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RED MOUNTAIN MINING LIMITED — Capital/Financing Update 2025
Feb 11, 2025
65719_rns_2025-02-11_86ade95b-e1d5-475f-a4e7-a73bf1efdc09.pdf
Capital/Financing Update
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ASX ANNOUNCEMENT
12 FEBRUARY 2025
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ASX: RMX
Red Mountain Mining Ltd ACN 119 568 106
Australia and Canada based Gold and Battery metals explorer
Fry Lake Gold Project Desktop Study Reveals Highly Prospective Gold Targets
HIGHLIGHTS
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After a highly successful program at Flicka Lake, Data Review highlights additional prospectivity of the three claims to the east, Fry Lake Stock, Fry-McVean Shear and Relyea Porphyry (collectively the four claims are the “Fry Lake Gold Project”)
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Review showed McVean gold trend appears to extend into the Fry-McVean claims, supported by historic drilling results and a more recent VTEM survey
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Series of historic drill holes border the Fry-McVean claim with gold hits in multiple down hole intersections, with intervals reporting up to 1.6 g/t Au.
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Results are highly complementary to Flicka Lake, with further exploration work to progress in the Canadian 2025 Field Season, after the Winter period ends
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New record highs with gold prices surging above US$2,900 an ounce this week -
provides an exciting macro-environment for further exploration at Fry Lake
Red Mountain Mining Limited (“RMX” or the “Company”) is pleased to advise that it has completed a detailed review of all the historical data in-and-adjacent to the Fry Lake Stock, Fry-McVean Shear and Relyea Porphyry claims areas. The review found high residual potential for all three claims areas, with very little previous exploration conducted. The claims also have attractive geological and structural targets with several alterations identified through previous Ontario Geological Survey rock chip sampling programs.
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Figure 1: Summary slide of all the drilling, rock chip and humus (soil) sampling conducted over three of the four claims areas that make up the Fry Lake Project .
redmountainmining.com.au
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Desktop Study Reveals Extensive Potential Gold Mineralisation Target at Fry-McVean
The desktop study revealed that the Fry-McVean Shear hosts promising gold mineralisation and this structure traverses the length of the Fry-McVean claims area. A series of historic drill holes border the Fry-McVean claim with gold hits in multiple down hole intersections, with intervals reporting up to 1.6 g/t Au.
Analysis undertaken by Red Mountain has generated further supporting data which correlates the gold anomaly to an electromagnetic conductive feature. A recent VTEM Survey (Geotech, 2016¹) highlighted a highly conductive and magnetic feature associated with the shear, this shear traverses 8km along Red Mountain’s Fry-McVean Claim.
Furthers details from the study include:
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In the east of Fry-McVean Shear, hole McV-92-11 reported 180ppb Au (Major General Resources, 1992) from 197.2-198.7m in graphitic argillite bands in chert-magnetite iron formation, with 10-15% pyrrhotite. This suggests gold mineralisation may be open to the west along the shear.
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To the east of the RMX claims, drill holes McV-92-5 to McV-92-10 (Major General Resources, 1992) reported multiple intersections from 94 to 198m depth of anomalous gold with the best intersection 1.6ppm Au at 95-96.5m depth in hole McV-92-5.
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Three holes drilled in the west of the claim area (1970 & 1974) targeted ground EM conductors from 1970’s surveys with shallow holes intersecting shallow (less than 30m) massive sulphides mainly pyrrhotite with minor pyrite, chalcopyrite in graphitic argillites. Analytical data was not available, indicating the potential for further work.
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Humus sampling along 100m spaced N-S traverses and 30m sample intervals (D. Brown²) reported up to 6ppb Au with possible NW trends parallel to the Fry-McVean shear. Previous analysis suggested that a number of Riedel shears exist in the area and have potential for mineralisation.
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A total of 5 rock samples have been collected by Ontario Geological Survey across the Fry-McVean claims, mafic and felsic metavolcanics and one felsic intrusion, none were tested for gold.
In summary, the review shows Fry-McVean possesses highly prospective follow-up targets and electromagnetic surveying would expedite exploration to define the most prospective areas for mineralisation.
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Figure 2: Summary slide of the historical drilling, rock chip and humus (soil) sampling reported in the area. The 1992 McV series holes report anomalous gold in holes as marked.
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Figure 3: 2016 VTEM survey flown by Geotech to the east of the Fry-McVean Shear claims highlighting the correlation of the 1992 anomalous gold holes and the conductive EM feature.
High Residual Gold and Copper Potential at Fry Lake Stock
Fry Lake Stock covers a large quartz-felspar porphyry intruding mafic meta volcanics where contact alteration includes iron, sericite, quartz, tourmaline, and sulphides. The Fry-McVean shear cuts through the northern part of the claims and intrusive gabbro.
The results of the data review at Fry Lake Stock found:
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29 rock samples collected across the licence by the Ontario Geological Survey, with samples from porphyry, syenite, gabbro and noted high calcium levels from extensive carbonatation of the basement. Some samples were tested for gold with up to 25ppb noted.
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Four holes on the southeast margin (drilled towards the stock) report trace levels of gold in the tuffaceous intervals of the mafic to intermediate volcanics. These are often reported up to tens of percent pyrrhotite with lower levels of pyrite, chalcopyrite and sphalerite. The Geological Survey report for this area (Number 24) also shows it is anomalous for copper and zinc.
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No soil/humus sampling has been reported in or near the claims.
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The contact margins of the quartz-feldspar porphyry are target areas for potentially hosting mineralisation.
The Fry Lake Stock review revealed drilling on the margins and rock chip sampling but no systematic exploration, providing good residual potential for discovery.
