefton Goldfield on New Zealand's South Island with over 120,000 hectares of tenements, in a district that historically produced over 2Moz of gold grading between 9 and 50g/t.

The Company's Glamorgan Project solidifies Rua Gold's position as a leading high-grade gold explorer on New Zealand's North Island. This highly prospective project is located within the North Islands' Hauraki district, a region that has produced an impressive 15Moz of gold and 60Moz of silver. Glamorgan is adjacent to OceanaGold Corporation's biggest gold mining project, Wharekirauponga.

For further information, please refer to the Company's disclosure record on SEDAR+ at www.sedarplus.ca.

TECHNICAL INFORMATION

Simon Henderson CP, AUSIMM, a qualified person under National Instrument 43-101 Standards of Disclosure for Mineral Projects and Chief Operating Officer and a director of Rua Gold, has reviewed and approved the technical disclosure contained herein. Mr. Henderson has participated in the geochemical sampling, and mapping programs to verify that they have been conducted in accordance with standard operating procedures. Mr. Henderson has verified the data disclosed by running checks on the location, analytical, and test data underlying the information in the technical disclosure herein.

QA/QC ROCK SAMPLES AND CHANNEL SAMPLES

Veins were sampled in 1 m intervals. Before sampling, outcrops were cleared of debris and alluvial sediments with shovels and hammers to uncover the full extent of the veins. 1m intervals were measure with a tape and marked with flagging tape or spray paint. A line was made along the outcrop, then chips were taken continuously along that line. Each 1m interval sample is 1.5kgs of material.

Rock samples were sent to SGS Laboratories, Westport for sample preparation. Samples were crushed and pulverized to 85% passing 75 µm. The pulverized rock-chips were split into two samples: a ~50 g sent for laboratory analysis, and the reject returned to RGL for pXRF analysis and storage. Pulverized rock-chip samples were analyzed for gold (Au) by 50-g fire assay with AAS finish at SGS Waihi (SGS Code FAA505); and for antimony (Sb) by Sodium Peroxide Fusion Analysis by ICP-MS at SGS Waihi.

Rua Gold Contact

Robert Eckford
Chief Executive Officer
Email: reckford@RUAGOLD.com
Website: www.RUAGOLD.com

This news release includes certain statements that may be deemed "forward-looking statements". All statements in this new release, other than statements of historical facts, that address events or developments that the Company expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects", "plans", "anticipates", "believes", "intends", "estimates", "projects", "potential" and similar expressions, or that events or conditions "will", "would", "may", "could" or "should" occur and specifically include statements regarding: the Company's strategies, expectations, planned operations or future actions, including but not limited to exploration programs at its Reefton and Glamorgan projects and the results thereof. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements.

Investors are cautioned that any such forward-looking statements are not guarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. A variety of inherent risks, uncertainties and factors, many of which are beyond the Company's control, affect the operations, performance and results of the Company and its business, and could cause actual events or results to differ materially from estimated or anticipated events or results expressed or implied by forward looking statements. Some of these risks, uncertainties and factors include: general business, economic, competitive, political and social uncertainties; risks related to the effects of the Russia-Ukraine war; risks related to climate change; operational risks in exploration, delays or changes in plans with respect to exploration projects or capital expenditures; the actual results of current exploration activities; conclusions of economic evaluations; changes in project parameters as plans continue to be refined; changes in labour costs and other costs and expenses or equipment or processes to operate as anticipated, accidents, labour disputes and other risks of the mining industry, including but not limited to environmental hazards, flooding or unfavorable operating conditions and losses, insurrection or war, delays in obtaining governmental approvals or financing, and commodity prices. This list is not exhaustive of the factors that may affect any of the Company's forward-looking statements and reference should also be made to the Company's short form base shelf prospectus dated July 11, 2024, and the documents incorporated by reference therein, filed under its SEDAR+ profile at www.sedarplus.ca for a description of additional risk factors.

Forward-looking statements are based on the beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change.

Table 1: Significant drilling intercepts for Auld Creek, full mineralized zone composites (1.5 g/t Au cut-off)1.

