Ontario Geological Survey
Permanent Link to this Record:
MDI42D14SE00057
Record Name(s) | McKenna-McCann Prospect - 1921, Two Macs - 1991, Morgain Mineral - 1983, Cook Lake Gold Mines Ltd. - 1937, Acker Property - 1972, Antelope Mine Syndicate - 1946, P.J. Sullivan Property - 9999, McKenna-McCann North - 9999, Cabin Carbonate Vein - 1989 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1991-Mar-31 |
Date Last Modified | 2023-Aug-03 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Copper, Silver, Lead, Sulphur/Pyrite
Township or Area: Priske
Latitude: 48° 49' 50.17" Longitude: -87° 13' 57.48"
UTM Zone: 16 Easting: 482927 Northing: 5408651 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 42D14SE, 42D14SW
Point Location Description: Shafts, diamond drill holes, trenches, stripped area.
Location Method: Conversion from MDI
Access Description: The property is located about 400 m west of Big Duck Creek between Hollinger Lake and the Schreiber Pyramid showings, approximately 5 km northeast of Schreiber in Priske Township. (claim TB 28130, claim map G 631, Priske Twp). Access may be gained using a 4x4 road that extends north and east of Schreiber to the old workings. Branches of this road lead to the southeast 2.5 km from north of Cook Lake. Secondary access is achieved by foot from Highway 17 following the existing trail that passes just west of the Gold Range property to the southeast end of Von Lake.
1921: Rich veins were first reported southeast of Cook Lake. 1934: Claims were staked by F.A. McKenna, D.T. McCann, and H. O'Brien. A discovery was made by McKenna and McCann in the northeast corner of TB12881. 1935: Trenching and stripping conducted. Property was optioned to Dumond Mining and Exploration Company Ltd. who then initiated a third party option with T.A. Johnson. T.A. Johnson drilled several holes under the main showing. 1937: Cook Lake Gold Mines acquired the property. Bulk sampling was performed; Harcourt of the Ontario Department of Mines identified 4 parallel veins; 2 compartment shaft initiated at main showing. 1938: Main vein length established at 183 m; Inspector of Mines shut down the shaft because of contraventions of the Mining Act. Cook Lake Gold Mines discontinued operations due to lack of funds. 1940: 17 claims cancelled. 1941-1972: Claim TB28130 was patented in 1941, then changed hands several times. 1946: J.D. Grant purchased the Cook Lake Mine property and formed the Antelope Syndicate. During winter mining operations, C. Martin shot J.D. Grant and A. Duchesneau at the Antelope Mine (McKenna-McCann). It came open in 1961, and was staked. 1972-77: Extensive mechanical work undertaken by W. Acker; shaft was dewatered and sampled. 1983: Morgain Minerals acquired the property and carried out line cutting and geological mapping. 1984: Channel sampling conducted for Morgain Minerals. 1985: RTC Precious Metals Inc. carried out stripping, trenching, road dev't, and minor property dev't. Minor tonnage was reportedly removed. 1986: Jim Kraehling bought the property from W. Acker. 50 tons of ore was bulk sampled. 1987: R. Otto bought the property. 1988: R. Otto drilled 1 DDH totalling 31.7 m. 1989: Acker and Otto stripped, trenched and sampled SE of the McKenna-McCann property; extensive carbonate alteration discovered and named the Cabin Carbonate Zone. 1990: The W3 vein system was discovered. 1991: W3 veins were stripped and trenched; McKenna-McCann shaft was dewatered. 1992: Acker and Otto died of CO poisoning while dewatering the shaft. 1993: McKenna-McCann property held by the estate of R. Otto. The W3, W3 Extension and Cabin Carbonate Zone held by the estate of W. Acker. 1995: Property optioned to RJK Explorations Ltd. 1998: The property was staked by A. Wing. 1999: A. Wing contracted C. Larouche to carry out a small mapping and sampling program. 2002: S. Kravchik carried out prospecting and sampling. 2007 & 2009: O. Kravchik contracted G. Daniels to do prospecting and sampling. 2010: O. Kravchik contracted Fladgate Exploration to do a soil sampling program. 2017: First Minerals Exploration Ltd. carried out channel sampling.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
2.6364 | 42D14SE0081 | 42D14SE0081 |
20 | 42D14SE0060 | 42D14SE0060 |
2.20646 | 42D14SE2005 | 42D14SE2005 |
2.46904 | 20000005982 | 20000005982 |
63.4254 | 42D14SE0079 | 42D14SE0079 |
63.5565 | 42D14SE0052 | 42D14SE0052 |
OP91-369 | 42D14SE0105 | 42D14SE0105 |
2.24365 | 42D14SE2008 | 42D14SE2008 |
2.42985 | 20000004367 | 20000004367 |
2.38671 | 20000003110 | 20000003110 |
2.58225 | 20000015121 | 20000015121 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Schreiber-Hemlo
Geological Age: Archean
Dec 07, 2005 (B Schnieders) - (See Nelson).
