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Sequoia Kimberlite Complex’s Indicator Mineral Chemistry Points to Large Diamonds, Diagras Project, NWT




– Diamond chemistry reported from Chuck Fipke using C.F. Minerals research lab confirms identical chemistry to those found in large…

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  • - Diamond chemistry reported from Chuck Fipke using C.F. Minerals research lab confirms identical chemistry to those found in large diamonds from Ekati, Letseng, Lucara, and Victor.

  • - Early Caustic Fusion diamond results are also consistent with large diamond population.

  • - Indicator and Diamond results demonstrate that different kimberlite types have sampled different parts of the lithosphere and will have different grades and diamonds.


September 9th, 2021 – TheNewswire - Vancouver, British Columbia – Arctic Star Exploration Corp. (“Arctic Star” or the “Company”) (TSXV:ADD) (Frankfurt:82A2) (WKN:A2DFY5) (OTC:ASDZF) is pleased to announce that it has received diamond indictor mineral results and an interpretation of these from Chuck Fipke for the first hole into the Sequoia Kimberlite complex. The results demonstrate the existence of a number of indicator types that occur with diamonds and strongly suggest the presence of diamonds. Furthermore, indicator minerals of identical multi-element chemistry to those found as inclusions in large >50 carat diamonds world-wide are abundant. The indicators from different kimberlite types are starkly different. These observations are in agreement with the caustic diamond results, which show the different kimberlite types have different stone/kg counts  and also hints at a coarse diamond distribution. Ultimately a bulk sample will be required to confirm the diamond distribution and this is the normal path of progress for diamond exploration. Prior to this a drill program defining the volumes of the different kimberlite types and their caustic fusion diamond distribution is planned for spring 2022.


Samples of kimberlite core were sent to C.F. Mineral Research Ltd. in Kelowna, BC for indicator mineral analysis. C.F. Minerals is a global-leading kimberlite and diamond analytical research facility lead by Chuck Fipke, one of the founders of the Ekati diamond mine. At the lab, the samples were lightly crushed with heavy minerals separated by dense media gravity methods. Oxides and silicates are split using magnetic separation.  Candidate diamond indicator minerals are selected by a minerologist, mounted, and scanned for chemical composition using a scanning electron microscope (SEM). Mineral grains that “light up” under different element scans are mapped and then assayed by electon microprobe. The microprobe results are presented here.


Mineral grains that grow concurrently while touching or within diamonds have distinct chemistry and are diagnostic of the presence diamonds and also of the rock types that host the diamonds  at great depths.


Readers should note the following deep mantle, high pressure rock types associated with diamond mineralization that are noted in this release.


Lherzolite: Garnet, Clinopyroxene, and Olivine. (certain types host >50carat diamonds)

Harzburgite: Garnet (low calcium, high chrome), Orthopyroxene, and Olivine. (Source of the desirable “G10” garnets and P type diamonds.)

Chromite: Harzburgite: A garnet poor, Chromite rich variety of above.

Eclogite:  Garnet and Pyroxene. Source of E Type diamonds


The samples analyzed thus far are from the Sequoia kimberlite, hole DG-2021-04 located in the geographical center of the complex. One sample from the interval 51m to 89m (5.1kg) from the Coherent Kimberlite (“CK”), another sample from the interval 105m to 136m (5.1kg) logged as Volcanoclasitc Kimberlite transitional (“VKt”) into Coherent Kimberlite and a sample from the interval 136m to 150m (5.3kg) logged as Volcanoclastic Kimberlite (“VK”).


Chuck Fipke reports:

“The two Volcanoclastic samples are dominated by diamond inclusion minerals (high calcium G10 garnets (classifying as G10-2 and G10-3) found in Lherzolite, (G11) garnets, and diamond inclusions (CP5) clinopyroxenes that have been found as inclusions in big diamonds ranging from 52 to 102 carat from the Ekati diamond mine (coined "Di$") as well as chromite rich harzburgite containing diamond inclusion chromites and orthopyroxenes. Current research suggests these larger diamonds come from great depths >400km.

The diamond inclusion minerals from lherzolite (DI$, CP5 G9/G11 indicators mentioned above) found in Sequoia are identical to those present in Letseng (In Lesotho), Victor (In Canada), and Lucara’s Karowe Mine (Botswana). These kimberlites are typically lower grade but contain very large high-quality diamonds routinely recovered during run-of-mine operations. This is based on analysis of inclusions from over 335 diamonds from these sources as well as Ekati’s large stones. The classification scheme relies on the multi-element analysis of the Sequoia indicator minerals having the same chemical composition as the indicators from known large diamond sources.

