VANCOUVER, British Columbia, Oct. 05, 2022 (GLOBE NEWSWIRE) — Rover Metals Corp. (TSXV: ROVR) (OTCQB: ROVMF) (FSE:4XO) (“Rover” or the “Company”) is pleased to announce that its new corporate presentation is now available on its website. The Company is also featuring a recently recorded interview with its CEO, Judson Culter, who has provided a corporate update and plans for Q4 of this year.
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 a diverse portfolio of mineral resource projects: (1) Nevada Claystone Lithium; (2) Zinc-Copper-Lead-Silver in NT, Canada; as well as (3) Gold in NT, Canada. The Company is exclusive to the mining jurisdictions of Canada and the U.S.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%2522Vancouver%253BRover_(marque)%253BTSX_Venture_Exchange%2522%252C%2522lmsid%2522%253A%2522a0770000002m0AbAAI%2522%252C%2522revsp%2522%253A%2522globenewswire.com%2522%252C%2522lpstaid%2522%253A%2522b243763e-490c-3642-8311-1f09ba99905e%2522%252C%2522pageContentType%2522%253A%2522story%2522%257D
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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
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Vancouver, British Columbia–(Newsfile Corp. – October 4, 2022) – Goldshore Resources Inc. (TSXV: GSHR) (OTCQB: GSHRF) (FSE: 8X00) (“Goldshore” or the “Company“), is pleased to announce assay results from its initial scout drilling campaign testing the historic North Coldstream copper mine (“North Coldstream“) at the Moss Lake Project in Northwest Ontario, Canada (the “Moss Lake Gold Project“).
Highlights:
Initial results from one North Coldstream hole confirm significant copper, cobalt and gold mineralization hosted within a sheared volcanic massive sulphide deposit with best intercepts of:
62.8m @ 0.88% CuE (0.36% Cu, 0.06% Co, 0.30 ppm Au and 3.1 ppm Ag) from 8.2m depth in CND-22-006, including
13.35m @ 1.18% CuE (0.54% Cu, 0.07% Co, 0.39 ppm Au and 3.5 ppm Ag) from 8.2m
14.65m @ 1.30% CuE (0.57% Cu, 0.09% Co, 0.39 ppm Au and 4.4 ppm Ag) from 23.1m
These copper and cobalt results confirm that North Coldstream hasimportant critical mineral value and highlights multiple deposit styles in the district, which is a hallmark of important mineral districts worldwide.
North Coldstream was mapped by last year’s VTEM survey (press release dated March 10, 2022) as a discrete magnetic conductor. There are twelve similar targets in the Moss Lake Project, highlighting the potential for similar copper-cobalt-gold deposits.
Drilling also identified a gold only intercept of 2.1m @ 1.88 g/t Au from 98.9m in the footwall to the North Coldstream VMS deposit, which is related to the East Coldstream style of mineralization 1.6 kilometers to the east, suggesting greater continuity of the gold-bearing structures.
President and CEO Brett Richards stated: “Although we are very focused on the Moss Lake drilling and defining a higher-grade resource within the lower grade historical resource; these findings at North Coldstream are extremely encouraging and provide tremendous potential optionality in the future. As we have illustrated previously to the market, North Coldstream was a past producing copper-gold mine, so these results are not unexpected. However, I think the exciting story is the emergence and identification of cobalt in the historic mine. These drill results prove the value and priority of further drilling and exploration at the North Coldstream deposit, and could identify it as a critical mineral asset, which is important for the development of renewable energies, electrification of vehicles and global decarbonization initiatives.”
Figure 1 shows the location of North Coldstream relative to the main Moss Lake Gold Deposit. Figures 2 and 3 show a plan and long section of the historic workings, respectively, with the location of CND-22-006. Figure 4 shows a photograph of the drill core to illustrate the style of mineralization. Table 1 shows the hole details and Table 2 shows the significant intercepts.