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Geotech (2016) VTEM survey McVean Property, Pickle Lake, Ontario for Gray Jay Resources. OGS Record 20009132
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D Brown (2012) Assessment Work Report, Humus Geochemical Survey on the Fry McVean Claims. OGS 20011469
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Figure 4 : Fry Lake Stock claims covering the central Quartz-feldspar Porphyry with known drilling in the southeast producing trace gold and anomalous copper and zinc .
Additional Gold and Copper Potential at Relyea Porphyry
Red Mountain’s study has identified a central quartz-feldspar porphyry intruding mafic metavolcanics, with pyrite mineralisation concentrated along the contact zone. To the south, a gabbro intrusion cuts through the mafic metavolcanic sequence, while in the north, clastic metasedimentary rocks are in contact with mafic metavolcanics, defining a priority target zone.
At Relyea Porphyry, 8 rock samples have been reported by the Ontario Geological Survey, being dominantly syenitic but also an argillite, gabbro and sandstone were also collected. Only 5 were analysed from gold, with the argillite showing grades of 56.9ppb Au while one of the syenites reported 6.2ppb Au. The 2016 VTEM survey was also conducted to the SE of the claims area and revealed a NW striking magnetic feature with associated conductor, which may extend in RMX’s claims area.
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Figure 5: Relyea Porphyry claims showing how little work has been done in the area and the VTEM conductor with associated magnetic feature may extrapolate into the claims area.
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Forward Strategy at Fry Lake Gold Project
In summary, the review found that known gold mineralisation in the area is associated with strong alteration (iron & carbonatisation sulphides) with geological contacts and /or shearing, quartz-carbonate veining in favourable geological units, graphitic argillites, intrusive porphyries, and some tuffaceous units. These favourable features are found in all three claims areas under review. It was also noted that VTEM is an effective tool to refine the target areas.
In view of the Flicka Lake results to the west and findings from the historical data compilation, the strategy going forward will include:
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Flicka Lake – target the high gold grade areas of quartz-vein hosted gold mineralisation at the Flicka Zone, where initial results provided justification for further surface sampling and drill testing of this target to better understand its extent.
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Flicka Lake – target the two new areas with highly anomalous gold in soil, which represent two new potential high-grade orogenic gold targets within the Flicka Lake project. These prospects will be followed up by further detailed surface sampling, possibly including trenching to expose underlying basement geology during the 2025 Canadian Field season, followed up by drill-testing if results are positive.
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Flicka Lake – target the two copper-rich polymetallic soil anomalies that are consistent with volcanichosted massive sulfide mineralization. The northernmost of these anomalies partially overlaps the northern gold target and lies immediately south of an area where massive sulfides were drilled in 1988. It remains open to the north, northwest and east. Further surface sampling will also be undertaken at these prospects and also across the unsampled northern part of the Flicka Lake project area, followed by drill-testing, if results are positive.
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Consideration of using VTEM to refine suitable conductive targets for follow-up by potential drilling.
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Selective sampling over the target areas within the Fry Lake Stock, in particular the porphyry margins, FryMcVean Shear – the shear itself and Relyea Porphyry – the porphyry margins.
Geological Context of Flicka Lake
The Flicka Lake claims lie in the Archaean Meen-Dempster Greenstone Belt within the Uchi Lake Subprovince of the Superior Province of Canada. Flicka Lake is one of four recently acquired 100% RMX-owned properties within the relatively underexplored southwest portion of the Belt (Figure 6).
The Superior Province is globally recognised as a Tier 1 exploration destination for synvolcanic base metal and structurally controlled Archaean orogenic gold mineralisation. Numerous orogenic gold prospects and mineral occurrences are recorded for the Meen-Dempster Greenstone Belt, including significant historical production from the Golden Patricia, Pickle Crow and Dona Mines (Figure 6). The four 100% RMX owned properties, collectively termed the Fry Lake Projects, have seen only limited previous exploration and are considered to have significant potential for undiscovered orogenic gold and possible base metal mineralisation.
The Archaean geology of the Flicka Lake property primarily comprises mafic and intermediate metavolcanic units that have been intruded locally by a series of gabbroic sills. Metasedimentary units are rare and consist
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of a few isolated outcrops of conglomerate, greywacke and banded iron formations up to 5m in thickness. Local metamorphism ranges from greenschist facies in the southern part of the property, where chlorite and epidote are more prevalent within mafic and intermediate units, to amphibolite facies further north, where hornblende is more abundant.
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Figure 6: Geology, orogenic gold prospects and mineral occurrences, significant historical gold mines and RMX properties within the Meen-Dempster Greenstone Belt, Superior Province, Canada. Geology simplified from 1:250 000 Scale Bedrock Geology of Ontario (https://www.geologyontario.mines.gov.on.ca/publication/MRD126REV1). Gold prospects and occurrences, and historical production figures from Ontario Mineral Inventory (https://www.geologyontario.mndm.gov.on.ca/mines/ogs/databases/OMI.zip).
The greenstones are variably sheared. Three prominent NNE-trending shears cross the property and are associated with the gold mineralisation at the Flicka Zone and Fry Lake #9. Carbonate-chlorite-pyrite and less-common sericite-pyrite alteration is most strong developed in more sheared rocks.
High-grade gold mineralisation at the Flicka Zone comprises three main gold bearing quartz veins containing minor disseminated pyrite, arsenopyrite and tourmaline hosted in a coarse gabbroic sill. The veins strike approximately north-south over a distance of approximately 100m and dip 55° to 65° to the east. Economic gold values have been reported from the mineralised quartz veins and from the metagabbroic country rock, which hosts narrow iron-stained quartz stringers.
