Vancouver, British Columbia–(Newsfile Corp. – September 20, 2022) – StrikePoint Gold Inc. (TSXV: SKP) (OTCQB: STKXF) (“StrikePoint” or the “Company”) is pleased to announce that the company has signed a Definitive Agreement dated September 19, 2022, with Snowline Gold (“Snowline”) (CSE: SGD) (OTCQB: SNWGF) with respect to the acquisition by Snowline of StrikePoint’s Yukon properties. The terms of the transaction set out in the Definitive Agreement include:
Snowline will make a cash payment to StrikePoint of $500,000;
Snowline will issue 500,000 shares to StrikePoint (valued at $1,375,000);
CEO and Director of StrikePoint, Shawn Khunkhun commented, “We have now positioned ourselves as shareholders in Snowline Gold, an exciting, Yukon-focused exploration company with a new discovery, while remaining focused on advancing our Golden Triangle properties.”
The properties being divested include: Golden/Nug/Oly, Can East, Horn, How, MacEast, Nordic, Otter, PPM, TET and Tintina. The projects are located mainly in the Mayo and Watson Lake Mining districts. The Golden Oly project an intrusive-related gold system, located approximately 75 kilometers south of Snowline Gold’s flagship Rogue.
StrikePoint is wrapping up its 2022 exploration programs at its two Golden Triangle properties: the Willoughby gold-silver property and the Porter silver property. To-date, 1,382 drill core samples and 203 surface samples have been shipped from drill and surface exploration programs on both properties with all assays pending.https://embed.fireplace.yahoo.com/embed?
About StrikePoint
StrikePoint Gold is an exploration company focused on discovering high-grade precious metals resources in Canada. The Company controls two advanced-stage exploration assets in BC’s Golden Triangle. The past-producing Porter silver project and the Willoughby gold project, located adjacent to Ascot Gold’s Red Mountain development project. The company also owns a portfolio of gold properties in the Yukon.
ON BEHALF OF THE BOARD OF DIRECTORS OF STRIKEPOINT GOLD INC.
“Shawn Khunkhun”
Shawn Khunkhun Chief Executive Officer and Director
Statements in this release that are forward-looking statements are subject to various risks and uncertainties concerning the specific factors disclosed under the heading “Risk Factors” and elsewhere in the company’s filings with Canadian securities regulators. Such information contained herein represents management’s best judgment as of the date hereof based on information currently available. The company does not assume any obligation to update any forward-looking statements, save and except as may be required by applicable securities laws.
Neither the TSX Venture Exchange nor it’s 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.
For further information: Shawn Khunkhun, CEO & Director, 1-604-609-5137, www.strikepointgold.com
Vancouver, British Columbia–(Newsfile Corp. – September 15, 2022) – EMX Royalty Corporation (NYSE American: EMX) (TSXV: EMX) (FSE: 6E9) (the “Company” or “EMX”) is pleased to announce the receipt of initial royalty production payments from its Balya North royalty property in western Turkey. EMX holds an uncapped 4% net smelter return (“NSR”) royalty on metals production from Balya North, a newly commissioned lead-zinc-silver mine operated by Esan Eczacibaşi Endüstriyel Hammaddeler San. ve Tic. A.Ş. (“Esan”), a private Turkish company.
In the first half of 2022, Esan’s advancement of the Balya North asset consisted of mine development and opening of production headings and faces for exploitation in Q3 and Q4 of 2022 (see EMX News Release dated December 20, 2021). Production and processing of materials from Balya North in the first half of 2022 largely consisted of material stockpiled during the construction process. EMX has received payments from the processing of this material totaling US$98,787, inclusive of US$15,069 in Value Added Tax (“VAT”). These royalty payments are from 30,223 tonnes of processed material averaging 1.68% lead, 1.34% zinc, and 39.9 g/t silver.
The Balya North Mine is now operational. From current technical information provided by the operator, EMX anticipates that production will now ramp up to reach a projected production total of approximately 170,000 tonnes of material in 2022. Further, EMX anticipates production of approximately 450,000 tonnes of material from Balya North in 2023. It should be noted that the grades of material mined so far at Balya North are from materials removed during the construction and development process. Grades are expected to be significantly higher as commercial production progresses.
Balya North Lead-Zinc-Silver Deposit: The Balya North lead-zinc-silver deposit is situated in the historic Balya mining district of northwestern Turkey. Mining at Balya has taken place since antiquity, with several generations of historical operations. The Balya North property contains extensive zones of shear-zone hosted and carbonate replacement style (“CRD”) lead-zinc-silver mineralization in addition to skarn and more copper-rich styles of mineralization developed at depth.
Esan acquired the EMX royalty property at the end of 2019 (See EMX news release dated January 7, 2020) and is a private Turkish company that operates 40 mines and eight processing plants. Most importantly, Esan operates a lead-zinc mine and flotation mill on the property immediately adjacent to EMX’s Balya North royalty property. The mineralization at Balya North is effectively an extension of the mineralization currently being mined by Esan in the main Balya deposit.
Esan is also continuing extensive exploration programs at Balya North to expand the currently defined zones of mineralization and to find new bodies of mineralization on the EMX royalty property.
More information on the Balya royalty asset can be found at www.EMXroyalty.com.
Dr. Eric P. Jensen, CPG, a Qualified Person as defined by National Instrument 43-101 and employee of the Company, has reviewed, verified and approved the disclosure of the technical information contained in this news release.
About EMX. EMX is a precious, base and battery metals royalty company. EMX’s investors are provided with discovery, development, and commodity price optionality, while limiting exposure to risks inherent to operating companies. The Company’s common shares are listed on the NYSE American Exchange and the TSX Venture Exchange under the symbol EMX, and also trade on the Frankfurt exchange under the symbol “6E9”. Please see www.EMXroyalty.com for more information.
For further information contact:
David M. Cole President and Chief Executive Officer Phone: (303) 973-8585 Dave@emxroyalty.com
Scott Close Director of Investor Relations Phone: (303) 973-8585 SClose@emxroyalty.com
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Forward-Looking Statements
This news release may contain “forward-looking statements” that reflect the Company’s current expectations and projections about its future results. These forward-looking statements may include statements regarding perceived merit of properties, exploration results and budgets, mineral reserve and resource estimates, work programs, capital expenditures, timelines, strategic plans, market prices for precious and base metal, or other statements that are not statements of fact. When used in this news release, words such as “estimate,” “intend,” “expect,” “anticipate,” “will”, “believe”, “potential”, “go forward” and similar expressions are intended to identify forward-looking statements, which, by their very nature, are not guarantees of the Company’s future operational or financial performance, and are subject to risks and uncertainties and other factors that could cause the Company’s actual results, performance, prospects or opportunities to differ materially from those expressed in, or implied by, these forward-looking statements. These risks, uncertainties and factors may include, but are not limited to: unavailability of financing, failure to identify commercially viable mineral reserves, fluctuations in the market valuation for commodities, difficulties in obtaining required approvals for the development of a mineral project, increased regulatory compliance costs, expectations of project funding by joint venture partners and other factors.
Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this news release or as of the date otherwise specifically indicated herein. Due to risks and uncertainties, including the risks and uncertainties identified in this news release, and other risk factors and forward-looking statements listed in the Company’s MD&A for the quarter ended June 30, 2022 (the “MD&A”) and the most recently filed Annual Information Form (the “AIF”) for the year ended December 31, 2021, actual events may differ materially from current expectations. More information about the Company, including the MD&A, the AIF and financial statements of the Company, is available on SEDAR at www.sedar.com and on the SEC’s EDGAR website at www.sec.gov.
North Vancouver, British Columbia–(Newsfile Corp. – September 15, 2022) – Lion One Metals Limited (TSXV: LIO) (OTCQX: LOMLF) (ASX: LLO) (“Lion One” or the “Company”) is pleased to announce the results from drillhole TUDDH-608 a direct follow-up to the TUG-141/TUDDH-601 high-grade zone discovery at its fully permitted Tuvatu Alkaline Gold Project in Fiji.
TUDDH-608 intersected:
19.60m at 21.16 g/t Au from 594.5-614.1m, which includes a zone of 16.20m at 25.28 g/t Au from 596.7-612.9m.
The dip of this hole at this depth was approximately 60° equating to a true horizontal width of 11.85m.
TUDDH-608 was drilled from surface at an azimuth of approximately N090°E, aimed at intersecting the TUG-141/TUDDH-601 high-grade zone at a high angle to determine the true width of the high-grade zone at this location.https://embed.fireplace.yahoo.com/embed?ctrl=Monalixa&m_id=monalixa&m_mode=document&site=sports&os=android&pageContext=%257B%2522wiki_topics%2522%253A%2522Lion%2522%252C%2522lmsid%2522%253A%2522a0V0W00000HOPDcUAP%2522%252C%2522revsp%2522%253A%2522newsfile_64%2522%252C%2522lpstaid%2522%253A%25229b04419e-750c-3224-9125-6febee8bd22b%2522%252C%2522pageContentType%2522%253A%2522story%2522%257D
Figure 1 show the trace of TUDDH-608 and its location relative to the current interpretation of the TUG-141/TUDDH-601 high-grade dilation zone, and indicates that TUDDH-608 intersected high-grade Au mineralization approximately 20m north of subvertical hole TUDDH-601, and 15m below the discovery hole TUG-141. The trace of the currently drilling TUG-147 drillhole, designed to intersect the high-grade mineralized zone an additional 90 to the north of TUDDH-608 is also shown on Figure 1. TUG-147 is expected to cross the target rocks in the next 7-10 days.
