View Financial HealthThis company listing is no longer activeThis company may still be operating, however this listing is no longer active. Find out why through their latest events.See Latest EventsFrontline Gold 配当と自社株買い配当金 基準チェック /06Frontline Gold配当金を支払った記録がありません。主要情報n/a配当利回りn/aバイバック利回り総株主利回りn/a将来の配当利回りn/a配当成長n/a次回配当支払日n/a配当落ち日n/a一株当たり配当金n/a配当性向n/a最近の配当と自社株買いの更新更新なしすべての更新を表示Recent updatesお知らせ • Feb 13Frontline Gold's Listing to Transfer to NEXIn accordance with TSX Venture Policy 2.5, Frontline Gold Corporation (the 'Company’) has not maintained the requirements for a TSX Venture Tier 2 company. Therefore, effective at the opening on February 14, 2024, the Company's listing will transfer to NEX, the Company's Tier classification will change from Tier 2 to NEX, and the Filing and Service Office will change from Montreal to NEX. As of February 14, 2024, the Company is subject to restrictions on share issuances and certain types of payments as set out in the NEX policies. The trading symbol for the Company will change from FGC to FGC.H. The symbol extension differentiates NEX symbols from Tier 1 or Tier 2 symbols within the TSX Venture market. Further to the Exchange bulletin issued May 8, 2023, trading in the shares of the Company will remain suspended. Members are prohibited from trading in the securities of the Company during the period of the suspension or until further notice.お知らせ • Jan 26Frontline Gold Corporation Receives High-Grade Assays from 2022 Field Program Rock Samples on Its Epworth PropertyFrontline Gold Corporation announced that rock sampling results have been received from the 2022 field program on its Epworth Property (`the Property'), Nunavut. Fifty-seven rock samples were collected, mainly along the Metallic Trend outlined in 2021 and its strike extension to the north and south. The Metallic Trend consists of locally high-grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization over a strike length of 1.15 km. Some sampling was also carried out at the historical Puppet and DD North Showings. Additional sampling along the Metallic Trend in 2022 yielded results of up to: 8.59% Cu & 884 ppb Au (with 0.18% Zn, 0.1% Co, 876 ppm As & 692 ppm V), from dolomite with red cherty fragments and stringers of possible chalcocite, chalcopyrite and pyrite and several % malachite staining. These were the highest Cu, Au & V grades of the 2022 program; 27.4% Zn (with 5.37% Pb, 0.22% Cu, 218 ppm Co, 66 ppm Ag, 404 ppm Cd & 5.64 ppm Ge) at the south end of the Metallic Trend from large dolomite felsenmeer. This was the highest Zn grade of both the 2021 and 2022 programs. The previous highest grade was 19.2% Zn at the north end of the Metallic Trend. Cd, Ge and V are common accessory elements in sediment-hosted Zn-Pb-(Cu) deposits; 16.7% Pb & 71.4 ppm Ag (with 8.26% Zn), also at the south end of the Metallic Trend, from a sample described as white dolomite with minor contorted red chert bands and 10% galena from frost heave. Possible dissolution collapse breccia was noted here. This was the highest Pb value obtained along the Metallic Trend from both the 2021 and 2022 programs; 1420 ppm Co & 7190 ppm As (with 1.31% Cu, 532 ppm Pb, 296 ppm Zn & 63 ppb Au) from an additional sample at the Metallic Showing, described as white-grey dolomite with malachite and azurite staining, pyrite, galena and sphalerite. Sampling up to 175 m north of the north end of the Metallic Trend yielded Cu-in-rock anomalies up to 0.15%. Sampling up to 1.5 km south of the south end of the Metallic Trend yielded anomalies in rock up to 0.61% Cu, 0.75% Zn, 0.46% Pb and 201 ppm Co.