Authorised for and on behalf of the Board,
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Mauro Piccini
Company Secretary
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Table 1: Summary of Holes in the Fry Lake Project area and surroundings.
| Hole_ID | **Easting ** | **Northing ** | **RL_m ** | **EOH_m ** | **Azm ** | **Dip ** | Type | **Year ** | Company | Project | OGS -REF | Location |
|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 84-1 | 613793 | 5677585 | 381 | 37.5 | 240 | -45 | Diamond | 1984 | RockmereLakeExploration | FryLakeArea | 52O03NW9035 | FryLake |
| 84-10 | 613872 | 5678614 | 401 | 63.1 | 360 | -45 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake | 52O03NW9037 | Fry Lake |
| 84-11 | 613716 | 5677643 | 384 | 46.3 | 180 | -60 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake Area | 52O03NW9037 | Fry Lake |
| 84-12 | 613714 | 5677686 | 384 | 65.8 | 180 | -60 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake Area | 52O03NW9037 | Fry Lake |
| 84-13 | 613752 | 5677664 | 382 | 37.5 | 180 | -60 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake Area | 52O03NW9037 | Fry Lake |
| 84-2 | 613803 | 5677572 | 381 | 44.5 | 240 | -45 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake Area | 52O03NW9035 | Fry Lake |
| 84-3 | 613810 | 5677558 | 381 | 47.6 | 240 | -45 | Diamond | 1984 | Rockmere Lake Exploration | Fry Lake Area | 52O03NW9035 | Fry Lake |
| 84-4 | 613785 | 5677598 | 381 | 48.2 | 240 | -45 | Diamond | 1984 | Rockmere Lake Exploration | FryLake Area | 52O03NW9035 | FryLake |
| 84-5 | 613757 | 5677616 | 382 | 58.2 | 245 | -60 | Diamond | 1984 | Rockmere Lake Exploration | FryLake Area | 52O03NW9037 | FryLake |
| 84-6 | 613734 | 5677683 | 383 | 82.9 | 360 | -60 | Diamond | 1984 | Rockmere Lake Exploration | FryLake Area | 52O03NW9037 | FryLake |
| 84-7 | 613442 | 5677360 | 383 | 60.7 | 180 | -45 | Diamond | 1984 | Rockmere Lake Exploration | FryLake | 52O03NW9037 | FryLake |
| 84-8 | 613674 | 5678353 | 400 | 67.4 | 360 | -45 | Diamond | 1984 | Rockmere Lake Exploration | FryLake | 52O03NW9037 | FryLake |
| 84-9 | 612986 | 5678351 | 392 | 91.5 | 360 | -45 | Diamond | 1984 | RockmereLakeExploration | FryLake | 52O03NW9037 | FryLake |
| 87-1 | 612030 | 5678370 | 410 | 166.5 | 167 | -50 | Diamond | 1987 | SherrittGordon | FryLake | 52O03NW9039 | FryLake |
| 87-10 | 611860 | 5677670 | 385 | 139.1 | 167 | -50 | Diamond | 1987 | SherrittGordon | FryLake | 52O03NW9039 | FryLake |
| 87-11 | 614590 | 5677250 | 387 | 139.1 | 347 | -50 | Diamond | 1987 | SherrittGordon | FryLake | 52O03NW9039 | FryLake |
| 87-2 | 612200 | 5677780 | 385 | 135.0 | 167 | -50 | Diamond | 1987 | SherrittGordon | FryLake | 52O03NW9039 | FryLake |
| 87-3 | 611600 | 5677520 | 387 | 151.3 | 167 | -50 | Diamond | 1987 | SherrittGordon | FryLake | 52O03NW9039 | FryLake |
| 87-4 | 611400 | 5677510 | 382 | 209.2 | 347 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 87-5 | 611410 | 5677140 | 384 | 137.3 | 210 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 87-6 | 612480 | 5677250 | 385 | 200.1 | 347 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 87-7 | 612560 | 5678310 | 394 | 126.9 | 167 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 87-8 | 614540 | 5677210 | 388 | 230.6 | 347 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 87-9 | 612750 | 5677350 | 389 | 123.8 | 167 | -50 | Diamond | 1987 | Sherritt Gordon | Fry Lake | 52O03NW9039 | Fry Lake |
| 88-1 | 613912 | 5679561 | 411 | 76.6 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | Fry Lake |
| 88-10 | 615094 | 5679594 | 386 | 52.8 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | FryLake |
| 88-11 | 615371 | 5679505 | 385 | 12.2 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | FryLake |
| 88-12 | 615464 | 5679653 | 292 | 13.7 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | FryLake |
| 88-13 | 615192 | 5679561 | 383 | 66.2 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | FryLake |
| 88-14 | 615005 | 5679713 | 389 | 65.0 | 210 | -50 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | FryLake |
