This company listing is no longer activeThis company may still be operating, however this listing is no longer active.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 (FLDP.F) 주식 개요A junior mineral exploration company, engages in the acquisition, exploration, and evaluation of gold properties in Canada and Turkey. 자세히 보기FLDP.F 펀더멘털 분석스노우플레이크 점수가치 평가0/6미래 성장0/6과거 실적0/6재무 건전성0/6배당0/6위험 분석의미 있는 시가총액이 없습니다($1M)수익이 USD$1m 미만입니다(CA$0)마이너스 주주 지분주식은 유동성이 매우 낮습니다+ 위험 1건 추가모든 위험 점검 보기FLDP.F Community Fair Values Create NarrativeSee what others think this stock is worth. Follow their fair value or set your own to get alerts.Your Fair ValueUS$Current PriceUS$0.00056해당 없음내재 할인율Est. Revenue$PastFuture-2m2m2016201920222025202620282031Revenue CA$1.0Earnings CA$0.1AdvancedSet Fair ValueView all narrativesFrontline Gold Corporation 경쟁사Patriot GoldSymbol: OTCPK:PGOLMarket cap: US$2.8mAthena GoldSymbol: OTCPK:AHNR.FMarket cap: US$17.2mGold ResourceSymbol: NYSEAM:GOROMarket cap: US$208.8mNovo ResourcesSymbol: OTCPK:NSRP.FMarket cap: US$22.5m가격 이력 및 성과Frontline Gold 주가의 최고가, 최저가 및 변동 요약과거 주가현재 주가CA$0.0005652주 최고가CA$0.0005652주 최저가CA$0.00056베타2.111개월 변동0%3개월 변동n/a1년 변동n/a3년 변동-30.00%5년 변동-94.17%IPO 이후 변동-75.65%최근 뉴스 및 업데이트공시 • 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.공시 • 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.공시 • 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.공시 • 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.공시 • 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).더 많은 업데이트 보기Recent updates공시 • 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.공시 • 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.공시 • 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.공시 • 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.공시 • 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).주주 수익률FLDP.FUS Metals and MiningUS 시장7D0%1.7%1.2%1Yn/a85.5%28.7%전체 주주 수익률 보기수익률 대 산업: FLDP.F의 US Metals and Mining 산업 대비 성과를 판단하기에 데이터가 부족합니다.수익률 대 시장: FLDP.F의 US 시장 대비 성과를 판단하기에 데이터가 부족합니다.주가 변동성Is FLDP.F's price volatile compared to industry and market?FLDP.F volatilityFLDP.F Average Weekly Movementn/aMetals and Mining Industry Average Movement9.5%Market Average Movement7.2%10% most volatile stocks in US Market16.4%10% least volatile stocks in US Market3.1%안정적인 주가: FLDP.F는 지난 3개월 동안 US 시장에 비해 주가 변동성이 크지 않았습니다.시간에 따른 변동성: Insufficient data to determine FLDP.F의 변동성 변화를 판단할 수 없습니다.회사 소개설립직원 수CEO웹사이트2008n/aWalter Henrywww.frontlinegold.com더 보기Frontline Gold Corporation 기초 지표 요약Frontline Gold의 순이익과 매출은 시가총액과 어떻게 비교됩니까?FLDP.F 기초 통계시가총액US$1.46m순이익 (TTM)-US$248.42k매출 (TTM)n/a0.0x주가매출비율(P/S)-5.9x주가수익비율(P/E)FLDP.F는 고평가되어 있습니까?공정 가치 및 평가 분석 보기순이익 및 매출최근 실적 보고서(TTM)의 주요 수익성 지표FLDP.F 손익계산서 (TTM)매출CA$0매출원가CA$0총이익CA$0기타 비용CA$334.27k순이익-CA$334.27k최근 보고된 실적Sep 30, 2022다음 실적 발표일해당 없음주당순이익(EPS)-0.0026총이익률0.00%순이익률0.00%부채/자본 비율-160.6%FLDP.F의 장기 실적은 어땠습니까?과거 실적 및 비교 보기View Valuation기업 분석 및 재무 데이터 상태데이터최종 업데이트 (UTC 시간)기업 분석2023/01/31 05:10종가2022/11/03 00:00수익2022/09/30연간 수익2021/12/31데이터 소스당사의 기업 분석에 사용되는 데이터는 S&P Global Market Intelligence LLC에서 제공됩니다. 아래 데이터는 이 보고서를 생성하기 위해 분석 모델에서 사용됩니다. 데이터는 정규화되므로 소스가 제공된 후 지연이 발생할 수 있습니다.패키지데이터기간미국 소스 예시 *기업 재무제표10년손익계산서현금흐름표대차대조표SEC 양식 10-KSEC 양식 10-Q분석가 컨센서스 추정치+3년재무 예측분석가 목표주가분석가 리서치 보고서Blue Matrix시장 가격30년주가배당, 분할 및 기타 조치ICE 시장 데이터SEC 양식 S-1지분 구조10년주요 주주내부자 거래SEC 양식 4SEC 양식 13D경영진10년리더십 팀이사회SEC 양식 10-KSEC 양식 DEF 14A주요 개발10년회사 공시SEC 양식 8-K* 미국 증권에 대한 예시이며, 비(非)미국 증권에는 해당 국가의 규제 서식 및 자료원을 사용합니다.별도로 명시되지 않는 한 모든 재무 데이터는 연간 기간을 기준으로 하지만 분기별로 업데이트됩니다. 이를 TTM(최근 12개월) 또는 LTM(지난 12개월) 데이터라고 합니다. 자세히 알아보기.분석 모델 및 스노우플레이크이 보고서를 생성하는 데 사용된 분석 모델에 대한 자세한 내용은 당사의 Github 페이지에서 확인하실 수 있습니다. 또한 보고서 활용 방법에 대한 가이드와 YouTube 튜토리얼도 제공합니다.Simply Wall St 분석 모델을 설계하고 구축한 세계적 수준의 팀에 대해 알아보세요.산업 및 섹터 지표산업 및 섹터 지표는 Simply Wall St가 6시간마다 계산하며, 프로세스에 대한 자세한 내용은 Github에서 확인할 수 있습니다.분석가 소스Frontline Gold Corporation는 1명의 분석가가 다루고 있습니다. 이 중 명의 분석가가 우리 보고서에 입력 데이터로 사용되는 매출 또는 수익 추정치를 제출했습니다. 분석가의 제출 자료는 하루 종일 업데이트됩니다.분석가기관Andrey LitvinEdison Investment Research
공시 • 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.
공시 • 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.
공시 • 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.
공시 • 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.
공시 • 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).
공시 • 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.
공시 • 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.
공시 • 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.
공시 • 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.
공시 • 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).