Figure 2 includes some photos of the mineralization intersected by hole TUDDH-608. All results >0.5 g/t Au are summarized below in Table 1.
Lion One Sr. Vice-President of Exploration Sergio Cattalani, stated “This is yet another exceptional set of results from the ongoing drilling of the high-grade zone defined by the previous drill holes TUG-141 and TUDDH-601. Our current interpretation of this portion of the 500 Zone feeder is that of a wide zone of dilation associated with the interplay of major structural corridors (UR1 and UR4) and the main lithological contact between monzonite and andesite that has the potential to extend for tens to hundreds of meters both vertically and along the NS direction. True widths exceeding 10m at the narrower apex of this dilational zone suggest a significant increase in gold ounces once this zone has been adequately drilled off, and this, independent of the rest of the extensive vertical 500 zone feeder that is known to exceed 1100m in vertical extent. We will continue to expand this critical zone of high-grade mineralization with ongoing drilling both from surface as well as from the underground decline.”
Figure 1: Oblique views looking N320° and down 45° (A) and looking N060° and down 20° (B) of a 100m thick horizontal slice of the UR1-UR4 high-grade mineralized zone. Yellow trace is the projected trace of TUG-147 (in progress).
Figures 2: Photos from TUDDH-608 drill core, as follows: A) 571.5m, 17.03 g/t Au; B) 601.9m, 23.21 g/t Au; C) 599.5m, 108.31 g/t Au; D) 606.5m, 54.54 g/t Au; E) 611.8m, 45.02 g/t Au; F) close-up of cut core from photo E showing VG.
Table 1: Drilling intervals for diamond drill hole TUDDH-608 returning >0.5 g/t Au (intervals > 3.0 g/t Au cutoff are shown in red, and intervals >9.0 g/t Au or longer than 1.2m are bolded).
Hole ID
From (m)
To (m)
Interval (m)
Grade (g/t Au)
TUDDH-608
38.0
38.6
0.6
1.03
263.8
264.4
0.6
0.71
285.1
285.7
0.6
0.69
493.6
493.9
0.3
3.07
503.2
510.0
6.8
2.45
Incl.
506.7
507.3
0.6
10.49
511.2
515.7
4.5
1.45
517.8
518.1
0.3
1.08
519.3
523.2
3.9
1.49
557.1
557.7
0.6
9.08
Incl.
557.1
557.4
0.3
11.64
Incl.
557.4
557.7
0.3
6.51
559.2
559.8
0.6
3.02
571.4
572.6
1.2
9.41
Incl.
571.4
572.6
0.6
17.02
576.5
577.4
0.9
0.51
594.5
618.2
19.6
21.16
Incl.
596.7
597.9
1.2
85.09
Incl.
597.9
598.6
0.7
9.42
Incl.
598.6
598.9
0.3
8.38
Incl.
598.9
599.2
0.3
11.44
Incl.
599.2
599.5
0.3
6.98
Incl.
599.5
599.8
0.3
36.39
Incl.
599.8
600.4
0.6
108.31
Incl.
600.4
600.7
0.3
21.69
Incl.
600.7
601.7
1.0
13.54
Incl.
601.7
602.2
0.5
23.39
Incl.
602.2
602.5
0.3
0.72
Incl.
602.5
603.1
0.6
80.01
Incl.
603.1
603.7
0.6
7.05
Incl.
603.7
604.0
0.3
11.97
Incl.
604.0
604.6
0.6
3.09
Incl.
604.6
605.2
0.6
2.93
Incl.
605.2
606.0
0.8
1.41
Incl.
606.0
606.6
0.6
54.53
Incl.
606.6
607.2
0.6
11.99
Incl.
607.2
607.8
0.6
8.30
Incl.
607.8
608.4
0.6
29.56
Incl.
608.4
609.3
0.9
1.34
Incl.
609.3
609.6
0.3
24.31
609.6
610.2
0.6
2.61
Incl.
610.2
610.8
0.6
10.85
Incl.
610.8
611.1
0.3
7.54
611.1
611.4
0.3
2.90
Incl.
611.4
612.1
0.7
45.02
Incl.
612.1
612.9
0.8
13.31
612.9
613.8
0.9
0.54
613.8
614.1
0.3
1.87
616.1
618.2
2.1
4.25
Incl.
616.1
616.7
0.6
11.72
670.2
670.5
0.3
0.97
Table 2: Survey details of diamond drill holes referenced in this release. Previously released drill holes are not included here.
Hole No
Coordinates (Fiji map grid)
RL
final depth
dip
azimuth
N
E
m
(TN)
TUDDH-608
1876280
3920472
286.51
678.1
-64
089
TUG-147
1876435
3920584
116
in progress
-75
099
Qualified Person
In accordance with National Instrument 43-101 – Standards of Disclosure for Mineral Projects (“NI 43-101”), Sergio Cattalani, P.Geo, Senior Vice President Exploration, is the Qualified Person for the Company and has reviewed and is responsible for the technical and scientific content of this news release.
QAQC Procedures
Lion One adheres to rigorous QAQC procedures above and beyond basic regulatory guidelines in conducting its sampling, drilling, testing, and analyses. The Company utilizes its own fleet of diamond drill rigs, using PQ, HQ and NQ sized drill core rods. Drill core is logged and split by Lion One personnel on site. Samples are delivered to and analysed at the Company’s geochemical and metallurgical laboratory in Fiji. Duplicates of all samples with grades above 0.5 g/t Au are both re-assayed at Lion One’s lab and delivered to ALS Global Laboratories in Australia (ALS) for check assay determinations. All samples for all high-grade intercepts are sent to ALS for check assays. All samples are pulverized to 80% passing through 75 microns. Gold analysis is carried out using fire assay with an AA finish. Samples that have returned grades greater than 10.00 g/t Au are then re-analysed by gravimetric method. For samples that return greater than 0.50 g/t Au, repeat fire assay runs are carried out and repeated until a result is obtained that is within 10% of the original fire assay run. For samples with multiple fire assay runs, the average of duplicate runs is presented. Lion One’s laboratory can also assay for a range of 71 other elements through Inductively Coupled Plasma Optical Emission Spectrometry (ICP-OES), but currently focuses on a suite of 9 important pathfinder elements. All duplicate anomalous samples are sent to ALS labs in Townsville QLD and are analysed by the same methods (Au-AA26, and Au-GRA22 where applicable). ALS also analyses for 33 pathfinder elements by HF-HNO3-HClO4 acid digestion, HCl leach and ICP-AES (method ME-ICP61).
About Lion One Metals Limited
Lion One’s flagship asset is 100% owned, fully permitted high grade Tuvatu Alkaline Gold Project, located on the island of Viti Levu in Fiji. Lion One envisions a low-cost high-grade underground gold mining operation at Tuvatu coupled with exciting exploration upside inside its tenements covering the entire Navilawa Caldera, an underexplored yet highly prospective 7km diameter alkaline gold system. Lion One’s CEO Walter Berukoff leads an experienced team of explorers and mine builders and has owned or operated over 20 mines in 7 countries. As the founder and former CEO of Miramar Mines, Northern Orion, and La Mancha Resources, Walter is credited with building over $3 billion of value for shareholders.
On behalf of the Board of Directors of Lion One Metals Limited “Walter Berukoff“ Chairman and CEO
Neither the TSX Venture Exchange nor its Regulation Service Provider accepts responsibility for the adequacy or accuracy of this release.
This press release may contain statements that may be deemed to be “forward-looking statements” within the meaning of applicable Canadian securities legislation. All statements, other than statements of historical fact, included herein are forward looking information. Generally, forward-looking information may be identified by the use of forward-looking terminology such as “plans”, “expects” or “does not expect”, “proposed”, “is expected”, “budget”, “scheduled”, “estimates”, “forecasts”, “intends”, “anticipates” or “does not anticipate”, or “believes”, or variations of such words and phrases, or by the use of words or phrases which state that certain actions, events or results may, could, would, or might occur or be achieved. This forward-looking information reflects Lion One Metals Limited’s current beliefs and is based on information currently available to Lion One Metals Limited and on assumptions Lion One Metals Limited believes are reasonable. These assumptions include, but are not limited to, the actual results of exploration projects being equivalent to or better than estimated results in technical reports, assessment reports, and other geological reports or prior exploration results. Forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause the actual results, level of activity, performance or achievements of Lion One Metals Limited or its subsidiaries to be materially different from those expressed or implied by such forward-looking information. Such risks and other factors may include, but are not limited to: the stage development of Lion One Metals Limited, general business, economic, competitive, political and social uncertainties; the actual results of current research and development or operational activities; competition; uncertainty as to patent applications and intellectual property rights; product liability and lack of insurance; delay or failure to receive board or regulatory approvals; changes in legislation, including environmental legislation, affecting mining, timing and availability of external financing on acceptable terms; not realizing on the potential benefits of technology; conclusions of economic evaluations; and lack of qualified, skilled labour or loss of key individuals. Although Lion One Metals Limited has attempted to identify important factors that could cause actual results to differ materially from those contained in forward-looking information, there may be other factors that cause results not to be as anticipated, estimated or intended. Accordingly, readers should not place undue reliance on forward-looking information. Lion One Metals Limited does not undertake to update any forward-looking information, except in accordance with applicable securities laws.