Hole IDAzimuthDip (⁰)Easting (NZTM)Northing (NZTM)From (m)To (m)Downhole Interval (m)Au (g/t)Sb (%)
ACDDH00445-601507194533297651.7257.96.181.590,01
ACDDH00445-6015071945332976116.19136.8420.655.412.17
ACDDH005100-601507194533297657.6664.416.751.640.06
ACDDH005100-601507194533297665.880.3514.552.070.10
ACDDH00740-5815071855332881123.22148.4525.233.140.07
ACDDH008100-581507186533288172.1476.354.211.550.02
ACDDH011130-811507212533305175.383.48.12.734.33
ACDDH015158-581507204533313969.68212.45.1913.65
ACDDH015158-5815072045333139105132.427.43.670.2
ACDDH016330-55150720253331416590256.550.29

Table 2: Fiery Cross Rock Sampling

Sample IDEastingNorthingAu (g/t)Sb %
GERS37211511843534156423.520.60
GERS3722151184353415753.993.37
GERS3723151183753415731.68.16
GERS3724151185053415790.7516.80
GERS3725151187053416097.5316.70
GERS37261511865534160752.316.00
GERS3727151185353416083.852.08
GERS3728151185553416119.224.50
GERS37291512081534168174.30.02

Table 3: Golden Treasure trench results outcropping Antimony lode

TrenchSample ID EastingNorthing FromToInterval Au (g/t)Sb%
GT01GERS6024151001853352750115.920.0168
GT01GERS6025151001853352751214.870.0158
GT01GERS6026 151001853352752310.60.0172
GT02GERS60271510016533526601110.81.7212
GT02GERS6028151001653352661213.663.8173
GT02GERS6029 151001653352662310.30.213
GT02GERS60301510016533526634110.80.0223
GT02GERS5651 1510016533526645110.0124
GT02GERS5652151001653352665611.530.0123
GT02GERS56531510016533526667119.80.0161

Table 4: Golden Treasure rock chip sampling from tip head and creek float adjacent to level 1.

SampleEastingNorthing Au (g/t)Sb %
GERS37111510018533527512.41.07
GERS3712151001653352664.333.71
GERS3713151002053352491.740.371
GERS3714151009653351702.2940.3
GERS37151510097533517013.37.46
GERS3716151009653351716.7226.91
GERS3717151009553351717.039.88
GERS3718151009453351730.0524.7
GERS3719151009853351731.8530.3
GERS3720151009653351764.7723.3

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An emerging gold explorer in New Zealand’s historical goldfields

RUA GOLD Completes the Second Phase of Surface Exploration and Drill Targeting at the Glamorgan Project, New Zealand

RUA GOLD Completes the Second Phase of Surface Exploration and Drill Targeting at the Glamorgan Project, New Zealand

Rua Gold Inc. (TSXV: RUA) (OTCQB: NZAUF) (WKN: A4010V) ("Rua Gold" or the "Company") is pleased to announce the completion of the second phase of surface exploration on its Glamorgan Project, an epithermal gold system in the Hauraki Goldfield, North Island, New Zealand.

The Hauraki Goldfield is a major epithermal gold province, with over 50 historic mines having produced more than 15 million ounces of gold. The Glamorgan Project lies adjacent to OceanaGold's Wharekirauponga deposit, with Indicated Mineral Resources of 1.4Moz at 17.9 g/t Au and is scheduled to enter construction in the second half of 20251.

Highlights: 

  • The Company has completed its second phase of surface exploration, identified initial drill targets, and will submit its Access Agreement application at the end of May. 

  • Results indicate classic features of a major epithermal gold-silver system and are identical to the surface features of neighboring OceanaGold Project, Wharekirauponga. 

  • Four significant gold-arsenic soil anomalies trending north, north-east and north-northwest strike out individually over 4 kms in length. 

  • Rock chip samples containing up to 43 g/t Au highlight specific targets for evaluation, coincident with the intersection of two gold-arsenic soil anomalies. 

  • TerraSpec soil and clay mineralogy has identified a zonal clay distribution that reflects high-level epithermal alteration coincident with gold anomalism. 

  • Ground-based geophysics Controlled-source Audio-frequency Magnetotellurics (CSAMT) has identified three major resistive structures coincident with surface alteration and gold mineralization. These resistive structures may represent pervasive silica-quartz at depth - key criteria for targeting the drilling within a major epithermal gold system. 

  • All of the above results are being uploaded to the VRIFY AI-platform, where geological modelling is starting to assist in the systematic identification and ranking of drill targets.