As well as passing through and sampling of lherzolite, the Sequoia kimberlite has sampled diamond bearing chromite harzburgite as evidence by the abundant 99 diamond inclusion composition chromites and 45 diamond inclusion orthopyroxenes present. These additional mineralogies could account for any smaller diamonds recovered. The two Volcanoclastic samples have relatively few eclogitic type garnets which can also be associated with diamond mineralization.

In contrast to the VK samples, the CK sample from 51 to 89 meters has abundant
Group1 eclogitic garnets where the EMP yields 51 diamond inclusion eclogite grains. This sample also has the large diamond inclusion llerzolite minerals and the subordinate diamond bearing (low calcium-high chrome G10-7 and G10-9) pyrope garnet bearing harzburgite not present in the VK as well as chromite harzburgite present in the VK. A total of 80 diamond inclusion composition chromites and 10 diamond inclusion olivines were recovered from the chromite harzburgite.

It is also worthy to note that the overall abundance of the lherzolite (DI$, CP5 G9/G11 indicators) large diamond inclusion minerals recovered from the three Sequoia DG 2021-04 drill hole samples exceeds, per sample weight, that of any of the diamond bearing (lherzolitic) kimberlites in the C.F. Minerals database. These results indicate that large diamonds should be present if sufficiently large tonnages of this kimberlite are processed by methodology that recovers large diamonds. The presence of abundant diamond inclusion chromites and orthopyroxenes, as well as abundant diamond inclusion Group 1 eclogitic garnets, and subordinate low calcium-high chrome G10 garnets and diamond inclusion olivines indicate smaller potentially commercial diamonds may also be present.”


Buddy Doyle, VP Exploration for Arctic Star commented, “It is interesting that the caustic fusion microdiamond results also hint at a coarser diamond distribution. Table 1 shows the published results from the Jack Pine Kimberlite which makes up the southern 200m of the Sequoia complex, and the diamond results received from Arctic Star’s caustic fusion results from the center of Sequoia. These results, plotted on a size vs frequency plot (figure 1), clearly show a coarser diamond population for our recent Sequoia results. Table 3 shows the diamond counts from the different rock types from this drill hole. Like the indicators there seems distinct populations of diamonds from the different rock types.  The company has decided to send the remaining half-split core of Sequoia to the lab to get more diamond results to help construct a more robust curve of the size distribution. It is likely we will need more samples than this to get a good view of the grade and the presence of the larger stones. Given the evidence presented by Chuck Fipkes’s analysis, if big diamonds are proven to be there it will be worth it. “



Table 1. Caustic Fusion Results, Sequoia Kimberlite, Arctic Star


Drill hole










Total stones


Sequoia Total












Table 2. Historic Caustic fusion Results, Jack Pine Kimberlite, Drilled by De Beers 1990s

Drill hole










Total stones


Jack Pine






0 0





Click Image To View Full Size


Figure 1 Size Frequency plot: Diamond size distribution. Sequoia in Orange, Jack Pine in Green. The Sequoia samples appear to have two populations of diamonds, and clearly has a higher frequency of larger diamonds than the Jack Pine sample. Figure 1 also depicts possible trajectories for the Sequoia diamond distribution. For this small sample of less than 300kg, the spread of trajectories is large. Further caustic fusion samples would narrow down this spread. It is desirable to have several commercial size stones from caustic fusion before predicting grade and size distribution with great accuracy.


Mr. Buddy Doyle further commented, “The next step for the Sequoia kimberlite complex is to do more small diameter drilling to further understand the geology, we already have diamond and indicator mineral data that suggests the different types of kimberlite in this complex have different diamond populations and grade. Drilling this body at 100m then where needed 50m centers and conduct caustic fusion analysis would achieve this and fill out the size frequency curve shown in figure 1. Should this prove encouraging and confirm the possibility of large diamonds, a bulk sample using either a large diameter drill rig or underground bulk sampling would be the next step. Which on completion would allow for a feasibility study. Given that there are two operating diamond mines within 35km Arctic Star could also seek out scenarios involving these, along the way.”


Table 3 shows the geology of drill hole DG 2021 04 and each individual rock types Caustic fusion diamond count for stones over 105 microns, illustrating the diamond count differences, which will be reflected in the commercial grade. The next round of work will outline the distribution of these rock types while continuing to make a more robust size frequency curve.


