2025 Drill Program Completed on the BiTe Showing and New Gold Discovery Reported at Manta
(TheNewswire)
Vancouver, British Columbia – TheNewswire - September 8, 2025– Rackla Metals Inc. (TSX-V: RAK) (the “Company”) is pleased toannounce that the Company has completed the 2025 drill program at theBiTe showing on the Grad Property. Additionally, the Company reportsthat it has made a new discovery from surface sampling on the Mantaintrusion, 2 km south of the BiTe showing.
Rackla has also been informed by the lab that resultsfrom the first three drill holes will not be completed until after the21 st of September.
The final two drill holes (G25-009 and 010) weredrilled on the southern margin of the intrusion and encounteredimpressive alteration zones and abundant sheeted veining.
Sheeted veining and bismuth-sulphide/telluride(?)mineralization has been observed in all holes drilled in theprogram.
Core samples from all holes have been delivered to thelab and the Company still awaits the analytical results.
The first rock samples collected in the vicinity of theManta intrusive have returned several multi-gram gold resultsassociated with sheeted veining and bismuth mineralization.
The drill program at the BiTe showing was completed onSeptember 4 and the drill crew has demobilized for the season. In2025, 10 holes were completed for a total of 4,486 m. The drillprogram tested an area measuring 600 x 360 x 550 m.
The area tested has demonstrated a con sistent set of sheetedquartz/sulphide + tourmalineveins with 3 dominant vein orientations (Figure 1). A broad zone withintense quartz and quartz-tourmaline veining and elevated bismuthcontent was intersected at the top of holes G25-004 and 005. This zonehas been intersected in holes G25-006, G25-007, G25-009 and G25-010. The zone shows good continuity and appears robust with increasingstrength and width as the intercepts get deeper.
Sampling of quartz-arsenopyriteveins on the ridge top and high on the north face of the intrusivehave returned low gold values. Little work has been done below theupper most reaches of this face. Sampling on the west and east ridgeshas observed quartz veining with bismuth sulfides/tellurides. Results from this sampling are pending.
2026 will see a focus of drilling from the ridge top,testing the core of the Grad intrusive. Several areas have beenidentified where pads can be established. The Company had planned todrill this area from Pad E in 2025, however determined to delay thishole until 2026 due to inclement weather and the related safetyhazards.
Figure 1 – Plan map of the BiTeshowing drill hole traces with vein density counts.
The last 2 holes, G25-009 and G25-010, tested theintrusive-sediment contact area and each intersected an intenselyaltered interval of silica-sericite-chlorite alteration with abundantdisseminated bismuthinite mineralization. A variety of vein andmineralization types were encountered in hole G25-009 and examples areshown in Figure 2. The hole was collared in sediments and continued insediments until 127.14 m. A few narrow intrusive dykes cut thesediments and were well altered and mineralized with bismuthinite(Figure 2 A). The sediments were also well veined withquartz-carbonate veins, occasionally containing a white-blue bismuthalloy mineral (Figure 2 D). Further down the hole sheeted quartz veinswere observed to contain abundant bismuthinite and chalcopyrite(Figures 2 B and C).
Figure 2 – Selected photos ofmineralization in hole G25-009: A – large bismuthinite grain at145.75 m; B – quartz-chalcopyrite-bismuthinite vein at 520 m; C –bismuthinite-chalcopyrite vein at 561.4 m; D –bismuth alloy inquartz-carbonate vein at 124.50 m.
Hole G25-010 tested the sediment-intrusive contact atthe southwestern edge of the BiTe Zone and was a significant step out. The top of the hole down to 218 m had relatively low vein densitycount, but from 218 m to 452 m the vein density was some of thehighest observed to date, averaging 24 veins-per-metre (Figure 1).Importantly, the veins within this interval contained abundant bismuthminerals (Figure 3).
Figure 3 – Selected photos ofmineralization in hole G25-010: A – Sheeted vein density for theinterval 353 to 366 m; B – bismuthinite in quartz veins at 436 m; C– bismuthinite in quartz veins at 428 m; D – bismuthinite inquartz veins at 319 m.
All samples from the drilling have been sent to the lab. Rackla hasnot received any drill sample analytical results as of this pressrelease, however the Company does expect the initial results withinthe coming weeks and a steady flow of results following that.
Diamond drill hole collar information:
Hole | Easting | Northing | Elevation | Dip | Azimuth | Depth (m) |
G25-001 | 517697 | 6959397 | 1805 | -50 | 88 | 208.79 |
G25-002 | 517697 | 6959397 | 1805 | -50 | 78 | 336.70 |
G25-003 | 517712 | 6959342 | 1781 | -50 | 90 | 425.20 |
G25-004 | 517637 | 6959447 | 1803 | -50 | 90 | 416.05 |
G25-005 | 517637 | 6959447 | 1803 | -50 | 60 | 431.20 |
G25-006 | 517504 | 6959464 | 1765 | -50 | 90 | 516.64 |
G25-007 | 517504 | 6959464 | 1765 | -70 | 90 | 537.97 |
G25-008 | 517504 | 6959464 | 1765 | -50 | 60 | 533.40 |
G25-009 | 517709 | 6959272 | 1782 | -50 | 60 | 607.77 |
G25-010 | 517433 | 6959292 | 1713 | -50 | 65 | 472.44 |
New Discovery: Manta Intrusion
The Company would also like to report a significant newsurface discovery at a previously unmapped intrusion which the Companyhas named the Manta intrusion. The Mantaintrusion is within the Grad property, 2 km south of the BiTe showing,and was discovered by Rackla crews during reconnaissance prospectingin 2024. Prior to discovery the intrusion was not identified ongovernment maps.