| 88-2 | 613924 | 5679601 | 411 | 78.7 | 210 | -55 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-3 | 613870 | 5679600 | 411 | 74.4 | 210 | -45 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-4 | 613870 | 5679600 | 411 | 72.9 | 210 | -60 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-5A | 613804 | 5679612 | 412 | 14.0 | 210 | -45 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-5B | 613810 | 5679629 | 412 | 73.5 | 210 | -45 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-6 | 613623 | 5679713 | 411 | 82.7 | 210 | -45 | Diamond | 1988 | Casabar ResourcesInc | NabemakosekaLake | 52O06SW0003 | FryLake |
| 88-7 | 613524 | 5679625 | 408 | 99.4 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | Fry Lake |
| 88-8 | 614013 | 5679605 | 411 | 101.0 | 210 | -45 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | Fry Lake |
| 88-9B | 614188 | 5679517 | 410 | 31.1 | 210 | -43 | Diamond | 1988 | Casabar Resources Inc | Nabemakoseka Lake | 52O06SW0003 | Fry Lake |
| B-13-71-4 | 628808 | 5674063 | 407 | 7.9 | 20 | -45 | Diamond | 1971 | Cochenour Williams | Bamaji | 52O03NE0020 | Fry McVean |
| B-13-71-4a | 628808 | 5674063 | 407 | 6.1 | 20 | -50 | Diamond | 1971 | Cochenour Williams | Bamaji | 52O03NE0020 | Fry McVean |
| B-13-71-4b | 628808 | 5674063 | 407 | 30.8 | 20 | -60 | Diamond | 1971 | Cochenour Williams | Bamaji | 52O03NE0020 | Fry McVean |
| B-13-71-5 | 629690 | 5674360 | 407 | 37.5 | 20 | -45 | Diamond | 1971 | Cochenour Williams | Bamaji | 52O03NE0020 | Fry McVean |
| B-13-71-6 | 629750 | 5674330 | 409 | 33.2 | 20 | -45 | Diamond | 1971 | Cochenour Williams | Bamaji | 52O03NE0020 | FryMcVean |
| B-14-70-1 | 631155 | 5679092 | 400 | 30.8 | 30 | -45 | Diamond | 1970 | Cochenour Willans | Drum Lake | 52O03NE0025 | Lake Relyea |
| B-14-71-2 | 629762 | 5679066 | 390 | 56.4 | 30 | -45 | Diamond | 1971 | Cochenour Willans | Drum Lake | 52O03NE0026 | Lake Relyea |
| B-15-71-1 | 631283 | 5675617 | 406 | 56.1 | 30 | -45 | Diamond | 1971 | Cochenour Williams | Drum Lake | 52O03NE0027 | FryMcVean |
| B-15-71-2 | 631369 | 5675670 | 406 | 32.8 | 30 | -45 | Diamond | 1971 | Cochenour Williams | Drum Lake | 52O03NE0027 | FryMcVean |
| B-15-71-3 | 631712 | 5675730 | 403 | 43.9 | 30 | -45 | Diamond | 1971 | Cochenour Williams | Drum Lake | 52O03NE0027 | FryMcVean |
| B-37-70-1 | 614976 | 5678779 | 385 | 34.4 | 195 | -60 | Diamond | 1970 | Cochenour Willans GoldMines | NabemakosekaLake | 52O03NW0046 | FryLake |
| B-37-70-2 | 615085 | 5678994 | 387 | 39.0 | 195 | -60 | Diamond | 1970 | Cochenour Willans GoldMines | NabemakosekaLake | 52O03NW0046 | FryLake |
| B-38-71-1 | 613030 | 5677967 | 390 | 76.9 | 345 | -55 | Diamond | 1971 | Cochenour Willans GoldMines | FryLakeArea | 52O03NW0047 | FryLake |
| B-38-71-2 | 612798 | 5677921 | 381 | 32.3 | 345 | -55 | Diamond | 1971 | Cochenour Willans GoldMines | FryLakeArea | 52O03NW0047 | FryLake |
| B-38-71-2A | 612798 | 5677921 | 381 | 30.8 | 345 | -55 | Diamond | 1971 | Cochenour Willans GoldMines | FryLakeArea | 52O03NW0047 | FryLake |
| B-38-72-3 | 611726 | 5678779 | 409 | 61.6 | 180 | -45 | Diamond | 1972 | Cochenour Willans Gold Mines | Fry Lake Area | 52O03NW0044 | Fry Lake |
| B-38-72-4 | 611330 | 5678456 | 400 | 38.4 | 180 | -45 | Diamond | 1972 | Cochenour Willans Gold Mines | Fry Lake Area | 52O03NW0044 | Fry Lake |
| B-39-71-3 | 623763 | 5677760 | 383 | 63.1 | 15 | -55 | Diamond | 1971 | Cochenour Williams | Drum Lake | 52O03NE0029 | Fry McVean |
| B-42-70-1A | 613790 | 5679620 | 412 | 39.7 | 210 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake | 52O03SW0010 | Fry Lake |
| B-42-70-2 | 613868 | 5679332 | 409 | 34.5 | 210 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake | 52O03SW0010 | Fry Lake |
| B-42-70-3 | 613518 | 5679152 | 405 | 18.0 | 210 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake | 52O03SW0010 | Fry Lake |
| B-42-70-3A | 613526 | 5679165 | 405 | 48.2 | 210 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake | 52O03SW0010 | Fry Lake |
| B-42-70-4 | 614468 | 5679501 | 411 | 17.7 | 210 | -50 | Diamond | 1970 | Cochenour Willans Gold Mines | FryLake | 52O03SW0010 | FryLake |