VANCOUVER, British Columbia, Sept. 14, 2022 (GLOBE NEWSWIRE) — Rover Metals Corp. (TSXV: ROVR) (OTCQB: ROVMF) (FSE:4XO) (“Rover” or the “Company”) announces that further to its release of August 16, 2022, the Company has signed a definitive option agreement (the “Option Agreement”) with Panarc Resources Ltd. (“Panarc”) for the staged acquisition of up to a 90% ownership interest in the Indian Mountain Lake VMS project, NT, Canada (the “Project”).
Indian Mountain Lake VMS Project The Indian Mountain Lake VMS Project has had exploration dating back to the 1940s and has a historical resource spread across four zones on the project. The BB Zone and Kennedy Lake Zone have a combined historic resource of 1,400,000 tons grading 10% combined zinc and lead with 3.5 OPT (ounces per ton) of silver*. Approximately 900 metres west of the BB Zone, the Kennedy Lake West Zone has a historic resource of 610,000 tons grading 1.15% copper*. About 8 km southeast of the BB Zone, the Susu Lake Zone, has a historical resource consisting of 142,500 tons grading 0.95% copper*.
The property is located approximately 195 km east-northeast of Yellowknife, NT, off the eastern arm of Great Slave Lake. Seasonal access relies upon fixed or rotor wing support. A right of way was cleared to the Project from Thompson Landing in the 1970s. If this right of way were to be brushed out, it would provide barge access at Thompson Landing, from Yellowknife, with ground transportation, considerably lowering any logistical costs. Future Government of Canada federally funded hydro-energy infrastructure could come close to the Project if the Taltson Hydro Dam expansion proceeds through the eastern arm of Great Slave Lake into Yellowknife. At the southwest-end of Great Slave Lake, Osisko Metals is gearing up to reopen the Pine Point Zinc-Lead Mine. At nearby Hay River, NT, there is a rail line to the Teck Resources Zinc Refinery in Trail, BC.
*These resources are historic in nature. Further drilling is needed to bring them up to CIM Definition Standards. The historic data has not been verified by Rover. The historic information is provided in the 2103 Assessment Report for Indian Mountain Lake which is in public record with the Government of the Northwest Territories.
Technical information has been approved by Gary Vivian, M.Sc., P.Geo., QP for the purposes of NI 43-101.
Summary of the First Year Terms of the Indian Mountain Lake Definitive Option Agreement In accordance with the terms of the Option Agreement, during the first year following the date of the Option Agreement, the Company has committed to incurring $200,000 in exploration expenditures on the Project and making a cash payment of $20,000 to Panarc. In addition, and subject to the approval by the TSX Venture Exchange, Rover will issue Panarc an aggregate of 3,500,000 common shares in the capital of the Company (the “Common Shares”) within six months of the signing of the Option Agreement. The Common Shares, if authorized for issuance, will be subject to the standard four-month regulatory hold period.
Upcoming Conference Rover Metals will be presenting at the Redefining Electric Metals Conference in Calgary, AB, on September 19th and 20th. Registration is at www.redefiningelectricalmetals.com
Judson Culter, CEO at Rover Metals, states “We see tremendous growth coming for critical minerals fueled by domestic EV demand in the U.S. and Canada. 97% of the Indian Mountain Lake greenstone belt, or approximately 30,000 acres, remains largely unexplored with the drill bit, so we are very excited about this project’s future.”
Corporate Update A Q&A interview with Rover’s CEO, Judson Culter, is now also available for viewing here.
About Rover Metals Rover is a publicly traded junior mining company that trades on the TSXV under symbol ROVR, on the OTCQB under symbol ROVMF, and on the FSE under symbol 4XO. The Company is now developing both: (1) critical minerals projects; as well as (2) precious metals projects. The Company is exclusive to the mining jurisdictions of Canada and the U.S. Five of the Company’s mineral resource development projects are located near to the city of Yellowknife, 60th parallel, Canada.
ON BEHALF OF THE BOARD OF DIRECTORS “Judson Culter” Chief Executive Officer and Director
For further information, please contact: Email: info@rovermetals.com Phone: +1 (778) 754-2617
Statement Regarding Forward-Looking Information This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause Rover’s actual results, performance or achievements, or developments in the industry to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur. There can be no assurance that such statements prove to be accurate. Actual results and future events could differ materially from those anticipated in such statements, and readers are cautioned not to place undue reliance on these forward-looking statements. Any factor could cause actual results to differ materially from Rover’s expectations. Rover undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.
THE FORWARD-LOOKING INFORMATION CONTAINED IN THIS NEWS RELEASE REPRESENTS THE EXPECTATIONS OF THE COMPANY AS OF THE DATE OF THIS NEWS RELEASE AND, ACCORDINGLY, IS SUBJECT TO CHANGE AFTER SUCH DATE. READERS SHOULD NOT PLACE UNDUE IMPORTANCE ON FORWARD-LOOKING INFORMATION AND SHOULD NOT RELY UPON THIS INFORMATION AS OF ANY OTHER DATE. WHILE THE COMPANY MAY ELECT TO, IT DOES NOT UNDERTAKE TO UPDATE THIS INFORMATION AT ANY PARTICULAR TIME EXCEPT AS REQUIRED IN ACCORDANCE WITH APPLICABLE LAWS.
NEITHER THE TSX VENTURE EXCHANGE NOR ITS REGULATION PROVIDER (AS THAT TERM IS DEFINED IN THE POLICIES OF THE TSX VENTURE EXCHANGE) ACCEPTS RESPONSIBILITY FOR THE ADEQUACY OF THIS RELEASE.
Vancouver, British Columbia–(Newsfile Corp. – September 13, 2022) – Riverside Resources Inc.(TSXV: RRI) (OTCQB: RVSDF) (FSE: 5YY) (“Riverside” or the “Company”) is pleased to report assay results for the remaining 7 drillholes of its twelve-hole, 1700-meter diamond drill program completed at the Oakes Gold Project (the “Project”) in northwestern Ontario, Canada. The primary focus of the first drill program at Oakes was to test the ‘HG’ Target identified by geophysics and trenching programs for gold grades and continuity. The results came back favorable with hole 22-11 returning 5 intervals of gold over a total interval of 55 meters and hole 22-06 returning 4m @ 1.7 g/t Au. The Induced Polarization (IP) work conducted by Riverside in the summer of 2021 showed the HG IP Target extended westward beyond the area of trenching and sampling. Drilling this year has now confirmed the gold continuity of over 1.2 kilometer strike, hitting the mineralized structure and further open in both east and west. The drill results announced here fit with the orogenic gold model and further drilling can be progressed with confidence as all the holes of this program were shallow, with intercepts at less than 120m for most cases, while the system is wide open at depth.
This drill campaign has now successfully expanded the known gold mineralization well beyond the outcrops and laid the groundwork for the next drill campaign to continue expanding the Oakes gold camp. IP data provided strong conductivity and complimentary resistivity anomaly trending roughly east-west parallel to the geological units with greater confidence. The 7 holes announced here intercepted favorable geology of metavolcanics, “greenstone”, consistent with the geology noted in the first five holes and further geological constraints. As this part of Oakes has never been drilled, the first drill program comprised of shallow holes with the intent of intercepting the target at 100 m vertical below surface. The mineralized zone on surface is known to pinch and swell and averages about 5 m in width. The best hole in the second batch of reporting was DDH-22-06 which returned 1.7 g/t over 4 m with one sample being almost 5 g/t gold. The best intercept in the program was 8.4 g/t over 1 m in Hole #2.
Table 1: Spring 2022 Drill Program Highlights at Oakes (holes 6-12)
Hole No.