Figure 1: Location map showing North Coldstream relative to Moss Lake
Intersections calculated above a 0.1% Cu cut off with no top cut and a maximum internal waste interval of 2 metres. Bordered intervals are higher grade intersections above a 0.2% Cu cut off. Copper equivalent values assume prices of $3.50/lb Cu, $25/lb Co, $1700/oz Au and $19/oz Ag. Metallurgical recoveries are assumed at 90% Cu, 70% Co, 70% Au and 70% Ag based on similar mineralization in the Copperbelt, however, metallurgical test work is yet to be conducted. True widths are approximate and assume a subvertical body.
Figure 2: Drill plan showing drill hole relative to the historic copper mine
The Company has completed six scout holes to test the geology and multi-element chemistry of the North Coldstream deposit that was mined for copper between 1957 and 1967. The challenging aspect of this program has been drilling to avoid the historic stopes, which has meant, at this stage, drilling the fringes of the deposit as we target extensions to shoots.
CND-22-006 intersected a broad zone of copper mineralization associated with the western edge of the historic workings. While gold and silver credits were expected, based on historic production figures, elevated levels of cobalt in the range of 0.02 to 0.2% Co suggest previously unrecognized critical mineral value at North Coldstream.
A review of the geology has confirmed that the deposit is a sheared volcanic massive sulphide deposit with chalcopyrite-pyrite-pyrrhotite mineralization associated with brecciated siliceous cherts containing variable amounts of syngenetic magnetite (Figure 4). Minor sphalerite mineralization defines a very distinct 40-meter halo around the main massive sulphide lens, bolstering the interpretation of a VMS setting for the mineralization. Within the massive sulphide lens copper, cobalt, gold, and silver grades track each other closely, indicating that they precipitated as part of a single event. In contrast, the narrow intervals of gold mineralization outboard of the main lens are associated with quartz-carbonate veining and have only minor silver and weak copper-cobalt values. These are likely related to the gold mineralization 1.6 kilometers along strike at the East Coldstream deposit and highlight the prospectivity of this trend for additional gold targets.
Figure 4: Photograph of drill core in the main high-grade zone (CND-22-006: 25.9-38.15m averages 1.34% CuE, including 0.59% Cu, 0.09% Co, 0.41 ppm Au and 4.5 ppm Ag)
The Company will address the backlog of North Coldstream core once it has cleared the balance of drill core from Moss Lake. Future drilling will target pillars within the deposit, potential depth extensions, and test similar targets in the district that are characterized by magnetic conductors (press release dated March 10, 2022).
Pete Flindell, VP Exploration for Goldshore, said, “These drill results confirm our expectations of high-grade copper mineralization, especially as we are on the margin of the volcanic massive sulphide lens, and are extremely encouraging with respect to Cobalt grades. While the five pending holes are also around the margin of the system, and therefore likely to contain similar grades, I look forward to drilling closer to the core of the deposit to understand how the critical mineral elements may increase. These data will be invaluable in guiding our future drilling of similar, untested targets within the Moss Lake Project.”
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 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 Gold Mines Ltd. (“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:
(1) 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.
(2) 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. Resource 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.
(3) 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::
(4) 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.
Vancouver, British Columbia–(Newsfile Corp. – October 4, 2022) – EMX Royalty Corporation (NYSE American: EMX) (TSXV: EMX) (FSE: 6E9) (the “Company” or “EMX”) is pleased to announce that it will receive a US$3 million milestone payment from Arizona Sonoran Copper Company, Inc. (TSX: ASCU) (“ASCU”) for the Parks-Salyer royalty property (the “Royalty Property”) in Arizona. The Royalty Property was held under a lease arrangement by EMX’s wholly owned subsidiary Bronco Creek Exploration Inc., and was transferred to ASCU via Assignment and Royalty Agreements (the “Agreements”) executed earlier this year (see EMX news release dated February 10, 2022). EMX’s Royalty Property covers 158 acres of ASCU’s Parks-Salyer copper project. The milestone payment results from ASCU’s maiden resource estimate for the Parks-Salyer project that exceeds thresholds for contained copper included within EMX’s Royalty Property footprint. The Company also retains a 1.5% net smelter return (“NSR”) royalty covering the Royalty Property.