| B-42-70-5 | 614468 | 5679501 | 406 | 17.4 | 210 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | FryLake | 52O03SW0010 | FryLake |
| B-42-72-6 | 613139 | 5679676 | 409 | 38.1 | 210 | -45 | Diamond | 1972 | Cochenour Willans Gold Mines | FryLake | 52O03SW0010 | FryLake |
| B-42-72-6A | 613140 | 5679675 | 409 | 30.8 | 210 | -50 | Diamond | 1972 | Cochenour WillansGold Mines | FryLake | 52O03SW0010 | FryLake |
| B-42-72-7 | 613382 | 5679352 | 406 | 38.4 | 210 | -45 | Diamond | 1972 | Cochenour Willans Gold Mines | FryLake | 52O03SW0010 | FryLake |
| B-43-70-2 | 621890 | 5676430 | 394 | 33.2 | 360 | -45 | Diamond | 1970 | Cochenour Williams | Bamaji | 52O03NW9042 | FryMcVean |
| B-43-70-3 | 622010 | 5677030 | 382 | 45.4 | 360 | -55 | Diamond | 1970 | Cochenour Williams | Bamaji | 52O03NW9042 | FryMcVean |
| B-9-70-1 | 620620 | 5675250 | 389 | 100.3 | 350 | -45 | Diamond | 1970 | Cochenour ExplorationsLimited | Bamaji | 52O03NW0049 | FryLake Stock |
| B-9-70-2 | 620860 | 5675320 | 389 | 81.1 | 350 | -45 | Diamond | 1970 | Cochenour ExplorationsLimited | Bamaji | 52O03NW0049 | FryLake Stock |
| B-9-70-3 | 621090 | 5675320 | 392 | 69.8 | 350 | -45 | Diamond | 1970 | Cochenour ExplorationsLimited | Bamaji | 52O03NW0049 | FryLake Stock |
| B-F-11_70-2 | 613978 | 5678768 | 401 | 27.4 | 180 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake Area | 52O03NW0045 | Fry Lake |
| B-F-11_70-3 | 613768 | 5678290 | 402 | 17.4 | 180 | -50 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake Area | 52O03NW0045 | Fry Lake |
| B-F-11-70-1 | 614025 | 5678526 | 399 | 26.5 | 180 | -45 | Diamond | 1970 | Cochenour Willans Gold Mines | Fry Lake Area | 52O03NW0045 | Fry Lake |
| C-185 | 621925 | 5676570 | 393 | 57.9 | 360 | -45 | Diamond | 1974 | Union Miniere Exp & Mining | Fry Lake | 52O03NW0048 | Fry McVean |
| G-9-70-1 | 620703 | 5674926 | 399 | 80.8 | 350 | -45 | Diamond | 1970 | Cochenour Explorations Limited | Bamaji | 52O03NW0049 | Fry Lake Stock |
| McV-91-01 | 631424 | 5675119 | 411 | 240.5 | 30 | -45 | Diamond | 1991 | Major General Resources | McVean Lake | 52P12SW0001 | Fry McVean |
| McV-91-02 | 633193 | 5673558 | 410 | 313.3 | 15 | -48 | Diamond | 1991 | Major General Resources | Drum Lake | 52P12SW0001 | Fry McVean |
| McV-91-03 | 631318 | 5674188 | 410 | 161.2 | 15 | -50 | Diamond | 1991 | Major General Resources | McVean Lake | 52P12SW0001 | FryMcVean |
| McV-91-04 | 634031 | 5673083 | 406 | 149.1 | 50 | -55 | Diamond | 1991 | Major General Resources | McVean Lake | 52P12SW0001 | FryMcVean |
| McV-92-10 | 631165 | 5674536 | 410 | 155.2 | 15 | -50 | Diamond | 1992 | Major General Resources | Drum Lake | 20000005715 | FryMcVean |
| McV-92-11 | 629868 | 5674674 | 407 | 246.6 | 15 | -45 | Diamond | 1992 | Major General Resources | Drum Lake | 20008073 | FryMcVean |
| McV-92-5 | 631543 | 5674486 | 414 | 280.0 | 17 | -45 | Diamond | 1992 | MajorGeneral Resources | Drum Lake | 20000005715 | FryMcVean |
| McV-92-6 | 631332 | 5674404 | 411 | 246.6 | 15 | -50 | Diamond | 1992 | MajorGeneral Resources | Drum Lake | 20000005715 | FryMcVean |
| McV-92-7 | 631710 | 5674434 | 417 | 164.0 | 15 | -50 | Diamond | 1992 | MajorGeneral Resources | Drum Lake | 20000005715 | FryMcVean |
| McV-92-8 | 632008 | 5674378 | 420 | 243.5 | 195 | -50 | Diamond | 1992 | MajorGeneral Resources | Drum Lake | 20000005715 | FryMcVean |
| McV-92-9 | 631238 | 5674522 | 411 | 167.3 | 15 | -50 | Diamond | 1992 | MajorGeneral Resources | Drum Lake | 20000005715 | FryMcVean |
Datum NAD83 (z15), Source Ontario Geological Survey (OGS)
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Table 2: Analytical Results, threshold ≥160ppb Au
| Hole_ID | **Sample_No ** | **From_m ** | **To_m ** | **Interval_m ** | **Au_ppb ** | Au g/t |
|---|---|---|---|---|---|---|
| 84-1 | 609 | 23.6 | 23.8 | 0.24384 | 19906 | 19.906 |
| 84-3 | 626 | 20.2 | 20.3 | 0.1524 | 14463 | 14.463 |
| 84-3 | 627 | 20.3 | 21.0 | 0.70104 | 9642 | 9.642 |
| 84-2 | 621 | 22.4 | 22.9 | 0.4572 | 8864 | 8.864 |
| 84-4 | 642 | 45.0 | 45.4 | 0.39624 | 3421 | 3.421 |
| 87-8 | 4255 | 7.9 | 8.5 | 0.6096 | 3110 | 3.110 |