Simon Henderson, COO of Rua Gold, commented: "This comprehensive, district-wide surface work has provided valuable new information, highlighting not just one, but three significant zones of potential mineralization for drill testing. These targets will be included in the Access Agreement for drilling, which is scheduled for submission at the end of May 2025.

Following detailed surface geological mapping, comprehensive soil geochemistry, specialist clay mineralogy, ultra-high resolution UAV magnetics, and proven depth-penetrating CSAMT geophysics, three significant zones have emerged as high-potential targets for drill testing. High-grade rock chip samples further support the potential to discover a major epithermal gold-silver vein system.

Results from this inaugural district-wide program are now streaming in and are being compiled, reviewed and actively prioritized in partnership with the VRIFY AI-platform to confirm and prioritize the drill program. The exploration team is excited to advance to the drilling phase of this unique and prospective target area."

Program Overview

Exploration activities - including extensive geological mapping, TerraSpec clay mineralogy, and ultra detailed magnetic and resistivity surveys - have focused on four major alteration cells that envelope these structures. These cells are directly associated with surface quartz veins, platy quartz after calcite, quartz-adularia minerals, and sinter-like textures, all indicative of the high levels of an epithermal gold-silver system.

The principle components of the surface work are detailed below.

Geological Mapping

Exploration in the first quarter of 2025 included the completion of geological mapping across the major drainages within the Glamorgan prospect, along with detailed examination of areas exhibiting intense alteration and mineralization identified in Stage 1. The Company also completed follow-up testing of the significant gold grades (8-43.1 g/t Au) previously reported in rock float and insitu rock samples (reported on January 25, 2025). Additional rock chip sampling (2-8 g/t Au) has identified key areas proximal to resistive zones and high-level clay alteration.

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Figure 1: Geological map of the Glamorgan area.

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TerraSpec Clay Mineralogy

A TerraSpec 4 High-Res portable spectrometer was used to analyze all soil and rock-chip samples, as well as available historical drill core. The hyperspectral reflectance data collected were interpreted using the cloud-based AI software program, aiSIRIS.

  • Anomaly A trends north-northwest for 4.2 kms with conjugate gold-arsenic trends extending in a northeast direction (Anomalies C and D). Montmorillonite clays mirror this anomaly, indicating strong structural control on fluid flow along this trend.

  • Anomaly B trends northerly, following north to northeasterly quartz veins mapped over 4 kms that remain open to the north and south. The southern end of this anomaly coincides with historical mine workings. This anomaly is highlighted by strong illite clay alteration enveloping quartz-calcite veins observed in mapping.

  • Anomalies C and D trend northeast, parallel to insitu quartz veining in the Phoenix Stream (Anomaly C), and silica-clay alteration along Wires Ridge (Anomaly D) (Figure 2).

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Figure 2: Arsenic-Gold soil geochemistry with strong anomalies outlined.

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Magnetics
Ultra detailed UAV magnetics flown by the Rua Gold team highlight strong alteration (de-magnetization of the host rocks) enveloping the four anomalies and demonstrating a major alteration cell indicative of a significant epithermal system.

Resistivity
A CSAMT survey was completed in February 2025 by the Rua Gold team. CSAMT is particularly effective at detecting ground resistivities to depths of several hundred meters, which can be interpreted to represent strong silicification and quartz veining when directly related to an area of intense alteration.

The survey identified several major, deep structures that align with features previously identified by UAV magnetics, gold-arsenic geochemistry anomalies, and mapped quartz veins, silicification and clay alteration (Figure 3).

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Figure 3: CSAMT and IP resistivity results.

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Glamorgan Exploration Overview

Following grant of a drone concessions in May 2024, and minimum impact exploration in July 2024, Rua Gold's exploration commenced with UAV ultra detailed magnetic surveying completing 590-line kms of flying using Geometrics MagArrow magnetometer suspended under a DJI M300 drone. Interpretation of the data has assisted in defining key aspects of lithology and alteration of the Whitianga Group rhyolites, and Coromandel Group andesites. Major structural elements are interpreted in the data aligning with regional mineralization trends.

