Langis-Hudson Bay Silver-Cobalt Project Summary

The Langis Mine (past producer of high-grade silver) Project is located near Cobalt in eastern Ontario, 15 km north from Temiskaming shores and 500 km north from Toronto. Highway 65 runs through the property and many secondary roads are established providing year round access. Power, railways, mills, a permitted refinery and assay lab are located in or near the site.

The Langis Project represents unique opportunity to a silver district that has not seen much modern exploration techniques applied. New discovery potential is high and a strong possibility exists to generate mineral resources from extensions to historical workings and new exploration.

The Langis Mine has produced historically over 10.4M oz Ag with a recovered grade of ~25 oz/t Ag from shallow depths and 358,340 lbs of Cobalt. (see production history)

The Hudson Bay Mine has produced historically 6.4M oz of Ag at 123 opt silver and 185,570 lbs of Cobalt from 58,000 tons.

The Langis and the Hudson Bay Projects do not currently contain any mineral resources or mineral reserves.

View video: Overview of Silver-Cobalt Project

2018 Hudson Bay Silver-Cobalt Drill Results

Highlights from drill holes

  • Drill hole HB18-01 intersected 1.00% Co, 11.10 g/t Ag, 0.95% Cu and 0.72% Ni or 1.25% CoEq over 0.80 metres from 52.20m depth
  • Drill hole HB18-03 intersected 0.28% Co (0.34% CoEq) over 1.83 metres from 53.17m depth
  • Drill hole HB18-06 intersected 6.70 metres of 625.80 g/t Ag, 0.26% Cu, 0.45% Zn and 0.12% Pb (937.29 g/t AgEq) from 36.00m depth
  • Drill hole HB-18-04 intersected 3.00m of 0.22% Co and 0.48% Cu, 17.3 g/t Ag (0.25% CoEq) from 46.00m depth
  • Drill hole HB-18-05 intersected 0.71% Co, 10.3 g/t Ag, 0.46% Ni, 0.37% Zn (0.80% CoEq) over 1.00 metres from 56.00m depth
  • Drill hole HB18-07 intersected 5.00m of 236.36 g/t Ag, 0.04% Co including 2,050 g/t Ag and 0.42% Co (2.24% CoEq) over 0.50 metres from 56.00m depth

Hudson Bay Location Map:

To date, the Company has drilled approximately 1,182 metres at Hudson Bay. Drilling was designed to test possible extensions of the previously mined cobalt and silver mineralization. The reported drill holes have confirmed the presence of additional cobalt and silver mineralization at the Hudson Bay project.

A summary table of assay results from the first three holes:

*Cobalt Equivalent values (CoEq) were calculated using the formula CoEq = $17 x Ag g/t ÷ 31.104 + $3 x % Cu ÷ 100 x 2204.63 + $28 x % Co ÷ 100 x 2204.63 + $5.50 x % Ni ÷ 100 x 2204.63 ÷ $28 ÷ 2204.63*100. This method assumes full metal recoveries. Metal prices used in this calculation include: $17 per ounce for Ag, $3 per pound for Cu, $5.5 per pound for Ni and $28 per pound for Co. The true width of the veins has not been determined at this time.

Hole HB18-01 intersected 1.00% Co, 11.10 g/t Ag, 0.72% Ni and 0.95% Cu over 0.80 metres from 52.20 meters. The hole was drilled to a total depth of 177 metres (Azimuth: 1900, DIP: -400). Mineralization generally consists of cobalt and nickel minerals as disseminated, veinlets to centimetres wide veins and is hosted in locally brecciated and chloritized cherty mafic-intermediate pillows (Archean Volcanics). Locally, pyrite, chalcopyrite and sphalerite are also present.

Hole HB18-02 returned 13.00 metres of 16.20 g/t Ag starting at 18.00 metres. The hole was drilled to a depth of 120 metres (Azimuth: 1650, DIP: -390). Mineralization consists mainly of silver minerals with elevated cobalt values of up to 804 ppm (0.08%) and is hosted by the Huronian conglomerate sedimentary unit.

Hole HB18-03 returned 0.28% Co, 8.30 g/t Ag, 0.15% Ni and 0.18% Cu over 1.83 metres starting at 53.17 metres. The hole was drilled to a total depth of 192 metres (Azimuth: 1850, DIP: -380). The hole was designed to test the extension on strike of the cobalt mineralization intersected in Hole 01. The cobalt mineralization is hosted in locally brecciated and chloritized cherty mafic-intermediate volcanic pillows and consists of disseminated cobalt minerals as well as fine-to-medium grained intergrown cobalt minerals accumulated along pink carbonate-quartz vein walls. Fine grained disseminated chalcopyrite and nickel minerals are observed throughout brecciated and sheared host rock proximal to veinlets.


Significant cobalt mineralization was intersected in drill holes HB-18-04 and HB-18-05 and consists of cobalt, nickel and copper minerals as disseminated and centimeters wide veinlets. The mineralization is hosted in locally brecciated and chloritized cherty mafic-intermediate pillows (Archean Volcanics). It appears that the cobalt mineralization intersected in drill holes 04 and 05 are part of a northwest trending cobalt mineralization system that was also intersected in holes 01 and 03  that wasn’t previously mined out.