from (m)
to (m)
length (m)
Au (g/t)
OAKES-22-06
72
76
4
1.7
including
72
73
1
4.9
OAKES-22-06
85
88
3
1.0
OAKES-22-07
98
100
2
0.9
OAKES-22-08
9
10.5
1.5
0.4
OAKES-22-09
18
18.5
0.5
1.0
OAKES-22-11
22
23
1
2.2
OAKES-22-11
96.5
98
1.5
1.0
OAKES-22-11
113.5
115
1.5
1.1
OAKES-22-11
125.5
127
1.5
2.3
OAKES-22-11
151
152
1
0.9
OAKES-22-12
106.5
108
1.5
2.4
OAKES-22-12
130
131
1
0.4
All samples comprised half-core, saw-cut samples with QA/QC described below and further at www.rivres.com. Samples are generally considered to be 90-95% to true width.https://embed.fireplace.yahoo.com/embed?ctrl=Monalixa&m_id=monalixa&m_mode=document&site=sports&os=android&pageContext=%257B%2522ctopid%2522%253A%25221542500%253B1577000%2522%252C%2522hashtag%2522%253A%25221542500%253B1577000%2522%252C%2522wiki_topics%2522%253A%2522Target_Corporation%253BDrill%253BTom%25C3%25A1%25C5%25A1_Hole%25C5%25A1%253BDrilling%253BCompany%2522%252C%2522lmsid%2522%253A%2522a0V0W00000HOPDcUAP%2522%252C%2522revsp%2522%253A%2522newsfile_64%2522%252C%2522lpstaid%2522%253A%25220b3e363e-27c8-3807-828c-310b2cededf8%2522%252C%2522pageContentType%2522%253A%2522story%2522%257D
Technical Interpretations & Observations
DDH-22-06 & 07 were designed to intercept the HG Zone beneath Trench 1 at about 100 m depth. The target zone comprises strongly foliated, fine grained, metavolcanic rocks showing strong silicified zones with narrow bleached sections. Alteration comprises abundant biotite and chlorite bands, the top of the unit shows quartz veining with semi-massive pyrite-pyrrhotite and trace chalcopyrite which generally described the mineralized environment at Oakes. Quartz carbonate veinlets and stringers are more frequent from 80 m to 110 m down the hole consistent with the drill target gold bearing area. The overall 25-30m mineralization halo and main zone which is near vertical, now demonstrates strong consistency and provides the Company confidence of a significant gold system at Oakes. DDH-22-08 hit a fault and could not reach the target. DDH-22-09 was the setback collared to drill the Brinklow IP anomaly south of HG Zone, while DDH-22-10 was collared on the Crib Road with the intent to test the IP anomaly associated with the metasediment/metavolcanic contact boundary mapped at this location. Holes 8, 9 and 10 were not intended to evaluate the HG target and were instead testing parallel features. Holes 6, 7, 11, 12 provide technical data specific to the HG trend and give positive results for further exploration at Oakes which lies 25 km east of the Hard Rock Mine currently being constructed by Greenstone Gold (Equinox Gold) with a Proven & Probable Reserves of 5.5Moz at 1.27 g/t Au.[1]
Figure 1: Collars and projected drill holes for 12 holes plotted on IP Chargeability Map
DDH-22-11 was targeting an IP conductivity anomaly associated with the HG Zone on trend with the mineralization defined on surface (and in drill core) at Hole 6 located 600 m to the east along what is believed to be the same structure. Assays returned gold results associated with veining throughout the hole and as high as 2.3 g/t gold. Hole 11 was collared in metasedimentary rocks and drilled northward into metavolcanic rocks. Bedding and the contact between the two units was measured at 50 degrees to the core axis whereas foliation and shearing is at about 45 degrees. Alteration comprises moderately to strong biotitic and weak to strong chlorite zones sometimes associated with carbonate zones. Quartz veining and silica content increases starting at 80 m downhole. Sulphides are associated with quartz veins and comprise 2-5% disseminated Pyrite-Pyrrhotite seen within local fracture fillings and stringers.
Figure 2: Interpreted North – South Cross Section DDH-22-11 demonstrating the progression from brittle down into brittle-ductiledeformation as the targeting model having found gold over 55m drill width zone in hole 11
DDH-22-12 was collared in gabbro and drilled north through metasedimentary rock into metavolcanics. Mineralization is noted within similar altered rock but only within shears in the mafic volcanics and does not appear to be associated with the contact zones. Sheared zones commonly a focus for gold mineralization in orogenic systems like this one are expressed as altered, fine-grained, metavolcanics with moderate to strong chlorite-biotite alteration with quartz-carbonate veins and stringers with 1-2% disseminated pyrite and pyrrhotite.
Conclusions
The HG Zone at Oakes has been proven to extend well beyond the strike extent defined by trenching and has now been drill proven to at least 1.1 km in length. To date the drilling has only tested the upper 100 m of the structure where mineralization appears associated with quartz veins that show visible gold within pyrite rich veins. The gold mineralization is associated with quartz and quartz-carbonate veins in shear zones within metavolcanic rocks often (near-vertical which can bode well for potential future mining and predicting the next round of drilling). Quartz veins that are subparallel to foliation appear to be the veins that carry gold and are cut by later quartz carbonate veins that do not have sulfides. The quartz veins are mostly associated with brittle type fracturing with lesser semi-ductile type, potentially indicating that drilling was approaching the upper brittle-ductile transition which can be highly favorable in large orogenic gold deposits. The nature of the fracturing suggests that the shallow drilling is primarily within the upper brittle deformation zone as shown in Figure 2. The fact that the gold veins can now be traced in drill holes more than 3x beyond the previous surface trenching expands the Oakes project potential greatly.
The Oakes property is located along the general metallogenic boundary of the Wabigoon and Quetico sub-provinces and this boundary is commonly a major fault breaks, and large gold resources are associated with these breaks generally in secondary shear zones in the Canadian shield geologic provinces. The Hemlo Gold Mine to the south is hosted in a brittle fracture environment and the Black Fox gold mine to the east in Matheson is hosted in a semi-ductile fracture system at depth and more brittle near the surface. Riverside sees the potential for brittle fracture zones progress into semi ductile and ductile zones at depth in general becoming wider and potentially richer as has commonly been found and further drilling is warranted.
Riverside’s President and CEO, John-Mark Staude:“Riverside has expanded the gold zone at Oakes along strike over 1 km and begun showing the continuity on surface and to depth, consistent with the goals for the 2022 drill program. Next steps will include more geophysics to map the structural features to trace the HG Zone and gold mineralization. We are very encouraged by these good results covered in this and the prior news release and are pleased to see how effective the geophysical surveys were at finding mineralization and predicting extensions. Moreover, we remain very cautiously optimistic to see our first program of shallow drilling demonstrate continuity of mineralization along strike and at depth. Riverside continues to pursue the Prospect Generator hybrid model, by providing shareholders with the upside for discovery on multiple projects, and with different partners, along with the current self-funded value adding project.”
Qualified Person & QA/QC: As part of the quality control Riverside inserted blanks, duplicates and two different standards, into the sample stream prior to delivery at Activation Laboratories in Thunder Bay. Logged core was delivered from site to a core cutting facility in Thunder Bay by Riverside and trucked to Activation Laboratories from this facility typically in batches of 2 to 4 holes at a time. Multi-Element Analysis using Aqua Regia Extraction and (40 element) Inductively Coupled Plasma Atomic Emission Spectrometry Analytical and fire assay for gold methods where used. Activation Laboratories is an ISO/IEC accredited laboratory.
The scientific and technical data contained in this news release was reviewed and approved by Freeman Smith, P.Geo., a non-independent qualified person to Riverside Resources, who is responsible for ensuring that the geologic information provided within this news release is accurate and who acts as a “qualified person” under National Instrument 43-101 Standards of Disclosure for Mineral Projects.
About Riverside Resources Inc.: Riverside is a well-funded exploration company driven by value generation and discovery. The Company has over $4M in cash, no debt and less than 80M shares outstanding with a strong portfolio of gold-silver and copper assets and royalties in North America. Riverside has extensive experience and knowledge operating in Mexico and Canada and leverages its large database to generate a portfolio of prospective mineral properties. In addition to Riverside’s own exploration spending, the Company also strives to diversify risk by securing joint-venture and spin-out partnerships to advance multiple assets simultaneously and create more chances for discovery. Riverside has properties available for option, with information available on the Company’s website at www.rivres.com.
ON BEHALF OF RIVERSIDE RESOURCES INC.
“John-Mark Staude”
Dr. John-Mark Staude, President & CEO
For additional information contact:
John-Mark Staude President, CEO Riverside Resources Inc. info@rivres.com Phone: (778) 327-6671 Fax: (778) 327-6675 Web: www.rivres.com
Certain statements in this press release may be considered forward-looking information. These statements can be identified by the use of forward-looking terminology (e.g., “expect”,” estimates”, “intends”, “anticipates”, “believes”, “plans”). Such information involves known and unknown risks — including the availability of funds, the results of financing and exploration activities, the interpretation of exploration results and other geological data, or unanticipated costs and expenses and other risks identified by Riverside in its public securities filings that may cause actual events to differ materially from current expectations. Readers are cautioned not to place undue reliance on these forward-looking statements, which speak only as of the date of this press release.
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.
Vancouver, British Columbia–(Newsfile Corp. – September 13, 2022) – Dolly Varden Silver Corporation (TSXV: DV) (OTCQX: DOLLF) (the “Company” or “Dolly Varden“) is pleased to announce results from drilling at the Wolf Vein, including step-out hole DV22-300 which returned a significant, high-grade silver intercept. Based on the grade and strength of the mineralizing system, the Company has prioritized continued step-out drilling at Wolf during for the remainder of the 2022 season.
DV22-300 encountered a wide interval of multi-phase veins and breccia, intersecting 19.85m (13.90m true width) averaging 584 g/t Ag, 0.92 %Pb, 0.56% Zn and 0.19 g/t Au, with bonanza grade silver mineralization grading 4,326 g/t Ag, 4.21% Pb, 1.36% Zn and 1.00 g/t Au over 1.60m (1.12m true width) within a sulphide and silver sulphosalt matrix vein breccia in the main veined interval.