| 87-8 | 4291 | 147.8 | 148.1 | 0.3048 | 2488 | 2.488 |
| 84-2 | 620 | 22.0 | 22.4 | 0.36576 | 1866 | 1.866 |
| 87-8 | 4256 | 9.1 | 9.8 | 0.6096 | 1866 | 1.866 |
| McV-92-5 | 32049 | 95.0 | 96.5 | 1.5 | 1600 | 1.600 |
| 84-3 | 628 | 21.0 | 21.9 | 0.9144 | 1244 | 1.244 |
| McV-92-7 | 32170 | 119.2 | 120.3 | 1.1 | 1040 | 1.040 |
| McV-91-3 | 28382 | 69.4 | 70.9 | 1.5 | 1030 | 1.030 |
| McV-91-3 | 28421 | 119.7 | 121.2 | 1.5 | 1000 | 1.000 |
| McV-91-3 | 28373 | 57.4 | 58.9 | 1.5 | 672 | 0.672 |
| 84-4 | 640 | 43.7 | 44.8 | 1.0668 | 622 | 0.622 |
| 84-4 | 641 | 44.8 | 45.0 | 0.21336 | 622 | 0.622 |
| 84-3 | 625 | 19.5 | 20.2 | 0.67056 | 622 | 0.622 |
| 87-11 | 4416 | 27.1 | 28.0 | 0.9144 | 622 | 0.622 |
| 87-11 | 4435 | 113.1 | 113.7 | 0.6096 | 622 | 0.622 |
| 87-8 | 4257 | 9.8 | 10.1 | 0.3048 | 622 | 0.622 |
| 87-9 | 4372 | 93.9 | 94.8 | 0.9144 | 622 | 0.622 |
| McV-92-7 | 32169 | 117.7 | 119.2 | 1.5 | 530 | 0.530 |
| McV-92-7 | 32184 | 139.5 | 140.5 | 1 | 520 | 0.520 |
| McV-91-3 | 28419 | 116.7 | 118.2 | 1.5 | 488 | 0.488 |
| McV-92-5 | 32032 | 71.0 | 71.5 | 0.5 | 430 | 0.430 |
| McV-92-5 | 32060 | 111.0 | 112.5 | 1.5 | 430 | 0.430 |
| McV-92-5 | 32056 | 105.0 | 106.5 | 1.5 | 320 | 0.320 |
| McV-92-8 | 32210 | 94.0 | 95.5 | 1.5 | 320 | 0.320 |
| 84-4 | 632 | 22.9 | 23.8 | 0.97536 | 311 | 0.311 |
| 84-1 | 608 | 22.4 | 23.1 | 0.73152 | 311 | 0.311 |
| 84-1 | 610 | 23.8 | 24.4 | 0.57912 | 311 | 0.311 |
| 87-10 | 4386 | 60.8 | 61.7 | 0.9144 | 311 | 0.311 |
| 87-11 | 4415 | 26.2 | 27.1 | 0.9144 | 311 | 0.311 |
| 87-11 | 4417 | 28.0 | 29.0 | 0.9144 | 311 | 0.311 |
| 87-11 | 4431 | 109.4 | 110.3 | 0.9144 | 311 | 0.311 |
| 87-2 | 1855 | 25.3 | 25.9 | 0.6096 | 311 | 0.311 |
| 87-2 | 1894 | 107.9 | 108.8 | 0.9144 | 311 | 0.311 |
| 87-4 | 4143 | 188.4 | 189.1 | 0.762 | 311 | 0.311 |
| 87-4 | 4081 | 23.5 | 26.2 | 2.7432 | 311 | 0.311 |
| 87-4 | 4101 | 120.1 | 121.0 | 0.9144 | 311 | 0.311 |
| 87-6 | 4200 | 84.6 | 85.0 | 0.4572 | 311 | 0.311 |
| 87-8 | 4259 | 11.0 | 11.9 | 0.9144 | 311 | 0.311 |
| 87-8 | 4297 | 149.7 | 150.0 | 0.3048 | 311 | 0.311 |
| 87-8 | 4298 | 150.0 | 150.3 | 0.3048 | 311 | 0.311 |
| 87-8 | 4325 | 195.4 | 195.8 | 0.4572 | 311 | 0.311 |
| 87-9 | 4371 | 91.1 | 91.7 | 0.6096 | 311 | 0.311 |
| McV-91-3 | 28435 | 134.3 | 135.5 | 1.2 | 284 | 0.284 |
| McV-92-10 | 32402 | 109.5 | 110.0 | 0.5 | 260 | 0.260 |
| McV-91-3 | 28412 | 109.3 | 110.8 | 1.5 | 248 | 0.248 |
| McV-92-6 | 32091 | 138.1 | 139.6 | 1.5 | 244 | 0.244 |
| McV-91-3 | 28434 | 133.8 | 134.3 | 0.5 | 235 | 0.235 |
| McV-91-3 | 28394 | 87.4 | 88.6 | 1.15 | 222 | 0.222 |
| McV-92-10 | 32403 | 110.0 | 110.8 | 0.8 | 220 | 0.220 |
| McV-91-3 | 28383 | 70.9 | 72.4 | 1.5 | 217 | 0.217 |
| McV-91-3 | 28443 | 143.2 | 144.6 | 1.4 | 215 | 0.215 |
| McV-92-6 | 32130 | 207.2 | 208.7 | 1.5 | 214 | 0.214 |
| McV-92-7 | 32177 | 130.5 | 131.5 | 1 | 210 | 0.210 |
| McV-91-3 | 28440 | 139.4 | 140.6 | 1.2 | 204 | 0.204 |
| McV-92-9 | 32357 | 125.5 | 126.5 | 1 | 200 | 0.200 |
| McV-92-6 | 32125 | 197.0 | 198.5 | 1.5 | 197 | 0.197 |
| McV-92-7 | 32178 | 131.5 | 133.0 | 1.5 | 190 | 0.190 |
| McV-92-9 | 32339 | 99.0 | 100.5 | 1.5 | 190 | 0.190 |
| McV-92-11 | 32461 | 197.2 | 198.7 | 1.5 | 180 | 0.180 |
| McV-91-3 | 28442 | 141.7 | 143.2 | 1.5 | 176 | 0.176 |
| McV-92-6 | 32132 | 210.1 | 211.1 | 1 | 167 | 0.167 |
| McV-92-5 | 32057 | 106.5 | 108.0 | 1.5 | 160 | 0.160 |
| McV-92-7 | 32186 | 141.5 | 142.5 | 1 | 160 | 0.160 |
| McV-92-7 | 32187 | 142.5 | 144.0 | 1.5 | 160 | 0.160 |
| McV-92-8 | 32212 | 97.0 | 98.5 | 1.5 | 160 | 0.160 |
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About Red Mountain Mining
Red Mountain Mining Limited (ASX: RMX) is a mineral exploration and development company. Red Mountain has a portfolio of critical minerals including gold, lithium, rare earth and base metal projects, located in Canada, Australia and USA. Red Mountain is progressing its Fry Lake project, based in the strategic Gold district in Ontario, Canada and the Kiabye Gold Project in Western Australia. In addition, Red Mountain’s project portfolio includes the Monjebup Rare Earths Project, and Nevada Lithium Projects.