Table 3: Diamond variance counts from each rock type Sequoia, Drill Hole DG 2021 04





Diamond count





Not assayed





68/100 kg




























Table 3 demonstrates that the different kimberlite types have variable diamond counts. The volcanoclastic rock types have significantly less diamonds than the cohernet kimberlite rock type. (Results from Caustic fusion SRC laboraties and independent laboratory see NR dated July 6th 2021 for details).


Analysis of mineral indicator minerals from the other kimberlites is awaited. The rest of the caustic fusion diamond results from the other kimberlite discoveries are expected before the end of this week. The second round of Sequoia results where we have sampled the other half of drill holes DG 2021 04 and 05 should also be in the next weeks.


Qualified Person

The Qualified Person for this news release is Buddy Doyle, AUSIMM, a Geologist with over 35 years of experience in diamond exploration, discovery, and evaluation. A Qualified Person under the provisions of the National Instrument 43-101.


About Arctic Star

Arctic Star is predominantly a diamond explorer, recently discovering 5 new kimberlites in the prolific Lac De Gras kimberlite field that supports 2 multi-billion dollar kimberlite mining complexes. The company also has a 958Ha Exploration permit containing several diamond bearing kimberlites on its Timantti project, Kuusamo Finland. Arctic Star has optioned its Stein diamond project in Nunavut to GGL diamonds who plan work once Covid restrictions lift. The company continues to look for appropriate diamond opportunities elsewhere.




Patrick Power, President & CEO
+1 (604) 218-8772

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release. 


Cautionary Statement Regarding “Forward-Looking” Information

This news release contains “forward-looking statements” including but not limited to statements with respect to Arctic Star’s plans, the estimation of a mineral resource and the success of exploration activities. In this release it is not certain if the kimberlite discovered will be economic or not as this depends on many factors. Forward-looking statements, while based on management’s best estimates and assumptions, are subject to risks and uncertainties that may cause actual results to be materially different from those expressed or implied by such forward-looking statements. There can be no assurance that such statements will prove to be accurate, as actual results and future events could differ materially from those anticipated in such statements. Factors that could affect our plans include our potential inability to raise funds as intended, and in such event we may require all funds raised, if any, to be used for working capital rather than the intended uses as outlined. Accordingly, readers should not place undue reliance on forwardlooking statements. Arctic Star undertakes no obligation or responsibility to update forwardlooking statements, except as required by law.

Copyright (c) 2021 TheNewswire - All rights reserved.

Today’s News

Canada One to Option Franelle Copper Project, Quebec Canada

Vancouver, Canada – TheNewswire – September 16, 2021 – Canada One Mining Corp. (the “Company” or “Canada One”) (TSXV:CONE) is pleased to announce…

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Vancouver, Canada – TheNewswire - September 16, 2021 – Canada One Mining Corp. (the “Company” or “Canada One”) (TSXV:CONE) is pleased to announce that it has entered into an option agreement, effective date August 31st, 2021 (the “Agreement”), pursuant to which the Company will acquire the right to earn a 100% interest, subject to a 2% royalty, in the Franelle Copper Project (the “Project”, or the “Property”), a 31 square kilometre contiguous property located 90 kilometres northwest of Schefferville, Quebec, from Messrs. Fayz and Ramy Yacoub (the “Vendors”), arm’s length parties (the “Transaction”).

Key Highlights

  • - The Project hosts 4 mineralized zones: Franelle, Bennelle, Reuben and Beluet

    - The Franelle zone currently extends westwardly 2,600 metres along a 7000-metre gabbro dyke that has an average width of 60 to 75 metres

    - Three programs of diamond drilling at the Franelle zone intersected significant widths of copper mineralization, including:

    • - 2.42% copper over 13.7m within 32m of 1.12% copper

      - 0.86% copper over 25.3m within 50.3m of 0.51% copper;

      - 0.80% copper over 14.9m within 33.2m of 0.59% copper within 173.4m of 0.29% copper;

      - 0.56% copper over 39m

    - Grab sample copper highlights include: 6.15% and 4.83% from the Beluet zone, 2.06%, 1.73% and 1.68% from the Bennelle zone

    - Chip sample highlights include: 4% copper and 6.9 g/t silver over 0.40 metres and 2.61% copper and 2.5 g/t silver over 2.5 metres from Reuben zone


Canada One cautions investors selected grab samples are selected samples and are not necessarily representative of mineralization hosted on the Project. The true width of the mineralization is unknown at this time.