EMX’s Parks-Salyer Royalty Property provides an example of a significant pre-production payment to the Company resulting from its copper porphyry royalty generation program in Arizona. The Property’s porphyry targets, which are concealed beneath post-mineral cover, were identified by EMX based upon structural geological assessments of historical exploration data. The open ground covering these targets was acquired by EMX at minimal cost. The 158 acres transferred to ASCU complemented the property position at its Parks-Salyer project, while providing EMX with pre-production payments and exploration, development, and royalty upside optionality at no additional cost to the Company.
Commercial Terms and Property Summary (all dollar amounts in USD). The Agreements provided for a one-time cash payment to EMX for the assignment of EMX’s rights covering the Property, as well as the 1.5% NSR royalty interest (ASCU may buy back 1% of the royalty for $500,000), work commitments, annual advance royalty (“AAR”) payments, and the $3 million milestone payment to EMX based upon declared resources totaling 200 million pounds or more of contained copper covered by EMX’s Royalty Property. ASCU’s (global) maiden resources for its Parks-Salyer project were disclosed in a news release dated September 28, 2022.
Parks-Salyer is located approximately five kilometers northwest of Casa Grande, Arizona and approximately 1.5 kilometers southwest of the historical Sacaton open pit copper mine. Sacaton was a porphyry copper-molybedenum mine operated by Asarco (1974-1984), and is now being advanced by ASCU as the PEA stage Cactus Project. The Parks-Salyer deposit lies beneath post-mineral gravels and represents a tilted, and fault-displaced portion of the Casa Grande-Santa Cruz porphyry system.
Qualified Person. Michael P. Sheehan, 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.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%2522Arizona%253BCompany%253BCasa_Grande%252C_Arizona%253BCopper_Project%2522%252C%2522lmsid%2522%253A%2522a0V0W00000HOPDcUAP%2522%252C%2522revsp%2522%253A%2522newsfile_64%2522%252C%2522lpstaid%2522%253A%2522d7d1d544-54c0-352e-9892-db00e84c428c%2522%252C%2522pageContentType%2522%253A%2522story%2522%257D
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.
About Arizona Sonoran Copper Company. ASCU’s objective is to become a mid-tier copper producer with low operating costs, develop the Cactus and Parks-Salyer Project that could generate robust returns for investors, and provide a long term sustainable and responsible operation for the community and all stakeholders. The Company’s principal asset is a 100% interest in the Cactus Project (former ASARCO, Sacaton mine) and Parks-Salyer deposit which is situated on private land in an infrastructure-rich area of Arizona.
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” 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 and the year ended December 31, 2021 (the “MD&A”), and the most recently filed Revised 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.
On February 16th the comedian running Ukraine began a massive shelling attack on the Donbas after murdering over 14,000 innocent civilians since 2014 in the region because they did not support the illegal coup d’état sponsored by the US.
In a speech given at the Munich Security Conference on February 19th the clown made it clear Ukraine wanted to regain its nuclear arsenal. Also on February 19th Brandon announced he knew Putin was about to attack Ukraine. That may have had something to do with Ukraine’s planned invasion of the Donbas scheduled for early March.
Russia responded with a preemptive attack on Ukraine on February 24th. Brandon called for more sanctions on Russia in response in addition to those imposed before Russia had done anything.
The European allies and US seized billions of dollars of Russian reserves in the west and other assets without even a shred of legal justification. The Ruble went into free fall going from 85 to the dollar on February 15th to a high of 147 on March 7th. Clearly the sanctions had an effect and cut the value of the Ruble almost in half.
Russia was prepared for yet another round of sanctions. They raised internal interest rates and demanded payment for their gas and oil in Rubles. Since then the Ruble has been the strongest currency in the world currently trading at 55 to the dollar. The Euro has fallen to below par with the Dollar, the British Pound is down over 20% and almost at par with the dollar. The sanctions hurt.