お知らせ • Nov 24Advance United Holdings Inc. and Frontline Gold Inc. Report on Geophysical Work Program on Paint Lake Road Project in Wawa, OntarioAdvance United Holdings Inc. and Frontline Gold Inc. reported numerous favorable geophysical anomalies have been identified on the Paint Lake Road JV (PLR JV) Property. The project is within the Wawa Abitibi Subprovince, prolifically known for its metal endowment. It has been estimated the Abitibi Subprovince has produced over 200 million ounces of gold and 400 million tonnes of base metal ore. The belt has recently been consolidated and the Paint Lake Road property is strategically located inside the consolidated area near the Mishi Open Pit and the former Magnacon Mines. The property comprises six (6) claim blocks totaling over 3,610 hectares 50km north of Wawa, Ontario and is located inside the Mishibishu Greenstone Belt which hosts the Wesdome Mines, the Eagle River Gold Mine, the Mishi Open Pit, and the former Magnacon Mine. Advance United has had success in the Wawa area having formerly developed and sold the Dorset Zone to current owners, Angus Ventures, which hosts a non-compliant resource of 100,000 oz. gold. The full story can be read here. The Paint Lake Road property sits along the Pukaskwa-Iron Lake (PIL) Shear Zone, known to host gold mineralization at the former Argo property and further south at Wesdome's Camp Lake occurrence. Further northeast the Iron Lake Shear Zone hosts Alamos' Island Lake Mine. The Paint Lake Road Property Geology The Property occurs within the Mishibishu greenstone belt that is a broad arcuate syncline 55 km long east-west and 16 km wide north-south. This belt is part of the Wawa Subprovince of the Archean age Superior Province. Supracrustal rocks in the belt are dominated by greenschist facies mafic to intermediate volcanic rocks with lesser sedimentary rocks including iron formation and intermediate to felsic volcanic rocks. The belt is surrounded by Archean granitic rocks and includes two internal granitic batholiths occupying the central portion of the belt. The northern limb of the belt, where the PLR JV Property and the Mishi Mine of Wesdome are located is dominated by an assemblage of clastic sedimentary rocks, felsic tuffs, and mafic flows. The southern limb, where the Eagle River Mine is located, is dominated by tholeiitic basalts and calc-alkaline andesites with minor interflow clastic sedimentary rocks and lean chert-magnetite iron formation. Promising Paint Lake Road Targets: The target for exploration on the PLR JV is shear-hosted orogenic gold similar to Wesdome's Eagle Deposit which is hosted by quartz veins in shear zones hosted by intrusive diorite. The presence of a regional scale shear zone is considered prospective for this type of deposit. Gold bearing quartz veins at Eagle River are hosted primarily by subvertical to steeply north dipping east-west striking shear zones within an elliptical quartz diorite stock Mineralized structures exhibit broad zones of deformed rock (3-20 m wide shear zones) affiliated with strong silicification over 20-50 m width. The PLR JV property is underlain by intrusive rocks and as such has been largely ignored in previous exploration programs. The identification of possible shear offsets from the main PIL shear will be further explored with prospecting and sampling.お知らせ • Nov 15Frontline Gold Corp Appoints James R. Atkinson as DirectorFRONTLINE GOLD CORP appointed Mr. James R. Atkinson, M.Sc., P. Geo as a member of the board of directors with immediate effect. Since 2018, Mr. Atkinson has been the President and CEO of Talisker Gold. An experienced exploration geologist and project manager with over 45 years of experience, Mr. Atkinson has spent his career in both mineral exploration and mining and in the environmental field as Vice President, Exploration Manager and Regional Manager with junior and major mining companies such as Newmont, Billiton and Agnico Eagle. He has reviewed, evaluated and acquired projects around the world and recently was part of the team responsible for mergers and acquisitions at American Silver. He has worked with investors to form and manage junior exploration companies.