“The Franelle Copper Project represents an excellent opportunity for Canada One shareholders,” commented CEO Peter Berdusco. “The strong copper grades over good widths immediately attracted us to the project and we plan to undertake a comprehensive review of the historical data to drive the upcoming exploration program.”


The Agreement

The Company can earn a 100% interest in the Franelle Copper Project, subject to a 2% net smelter return royalty by meeting the following terms:

  • - Issuing 3,000,000 shares as follows:

    • - 500,000 Shares within five business days of approval of the TSX Venture Exchange (the “Approval Date”);

      - An additional 500,000 Shares on or before the first anniversary of the Approval Date;

      - An additional 500,000 Shares on or before the second anniversary of the Approval Date;

      - An additional 500,000 Shares on or before the third anniversary of the Approval Date;

      - An additional 500,000 Shares on or before the fourth anniversary of the Approval Date; and

      - An additional 500,000 Shares on or before the fifth anniversary of the Approval Date.

    - Making cash payments totaling $300,000 as follows:

    • - $25,000 payable on signing of the Agreement as non-refundable deposit;

      - An additional $25,000 payable within 15 days from signing of the Agreement as further non-refundable deposit;

      - An additional $50,000 payable on or before the first anniversary of the Approval Date;

      - An additional $50,000 payable on or before the second anniversary of the Approval Date;

      - An additional $50,000 payable on or before the third anniversary of the Approval Date;

      - An additional $50,000 payable on or before the fourth anniversary of the Approval Date; and

      - An additional $50,000 payable on or before the fifth anniversary of the Approval Date.

    - Incurring $5,000,000 in Exploration Expenditures on the Property as follows:

    • - $250,000 within 12 months from the Approval Date;

      - An additional $250,000 within two years from the Approval Date;

      - An additional $250,000 within three years from the Approval Date;

      - An additional $250,000 within four years from the Approval Date;

      - An additional $250,000 within five years from the Approval Date; and

      - An additional $3,750,000 at any time, in any number of proportions and amounts, within five years from the Approval Date


In addition, in the event the Company files a technical report supporting the disclosure of a mineral reserve on the Project at any time prior to the acquisition of the Project, the Company shall issue an additional 1,000,000 shares as a bonus to the Vendors.


The Company can purchase 50% (or 1%) of the net smelter return royalty on the Project at any time for $2,000,000.


The Vendors of the Project, Messrs. Fayz and Ramy Yacoub, are arm’s length parties.  No finders’ fees or commissions are payable in connection with completion of the Transaction.  In connection with completion of the Transaction, it is contemplated that the Company will complete a non-brokered private placement to raise additional capital to satisfy obligations under the Agreement and to further develop the Project.  Further information regarding the terms of the placement will be provided as soon as available.


Closing of the Transaction remains subject to the completion of a technical report in respect of the Property, completion of financing on terms acceptable to the Company, and the approval of the TSX Venture Exchange. The Transaction cannot be completed until approval of the TSX Venture Exchange is received. Trading in the common shares of the Company has been halted on the TSX Venture Exchange and is expected to remain halted pending completion of further filings with the TSX Venture Exchange.


Project Overview


The Franelle Copper Project hosts 4 mineralized zones: Franelle, Bennelle, Beluet and Reuben.

The Franelle zone trends NNW 2600m along a 7000m long gabbro dyke with an average width of 60m to 75m. Mineralization consists of native copper, and copper oxides and sulfides with some potential supergene enrichment. Mineralization occurs as dissemination within the gabbro and with veins, veinlets and stockworks cutting the gabbro and the metasedimentary host rock. Three programs of diamond drilling tested the gabbo between the mid 1970’s and the mid-1990’s. A historic resource was calculated in 1976. The Company will to review the historic data before disclosure. (Diamond Drill Logs, Lac Musset Property, 1995 Energie et Ressources Naturelles Quebec Report GM 53794).


The Bennelle zone consists of veins, veinlets and disseminations of copper mineralization intersecting a gabbro sill intruded into arkosic red sandstone. The Franelle and Bennelle zones may lie along the same gabbro. Mineralization consists of native copper, and copper oxides and sulfides, and has been traced 450m along strike and ranges from 1m to 3m in thickness. Grab sample highlights include 2.06% copper, 1.73% copper and 1.68% copper. (Source: “Gitologie Des Indices De Cuivre Du Lac Musset, Fosse Du Labrador par B. Brassard (1984), Energie et Ressources Naturelles Quebec Report MB84-03).