Figure 1. Kitsault Valley trend and mineral deposits
To view an enhanced version of this graphic, please visit: https://images.newsfilecorp.com/files/1728/136919_ad8a8710944e89e1_002full.jpghttps://embed.fireplace.yahoo.com/embed?ctrl=Monalixa&m_id=monalixa&m_mode=document&site=sports&os=android&pageContext=%257B%2522ctopid%2522%253A%25221542500%253B1480989%253B1481489%2522%252C%2522hashtag%2522%253A%25221542500%253B1480989%253B1481489%2522%252C%2522wiki_topics%2522%253A%2522Company%253BBreccia%253BDrilling%2522%252C%2522lmsid%2522%253A%2522a0V0W00000HOPDcUAP%2522%252C%2522revsp%2522%253A%2522newsfile_64%2522%252C%2522lpstaid%2522%253A%2522edcf1f2a-bcfa-39ba-b8d2-b5dc80848c6b%2522%252C%2522pageContentType%2522%253A%2522story%2522%257D
“With an increase in vein intensity and silver grades, the Wolf Vein area is emerging as a large system, rivaling our Torbrit Deposit. With an established plunge length of over 500 meters from the historic underground workings, we are continuing to step out along this trend towards the Kitsol Vein, where we recently announced similar, high-grade mineralization over 1,400 meters away. The increasing gold and base metal content, in addition to the silver, is highly encouraging, as well as the significant widths that are potentially amenable to bulk underground mining techniques,” said Shawn Khunkhun, President and CEO of Dolly Varden Silver.
The mineralized interval in DV22-300 is a southwesterly step-out along strike and down dip from DV21-273, which returned 17.50m averaging 214 g/t Ag and 0.47% Pb including 1.22 m averaging 1,532 g/t Ag, 0.44 g/t Au, 2.11 % Pb and 1.07% Zn (see Dolly Varden news release, December 20, 2021) and projects as a mineralized shoot over 55m down plunge from DV21-273. High-grade silver in DV22-300 occurs within a very strong, multiphase vein and breccia system that also includes significant gold and base metal mineralization.
The strength of the mineralizing system, as well as silver and potentially gold appears to be increasing at depth and to the southwest; assays are pending for DV22-316, which encountered strong veining, alteration, brecciation and one occurrence of visible gold over 200m away from DV22-300 (see Figure 2). All of these drill holes tested below the Upper Hazelton sediment cap with associated strong potassic alteration; this trend continues south for 1,400 m to the Kitsol Vein (see Figure 1).
Figure 3. Geological Cross Section of Wolf Vein. 25 meter window width looking northwest. DV22-194 is same dip as DV22-300 approximately 30m off section.
The Wolf Vein is a steep dipping, high-grade silver vein deposit that is part of the current Mineral Resource Estimate at Dolly Varden’s Kitsault Valley trend. In 2021, geological modelling of the deposit showed expansion potential along strike to the southwest below the sediment cap that masks surface expression of the vein mineralization and associated alteration. With the discovery that the system continued to the southwest over 8,000m of follow up drilling has been completed thus far during the 2022 exploration program. This drilling has defined high grade silver mineralization to a depth of 500m below surface and extended the zone over 350m down plunge from historic drilling and over 500m from the historic underground workings.
Results have been received for the first six exploration drill holes testing the Wolf Vein extension. All holes were drilled from the same pad with varying azimuths and dips (see Table 2). These drill holes tested below the Upper Hazelton sediment cap and have encountered a robust, multi-phase vein and breccia mineralizing system that remains wide open along strike to the south and down dip. The associated strong potassic alteration, a key indicator for silver mineralization at the Kitsault Valley Project, continues below the sediment cap and south for 1,400m to the Kitsol Vein. All holes drilled during 2022, except DV22-280, intersected the extension of the Wolf Vein, suggesting a plunge at approximately 45 degrees to the southwest. DV22-280 came out of the sediment cap into the footwall of the vein. Drill hole DV22-281- intersected impressive base metal values in addition to silver: 3.75m (2.43m true width) averaging 170 g/t Ag,6.25% Pb, 14.12% Zn. In drill holes that hit the Wolf vein outside of the interpreted plunge of the high-grade silver zone, significant lead and zinc intervals are present.
Mineralization at the Wolf Vein consists of multiple epithermal silica vein and brecciation events along a NE trending, steeply NW dipping zone (Figures 4 and 5). Silver mineralization includes: silver sulphosalts, tennantite, argentite and argentiferous galena hosted in vein and vein breccia mineralization.
Figure 4. DV22-300 mineralized interval of multi-phase quartz vein and vein breccias
*AgEq was calculated using $US1650/oz Au, $US20/oz Ag, $US0.90/lb Pb and $US1.10/lb Zn
Table 2. Drill hole collar locations and orientations
Hole ID
Easting UTM83 (m)
Northing UTM83 (m)
Elev. (m)
Azimuth
Dip
Length (m)
DV22280
467089
6173630
388
120
-45
392.00
DV22281
467089
6173630
388
120
-65
495.00
DV22285
467089
6173630
388
120
-70
573.00
DV22288
467089
6173630
388
120
-73
720.00
DV22294
467089
6173630
388
110
-60
423.00
DV22300
467089
6173630
388
129
-60
396.00
Quality Assurance and Quality Control
The Company adheres to CIM Best Practices Guidelines for exploration related activities conducted on its property. Quality Assurance and Quality Control (QA/QC) procedures are overseen by the Qualified Person.
Dolly Varden QA/QC protocols are maintained through the insertion of certified reference material (standards), blanks and field duplicates within the sample stream. Drill core is cut in-half with a diamond saw, with one-half placed in sealed bags and shipped to the laboratory and the other half retained on site. Third party laboratory checks on 5% of the samples are carried out as well. Chain of custody is maintained from the drill to the submittal into the laboratory preparation facility.
Analytical testing was performed by ALS Canada Ltd. in North Vancouver, British Columbia. The entire sample is crushed and a 500 gram split is pulverized to minus 200mesh. Multi-element analyses were determined by Inductively-Coupled Plasma Mass Spectrometry (ICP-MS) for 48 elements following a 4-acid digestion process. High grade silver testing was determined by Fire Assay with either an atomic absorption, or a gravimetric finish, depending on grade range. Au is determined by Fire Assay on a 30g split.
Qualified Person
Rob van Egmond, P.Geo. Vice-President Exploration for Dolly Varden Silver, the “Qualified Person” as defined by NI43-101 has reviewed, validated and approved the scientific and technical information contained in this news release and supervises the ongoing exploration program at the Dolly Varden Project.
About Dolly Varden Silver Corporation
Dolly Varden Silver Corporation is a mineral exploration company focused on advancing its 100% held Kitsault Valley Project (which combines the Dolly Varden Project and the Homestake Ridge Project) located in the Golden Triangle of British Columbia, Canada, 25kms by road to tide water. The 163 sq. km. project hosts the high-grade silver and gold resources of Dolly Varden and Homestake Ridge along with the past producing Dolly Varden and Torbrit silver mines. It is considered to be prospective for hosting further precious metal deposits, being on the same structural and stratigraphic belts that host numerous other, on-trend, high-grade deposits, such as Eskay Creek and Brucejack. The Kitsault Valley Project also contains the Big Bulk property which is prospective for porphyry and skarn style copper and gold mineralization, similar to other such deposits in the region (Red Mountain, KSM, Red Chris).
Forward Looking Statements
This release may contain forward-looking statements or forward-looking information under applicable Canadian securities legislation that may not be based on historical fact, including, without limitation, statements containing the words “believe”, “may”, “plan”, “will”, “estimate”, “continue”, “anticipate”, “intend”, “expect”, “potential”, and similar expressions. Forward-looking statements involve known and unknown risks, uncertainties, and other factors which may cause the actual results, performance, or achievements of Dolly Varden to be materially different from any future results, performance, or achievements expressed or implied by the forward-looking statements. Forward looking statements or information in this release relates to, among other things, the 2022 drill program at the Kitsault Valley Project, the results of previous field work and programs and the continued operations of the current exploration program, interpretation of the nature of the mineralization at the project and that that the mineralization on the project is similar to Eskay and Brucejack, results of the mineral resource estimate on the project, the potential to grow the project, the potential to expand the mineralization and our beliefs about the unexplored portion of the property.
These forward-looking statements are based on management’s current expectations and beliefs and assume, among other things, the ability of the Company to successfully pursue its current development plans, that future sources of funding will be available to the company, that relevant commodity prices will remain at levels that are economically viable for the Company and that the Company will receive relevant permits in a timely manner in order to enable its operations, but given the uncertainties, assumptions and risks, readers are cautioned not to place undue reliance on such forward-looking statements or information. The Company disclaims any obligation to update, or to publicly announce, any such statements, events or developments except as required by law.
For additional information on risks and uncertainties, see the Company’s most recently filed annual management discussion & analysis (“MD&A“) and management information circular dated January 21, 2022 (the “Circular“), both of which are available on SEDAR at www.sedar.com. The risk factors identified in the MD&A and the Circular are not intended to represent a complete list of factors that could affect the Company.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX-V) accepts responsibility for the adequacy or accuracy of this news release.
Plan View of the Guayabales Project Highlighting the Apollo Target
Figure 2
Plan View of the Apollo Target Area Outlining the Porphyry and Breccia Targets, their Related Soil Anomalies and Drill Holes Completed or Currently Underway
Figure 3
Plan View with Traces of Drill Holes Completed to Date in the Main Breccia Discovery at Apollo with Current Holes, APC-6 & APC-8 in Red
Figure 4
Apollo Target Cross Section with Core Photo Highlights for APC-8
APC-8 intersected a broad, high-grade zone of breccia mineralization with multiple, overprinting carbonate base metal veins and returned:
APC-6 also intersected the main breccia zone with some interfingering, mineralized rock flour breccia towards the northern end of the hole resulting in a broad interval as follows:
As a result of the new drill holes reported today, the maximum dimensions of the Main Breccia have increased to 350 metres along strike by 100 metres across by 500 metres depth (prior dimensions were 300m x 100m x 400m) and remains open in all directions.