お知らせ • Nov 04Frontline Gold Corporation Receives Strongly Anomalous Soil Sampling Results from Its Epworth Property, NunavutFrontline Gold Corporation announced that soil sampling results have been received from the 2022 field program on its Epworth Property (`the Property'), Nunavut. Humus (A horizon) and B horizon /clay samples were collected across the `Metallic Trend' discovered in 2021, as well as the strike extension of the Trend to the north and south. The Metallic Trend consists of locally high-grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization over a strike length of 1.1 km (see Project Background below). The soil sampling survey consisted of seven east-northeast-west-southwest lines over a distance of 2.8 km, with lines ranging in length from 75 to 150 meters and sample station spacing at 12.5 m. Either a humus sample or B horizon /clay sample were collected at each station. The latter were frequently collected in frost boils. The best results were obtained from frost boils which turned up mineralized rock (sampled in 2021, see Project Background below). Humus samples returned strongly anomalous results adjacent to these frost boils but also in low, marshy ground. Top results for B horizon /clay samples are as follows: 2970 ppm Cu (TD-ICP); 2710 ppm Zn (TD-ICP); 2010 ppm Pb (TD-ICP); 127 ppm Co (TD-ICP); 8.6 ppm Ag (TD-ICP); 99 ppb Au (FA-AA). Top results for Humus (A horizon) samples are as follows: 542 ppm Cu (TD-ICP); 960 /848 ppm Zn (INAA /TD-ICP); 101 ppm Pb (TD-ICP); 54 /32 ppm Co (INAA /TD-ICP); <2 /0.4 ppm Ag (INAA /TD-ICP); 4 ppb Au (INAA) *TD-ICP stands for `Total Digestion Inductively Coupled Plasma', an analytical method used by Activation Laboratories. FA-AA stands for `Fire Assay Atomic Absorption', an analytical method used by Activation Laboratories; INAA stands for `Instrumental Neutron Activation Analysis', an analytical method used by Activation Laboratories. The highest-value soil anomalies were obtained along the 1.1 km high-grade trend identified in 2021, but weaker anomalies were obtained to the north and south, suggesting that the trend continues (to possibly 2.8 km long and still open along strike). Depth of overburden may play a role in the weaker values on some lines, though mineralization may also not be as intense in these locations. Anomalies were frequently obtained at multiple stations on individual lines, suggesting wide mineralized zones or parallel horizons. . Final results for rock-grab samples collected during the program are pending and will be reported once received. The Metallic Trend follows the contact zone between Upper Odjick Formation red shales and Lower Rocknest Formation dolomites, often forming a valley which can be up to 100 meters wide. Mineralization occurs within grey (reduced) Rocknest dolomite flanked by red (oxidized) dolomite. Redox boundaries are thought to be a crucial control on mineralization. Data collected during the 2022 program suggest that there are at least two parallel reduced, mineralized horizons along the Trend. Multi-station geochemical anomalies appear to support this. Where exposed on surface, the mineralized horizons are up to 12 meters wide and host sulphide-rich quartz-carbonate veins up to 0.4 meters wide. Alternatively, these `parallel horizons' may be explained by repetition of a single horizon by folding or structural duplication by thrust faulting. Larger-scale folding and /or thrusting likely explains the parallel trends that exist to the west and east of the Metallic Trend. Future diamond drilling programs should help establish the geometries of these zones and their vertical extent. Project Background: The Epworth Project is located 85km south of the village of Kugluktuk (Coppermine), containing three main previously known areas of high-grade polymetallic mineralization from 1-25m wide occurring for more than 15km along strike. Historical surface grab samples have reported spectacular high-grade mineralization including: 61.2% Cu & 5600 gpt Ag (Payback Showings); 19.22% Zn with 810 gpt Ag, 3% Cu & 1.86 gpt Au (Metallic Showing). The Metallic trend was identified in 2021 while investigating the historical Metallic Showing (formerly named `Dead Showing') in the northern part of the property, consisting of dolomite with sulphide-rich quartz-carbonate veining in outcrop. Mineralized angular float boulders, subcrop (felsenmeer, frost boil rings) and outcrop were found to extend much further to the south than previously identified, along a well-defined north-northwest-south-southeast-trending corridor. Samples along the Metallic Trend returned strongly anomalous to high-grade Cu-Zn-Pb as well as consistently anomalous Au, locally high-grade Ag and anomalous Co with values up to: 37.8% Cu (with 184 ppb Au, 2970 ppm Zn, 449 ppm Pb, 356 ppm Co & 45 ppm Ag); 3.01 gpt Au (with 7860 ppm Cu & 579 ppm Co); 19.3% Zn, 10% Pb & 1130 ppm Ag (with 1.85 gpt Au, 3.01% Cu & 1010 ppm Co); 1700 ppm Co (with 201 ppb Au, 6090 ppm Cu, 8.93% Zn, 1.78% Pb & 154 ppm Ag).決済の安定と成長配当データの取得安定した配当: FLDP.Fの 1 株当たり配当が過去に安定していたかどうかを判断するにはデータが不十分です。増加する配当: FLDP.Fの配当金が増加しているかどうかを判断するにはデータが不十分です。配当利回り対市場Frontline Gold 配当利回り対市場FLDP.F 配当利回りは市場と比べてどうか？セグメント配当利回り会社 (FLDP.F)n/a市場下位25% (US)1.4%市場トップ25% (US)4.2%業界平均 (Metals and Mining)1.5%アナリスト予想 (FLDP.F) (最長3年)n/a注目すべき配当: FLDP.Fは最近配当金を報告していないため、配当金支払者の下位 25% に対して同社の配当利回りを評価することはできません。高配当: FLDP.Fは最近配当金を報告していないため、配当金支払者の上位 25% に対して同社の配当利回りを評価することはできません。株主への利益配当収益カバレッジ: FLDP.Fの 配当性向 を計算して配当金の支払いが利益で賄われているかどうかを判断するにはデータが不十分です。株主配当金キャッシュフローカバレッジ: FLDP.Fが配当金を報告していないため、配当金の持続可能性を計算できません。高配当企業の発掘7D1Y7D1Y7D1YUS 市場の強力な配当支払い企業。View Management企業分析と財務データの現状データ最終更新日（UTC時間）企業分析2023/01/31 05:07終値2022/11/03 00:00収益2022/09/30年間収益2021/12/31データソース企業分析に使用したデータはS&P Global Market Intelligence LLC のものです。本レポートを作成するための分析モデルでは、以下のデータを使用しています。データは正規化されているため、ソースが利用可能になるまでに時間がかかる場合があります。パッケージデータタイムフレーム米国ソース例会社財務10年損益計算書キャッシュ・フロー計算書貸借対照表SECフォーム10-KSECフォーム10-Qアナリストのコンセンサス予想+プラス3年予想財務アナリストの目標株価アナリストリサーチレポートBlue Matrix市場価格30年株価配当、分割、措置ICEマーケットデータSECフォームS-1所有権10年トップ株主インサイダー取引SECフォーム4SECフォーム13Dマネジメント10年リーダーシップ・チーム取締役会SECフォーム10-KSECフォームDEF 14A主な進展10年会社からのお知らせSECフォーム8-K* 米国証券を対象とした例であり、非米国証券については、同等の規制書式および情報源を使用。特に断りのない限り、すべての財務データは1年ごとの期間に基づいていますが、四半期ごとに更新されます。これは、TTM（Trailing Twelve Month）またはLTM（Last Twelve Month）データとして知られています。詳細はこちら。分析モデルとスノーフレーク本レポートを生成するために使用した分析モデルの詳細は当社のGithubページでご覧いただけます。また、レポートの使用方法に関するガイドやYoutubeのチュートリアルも掲載しています。シンプリー・ウォールストリート分析モデルを設計・構築した世界トップクラスのチームについてご紹介します。業界およびセクターの指標私たちの業界とセクションの指標は、Simply Wall Stによって6時間ごとに計算されます。アナリスト筋Frontline Gold Corporation これらのアナリストのうち、弊社レポートのインプットとして使用した売上高または利益の予想を提出したのは、 。アナリストの投稿は一日中更新されます。1 アナリスト機関Andrey LitvinEdison Investment Research
お知らせ • Feb 13Frontline Gold's Listing to Transfer to NEXIn accordance with TSX Venture Policy 2.5, Frontline Gold Corporation (the 'Company’) has not maintained the requirements for a TSX Venture Tier 2 company. Therefore, effective at the opening on February 14, 2024, the Company's listing will transfer to NEX, the Company's Tier classification will change from Tier 2 to NEX, and the Filing and Service Office will change from Montreal to NEX. As of February 14, 2024, the Company is subject to restrictions on share issuances and certain types of payments as set out in the NEX policies. The trading symbol for the Company will change from FGC to FGC.H. The symbol extension differentiates NEX symbols from Tier 1 or Tier 2 symbols within the TSX Venture market. Further to the Exchange bulletin issued May 8, 2023, trading in the shares of the Company will remain suspended. Members are prohibited from trading in the securities of the Company during the period of the suspension or until further notice.