Soil sampling commenced in July 2024 sampling along 250m spaced crosslines with a sample spacing of 20m. 3181 samples were collected, dried, sieved in Rua Gold's Waihi facility, then transported to Reefton for pXRF analysis. Each sample was also scanned using a TerraSpec 4 Hi-Res mineral analyzer to complete a picture of clay/alteration system enabling identification of the higher levels of the epithermal system. 50gms of soil was then freighted to ALS Brisbane for low-level precision gold assay. Arsenic anomalism with coincident gold anomalism highlights the four major soil anomalies A-D (Figure 2).

Anomaly A trends North north-west for 4.2 kms with conjugate gold-arsenic trends in a north-east direction. This anomaly remains open to the northeast. This north-east direction mirrors the orientation of the significant Wharekirauponga gold deposit 3 kms southeast of the Glamorgan permit.

Anomaly B trends northerly and follows north to northeasterly quartz veins mapped over 4 kms and open to the north and south. The southern end of this anomaly coincides with the Wentworth/Auckland historical mine workings.

Ultra detailed UAV magnetics flown by the Rua Gold team highlights strong alteration (de-magnetization of the host rocks) enveloping the two anomalies and demonstrating a major alteration cell indicative of the footprint of a major epithermal system.

Field mapping (ongoing) has highlighted broad alteration and veining in situ, and areas of quartz-adularia float displaying banded, platy quartz after calcite, and brecciated andesite with stockwork veining increasing toward the zones of interest. Rock sampling both float and in situ sampling has returned encouragingly anomalous gold (refer to Table 2 in the appendix below), coincident with the zones of high soil geochemistry.

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Figure 4: Location map with soil geochemical heatmap over the Wires area

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ABOUT Rua Gold

Rua Gold is an exploration company, strategically focused on New Zealand. With decades of expertise, our team has successfully taken major discoveries into producing world-class mines across multiple continents. The team is now focused on maximizing the asset potential of Rua Gold's two highly prospective high-grade gold projects.

The Company controls the Reefton Gold District as the dominant landholder in the Reefton Goldfield on New Zealand's South Island with over 120,000 hectares of tenements, in a district that historically produced over 2Moz of gold grading between 9 and 50g/t.

The Company's Glamorgan Project solidifies Rua Gold's position as a leading high-grade gold explorer on New Zealand's North Island. This highly prospective project is located within the North Islands' Hauraki District, a region that has produced an impressive 15Moz of gold and 60Moz of silver. Glamorgan is adjacent to OceanaGold Corporation's biggest gold mining project, Wharekirauponga.

For further information, please refer to the Company's disclosure record on SEDAR+ at www.sedarplus.ca.

TECHNICAL INFORMATION

Simon Henderson CP, AUSIMM, a qualified person under National Instrument 43-101 Standards of Disclosure for Mineral Projects and Chief Operating Officer and a director of Rua Gold, has reviewed and approved the technical disclosure contained herein. Mr. Henderson has participated in the geophysical, sampling, and mapping programs to verify that they have been conducted in accordance with the standard operating procedures. Mr. Henderson has verified the data disclosed by running checks on the location, analytical, and test data underlying the information in the technical disclosure herein.

QA/QC SOIL SAMPLES

A bulk sample of ~0.5-1 kg was collected in the field. Each sample was photographed in the field alongside the GPS with coordinates visible and each sample site marked in the field with biodegradable flagging tape. Samples were taken back to Rua Gold's Waihi facility for preparation. Samples were dried in a customized incubator, set at 38°C, for a minimum of two days. Once the samples were fully dried, they were sieved to

The 50-100-g fine-sieved (Rua Gold's Reefton facility for pXRF using an Olympus Vanta hand-held analyser, and then on to ALS Geochemistry, Brisbane, for Au-TL43 analysis. The ALS analysis consisted of 25-g sample digestion by aqua regia, followed by trace Au analysis by ICP-MS. The detection limit for Au by this method is 1ppb. ALS Brisbane is independent to Rua Gold.

Field duplicates were collected every 20th sample and underwent the same drying, sieving, pXRF, and gold assay process outlined above. Duplicates were checked and validated by Rua Gold's Isogonal data validation system to ensure compliance.

QA/QC ROCK-CHIP SAMPLES

Rock-chip samples were collected in the field during routine mapping and soil sampling. The location of each sample was recorded in the field with a Garmin GPSMAP 66i and details of the samples recorded in a notebook or mapping application. Samples were photographed and sent to SGS Waihi for sample preparation. Sample information was entered into .csv files and uploaded to an SQL database.