Mineralization at the Beluet zone is hosted in an altered shear zone within sandstones in fault contact with gabbros and consists of malachite, azurite and chrysocolla accompanied by chalcopyrite.  The shear zone has been traced 50m along strike and is 5m thick. Grab sample highlights include: 6.15% copper and 4.83% copper. (Source: Metallic Deposit 23O/11-004 1995 Energie et Ressources  Naturelles Quebec)


The Reuben zone, a 30-metre wide stockwork of gabbro hosting calcite and epidote veins carrying chalcopyrite and malachite, and has been traced intermittently 425 metres along strike. Individual showings along the trend range from 60 metres by 6 metres to 15 metres by 1.5 metres. Chip sample highlights include: 4% copper and 6.9 g/t silver over 0.40 metres and 2.61% copper and 2.5 g/t silver over 2.5 metres. Source:  (Diamond Drill Logs, Lac Musset Property, 1995 Energie et Ressources  Naturelles Quebec Report GM 53794).


Canada One cautions investors it has not yet verified the above historic data.


Qualified Person


R. Tim Henneberry, P Geo (British Columbia), a consultant to Canada One, is the Qualified Person who has reviewed and approved the technical content of this news release on behalf of the Company.


For further information, interested parties are encouraged to visit the Company’s profile on SEDAR ( or contact the Company by telephone at 1.877.844.4661.

On behalf of the Board of Directors of



Peter Berdusco

President and Chief Executive Officer

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

This news release may contain certain “Forward-Looking Statements” within the meaning of the United States Private Securities Litigation Reform Act of 1995 and applicable Canadian securities laws.  When used in this news release, the words “anticipate”, “believe”, “estimate”, “expect”, “target, “plan”, “forecast”, “may”, “schedule” and other similar words or expressions identify forward-looking statements or information.  These forward-looking statements or information may relate to future prices of commodities, accuracy of mineral or resource exploration activity, reserves or resources, regulatory or government requirements or approvals, the reliability of third party information, continued access to mineral properties or infrastructure, fluctuations in the market for gold, and other factors or information.  Such statements represent the Company’s current views with respect to future events and are necessarily based upon a number of assumptions and estimates that, while considered reasonable by the Company, are inherently subject to significant business, economic, competitive, political and social risks, contingencies and uncertainties.  Many factors, both known and unknown, could cause results, performance or achievements to be materially different from the results, performance or achievements that are or may be expressed or implied by such forward-looking statements.  The Company does not intend, and does not assume any obligation, to update these forward-looking statements or information to reflect changes in assumptions or changes in circumstances or any other events affections such statements and information other than as required by applicable laws, rules and regulations.


Copyright (c) 2021 TheNewswire - All rights reserved.

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Energy & Critical Metals

Benton and Sokoman Shares Rise After Confirming 1st High-Grade Lithium Discovery

Composite grab sampling returns 2.37% Li2OThunder Bay, Ontario–(Newsfile Corp. – September 16, 2021) – Benton Resources Inc. (TSXV: BEX) ("Benton") and…

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Composite grab sampling returns 2.37% Li2O

Thunder Bay, Ontario--(Newsfile Corp. - September 16, 2021) - Benton Resources Inc. (TSXV: BEX) ("Benton") and Sokoman Minerals Corp. (TSXV: SIC) (OTCQB: SICNF) ("Sokoman") (together, "the Alliance") are pleased to announce analyses for 35 of 58 follow-up samples from the recently discovered swarm of Lithium-bearing pegmatite dikes on the Golden Hope Joint Venture Project in southwestern Newfoundland. The 35 grab and chip samples were collected over a 1 km2 area over the swarm of poorly-exposed pegmatite and aplite dykes. The follow-up sampling has confirmed that the pegmatites carry significant Lithium values, the first significant occurrence of Lithium documented in the province of Newfoundland and Labrador, Canada.

  • 31.4% of the samples gave values >1% Li2O
  • The Lithium-bearing samples were taken over a poorly-exposed pegmatite swarm covering 1 km2
  • Additional results are pending (23 samples) along a 1 km strike of pegmatites
  • Lithium, Beryllium, Cesium, Rubidium and Tantalum values were located 2 km to the west of the initial discovery

Of the 35 samples, 11 gave values greater than 1% Li2O with three greater than 2% Li2O, and a high of 2.37% Li2O. The dominant Lithium-bearing mineral appears to be spodumene (LiAl(SiO3)2) which occurs as clusters of elongated prismatic crystals up to 5-cm-long in a grey-white matrix of glassy quartz and feldspar and a pale-green to white mica (see photo of sample 361716). Multiple samples from the aplite dikes give highly-anomalous Cesium (17 ppm to 508 ppm Cs), Rubidium (226 ppm to 1310 ppm Rb) and Tantalum (5 ppm to 179 ppm Ta), typical of evolved pegmatite swarms. Samples 361715-718 were a series of 0.5 m2 composite samples from the discovery outcrop that measures 10m x 3m and is 100% pegmatite. The dike margins are overburden covered and actual width of the dike is not known. All other samples were taken over the broader mineralized area. The following table gives the results for the composite samples and other higher-grade Li values from the area.