Competent Person Statement
The information in this announcement that relates to Exploration Results and other technical information complies with the 2012 Edition of the Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves (JORC Code). It has been compiled and assessed under the supervision of contract geologist Mark Mitchell. Mr Mitchell is a Member of the Australasian Institute of Geoscientists and has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken to qualify as a Competent Person as defined in the 2012 Edition of the JORC Code. Mr Mitchell consents to the inclusion in this announcement of the matters based on his information in the form and context in which it appears.
Disclaimer
In relying on the above mentioned ASX announcement and pursuant to ASX Listing Rule 5.23.2, the Company confirms that it is not aware of any new information or data that materially affects the information included in the above-mentioned announcement.
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JORC Code, 2012 Edition - Table 1
1.1 Section 1 Sampling Techniques and Data
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Criteria JORC Code explanation Commentary
Sampling Nature and quality of sampling (e.g. cut Historical Humus (Soil) sampling were
techniques channels, random chips, or specific taken along N-S orientated traverses at
specialised industry standard measurement 100m line spacing and 30m sample
tools appropriate to the minerals under spacings Material was taken from the
investigation, such as down hole gamma humus horizon by Dr Donald Brown
sondes, or handheld XRF instruments, etc). Rock samples were collected from
These examples should not be taken as outcrop by geologists Pettigrew and
limiting the broad meaning of sampling. Dinel from the OGS as representative
Include reference to measures taken to rock samples in the area
ensure sample representivity and the
appropriate calibration of any
measurement tools or systems used.
Aspects of the determination of
mineralisation that are Material to the
Public Report.
In cases where ‘industry standard’ work has
been done this would be relatively simple
(eg ‘reverse circulation drilling was used to
obtain 1 m samples from which 3 kg was
pulverised to produce a 30 g charge for fire
assay’). In other cases more explanation
may be required, such as where there is
coarse gold that has inherent sampling
problems. Unusual commodities or
mineralisation types (eg submarine
nodules) may warrant disclosure of detailed
information.
Drilling Drill type (e.g. core, reverse circulation, Diamond Drilling was done by various
techniques open-hole hammer, rotary air blast, auger, companies using a portable Winky G-15 or
Bangka, sonic, etc) and details (e.g. core Longyear 24 rigs and core sizes EX 7/8in, AXT
diameter, triple or standard tube, depth of 1&3/16in, or AX (30.1mm)
diamond tails, face-sampling bit or other
type, whether core is oriented and if so, by
what method, etc).
Drill sample Method of recording and assessing core and Core logged onsite, logs available, interval core
recovery chip sample recoveries and results assessed. loss recorded but no recovery percentages.
Measures taken to maximise sample Historical drilling limited information
recovery and ensure representative nature relationships not defined.
of the samples.
Whether a relationship exists between
sample recovery and grade and whether
sample bias may have occurred due to
preferential loss/gain of fine/coarse
material.
Logging Whether core and chip samples have been Drilling not to resource definition level.
geologically and geotechnically logged to a Rock and soil sampling is not used for resource
level of detail to support appropriate estimation.
Mineral Resource estimation, mining
studies and metallurgical studies.
Whether logging is qualitative or
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Criteria JORC Code explanation Commentary
quantitative in nature. Core (or costean,
channel, etc) photography.
The total length and percentage of the
relevant intersections logged.
Sub- If core, whether cut or sawn and whether Soil sampling was collected from
sampling quarter, half or all core taken. predetermined points based on
techniques If non-core, whether riffled, tube sampled,
generally a 100m spacing, no
and sample rotary split, etc and whether sampled wet
lakes/sediment was sampled. Rock chip
preparation or dry.
sampling was biased towards outcrop
For all sample types, the nature, quality and
that was representative.
appropriateness of the sample preparation
technique. Humus and rock sample taken raw, no
Quality control procedures adopted for all other details provided.
sub-sampling stages to maximise QAQC procedures unknown
representivity of samples. Core treatment is not recorded
Measures taken to ensure that the sampling
is representative of the in situ material
collected, including for instance results for
field duplicate/second-half sampling.
Whether sample sizes are appropriate to
the grain size of the material being
sampled.