Samples were crushed to 75% passing 2 mm (SGS code CRU75) and pulverised to 85% passing 75 µm (SGS code PUL85_CR). The pulverised rock-chips were split into two samples: a ~50 g sent for laboratory analysis, and the reject returned to Rua Gold for pXRF analysis and storage.

The 50 g sub-samples were analysed by AAS after fire assay at SGS Waihi (SGS code FAA505). Detection values for this method are 0.01-100 ppm Au.

SGS is independent to Rua Gold and its laboratories are accredited to applicable ISO/IEC 17025 standards.

Rua Gold Contact

Robert Eckford
Chief Executive Officer
Tel: +1 604 655 7354
Email: reckford@RUAGOLD.com
Website: www.RUAGOLD.com

This news release includes certain statements that may be deemed "forward-looking statements". All statements in this new release, other than statements of historical facts, that address events or developments that the Company expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects", "plans", "anticipates", "believes", "intends", "estimates", "projects", "potential" and similar expressions, or that events or conditions "will", "would", "may", "could" or "should" occur and specifically include statements regarding: the Company's strategies, expectations, planned operations or future actions, including but not limited to exploration programs at its Reefton project and the results thereof; and the Company's acquisition of Reefton Resources Pty Limited. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements.

Investors are cautioned that any such forward-looking statements are not guarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. A variety of inherent risks, uncertainties and factors, many of which are beyond the Company's control, affect the operations, performance and results of the Company and its business, and could cause actual events or results to differ materially from estimated or anticipated events or results expressed or implied by forward-looking statements. Some of these risks, uncertainties and factors include: general business, economic, competitive, political and social uncertainties; risks related to the effects of the Russia-Ukraine war; risks related to climate change; operational risks in exploration, delays or changes in plans with respect to exploration projects or capital expenditures; the actual results of current exploration activities; conclusions of economic evaluations; changes in project parameters as plans continue to be refined; changes in labour costs and other costs and expenses or equipment or processes to operate as anticipated, accidents, labour disputes and other risks of the mining industry, including but not limited to environmental hazards, flooding or unfavourable operating conditions and losses, insurrection or war, delays in obtaining governmental approvals or financing, and commodity prices. This list is not exhaustive of the factors that may affect any of the Company's forward-looking statements and reference should also be made to the Company's CSE Form 2A - Listing Statement filed under its SEDAR+ profile at www.sedarplus.ca for a description of additional risk factors.

This news release references projects near to the Glamorgan Project and historical production from certain areas of New Zealand. Mineralization on nearby projects is not necessarily indicative of mineralization on the Glamorgan Project. Historical production from the Reefton Gold District or the Hauraki District is not an necessarily an indication that significant production will be possible from the Glamorgan Project.

Forward-looking statements are based on the beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change

Table 1: Significant gold and arsenic assay results from soil samples.

Sample IDEasting_NZTMNorthing_NZTMAu (ppm)As (ppm)
WR10019184638758752390.661052
WR18022184545558734680.2815
WR14016184584358743980.2636
WR05107184853358754620.26367
WR07134184875858747610.2626
WR06119184862058751270.22487
WR15027184591158740720.19119
WR11057184692558746480.18398
WR10018184636958752490.18353
WR09143184866958742370.17241
WR04109184869158756600.141391
WR10019184638758752390.661052
WR04111184872658756410.06954
WR04110184870958756500.05922
WR01116184918258762440.10896
WR16124184747858729000.05877
WR15118184749658731770.12857
WR11048184676958747360.03784
WR10033184663058751020.06772
WR15149184803658728720.02607

 

Table 2: Significant assay results from rock-chip samples.

Sample IDLocationTypeEasting_NZTMNorthing_NZTMAu (ppm)
GERS1666Sutcliff StreamFloat184705658749598.25
GERS1669Sutcliff StreamFloat184709258751117.15
GERS1661Sutcliff StreamFloat184678758747634.37
GERS1663Sutcliff StreamFloat184691658747853.95
GERS1667Sutcliff StreamFloat184711358751202.46

 

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(TheNewswire)

Element79 Gold Corp.

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