Summary of Significant Results (>500 ppm Li)
Sample Li ppm* Conversion % Li2O
361715 1.10% 2.153 2.37
361716 8450 2.153 1.82
361717 7030 2.153 1.51
361718 5550 2.153 1.19
361725 9950 2.153 2.14
361726 4080 2.153 0.88
717102 3240 2.153 0.70
717103 1.01% 2.153 2.17
717104 5290 2.153 1.14
717105 7190 2.153 1.55
717106 6450 2.153 1.39
717107 3390 2.153 0.73
717110 734 2.153 0.16
717111 1080 2.153 0.23
717112 7240 2.153 1.56
717113 8410 2.153 1.81

* Li shown as ppm except where noted as %

Spodumene crystals in Sample 361716 (1.82% Li2O)

To view an enhanced version of this graphic, please visit:

The Alliance also discovered high-grade Beryllium values with 2 grab samples grading >5000 ppm Be, with others ranging from 6 ppm to >5000 ppm Be, with associated anomalous Lithium, Cesium, Rubidium and Tantalum values. These samples, mineralogy unknown, are located approximately 2 km to the west of the Li discovery, providing further evidence that it is an evolved pegmatite system. Additional samples, taken up to 1,000 m along strike, have been submitted for analysis and are pending.

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Map outlining Golden Hope Project Pegmatite Sampling

To view an enhanced version of this graphic, please visit:

Samples were submitted to Actlabs in Ancaster, Ontario for analysis by Sodium Peroxide Fusion ICPOES + ICPMS.

Benton's President and CEO Stephen Stares states: "The discovery of this new Lithium, Beryllium, Cesium, Tantalum and Rubidium mineralization in Newfoundland continues to show the Island's vast potential. Although this is the first discovery of Lithium in Newfoundland, the geological environment and setting to discover these types of large systems have already been proven and discovered in the Appalachian belt. This includes the important deposits held by Piedmont Lithium Inc in the Carolinas, eastern US, as well as the geologically equivalent Avalonia Project being advanced by Ganfeng Lithium in the Caledonides of Ireland. Benton and Sokoman will use these deposits for synergies and modeling as we advance this new discovery towards drilling."

Sokoman's President and CEO Tim Froude adds: "We are very pleased to have unequivocally verified high-grade Lithium mineralization at Golden Hope, the first such significant occurrence in Newfoundland. While still early days, significant Lithium mineralization in similar geological settings, elsewhere in the greater Appalachian belt, bodes well for the potential of this discovery to be of significance to our shareholders. While continuing to explore the pegmatites for Li and associated elements, the claims were originally staked for gold and we are presently processing and merging our recently-flown airborne data with pre-existing data to highlight gold targets on the 750 sq km property."

The Alliance has completed a 5,709 line-km Heliborne, High-Resolution, Aeromagnetic & Matrix Digital VLF-EM Survey, flown by Terraquest Ltd. The survey will provide the structural/ lithological setting to help identify gold-bearing structure extensions, as well as any unrecognized structures including those potentially related to the Lithium-bearing pegmatites.


This news release has been reviewed and approved by Timothy Froude, P.Geo., President and CEO of Sokoman Minerals Corp., and Nathan Sims, P.Geo., Senior Exploration Manager for Benton Resources Inc., both the 'Qualified Person' under National Instrument 43-101.

COVID-19 Protocols

To ensure a working environment that protects the health and safety of the staff and contractors, Sokoman and Benton are operating under federally and provincially mandated and recommended guidelines during the current COVID-19 alert level.

About Sokoman Minerals Corp.