*Cobalt Equivalent values (CoEq) were calculated using the formula CoEq = $17 x Ag g/t ÷ 31.104 + $3 x % Cu ÷ 100 x 2204.63 + $28 x % Co ÷ 100 x 2204.63 + $5.50 x % Ni ÷ 100 x 2204.63 ÷ $28 ÷ 2204.63*100. This method assumes full metal recoveries. Metal prices used in this calculation include: $17 per ounce for Ag, $3 per pound for Cu, $5.5 per pound for Ni and $28 per pound for Co. **Silver Equivalent values (AgEq) were calculated using the formula AgEq = 17 x Ag g/t ÷ 31.104 + $3 x % Cu ÷100 x 2204.63 +28 x % Co ÷ 100 x 2204.63 + 5.50 x % Ni ÷ 100 x 2204.63 ÷17 x 31.104. This method assumes full metal recoveries.

Drill hole HB-18-06 was drilled 76 metres northwest from drill hole HB-18-01 (1% Co over 0.8m reported on February 20, 2018 news release) and was successful in identifying silver and copper mineralization. See below highlights of the assays results from drill hole HB-18-06.

Drill hole HB-18-07 was designed to test the extension to the south of the silver-cobalt mineralization historically mined by previous operators. The drill hole intersected significant silver-cobalt mineralization and consisted of 2,050 g/t Ag and 0.42% Co over 0.5 metres. The mineralization consists of cobalt and silver minerals associated with chalcopyrite and arsenopyrite hosted in Huronian conglomerate.

Assays highlights from holes HB-18-07 to HB-18-10.

Chairman and CEO of Brixton, Gary R. Thompson stated, “We continue to have success from our first drill campaign at the Hudson Bay project. The intercepts are at shallow depths 36 to 57 metres deep. For reference 1% cobalt is equivalent to 12% copper or 1,600 g/t silver. We see the potential for both high grade narrow veins and broad low-moderate grade disseminated mineralized zones.”

Quality Assurance & Quality Control

Sealed samples were shipped by the Company geologists to ALS Minerals preparation lab in Sudbury, Ontario. ALS Minerals Laboratories are registered to ISO 9001:2008 and ISO 17025 accreditations for laboratory procedures.  Blank, duplicate and certified reference materials were inserted into the sample stream. Analysis for gold was done by Fire Assay with AA finish.  All other elements were analyzed by Aqua Regia Digest with ICP-AES finish. Cobalt over-limits were analyzed with Sodium Peroxide Fusion and AES finish. Silver over-limits were analyzed by fire assay with gravimetric finish. Base metal over-limits were analyzed with Aqua Regia Digest and AES finish. A copy of the QAQC protocols can be viewed here.

Mr. Sorin Posescu, P.Geo., is a Qualified Person as defined under National Instrument 43-101 standards and has reviewed and approved this update.

2017 Langis-Hudson Bay Silver-Cobalt Project Exploration Summary

Historical data compilation continues for the Langis area. Following the acquisition of the Penna lands from Agnico at the Langis site, four rock grab samples from the Penna #7 shaft dump area were submitted for analysis. The table below provides details which returned up to 18% silver and 16% Cobalt. Samples contained abundant native silver.

Langis Penna Shaft #7 Dump Rock Samples:

The actual location or source of the sampled material is unknown; however, it was likely sourced from underground workings between the #7 and #6 shaft. The qualified person has not done sufficient work to verify the sample locations. The grab samples by nature are selective samples and do not represent grades throughout the property. Cobalt was analyzed using four acid digestion and the silver was analyzed by Fire Assay Fusion and Gravimetric Finish and since the samples exceeded the upper limit of 10,000 ppm the samples were treated as concentrate by ALS Minerals.

Brixton added 178 hectares of mineral title lands to its Langis Project. The one hundred percent interest was acquired from Mid-North Engineering Services Ltd for consideration of 150,000 common shares of Brixton and $5,000. The title is subject to a 1% NSR in favour of the vendor where Brixton holds the right to purchase 0.5% NSR for $250,000.

The Langis Project is drill ready with both brownfield and greenfield high-grade Ag-Co targets. Subject to available funding the Company plans to conduct additional drilling at its Langis and Hudson Bay Projects this fall and winter season.


Brixton Metal’s mineral title holdings in the Silver-Cobalt Camp is 2,516 hectares. The high-grade silver mineralization occurs as steeply-dipping veins within any of the three main rock types: Archean volcanics, Coleman Member sediments and Nipissing diabase.

Archean Keewatin: These rocks comprise both metavolcanics and metasediments.  The volcanics are most commonly intermediate to mafic pillowed and massive flows.  Between flows, deep-water sedimentation prevailed with cherty and pyroclastic sediment laid down.  These interflow sediments are commonly rich pyrite, pyrrhotite, chalcopyrite, galena, and sphalerite. Throughout the area, the volcanics are intruded by various mafic and ultra-mafic dikes.

Algoman: A large hornblende syenite pluton intruding the mine property host potential for gold mineralization but has yet to see much exploration attention.