This year’s surface sampling has shown that theintrusion is multi-phase with the main portion being megacrysticgranodiorite measuring 1.2 by 0.7 km. The intrusion has a largecontact aureole with hornfelsing of quartzite and development of askarn horizon approximately 30 metres thick. The skarn horizon is acomplex unit composed of calc-silicate, diopside, garnet andquartz.
Mineralization at Manta consists of three main types:quartz±carbonate veins; disseminated and veined pyrrhotite, pyriteand bismuthinite; and disseminate sulphides in quartz-porphyrydykes . The quartz±carbonate veins are from 1 to 20 cm wide and contain bismuthinite.These are hosted in the quartzite and skarn. Surface sampling of theseveins in 2025 have returned grades of 52.1, 11.8, 8.4 and 5.7 g/t Aufrom grab samples (Figure 4).
The disseminated and veined pyrrhotite, pyrite andbismuthinite are restricted to the skarn unit on the western edge ofthe intrusion with locally massive sulphide lenses in the 5-10 cmrange. A 1.0 m composite chip sample from this area returned 48.3 g/tAu.
A grab sample of disseminate sulphides inquartz-porphyry dykes with quartz-sericite-pyrite alteration hasreturned 2.25 g/t Au.
The preliminary observations of the mineralizationstyles and these sampling results indicate that the Manta intrusion isanother Reduced Intrusion-Related Gold System target withskarnification of the contact sediments. A follow-up program ispresently underway consisting of channel sampling and detailed mappingof the prospect.
Figure 4 – Geological map of theManta intrusion and 2025 rock sample results for gold.
Rackla is working in consultation with the Sahtu Deneand Métis communities and remains committed to maintaining therespectful, collaborative relationships we’ve built with the Sahtu.As we advance exploration at the Grad Project, we will continueworking closely with local stakeholders and regulatory agencies toensure our activities create long-term value and reflect communitypriorities.
Qualified Person
Scott Casselman, B.Sc., P.Geo., Vice-PresidentExploration of the Company, is a member of the Association ofProfessional Engineers and Geoscientists of British Columbia and isthe Company’s Qualified Person as defined by National Instrument43-101. Mr. Casselman has reviewed and approved the technicalinformation contained in this news release.
AboutRackla
Rackla Metals Inc. (TSX-V: RAK) is a Vancouver, Canadabased junior gold exploration company. The Company is targetingReduced Intrusion-Related Gold Systems (RIRGS) mineralization on thesoutheastern part of the Tombstone Gold Belt in eastern Yukon andwestern Northwest Territories. Management believes that this area,which is underexplored for RIRGS deposit types, has the potential tobe the next frontier for the discovery of these large goldsystems.
ON BEHALF OF THE BOARD
Simon Ridgway,
CEO and Director
Tel: (604) 801-5432; Fax: (604) 662-8829
Email: info@racklametals.com
Website: www.racklametals.com
Neither the TSX Venture Exchange norits Regulation Services Provider (as that term is defined in thepolicies of the TSX Venture Exchange) accept responsibility for theadequacy or accuracy of this news release.
Forward-Looking Information
Certain statements contained in thisnews release constitute forward-looking statements within the meaningof Canadian securities legislation. All statements included herein,other than statements of historical fact, are forward- lookingstatements and include, without limitation, the expected timing ofreceipt of assay results; the Company’s future explorationactivities; and general business and economic conditions. Often, butnot always, these forward looking statements can be identified by theuse of words such as “estimate”, “estimates”, “estimated”,“potential”, “open”, “future”, “assumed”,“projected”, “used”, “detailed”, “has been”,“gain”, “upgraded”, “offset”, “limited”,“contained”, “reflecting”, “containing”, “remaining”,“to be”, “periodically”, or statements that events,“could” or “should” occur or be achieved and similarexpressions, including negative variations.
Forward-looking statements involveknown and unknown risks, uncertainties and other factors which maycause the actual results, performance or achievements of the Companyto be materially different from any results, performance orachievements expressed or implied by forward-looking statements. Suchuncertainties and factors include, among others, changes in generaleconomic conditions and financial markets; the Company or any jointventure partner not having the financial ability to meet itsexploration and development goals; risks associated with the resultsof exploration and development activities, estimation of mineralresources and the geology, grade and continuity of mineral deposits;unanticipated costs and expenses; and such other risks detailed fromtime to time in the Company’s quarterly and annual filings withsecurities regulators and available under the Company’s profile onSEDAR+ at www.sedarplus.ca .Although the Company has attempted to identify important factors thatcould cause actual actions, events or results to differ materiallyfrom those described in forward-looking statements, there may be otherfactors that cause actions, events or results to differ from those anticipated,estimated or intended.
Forward-looking statements containedherein are based on the assumptions, beliefs, expectations andopinions of management, including but not limited to: that theCompany’s stated goals and planned exploration activities at itsproperties will be achieved; that there will be no material adversechange affecting the Company, its properties or its securities; andsuch other assumptions as set out herein. Forward-looking statementsare made as of the date hereof and the Company disclaims anyobligation to update any forward-looking statements, whether as aresult of new information, future events or results or otherwise,except as required by law. There can be no assurance thatforward-looking statements will prove to be accurate, as actualresults and future events could differ materially from thoseanticipated in such statements. Accordingly, investors should notplace undue reliance on forward-looking statements.
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