Sokoman Minerals Corp. is a discovery-oriented company with projects in Newfoundland and Labrador, Canada. The Company's primary focus is its portfolio of gold projects: flagship, 100%-owned Moosehead, Crippleback Lake (optioned to Trans Canada Gold Corp.) and East Alder (optioned to Canterra Minerals Corporation) along the Central Newfoundland Gold Belt, and the district-scale Fleur de Lys project in northwestern Newfoundland, that is targeting Dalradian-type orogenic gold mineralization similar to the Curraghinalt and Cavanacaw deposits in Northern Ireland, and Cononish in Scotland. The company also recently entered into a strategic alliance with Benton Resources Inc. through three large-scale joint-venture properties including Grey River Gold, Golden Hope and Kepenkeck in Newfoundland. Sokoman now controls independently and through the Benton alliance over 150,000 hectares (>6,000 claims - 1,500 sq. km), making it one of the largest landholders in Newfoundland, Canada's newest and rapidly-emerging gold districts. The company also retains an interest in an early-stage antimony/gold project (Startrek) in Newfoundland, optioned to White Metal Resources Inc., and in Labrador, the Company has a 100%-interest in the Iron Horse (Fe) project that has Direct Shipping Ore (DSO) potential.

About Benton Resources Inc.

Benton Resources Inc. is a well-funded mineral exploration company listed on the TSX Venture Exchange under the symbol BEX. Following a project generation business model, Benton has a diversified, highly-prospective property portfolio in Gold, Silver, Nickel, Copper, and Platinum Group Elements and currently holds large equity positions in other mining companies that are advancing high-quality assets. Whenever possible, BEX retains Net Smelter Return (NSR) royalties for potential long-term cash flow. Benton has also recently entered into a 50/50 strategic alliance with Sokoman Minerals Corp. (TSXV: SIC) through three large-scale joint venture properties including Grey River, Golden Hope and Kepenkeck in Newfoundland that are now being explored.

For further information, please contact:

CHF Capital Markets
Cathy Hume, CEO
Phone: 416-868-1079 x251

Sokoman Minerals Corp.
Timothy Froude, P.Geo., President & CEO
Phone: 709-765-1726

Benton Resources Inc.
Stephen Stares, President & CEO
Phone: 807-475-7474

Twitter: @BentonResources, @SokomanMinerals
Facebook: @BentonResourcesBEX, @SokomanMinerals
LinkedIn: @BentonResources, @SokomanMinerals


The information contained herein contains "forward-looking statements" within the meaning of applicable securities legislation. Forward-looking statements relate to information that is based on assumptions of management, forecasts of future results, and estimates of amounts not yet determinable. Any statements that express predictions, expectations, beliefs, plans, projections, objectives, assumptions or future events or performance are not statements of historical fact and may be "forward-looking statements."

Forward-looking statements are subject to a variety of risks and uncertainties which could cause actual events or results to differ from those reflected in the forward-looking statements, including, without limitation: risks related to failure to obtain adequate financing on a timely basis and on acceptable terms; risks related to the outcome of legal proceedings; political and regulatory risks associated with mining and exploration; risks related to the maintenance of stock exchange listings; risks related to environmental regulation and liability; the potential for delays in exploration or development activities or the completion of feasibility studies; the uncertainty of profitability; risks and uncertainties relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits; risks related to the inherent uncertainty of production and cost estimates and the potential for unexpected costs and expenses; results of prefeasibility and feasibility studies, and the possibility that future exploration, development or mining results will not be consistent with the Companies' expectations; risks related to gold price and other commodity price fluctuations; and other risks and uncertainties related to the Companies prospects, properties and business detailed elsewhere in the Companies' disclosure record. Should one or more of these risks and uncertainties materialize, or should underlying assumptions prove incorrect, actual results may vary materially from those described in forward-looking statements. Investors are cautioned against attributing undue certainty to forward-looking statements. These forward-looking statements are made as of the date hereof and the Companies do not assume any obligation to update or revise them to reflect new events or circumstances. Actual events or results could differ materially from the Companies' expectations or projections.

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CopperBank Closes $5 Million Private Placement Financing

VANCOUVER, BC / ACCESSWIRE / September 16, 2021 / CopperBank Resources Corp. ("CopperBank" or the "Company") (CSE:CBK) announces that it has closed the…

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VANCOUVER, BC / ACCESSWIRE / September 16, 2021 / CopperBank Resources Corp. ("CopperBank" or the "Company") (CSE:CBK) announces that it has closed the previously announced non-brokered private placement offering (the "Offering") of units of the Company (the "Units") at a price of $0.40 per Unit, for aggregate gross proceeds to the Company of $5,000,000.