お知らせ • Jan 26Frontline Gold Corporation Receives High-Grade Assays from 2022 Field Program Rock Samples on Its Epworth PropertyFrontline Gold Corporation announced that rock sampling results have been received from the 2022 field program on its Epworth Property (`the Property'), Nunavut. Fifty-seven rock samples were collected, mainly along the Metallic Trend outlined in 2021 and its strike extension to the north and south. The Metallic Trend consists of locally high-grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization over a strike length of 1.15 km. Some sampling was also carried out at the historical Puppet and DD North Showings. Additional sampling along the Metallic Trend in 2022 yielded results of up to: 8.59% Cu & 884 ppb Au (with 0.18% Zn, 0.1% Co, 876 ppm As & 692 ppm V), from dolomite with red cherty fragments and stringers of possible chalcocite, chalcopyrite and pyrite and several % malachite staining. These were the highest Cu, Au & V grades of the 2022 program; 27.4% Zn (with 5.37% Pb, 0.22% Cu, 218 ppm Co, 66 ppm Ag, 404 ppm Cd & 5.64 ppm Ge) at the south end of the Metallic Trend from large dolomite felsenmeer. This was the highest Zn grade of both the 2021 and 2022 programs. The previous highest grade was 19.2% Zn at the north end of the Metallic Trend. Cd, Ge and V are common accessory elements in sediment-hosted Zn-Pb-(Cu) deposits; 16.7% Pb & 71.4 ppm Ag (with 8.26% Zn), also at the south end of the Metallic Trend, from a sample described as white dolomite with minor contorted red chert bands and 10% galena from frost heave. Possible dissolution collapse breccia was noted here. This was the highest Pb value obtained along the Metallic Trend from both the 2021 and 2022 programs; 1420 ppm Co & 7190 ppm As (with 1.31% Cu, 532 ppm Pb, 296 ppm Zn & 63 ppb Au) from an additional sample at the Metallic Showing, described as white-grey dolomite with malachite and azurite staining, pyrite, galena and sphalerite. Sampling up to 175 m north of the north end of the Metallic Trend yielded Cu-in-rock anomalies up to 0.15%. Sampling up to 1.5 km south of the south end of the Metallic Trend yielded anomalies in rock up to 0.61% Cu, 0.75% Zn, 0.46% Pb and 201 ppm Co.
お知らせ • Nov 24Advance United Holdings Inc. and Frontline Gold Inc. Report on Geophysical Work Program on Paint Lake Road Project in Wawa, OntarioAdvance United Holdings Inc. and Frontline Gold Inc. reported numerous favorable geophysical anomalies have been identified on the Paint Lake Road JV (PLR JV) Property. The project is within the Wawa Abitibi Subprovince, prolifically known for its metal endowment. It has been estimated the Abitibi Subprovince has produced over 200 million ounces of gold and 400 million tonnes of base metal ore. The belt has recently been consolidated and the Paint Lake Road property is strategically located inside the consolidated area near the Mishi Open Pit and the former Magnacon Mines. The property comprises six (6) claim blocks totaling over 3,610 hectares 50km north of Wawa, Ontario and is located inside the Mishibishu Greenstone Belt which hosts the Wesdome Mines, the Eagle River Gold Mine, the Mishi Open Pit, and the former Magnacon Mine. Advance United has had success in the Wawa area having formerly developed and sold the Dorset Zone to current owners, Angus Ventures, which hosts a non-compliant resource of 100,000 oz. gold. The full story can be read here. The Paint Lake Road property sits along the Pukaskwa-Iron Lake (PIL) Shear Zone, known to host gold mineralization at the former Argo property and further south at Wesdome's Camp Lake occurrence. Further northeast the Iron Lake Shear Zone hosts Alamos' Island Lake Mine. The Paint Lake Road Property Geology The Property occurs within