Drill holes APC-12, APC-13 and APC-14 are now complete at Apollo with the following visual observations from logging:
APC-12 and APC-14 intercepted the Main Breccia zone with both holes cutting more than 230 metres of potentially favourable mineralization; APC-13 unfortunately failed before reaching the Main Breccia zone but cut a narrow zone of sheeted veins at a shallow elevation.
TORONTO, Sept. 13, 2022 (GLOBE NEWSWIRE) — Collective Mining Ltd. (TSXV: CNL) (OTCQX: CNLMF) (“Collective” or the “Company”) is pleased to announce assay results from two additional holes completed at the Apollo target (“Apollo”) within the Company’s Guayabales project located in Caldas, Colombia. Apollo is a newly discovered high-grade copper-gold-silver porphyry-related breccia with previously announced intercepts including the discovery hole APC-2, which intersected 207.15 metres @ 2.68 g/t AuEq and APC-3, which intersected 180.60 metres @ 2.43 g/t AuEq. (See press releases dated August 10th and 29th respectively). As part of its fully funded 20,000+ metre drill program for 2022, there are currently three diamond drill rigs operating at the Apollo target with an additional rig drilling from underground at the Olympus target.
“Apollo continues to deliver continuous, broad, and consistent zones of well mineralized breccia with overall grades being enhanced by the overprinting, high-grade carbonate base metal veins. Importantly, this remarkable copper-silver-gold discovery continues to grow materially in tonnage as we continue with aggressive step-out drilling in multiple directions. We will remain aggressive for the balance of 2022 and look forward to receiving additional assay results in the near term,” commented Ari Sussman, Executive Chairman.
Details (See Table 1 and Figures 1 – 4)
Seven diamond drill holes with accompanying assay results have now been announced at Apollo and based on results, the Main Breccia at Apollo has expanded and now measures up to 350 metres along strike by 100 metres across by 500 metres vertical. The target remains open in all directions and has the potential to evolve into a significant high-grade, bulk tonnage mineralized system.
Drill holes APC-6 and APC-8 were drilled in opposite directions from two separate drill pads (Pads 3 and 2) to the northeast and southwest respectively and were designed to test the depth and strike continuity of the mineralized breccia previously intersected in holes APC-1, APC-1W, APC-2, APC-3 and APC-5. The following results are highlighted:
APC-6: 326.05 metres @ 1.07 g/t AuEq from 364.60 metres (295 metres vertical) including: 151.5 metres @ 1.20 g/t AuEq from 480.15 metres down hole, and 10.55 metres @ 4.64 g/t AuEq from 680.10 metres down hole.
APC-6 is the deepest diamond hole drilled to date and this long intercept consisted primarily of favorable angular breccia with interfingering of rock flour breccia, which is less porous and therefore lower grade. APC-6 was collared from Pad 3 and terminated at a final depth of 759 metres.
APC-8: 265.75 metres @ 2.44 g/t AuEq from 202.00 metres (157 metres vertical) including: 13.20 metres @ 4.29 g/t AuEq from 202.0 metres down hole, 18.45 metres @ 4.55 g/t AuEq from 239.05 metres down hole, 28.45 metres @ 4.18 g/t AuEq from 279.40 metres down hole, and 15.50 metres @ 5.21 g/t AuEq from 342.6 metres downhole.
APC-8 intercepted continuous mineralized angular breccia with a sulphide matrix consisting of pyrite, chalcopyrite and pyrrhotite which has been overprinted by carbonate-base metal porphyry veins (“CBM”) hosting sphalerite in various locations and particularly in the upper portion of the intercept. The breccia clasts are all quartz diorite and diorite in composition and this hydrothermal system is clearly linked to a porphyry system. APC-8 was collared from Pad 2 and terminated at a final depth of 523 metres.
Four rigs continue to drill at the Guayabales project with assay results anticipated in the near term for three holes from Apollo with the following encouraging visual intercepts:
APC-12 and APC-14 tested the Main Breccia discovery at Apollo with both holes intersecting more than 230 metres of potentially favourable mineralization.
APC-13 ran into technical difficulties prior to reaching the Main Breccia but intersected a 15 metres zone of sheeted CBM veins at a shallow depth.
The Apollo target area, as defined to date by surface mapping, rock sampling and copper and molybdenum soil geochemistry, covers an 800 metre X 700 metre area. The Apollo target area hosts the Company’s new Main Breccia discovery plus a vein system located above and on the eastern flank of the Main Breccia discovery and the Northern Breccia discovery located 250 metres to the north of the Main Breccia. Multiple additional untested breccia, porphyry and vein targets have been generated and will be drilled in due course. The overall Apollo target area also remains open for further expansion.
Table 1: Assays Results
HoleID
From (m)
To (m)
Intercept (m)
Au (g/t)
Ag (g/t)
Cu %
Zn %
Pb %
Mo %
AuEq (g/t)*
APC-6
364.60
690.65
326.05
0.85
10
0.04
0.04
0.02
0.001
1.07
Incl
480.15
631.65
151.50
0.96
11
0.04
0.06
0.03
0.001
1.20
680.10
690.65
10.55
4.67
7
0.05
0.01
0.00
0.000
4.64
APC-8
202.00
467.75
265.75
1.26
55
0.22
0.07
0.05
0.045
2.44
Incl
202.00
215.20
13.20
3.68
27
0.03
0.32
0.24
0.238
4.29
239.05
257.50
18.45
3.48
53
0.12
0.24
0.22
0.216
4.55
279.40
307.85
28.45
3.70
24
0.16
0.03
0.02
0.016
4.18
342.60
358.10
15.50
2.15
158
0.47
0.13
0.10
0.104
5.21
*AuEq (g/t) is calculated as follows: (Au (g/t) x 0.95) + (Ag g/t x 0.014 x 0.95) + (Cu (%) x 1.96 x 0.95) + (Mo (%) x 7.35 x 0.95)+(Zn(%)x 0.86 x 0.95)+ (Pb(%)x 0.44 x 0.95) utilizing metal prices of Cu – US$4.00/lb, Mo – US$15.00/lb, Zn – US$1.75/lb, Pb – US$0.9/lb, Ag – $20/oz and Au – US$1,400/oz and recovery rates of 95% for Au, Ag, Cu, Mo, Zn and Mo. Recovery rate assumptions are speculative as no metallurgical work has been completed to date. ** A 0.2 g/t AuEq cut-off grade was employed with no more than 15% internal dilution. True widths are unknown, and grades are uncut.
To see our latest corporate presentation and related information, please visit www.collectivemining.com
Collective Mining is an exploration and development company focused on identifying and exploring prospective mineral projects in South America. Founded by the team that developed and sold Continental Gold Inc. to Zijin Mining for approximately $2 billion in enterprise value, the mission of the Company is to repeat its past success in Colombia by making significant new mineral discoveries and advance the projects to production. Management, insiders and close family and friends own nearly 45% of the outstanding shares of the Company and as a result, are fully aligned with shareholders.
The Company currently holds an option to earn up to a 100% interest in two projects located in Colombia. As a result of an aggressive exploration program on both the Guayabales and San Antonio projects, a total of eight major targets have been defined. The Company has made significant grassroot discoveries at both projects with near-surface discovery holes at the Guayabales project yielding 302 metres at 1.11 g/t AuEq at the Olympus target, 163 metres at 1.3 g/t AuEq at the Donut target and recently, at the Apollo target, 207.15 metres at 2.68 g/t AuEq, 89.4 metres at 2.46 g/t AuEg and 87.8 metres at 2.49 g/t AuEg. At the San Antonio project, the Company intersected, from surface, 710 metres at 0.53 AuEq. (See related press releases on our website for AuEq calculations)
Qualified Person (QP) and NI43-101 Disclosure
David J Reading is the designated Qualified Person for this news release within the meaning of National Instrument 43-101 (“NI 43-101”) and has reviewed and verified that the technical information contained herein is accurate and approves of the written disclosure of same. Mr. Reading has an MSc in Economic Geology and is a Fellow of the Institute of Materials, Minerals and Mining and of the Society of Economic Geology (SEG).
Technical Information
Rock and core samples have been prepared and analyzed at SGS laboratory facilities in Medellin, Colombia and Lima, Peru. Blanks, duplicates, and certified reference standards are inserted into the sample stream to monitor laboratory performance. Crush rejects and pulps are kept and stored in a secured storage facility for future assay verification. No capping has been applied to sample composites. The Company utilizes a rigorous, industry-standard QA/QC program.
Contact Information
Collective Mining Ltd. Steven Gold, Vice President, Corporate Development and Investor Relations Tel. (416) 648-4065
FORWARD-LOOKING STATEMENTS
This news release contains certain forward-looking statements, including, but not limited to, statements about the drill programs, including timing of results, and Collective’s future and intentions. Wherever possible, words such as “may”, “will”, “should”, “could”, “expect”, “plan”, “intend”, “anticipate”, “believe”, “estimate”, “predict” or “potential” or the negative or other variations of these words, or similar words or phrases, have been used to identify these forward-looking statements. These statements reflect management’s current beliefs and are based on information currently available to management as at the date hereof.