"It is great to close this financing so soon after taking over as CEO and seeing such strong demand from seasoned, long-term resource investors," said Paul Harbidge, President and Chief Executive Officer. "This financing bolsters the balance sheet as the Company progresses the advanced Copper Creek project in Arizona, as well as the Contact Copper project in Nevada. We look forward to demonstrating the value of these projects by developing geological models, updating the resource estimates and technical studies, as well as commencing exploration drilling on both properties."

Each Unit consists of one common share of the Company (a "Common Share") and one common share purchase warrant of the Company (a "Warrant"). Each Warrant entitles the holder thereof to purchase one Common Share at an exercise price of $0.60 at any time up to five years following the closing of the Offering. No finder's fees were paid as part of this private placement.

The net proceeds received by the Company from the Offering will be used to advance the Company's Copper Creek and Contact Copper exploration projects, as well as for general working capital purposes.

The Common Shares and Warrants to be issued under the Offering will have a hold period of four months and one day from the closing of the Offering.

Paul Harbidge and Russell Ball, both insiders of the Company, subscribed for a total of 3,000,000 Units under the Offering, both of which subscriptions constitutes a "related party transaction" within the meaning of Multilateral Instrument 61-101 Protection of Minority Security Holders in Special Transactions ("MI 61-101"). The issuance to the insiders is exempt from the valuation requirement of MI 61-101 by virtue of the exemption contained in section 5.5(b) as the Company's shares are not listed on a specified market and from the minority shareholder approval requirements of MI 61-101 by virtue of the exemption contained in section 5.7(a) of MI 61-101 in that the fair market value of the consideration of the shares issued to the related parties did not exceed 25% of the Company's market capitalization.

About CopperBank

CopperBank is a Canadian exploration mining company focused on energy related metal exploration in The United States of America. The Company trades on the Canadian Securities Exchange under the symbol "CBK".

For additional information please contact:

Paul Harbidge, President and Chief Executive Officer

CopperBank Resources Corp.
Suite 1500, 409 Granville Street, Vancouver, BC V6C 1T2
Phone: 778-987-2761

Forward-Looking and Cautionary Statements

Certain information in this release constitutes forward looking statements or information ("forward-looking statements") under applicable securities laws and necessarily involves risks and uncertainties. Forward-looking statements included herein are made as of the date of this news release and, except as required by applicable law, CopperBank does not undertake any obligation to update or revise any of the forward-looking statements, whether as a result of new information, future events or otherwise. The forward-looking statements contained in this document are expressly qualified by this cautionary statement. Forward-looking statements relate to future events or future performance and reflect management of CopperBank's expectations or beliefs regarding future events. In certain cases, forward-looking statements can be identified by the use of words such as "plans", or "believes", or variations of such words and phrases or statements that certain actions, events or results "may", "could", "would", "might" or "will be taken", "occur" or "be achieved" or the negative of these terms or comparable terminology.

Examples of forward-looking statements in this news release include, but are not limited to, statements with respect the use of the net proceeds of the Offering by the Company. Although CopperBank believes that the expectations reflected in the forward-looking statements are reasonable, forward looking statements have been based on factors and assumptions concerning future events which may prove to be inaccurate. Those factors and assumptions are based upon currently available information available to CopperBank. Forward-looking statements are based, in part, on assumptions and factors that may change or prove to be incorrect, thus causing actual results, performance or achievements to be materially different from those expressed or implied by forward looking information.

Such factors and assumptions include, but are not limited to, the Company's ability to identify and complete one or more transactions involving the Company's portfolio assets that enhance shareholder value as part of management's ongoing review of strategic alternatives in the current market conditions. By their very nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements to be materially different from any future results, performance or achievements expressed or implied by forward-looking statements. Such factors include, but are not limited to, the risk that the Company will not be able to identify and complete one or more transactions involving the Company's portfolio assets that enhance shareholder value as part of management's ongoing review of strategic alternatives in the current market conditions. Although CopperBank has attempted to identify important factors that could cause actual actions, events or results to differ materially from forward-looking statements, there may be other factors that cause actions, events or results not to be as anticipated, estimated or intended. There can be no assurance that forward-looking statements will prove to be accurate, as actual results and future events could differ materially from those anticipated by such forward-looking statements. Accordingly, readers should not place undue reliance on forward-looking statements. For more information on CopperBank and the risks and challenges of its businesses, investors should review the continuous disclosure filings that are available under CopperBank's profile at

This press release does not constitute an offer to sell or a solicitation of an offer to buy any of the securities described herein. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act"), or any state securities laws and may not be offered or sold within the United States or to United States Persons unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.

SOURCE: CopperBank Resources Corp.

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