Proterozoic: Huronian Supergroup: Huronian rocks comprise the majority of exposed outcrop on the Langis property and consist of gently-dipping, unaltered clastic, glacially-derived sediments unconformably overlying the older Keewatin volcanic and intrusive rocks (Lowes, 1963).These sediments form the Coleman Member of the Gowganda Formation and consist of para- and ortho-conglomerates, pebbly sandstone and greywacke, and thinly-bedded argillites.

Early Proterozoic (Keewenawan): Rocks of this age are represented by the Nipissing diabase sill, a prominent and important rock type in the Cobalt Basin. The diabase intrudes in the form of extensive sheets as well as less prominent dikes and plugs.



The earliest structural event resulted in isoclinal folding of Keewatin volcanics and interflow sediments during the Kenoran Orogeny 2.5 billion years ago (Jambor, 1971a). Precambrian faults, fractures,and joints observed within the mine exhibit variable dips.

Regional faults occur as prominent north to northwest structures which extend for hundreds of kilometres and weak northeast-trending sets (Andrews et al., 1986).  Many smaller faults are present locally and are likely related to these large-scale faults. The major faults are believed to have been active in late Archean times; before, during, and after Huronian sedimentation; and during and after intrusion of the Nipissing diabase (Andrews et al., 1986).  Post-diabase activity is considered to be a possible mechanism for creating the structures hosting the silver-cobalt vein systems which are so important to the Cobalt camp (Andrews et al., 1986).


Generally, distribution of this alteration is within approximately 100m of the Nipissing diabase contacts wherever necessary conditions occur (Jambor, 1971d).  Carbonate is the most common gangue as calcite and dolomite and quartz is associated with the veins.

Economic Geology

Owsiacki (1988) indicates:

“Significant highgrade silver intersections have been recovered from within all three rock types being Nipissing Diabase, Coleman sediments, and, Archean volcanics at the western margin of this trough. One of the best assay to date is 50 ounces over 9.45 m, intersected in the volcanic rocks.”

The most important ore mineral is native silver and secondary metals are cobalt, nickel and copper.

All silver bearing veins in the Langis Mine area are steeply-dipping and are categorized as either single-vein or multiple-vein type structures (Jerome, 1969).


Silver-Cobalt Project – Structural Targets Map:

July 2016 Drilling Maps

Silver-Cobalt Project – Drilling Map:

Silver-Cobalt Project – Drilling Map:

Silver-Cobalt Project – Long Section Map:

Langis Mine Ore (photo source Cobalt Museum, Thompson 2015)

Silver recovery estimates range from 88% to 98% based on historical records.  IP resistivity and chargeability surveys over the Langis area by Canagco in 2012 image variably elongated and steeply dipping apparent structures. Drill testing will be needed to confirm that targets are hosting mineralization. Favorable geology exists for gold mineralization related to shear zones and syenite intrusions in the northern area of the project not previously explored.

The Langis project will benefit greatly from new knowledge and different views and the use of 3D modelling.  Basement structures offer new discovery potential for both silver & gold.

Langis Assay Results:

Silver Camp History

The camp produced historically over 420Moz of silver.  One of the reported mine workings from the Cobalt camp reached 255,146 g/t Ag or 9,000 oz/t Ag over 0.36 metres. This single stope at the 30m level on this vein produced 4.5Moz Ag.

The picture to the right shows some of the headframes established within the Cobalt mining camp (photo source: Cobalt museum).  While today most of the mine sites have been reclaimed or are under ongoing reclamation.

Silver was discovered at Cobalt in 1903 while the Timiskaming and Northern Ontario Railway was being constructed from North Bay to develop the agricultural land in the New Liskeard area. Fred LaRose, a blacksmith employed in the construction of the railway, is credited with the first discovery, but the first application for claims, filed on August 13, 1903, was made by J.H.McKinley and E.F.Darragh, subcontractors who supplied ties for the railroad. They found silver-bearing float at the south end of Cobalt Lake. The first assay results showed bismuth but no silver. McKinley subsequently sent the ore for assay to McGill University, and was informed by Dr. Milton Hersey of Montreal that the ore contained 4,000 ounces of silver per ton. Dr. Willet G. Miller, Ontario’s first provincial geologist, visited the area in November 1903 and found that four veins had been located, three very rich in silver. In addition, Tom Hebert had staked the property that later became the Nipissing Mine. Dr. Miller reported the news through an article in the Mining Journal of New York and through an Ontario Bureau of Mines publication. The final discovery in 1903 was made by Neil King who staked the property on which the O’Brien mine was to rise in 1906 and to continue production without a break until 1966 (Zoldy 2006).

Native silver from Langis Mine:

Information Sources: Cobalt Museum Thompson 2015; Technical Report on the Langis Project by Dale R. Alexander, P.Geo, May 17, 2013; Approved Filing Statement for Everfront Ventures Corp July 31, 2013; Annual Report, Agnico Eagle Mines 1987; Interim Report, Agnico Eagle Mines Q2-1986; Agnico Eagle Mines, Langis Mine-New Mine Site, Plan & Section 1987;