Forward-looking statements involve significant risk, uncertainties, and assumptions. Many factors could cause actual results, performance, or achievements to differ materially from the results discussed or implied in the forward-looking statements. These factors should be considered carefully, and readers should not place undue reliance on the forward-looking statements. Although the forward-looking statements contained in this news release are based upon what management believes to be reasonable assumptions, Collective cannot assure readers that actual results will be consistent with these forward-looking statements. These forward-looking statements are made as of the date of this news release, and Collective assumes no obligation to update or revise them to reflect new events or circumstances, except as required by law.
Neither the TSXV nor its Regulation Services Provider (as that term is defined in the policies of the TSXV) accepts responsibility for the adequacy or accuracy of this news release.
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Vancouver, British Columbia–(Newsfile Corp. – September 12, 2022) – Goldshore Resources Inc. (TSXV: GSHR) (OTCQB: GSHRF) (FSE: 8X00) (“Goldshore” or the “Company“), is pleased to announce assay results from eight holes drilled to test gold mineralization at the East Coldstream deposit at the Moss Lake Project in Northwest Ontario, Canada (the “Moss Lake Gold Project“).
Highlights:
Results for eight holes, drilled to better define the gold mineralization of the East Coldstream deposit, have confirmed three broad lenses of gold mineralization within the two main shear zones with best intercepts of:
23m @ 1.34 g/t Au from 244m depth in CED-22-004, including
7.35m @ 3.77 g/t Au from 254.2m
17.3m @ 1.55 g/t Au from 487m depth in CED-22-005
20m @ 1.15 g/t Au from 402m depth in CED-22-006
26m @ 1.66 g/t Au from 451m, including
7.9m @ 4.20 g/t Au from 465m
25.7m @ 2.07 g/t Au from 488m
37.05m @ 1.54 g/t Au from 209.3m depth in CED-22-007
27.9m @ 1.14 g/t Au from 387m depth in CED-22-008, including
13m @ 2.14 g/t Au from 401m
The better intercepts are all centered around five high-grade gold zones of mineralized breccia, including:
1.05m @ 15.8 g/t Au from 257.95m depth in CED-22-004
0.9m @ 14.3 g/t Au from 472m depth in CED-22-006, and
0.65m @ 13.5 g/t Au from 502m
0.85m @ 10.6 g/t Au from 244.35m depth in CED-22-007, and
0.4m @ 12.6 g/t Au from 418m
These results show that the three gold mineralized lenses have a clear steep plunge and highlight significant upside potential at depth within structurally controlled shoots.
President and CEO Brett Richards stated: “These first results are extremely encouraging and significant to the overarching strategy of developing a secondary resource to Moss Lake. This will provide optionality that can only help improve the new PEA study next year. The results also point to a second significant project within our land package, which highlights the potential for further discoveries.”
Technical Overview
Figure 1 shows the location of the East Coldstream deposit relative to the Moss Lake deposit and the Archean Shebandowan Greenstone Belt. Table 1 and Figure 3 show the significant intercepts. Table 2 and Figure 2 show the drill hole locations. Figures 4 and 5 show a cross section through CED-22-006 and long section along the southern zone, respectively.
Figure 1: Location map showing East Coldstream relative to Moss Lake
Intersections calculated above a 0.3 g/t Au cut off with a top cut of 30 g/t Au and a maximum internal waste interval of 10 metres. Bordered intervals are intersections calculated above a 1.0 g/t Au cut off. Intervals in bold are those with a grade thickness factor exceeding 20 gram x metres / tonne gold. True widths are approximate and assume a subvertical body.
Table 2: Location of drill holes in this press release
HOLE
EAST
NORTH
RL
AZIMUTH
DIP
EOH
CED-22-001
681,136
5,386,570
479
337°
-50°
483.0m
CED-22-002
681,420
5,386,640
479
335°
-50°
494.85m
CED-22-003
680,507
5,386,473
481
336°
-50°
360.0m
CED-22-004
680,008
5,386,430
477
155°
-60°
302.8m
CED-22-005
680,559
5,386,340
486
342°
-60°
810.1m
CED-22-006
680,010
5,386,586
475
140°
60°
600.0m
CED-22-007
680,085
5,386,604
473
138°
-59°
657.05m
CED-22-008
680,559
5,386,340
483
340°
-50°
603.0m
Approximate collar coordinates in NAD 83, Zone 15N
Results have been received for eight of the initial 17 holes in the first pass drilling program at East Coldstream. These drillholes tested the existing mineralized lenses, as well as possible eastern and down-dip extensions.
Our work on the mineralization paragenesis and its structural controls has shown that gold mineralization is related to pervasive silica-hematite alteration and sulfide veining associated with an extensional brecciation event following extensive shearing. At the deposit scale, this formed three lenticular bodies within two main shear zones (Figure 1). Based on structural measurements from oriented core, each body has a steeply west-dipping plunge and a gently east-pitching stretching lineation that creates an internal fabric to mineralization (Figure 4). This structural control creates the potential for additional high-grade mineralization to occur below the shallowly drilled portions of the shears zones such as encountered in CED-22-007.
CED-22-001 and -002 tested a similar geophysical feature to the east of the East Coldstream deposit. CED-22-001 was drilled closest to East Coldstream and encountered narrow zones of mineralization, while CED-22-002 was drilled 300 meters further east and did not encounter significant results. This sterilizes the immediate extension, but given the lenticular geometry of mineralization, leaves open the prospectively of the structure further to the east.
CED-22-003 and -004 drilled the North and Main Lenses, respectively. Both holes intersected broad low-grade mineralized zones, including 19.15m @ 0.61 g/t Au from 269.55m in CED-22-003; and 48m @ 0.39 g/t Au from 168m and 23m @ 1.34 g/t Au in CED-22-004.
Holes CED-22-005 to -008 tested down plunge extensions of the known mineralization. All holes intersected variable widths of higher grade mineralization, including 17.3m @ 1.55 g/t Au from 487m in CED-22-005; 20.0m @ 1.15 g/t Au from 402m, 26.0m @ 1.66 g/t Au from 451m, and 25.7m @ 2.07 g/t Au from 488m in CED-22-006; 37.05m @ 1.54 g/t Au from 209.3m in CED-22-007; and 27.9m @ 1.14 g/t Au from 387m in CED-22-008.
Pete Flindell, VP Exploration for Goldshore, said “Our analysis of drill results at East Coldstream confirms the two parallel shear zones that were modelled in the past. The recognition of a greater structural control within these shears has led to the modelling of three steeply dipping lenticular shoots that remain open at depth. A gently dipping internal fabric suggests that mineralization is focused within discrete structures that may allow us to model a higher-grade resource than exists in the historic estimate.”
Analytical and QA/QC Procedures
All samples were sent to ALS Geochemistry in Thunder Bay for preparation and analysis was performed in the ALS Vancouver analytical facility. ALS is accredited by the Standards Council of Canada (SCC) for the Accreditation of Mineral Analysis Testing Laboratories and CAN-P-4E ISO/IEC 17025. Samples were analyzed for gold via fire assay with an AA finish (“Au-AA23”) and 48 pathfinder elements via ICP-MS after four-acid digestion (“ME-MS61”). Samples that assayed over 10 ppm Au were re-run via fire assay with a gravimetric finish (“Au-GRA21”).
In addition to ALS quality assurance / quality control (“QA/QC”) protocols, Goldshore has implemented a quality control program for all samples collected through the drilling program. The quality control program was designed by a qualified and independent third party, with a focus on the quality of analytical results for gold. Analytical results are received, imported to our secure on-line database and evaluated to meet our established guidelines to ensure that all sample batches pass industry best practice for analytical quality control. Certified reference materials are considered acceptable if values returned are within three standard deviations of the certified value reported by the manufacture of the material. In addition to the certified reference material, certified blank material is included in the sample stream to monitor contamination during sample preparation. Blank material results are assessed based on the returned gold result being less than ten times the quoted lower detection limit of the analytical method. The results of the on-going analytical quality control program are evaluated and reported to Goldshore by Orix Geoscience Inc.
About Goldshore
Goldshore is an emerging junior gold development company, and owns the Moss Lake Gold Project located in Ontario. Wesdome Gold Mines Ltd. (“Wesdome“), is currently a large shareholder of Goldshore with an approximate 27% equity position in the Company. Well-financed and supported by an industry-leading management group, board of directors and advisory board, Goldshore is positioned to advance the Moss Lake Gold Project through the next stages of exploration and development.
About the Moss Lake Gold Project
The Moss Lake Gold Project is located approximately 100 km west of the city of Thunder Bay, Ontario. It is accessed via Highway 11 which passes within 1 km of the property boundary to the north. The Moss Lake Gold Project covers 14,292 hectares and consists of 282 unpatented and patented mining claims.