Quality of The nature, quality and appropriateness of Humus samples were analysed by aqua regia
assay data the assaying and laboratory procedures while rock samples were treated by whole
and used and whether the technique is
rock digestion for major and trace elements
laboratory considered partial or total.
by XRF and ICP MS.
tests For geophysical tools, spectrometers,
Drill samples were fire assayed for gold and in
handheld XRF instruments, etc, the
some cases XRF for base metals.
parameters used in determining the
analysis including instrument make and Fire Assay is considered an appropriate
model, reading times, calibrations factors method for gold.
applied and their derivation, etc. Quality control procedures , if any, are not
Nature of quality control procedures
documented.
adopted (e.g. standards, blanks, duplicates,
external laboratory checks) and whether
acceptable levels of accuracy (i.e. lack of
bias) and precision have been established.
Verification The verification of significant intersections Unknown what verification sampling and
of sampling by either independent or alternative assaying was done if any.
and company personnel.
assaying The use of twinned holes.
Documentation of primary data, data entry
procedures, data verification, data storage
(physical and electronic) protocols.
Discuss any adjustment to assay data.
Location of Accuracy and quality of surveys used to Data points were based on measurements
data points locate drill holes (collar and down-hole from claim boundaries and these were
surveys), trenches, mine workings and other converted to NAD83 UTM 15N.
locations used in Mineral Resource No DEM Topographic control was used, the
estimation. ground is relatively flat.
Specification of the grid system used. No mineral resource estimation was
Quality and adequacy of topographic conducted.
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Criteria JORC Code explanation Commentary
control.
Data Data spacing for reporting of Exploration Sample spacing (100m) is considered
spacing and Results. appropriate for initial first pass sampling.
distribution Whether the data spacing and distribution Being exploration results no work was
is sufficient to establish the degree of considered sufficient for any ore
geological and grade continuity appropriate determinations.
for the Mineral Resource and Ore Reserve No analytical compositing has been applied.
estimation procedure(s) and classifications
applied.
Whether sample compositing has been
applied.
Orientation Whether the orientation of sampling Most drill holes were sighted on targeting EM
of data in achieves unbiased sampling of possible conductors interpreted from ground surveys
relation to structures and the extent to which this is with orientation based on conductor shape or
geological known, considering the deposit type. ground mapping structures where available.
structure If the relationship between the drilling Exploration drilling so bias is not material.
orientation and the orientation of key
mineralised structures is considered to have
introduced a sampling bias, this should be
assessed and reported if material.
Sample The measures taken to ensure sample Sample security measures were not reported.
security security.
Audits or The results of any audits or reviews of It is unrecorded if audit or reviews of sampling
reviews sampling techniques and data. techniques and data has been undertaken.
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1.2 Section 2 Reporting of Exploration Results
(Criteria listed in the preceding section also apply to this section.)
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Criteria JORC Code explanation Commentary
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| Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
Criteria JORC Code explanation Commentary |
|---|---|---|
| Mineral tenement and land tenure status |
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
Four Active Mining Titles Claim Numbers are 893983 to 894170, 855170, 910158-910160 (192 claims) for Fry Lake Fry Lake Stock Relyea Porphyry Fry -McVean Shear Currently in RMX 100% Canadian subsidiary Red Mountain Mining CA Ltd There are no Known impediments to exploration, not in any “Mining Activity Restriction” areas. Negotiations with the First Nations are underway. |
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Criteria JORC Code explanation Commentary
Exploration Acknowledgment and appraisal of Limited exploration done in the licences,
done by other exploration by other parties. mainly rock chip sampling by the Ontario
parties Geological Survey (Open File Report 6208 in
2008)
Geology Deposit type, geological setting and style No deposit identified in the tenements, but
of mineralisation. lode style gold mineralisation is reported in
the broader area associated with shear zones
and sericite pyrite alteration, structurally
controlled by larger crustal deformational
features; underlying geology is the Meen-
Dempster Archaean Greenstone Belt.
Drill hole A summary of all information material to See tables in text.
Information the understanding of the exploration No material information has been excluded
results including a tabulation of the
following information for all Material drill
holes:
o easting and northing of the drill hole
collar
o elevation or RL (Reduced Level –
elevation above sea level in metres) of
the drill hole collar
o dip and azimuth of the hole
o down hole length and interception
depth
o hole length.
If the exclusion of this information is
justified on the basis that the information
is not Material and this exclusion does not
detract from the understanding of the
report, the Competent Person should
clearly explain why this is the case.
Data In reporting Exploration Results, No data aggregation has been applied
aggregation weighting averaging techniques,
methods maximum and/or minimum grade
truncations (e.g. cutting of high grades)
and cut-off grades are usually Material
and should be stated.
Where aggregate intercepts incorporate
short lengths of high grade results and
longer lengths of low grade results, the
procedure used for such aggregation
should be stated and some typical
examples of such aggregations should be
shown in detail.
The assumptions used for any reporting of
metal equivalent values should be clearly
stated.
Relationship These relationships are particularly No relationship is made between
between important in the reporting of Exploration mineralisation width and intercept lengths
mineralisation Results.
widths and If the geometry of the mineralisation with
intercept respect to the drill hole angle is known, its
lengths nature should be reported.
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| Criteria | JORC Code explanation | Commentary |
|---|---|---|
| If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. ‘down _hole length, true width not known’). _ |
||
| Diagrams | Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. |
Appropriate location diagram is presented in the text. |
| Balanced reporting |
Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. |
Only pertinent results are given as due to the relevance of the announcement. |
| Other substantive exploration data |
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples – size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
There is no other substantive exploration data provided or withheld as this announcement deals with this early phase exploration target. |
| Further work | The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling). Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
VTEM is under consideration given its effectiveness in the local area. Sampling is proposed in the areas of know alteration associated with intrusive contacts, lithological changes, shear zones and other structural targets . |
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