But they hurt Europe, they didn’t hurt Russia.
On March 1st I posted an article I had written in response to the sanctions. I called it The US, EU and Nato Just Committed Suicide. I’m going to take credit for being the first person in the world to write about how stupid and self-destructive the sanctions were. Since then the word suicide has been recognized by hundreds or thousands of other commentators. Everyone now understands just how much damage the sanctions have done to the economy of Europe and the US.
You see, there is no energy shortage. There is lots of natural gas available and coal and oil to any willing buyer. But at the insistence of the US upon their European sock puppets, Europe refused to agree to perfectly reasonable terms offered by Russia. This wasn’t a case of Russia refusing to sell resources to the EU. It was a case of the EU first stealing from Russia and then demanding Russia agrees to their terms.
Putin understood something that none of the “leaders” of the EU understood and most of the world still doesn’t get.
Europe needs Russia.
Russia does not need Europe.
So the cost of energy and food across the world has skyrocketed. This winter thousands of businesses in Europe are going to be forced to close because they cannot afford to pay their energy bills. Millions of Europeans are going to starve or freeze or be forced into poverty as a result of their own stupidity or all three at the same time.
I’ve been amazed because the solution to the problem was so simple but the actions of the “leaders” of the EU so obtuse.
Regardless of how they feel about the war, right or wrong on anyone’s part, if the sanctions hurt Europe and didn’t hurt Russia, all the EU had to do was declare victory and announce the end of the sanctions. Agree to pay on the terms Russia has offered to everyone and the economy recovers from this latest stupidity in government in a few months.
If Germany needs natural gas as a feedstock for their chemical plants and to provide heat for businesses and homes, all they had to do was turn on the Nord Stream II pipeline.
That was until September 27th when the US blew up Nord Stream I and Nord Stream II. Which Brandon has promised was in the works long ago.
So we are in one of those good news, bad news places. The good news is that thousands and perhaps millions of Europeans led by the Germans are going to starve, freeze and go bankrupt this year.
Because of this act of war on the part of the US, the probability of a nuclear exchange just went through the roof. We are closer to nuclear annihilation than we have ever been in history.
The bad news of course is that no matter how grim this winter is in Europe, they are totally fucked next year. Turning on the tap is no longer an option even if the EU sobered up.
Welcome to World War III brought to you by Brandon and the idiot neo-cons surrounding him. Is anyone stupid enough to believe Russia will not respond in kind?
About 5.7 tons of Russian bullion arrived in August, data show
Metal arrived from the UK, not under sanctions: Swiss customs
By
Eddie Spence+FollowSeptember 20, 2022, 4:26 AM EDTUpdated on
Switzerland’s imports of Russian gold surged to the highest in more than two years, a sign that more old bullion from the country may be being remelted to make it easier to sell.
About 5.7 tons — worth $324 million — of Russian metal was imported by the refining hub in August, according to data from the Swiss Federal Customs Administration. That’s the most since April 2020.
The shipment was Russian metal that arrived from the UK, the customs administration said in a statement on Tuesday. Swiss customs data show the last place the precious metal was refined, rather than where it was last shipped from.
Russia’s gold has become taboo since the country invaded Ukraine earlier in the year. New Russian gold has been sanctioned by the US, EU and Switzerland, but bars exported from the country before Aug 4. are not subject to the import ban, the customs authority said Tuesday.
Some investors with old Russian gold bars may wish to remelt them at Swiss refineries to make them easier to sell. Though the country’s bullion minted before the war can still be traded in most major centers, including London and Zurich, there’s a stigma around it. Russia — the world’s second-biggest gold miner globally — was previously a major supplier of new bullion to the UK market.
China is still importing Russian gold, though the quantities remain relatively low. The country bought 0.3 tons of the precious metal from Russia in August, a small fraction of its
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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.
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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.