The Moss Lake Gold Project hosts a number of gold and base metal rich deposits including the Moss Lake Deposit, the East Coldstream Deposit (Table 3), the historically producing North Coldstream Mine (Table 4), and the Hamlin Zone, all of which occur over a mineralized trend exceeding 20 km in length. A historical preliminary economic assessment (the “Moss Lake Historical Estimate“) was completed on the Moss Lake Gold Project in 2013 and published by Moss Lake Gold Mines Ltd. (“Moss Lake Gold Mines“)1,3. A historical mineral resource estimate (the “East Coldstream Historical Estimate“) was completed on the East Coldstream Deposit in 2011 by Foundation Resources Inc.2,3 In addition to these zones, the Moss Lake Gold Project also hosts a number of under-explored mineral occurrences which are reported to exist both at surface and in historically drilled holes. The Moss Lake Deposit is a shear-hosted disseminated-style gold deposit which outcrops at surface. It has been drilled over a 2.5 km length and to depths of 300 m with 376 holes completed between 1983 and 2017. The last drilling program conducted in 2016 and 2017 by Wesdome, which consisted of widely spaced holes along the strike extension of the deposit was successful in expanding the mineralized footprint and hydrothermal system 1.6 km to the northeast. Additionally, the deposit remains largely open to depth. In 2017, Wesdome completed an induced polarization survey which traced the potential extensions of pyrite mineralization associated with the Moss Lake Deposit over a total strike length of 8 km and spanning the entire extent of the survey grids.
The East Coldstream Deposit is a shear-hosted disseminated-style gold deposit which locally outcrops at surface. It has been drilled over a 1.3 km length and to depths of 200 m with 138 holes completed between 1988 and 2017. The deposit remains largely open at depth and may have the potential for expansion along strike. Historic drill hole highlights from the East Coldstream Deposit include 4.86 g/t Au over 27.3 m in C-10-15.
The historically producing North Coldstream Mine is reported to have produced significant amounts of copper, gold and silver4 from mineralization with potential iron-oxide-copper-gold deposit style affinity. The exploration potential immediately surrounding the historic mining area is not currently well understood and historic data compilation is required.
The Hamlin Zone is a significant occurrence of copper and gold mineralization, and also of potential iron-oxide-copper-gold deposit style affinity. Between 2008 and 2011, Glencore tested Hamlin with 24 drill holes which successfully outlined a broad and intermittently mineralized zone over a strike length of 900 m. Historic drill hole highlights from the Hamlin Zone include 0.9 g/t Au and 0.35% Cu over 150.7 m in HAM-11-75.
The Moss Lake, East Coldstream and North Coldstream deposits sit on a mineral trend marked by a regionally significant deformation zone locally referred to as the Wawiag Fault Zone in the area of the Moss Lake Deposit. This deformation zone occurs over a length of approximately 20 km on the Moss Lake Gold Project and there is an area spanning approximately 7 km between the Moss Lake and East Coldstream deposits that is significantly underexplored.
Table 3: Historical Mineral Resources1,2,3
INDICATED
INFERRED
Deposit
Tonnes
Au g/t
Au oz
Tonnes
Au g/t
Au oz
Moss Lake Historical Estimate
Open Pit Potential
39,795,000
1.1
1,377,300
48,904,000
1.0
1,616,300
Underground Potential
–
–
–
1,461,100
2.9
135,400
Moss Lake Total
39,795,000
1.1
1,377,300
50,364,000
1.1
1,751,600
East Coldstream Historical Estimate
East Coldstream Total
3,516,700
0.85
96,400
30,533,000
0.78
763,276
Combined Total
43,311,700
1.08
1,473,700
80,897,000
0.98
2,514,876
Notes:
Source: Poirier, S., Patrick, G.A., Richard, P.L., and Palich, J. “Technical Report and Preliminary Economic Assessment for the Moss Lake Project”, prepared for Moss Lake Gold Mines Ltd. The qualified persons for the Moss Lake Historical Estimate are Pierre-Luc Richard, MSc, PGeo (InnovExplo Inc), and Carl Pelletier, BSc, PGeo (InnovExplo Inc), and the effective date of the Moss Lake Historical Estimate is February 8, 2013. In-Pit results are presented undiluted and in situ, within Whittle-optimized pit shells. Underground results are presented undiluted and in situ, outside Whittle-optimized pit shells. The Moss Lake Historical Estimate includes 18 gold-bearing zones and 1 envelope containing isolated gold intercepts. Whittle parameters: mining cost = C$2.28; pit slope angle = 50.0 degrees; production cost = C$9.55; mining Dilution = 5%; mining recovery = 95%; processing recovery = 80% to 85%; gold price = C$1,500. In-Pit and Underground resources were compiled at cut-off grades from 0.3 to 5.0 g/t Au (for sensitivity characterization). A cut-off grade of 0.5 g/t Au was selected as the official in-pit cut-off grade and a cut-off grade of 2.0 g/t Au was selected as the official underground cut-off grade. The Moss Lake Historical Estimate is based on 352 diamond drill holes (90,978 m) drilled from 1983 and 2008. A fixed density of 2.78 g/cm3 was used. A minimum true thickness of 5.0 m was applied, using the grade of the adjacent material when assayed or a value of zero when not assayed. Capping was established at 35 g/t Au, supported by statistical analysis and the high grade distribution within the deposit. Compositing was done on drill hole sections falling within the mineralized zone solids (composite = 1 m). Resources were evaluated from drill hole samples using the ID2 interpolation method in a multi-folder percent block model using Gems version 6.4. Based on geostatistics, the ellipse range for interpolation was 75m x 67.5m x 40m. The Indicated category is defined by combining the blocks within the two main zones and various statistical criteria, such as average distance to composites, distance to closest composite, quantity of drill holes within the search area. Ounce (troy) = metric tons x grade / 31.10348. Calculations used metric units (metres, tonnes and g/t). The number of metric tonnes was rounded to the nearest thousand. Any discrepancies in the totals are due to rounding effects; rounding followed the recommendations in NI 43-101.
Source: McCracken, T. “Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario”, prepared for Foundation Resources Inc. and Alto Ventures Ltd. The East Coldstream Historical Estimate is based on a 0.4 g/t Au cut-off grade. The qualified persons for the East Coldstream Historical Estimate are Todd McCracken, P.Geo. (Tetratech Wardrop), and Jeff Wilson, Ph.D., P.Geo. (Tetratech Wardrop), and the effective date of the East Coldstream Historical Estimate is December 12, 2011. Resources are presented unconstrained, undiluted and in situ. The East Coldstream Historical Estimate includes 2 gold-bearing zones. A cut-off grade of 0.4 g/t Au was selected as the official resource cut-off grade. The East Coldstream Historical Estimate is based on 116 diamond drill holes drilled from 1986 to 2011. A fixed density of 2.78 g/cm3 was used. Capping was established at 5.89 g/t Au and 5.70 g/t Au for domains EC-1 and EC-2, respectively. This is supported by statistical analysis and the high-grade distribution within the deposit. Compositing was done on drill hole sections falling within the mineralized zone solids (composite = 1 m). Resources were evaluated from drill hole samples using the ID2 interpolation method in a multi-folder percent block model using Datamine Studio 3 version 3.20.5321.0. Recource categorization is based on spatial continuity based from the variography of the assays within the drillholes. Ounce (troy) = metric tons x grade / 31.10348. Calculations used metric units (metres, tonnes and g/t). The number of metric tonnes was rounded to the nearest thousand. Any discrepancies in the totals are due to rounding effects; rounding followed the recommendations in NI 43-101.
The reader is cautioned that the Moss Lake Historical Estimate East and the East Coldstream Historical Estimate (the “Historical Estimates“) are considered historical in nature and as such is based on prior data and reports prepared by previous property owners. The reader is cautioned not to treat them, or any part of them, as current mineral resources or reserves. The Company has determined these historical resources are reliable, and relevant to be included here in that they demonstrate simply the mineral potential of the Moss Lake Gold Project. A qualified person has not done sufficient work to classify the Historical Estimates as current resources and Goldshore is not treating the Historical Estimates as current resources. Significant data compilation, re-drilling, re-sampling and data verification may be required by a qualified person before the Historical Estimates can be classified as a current resource. There can be no assurance that any of the historical mineral resources, in whole or in part, will ever become economically viable. In addition, mineral resources are not mineral reserves and do not have demonstrated economic viability. Even if classified as a current resource, there is no certainty as to whether further exploration will result in any inferred mineral resources being upgraded to an indicated or measured mineral resource category. The Historical Estimates relating to inferred mineral resources were calculated using prior mining industry standard definitions and practices for estimating mineral resource and mineral reserves. Such prior definitions and practices were utilized prior to the implementation of the current standards of the Canadian Institute of Mining for mineral resource estimation, and have a lower level of confidence.
Table 4: Reported Historical Production from the North Coldstream Deposit4
Deposit
Tonnes
Cu %
Au g/t
Ag
Cu lbs
Au oz
Ag oz
Historical Production
2,700,0000
1.89
0.56
5.59
102,000,000
44,000
440,000
Note:
Source: Schlanka, R., 1969. Copper, Nickel, Lead and Zinc Deposits of Ontario, Mineral Resources Circular No. 12, Ontario Geological Survey, pp. 314-316.
Peter Flindell, P.Geo., MAusIMM, MAIG, Vice President – Exploration of the Company, a qualified person under NI 43-101 has approved the scientific and technical information contained in this news release.
Neither the TSXV nor its Regulation Services Provider (as that term is defined in the policies of the TSXV) accepts responsibility for the adequacy or accuracy of this release.
For More Information – Please Contact:
Brett A. Richards President, Chief Executive Officer and Director Goldshore Resources Inc.
This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.
Forward-looking statements in this news release include, among others, statements relating to expectations regarding the exploration and development of the Moss Lake Gold Project, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance; and the impact of COVID-19.
The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.
This news release does not constitute an offer to sell, or a solicitation of an offer to buy, any securities in the United States. 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 U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.