the Mishibishu greenstone belt that is a broad arcuate syncline 55 km long east-west and 16 km wide north-south. This belt is part of the Wawa Subprovince of the Archean age Superior Province. Supracrustal rocks in the belt are dominated by greenschist facies mafic to intermediate volcanic rocks with lesser sedimentary rocks including iron formation and intermediate to felsic volcanic rocks. The belt is surrounded by Archean granitic rocks and includes two internal granitic batholiths occupying the central portion of the belt. The northern limb of the belt, where the PLR JV Property and the Mishi Mine of Wesdome are located is dominated by an assemblage of clastic sedimentary rocks, felsic tuffs, and mafic flows. The southern limb, where the Eagle River Mine is located, is dominated by tholeiitic basalts and calc-alkaline andesites with minor interflow clastic sedimentary rocks and lean chert-magnetite iron formation. Promising Paint Lake Road Targets: The target for exploration on the PLR JV is shear-hosted orogenic gold similar to Wesdome's Eagle Deposit which is hosted by quartz veins in shear zones hosted by intrusive diorite. The presence of a regional scale shear zone is considered prospective for this type of deposit. Gold bearing quartz veins at Eagle River are hosted primarily by subvertical to steeply north dipping east-west striking shear zones within an elliptical quartz diorite stock Mineralized structures exhibit broad zones of deformed rock (3-20 m wide shear zones) affiliated with strong silicification over 20-50 m width. The PLR JV property is underlain by intrusive rocks and as such has been largely ignored in previous exploration programs. The identification of possible shear offsets from the main PIL shear will be further explored with prospecting and sampling.
お知らせ • Nov 15Frontline Gold Corp Appoints James R. Atkinson as DirectorFRONTLINE GOLD CORP appointed Mr. James R. Atkinson, M.Sc., P. Geo as a member of the board of directors with immediate effect. Since 2018, Mr. Atkinson has been the President and CEO of Talisker Gold. An experienced exploration geologist and project manager with over 45 years of experience, Mr. Atkinson has spent his career in both mineral exploration and mining and in the environmental field as Vice President, Exploration Manager and Regional Manager with junior and major mining companies such as Newmont, Billiton and Agnico Eagle. He has reviewed, evaluated and acquired projects around the world and recently was part of the team responsible for mergers and acquisitions at American Silver. He has worked with investors to form and manage junior exploration companies.
お知らせ • Nov 04Frontline Gold Corporation Receives Strongly Anomalous Soil Sampling Results from Its Epworth Property, NunavutFrontline Gold Corporation announced that soil sampling results have been received from the 2022 field program on its Epworth Property (`the Property'), Nunavut. Humus (A horizon) and B horizon /clay samples were collected across the `Metallic Trend' discovered in 2021, as well as the strike extension of the Trend to the north and south. The Metallic Trend consists of locally high-grade Cu-Zn-Pb-Ag mineralization and strongly anomalous Au & Co mineralization over a strike length of 1.1 km (see Project Background below). The soil sampling survey consisted of seven east-northeast-west-southwest lines over a distance of 2.8 km, with lines ranging in length from 75 to 150 meters and sample station spacing at 12.5 m. Either a humus sample or B horizon /clay sample were collected at each station. The latter were frequently collected in frost boils. The best results were obtained from frost boils which turned up mineralized rock (sampled in 2021, see Project Background below). Humus samples returned strongly anomalous results adjacent to these frost boils but also