Ontario Mineral Inventory

Ontario Geological Survey
Permanent Link to this Record: MDI52K13NW00006

Record: MDI52K13NW00006

General

Mineral Record Identification
Record Name(s) Faulkenham Lake - 1930, New Faulkenham Mines Ltd - 1930
Related Record Type Partial
Related Record(s)
Record Status Developed Prospect Without Reported Reserves or Resources
Date Created 1984-Apr-18
Date Last Modified 2023-May-12
Created By
Revised By

Commodities

Primary Commodities: Gold



Location

Township or Area: Baird

Latitude: 50° 56' 25.13"    Longitude: -93° 56' 7.09"

UTM Zone: 15    Easting: 434286.577   Northing: 5643603.996    UTM Datum: NAD83

Resident Geologist District: Red Lake

NTS Grid: 52K13NW

Point Location Description: Shaft symbol in Claim KRL 12881

Location Method: Conversion from MDI

Access Description: The New Faulkenham Mines Ltd. property is located in Baird Township 1050 metres south-southwest of the community of Starrett-Olsen and the past producing Starrett-Olsen Mine. An old road extends from the Starrett-Olsen townsite approximately 2150 m to the New Faulkenham property.



Exploration History

The property is part of the land package obtained from Madsen Gold Corp and held by Claude Resources Ltd. During the 1930s the property was explored by a shaft 344 feet deep with levels at 125, 225 and 325 feet, with a total of 1445 feet of drifts and crosscuts. There are published reserves of 15,000 tons of 0.428 ounce per ton gold (Holbrooke 1958). No production was recorded from this site but an ore dump was left at the shaft. This material was milled at the Madsen mill by Madsen Gold Corp. 2019-2021: Pacton Gold completed across the Red Lake Gold Project that includes Faulkenham a high-resolution magnetic, VLF, EM and Lidar survey and soil sampling. 10 drill holes were drilled across an IP anomaly at the property, extending mineralization across a 600 m strike length.


Assessment Work on File

Assessment Work on File
Office File Number Online Assessment File Identifier Online Assessment File Directory
20000020162 20000020162
20000019950 20000019950
20000020223 20000020223

Geology

Province: Superior

Subprovince: Uchi

Terrane: North Caribou

Domain: Uchi

Belt: Red Lake

Geological Age: Archean  



Geology Comments

Dec 07, 2005 (C Storey) - The New Faulkenham veins are part of a sheared and altered zone striking 110 and varying in width and degree of alteration. Alteration consists of silicification and sulphidation accompanied by epidote veinlets and pink hematite staining. The area is underlain by east-northeast striking intermediate to felsic rocks mapped as fragmental and grouped with the Confederation Assemblage. The host rock exposed at the surface is sheared dark grey feldspar porphyry, at least in part a felsic crystal tuff, similar in appearance to felsic rocks exposed on Highway 618 at Madsen. The rock at New Faulkenham contains feldspar phenocrysts but no quartz phenocrysts and is more highly deformed. Flattened wispy fragments appear on the weathered surface. The foliation is visible but not intense enough to make the rock schistose. Biotite is present in the foliation surfaces. A trace amount of euhedral pyrite is present. Mapping by Ferguson (1965) shows an east striking granodiorite dike immediately south of the main vein zone. The granodiorite is fine-grained, pink to deep pink in colour and has biotite as the mafic mineral phase. Epidote is present as veins cutting both rock types and as isolated clusters in the granodiorite. The main vein is white to light grey glassy quartz with variable amounts of pyrite and small amounts of chlacopyrite, sphalerite and galena. The host rock is silicified and also carries small amounts of sulphide minerals. Samples from the remaining material from the ore dump showed variable gold values accompanied by high base metal assays. The veins, as exposed in the shaft area trenches look quite barren while the host is mineralized with small amounts of pyrite and other sulphides. Assays of several quartz vein samples indicated that this is not the case. In the area to the east of the shaft the host rock is not apparently mineralized but is still anomalous in gold.




Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
Mafic lava flow-unsubdivided 1 Latite Adjacent
Granodiorite 2 Adjacent
Mylonite/Fault Gouge/Pseudotachylite 3 Shear Zone Contains

Mineralization

Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Alteration Style
5ChalcopyriteEconomicOre
10GalenaEconomicOre
15PyriteEconomicOre
20SphaleriteEconomicOre

Mineralization Comments

May 12, 2023 (Paul Malegus) - Diamond drilling in 2020 intersected mineralization associated with alteration and structures. Typically 1-2% disseminated pyrite and pyrrhotite, with local stringers of chalcopyrite and pyrrhotite up to 10%. The best Au intercept was 1.3 g/t over 0.8 m in hole PAC-20-045.


Sep 01, 2022 (Q Unknown) - A series of old trenches, pits and stripped areas on a property scale map by Horwood (1945) show the main vein exposed for 900 feet and two more veins to the north exposed for 125 and 60 feet each. The main vein strikes 107 and dips 85N, the vein pinches and swells with a maximum reported width of 24 inches.



Alteration Comments

May 12, 2023 (Paul Malegus) - Mineralization is associated with pervasive silica, sericite and potassium alteration.




Mineral Record Details

Reserves or Resources Data
Zone Year Category Tonnes Reference Comments Commodities
Faulkenham Lake 1958 Unclassified 13600 OFR6180, Table 14 (Holbrooke 1958) Grade: 14.67 g/t Au (15 000 tons of 0.428 opt Au) Gold 14.67 g/t

References

File - Resident Geologist files AF RL 1958 Baird #13

Publication Number: Date: 1996

Author: Holbrooke, G.L.

Publisher Name:

Location: Red Lake RGP


Map - Baird Township, eastern part, Kenora District

Publication Number: M2072 Scale: 1:12,000    Date: 1997

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines

Location:


File - Resident Geologist files AF RL 1963 Baird #21

Publication Number: Date: 1996

Author:

Publisher Name:

Location: Red Lake RGP


Part - Geology and mineral deposits of the Red Lake area

Publication Number: ARV49-02 Page: 103-106  Date: 1998

Author: Horwood H.C.

Publisher Name: Ontario Dept. of Mines

Location:


MonoMap - Geology of the eastern part of Baird Township, District of Kenora

Publication Number: R039 Page: 28-29  Date: 1997

Author: Ferguson S.A.

Publisher Name: Ontario Dept. of Mines

Location:


Mono - Report of Activities 2000, Resident Geologist Program, Red Lake Regional Resident Geologist Report: Red Lake and Kenora Districts

Publication Number: OFR6047 Date: 2001

Author: Lichtblau A.F., Raoul A., Ravnaas C., Storey C.C., Kosloski L., Debicki R.L., Drost A.P.

Publisher Name: Ontario Geological Survey

Location:


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For detailed information regarding this mineral record please contact the Red Lake Resident Geologist District Office