in low, marshy ground. Top results for B horizon /clay samples are as follows: 2970 ppm Cu (TD-ICP); 2710 ppm Zn (TD-ICP); 2010 ppm Pb (TD-ICP); 127 ppm Co (TD-ICP); 8.6 ppm Ag (TD-ICP); 99 ppb Au (FA-AA). Top results for Humus (A horizon) samples are as follows: 542 ppm Cu (TD-ICP); 960 /848 ppm Zn (INAA /TD-ICP); 101 ppm Pb (TD-ICP); 54 /32 ppm Co (INAA /TD-ICP); <2 /0.4 ppm Ag (INAA /TD-ICP); 4 ppb Au (INAA) *TD-ICP stands for `Total Digestion Inductively Coupled Plasma', an analytical method used by Activation Laboratories. FA-AA stands for `Fire Assay Atomic Absorption', an analytical method used by Activation Laboratories; INAA stands for `Instrumental Neutron Activation Analysis', an analytical method used by Activation Laboratories. The highest-value soil anomalies were obtained along the 1.1 km high-grade trend identified in 2021, but weaker anomalies were obtained to the north and south, suggesting that the trend continues (to possibly 2.8 km long and still open along strike). Depth of overburden may play a role in the weaker values on some lines, though mineralization may also not be as intense in these locations. Anomalies were frequently obtained at multiple stations on individual lines, suggesting wide mineralized zones or parallel horizons. . Final results for rock-grab samples collected during the program are pending and will be reported once received. The Metallic Trend follows the contact zone between Upper Odjick Formation red shales and Lower Rocknest Formation dolomites, often forming a valley which can be up to 100 meters wide. Mineralization occurs within grey (reduced) Rocknest dolomite flanked by red (oxidized) dolomite. Redox boundaries are thought to be a crucial control on mineralization. Data collected during the 2022 program suggest that there are at least two parallel reduced, mineralized horizons along the Trend. Multi-station geochemical anomalies appear to support this. Where exposed on surface, the mineralized horizons are up to 12 meters wide and host sulphide-rich quartz-carbonate veins up to 0.4 meters wide. Alternatively, these `parallel horizons' may be explained by repetition of a single horizon by folding or structural duplication by thrust faulting. Larger-scale folding and /or thrusting likely explains the parallel trends that exist to the west and east of the Metallic Trend. Future diamond drilling programs should help establish the geometries of these zones and their vertical extent. Project Background: The Epworth Project is located 85km south of the village of Kugluktuk (Coppermine), containing three main previously known areas of high-grade polymetallic mineralization from 1-25m wide occurring for more than 15km along strike. Historical surface grab samples have reported spectacular high-grade mineralization including: 61.2% Cu & 5600 gpt Ag (Payback Showings); 19.22% Zn with 810 gpt Ag, 3% Cu & 1.86 gpt Au (Metallic Showing). The Metallic trend was identified in 2021 while investigating the historical Metallic Showing (formerly named `Dead Showing') in the northern part of the property, consisting of dolomite with sulphide-rich quartz-carbonate veining in outcrop. Mineralized angular float boulders, subcrop (felsenmeer, frost boil rings) and outcrop were found to extend much further to the south than previously identified, along a well-defined north-northwest-south-southeast-trending corridor. Samples along the Metallic Trend returned strongly anomalous to high-grade Cu-Zn-Pb as well as consistently anomalous Au, locally high-grade Ag and anomalous Co with values up to: 37.8% Cu (with 184 ppb Au, 2970 ppm Zn, 449 ppm Pb, 356 ppm Co & 45 ppm Ag); 3.01 gpt Au (with 7860 ppm Cu & 579 ppm Co); 19.3% Zn, 10% Pb & 1130 ppm Ag (with 1.85 gpt Au, 3.01% Cu & 1010 ppm Co); 1700 ppm Co (with 201 ppb Au, 6090 ppm Cu, 8.93% Zn, 1.78% Pb & 154 ppm Ag).