Dec 07, 2005 (B Nelson) - The general geology consists of predominantly mafic, spherulitic pillowed metavolcanic flow rocks, and minor iron formation which have been intruded by metagabbro and metadiorite dykes, lamprophyre dykes and small quartz feldspar porphyry stocks or dykes. Pillow cusps indicate tops to the northeast. Air photo interpretation and field evidence suggest several major northwest trending lineaments, including a Big Duck Creek Hays Lake lineament, Hollinger Lake lineament and a Craft Lake Lamont Lake lineament. A secondary or minor fault set trending southwest northeast, and occasionally north south is present within this area. This conjugate fault set appears common in areas of gold mineralization. The northwest trending shear zones are sub parallel to the long axis of the stretched pillows. An approximate 5 by 3 km rectangular parcel of land in this area, bounded by the Croft Lake lineaments discussed is highly recommended for prospecting and exploration. The quartz vein system at the McKenna McCann property displays many similarities in style and appearance to quartz veins at the Johnston McKenna, Schreiber Pyramid, W3 and W3 Extension properties. Gold bearing quartz veins occupy shear zones or shear dilatant zones within metavolcanic rocks. The host metavolcanic rocks are predominantly mafic pillow flows, however minor massive flows are present. The metavolcanic rocks commonly display carbonatization in the vicinity of gold mineralization. A parallel set of 4 en echelon quartz veins (Nos. 8 through 11) strike to the northwest, varying from 180 degrees to 330 degrees and dip 55 degrees to 70 degrees SW. The zone containing the veins is approximately 25 m wide. The zones vary from composite veins to individual veins which are lenticular and average 33 cm in width and have been traced along strike for up to 225 m. The veins commonly display a crack seal or ribbon texture, and occasionally a brecciated texture.
Rock Type | Rank | Composition | Texture | Relationship | Mafic pillowed flow | 1 | Pillowed Flow | Host |
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Ironstone-unsubdivided | 2 | Near | ||
Gabbro | 3 | Gabbro | Host | |
Diorite | 4 | Diorite | Host | |
Lamprophyre-Unsubdivided | 5 | Near | ||
Quartz-Feldspar Porphyry | 6 | Host | ||
Vein | 7 | Quartz | Host |
Dec 07, 2005 (B Nelson) - The host metavolcanic rocks are predominantly mafic pillow flows, however minor massive flows are present. The metavolcanic rocks commonly display carbonatization in the vicinity of gold mineralization.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Chalcopyrite | Economic | Ore | ||||
2 | Galena | Economic | Ore | ||||
3 | Gold | Economic | Ore | ||||
4 | Pyrite | Economic | Ore | ||||
5 | Pyrrhotite | Economic | Ore | ||||
6 | Telluride | Economic | Ore | ||||
1 | Quartz | Economic | Gangue | ||||
2 | Fuchsite | Economic | Gangue | ||||
Quartz | Alteration | Silicification | 1 | Unknown | Disseminated | ||
Carbonate | Alteration | Carbonatization | 2 | Unknown | Disseminated | ||
Chlorite | Alteration | Chloritic | 3 | Unknown | Disseminated | ||
Sericite | Alteration | Sericitization | 4 | Unknown | Disseminated |
Dec 07, 2005 (B Nelson) - Visible gold was observed by Ekstrom (1983) in up to 6 locations. However, the gold mineralization is both erratic and sporadic. The veins have been designated from southwest to northeast as Nos. 8, 9, 10, and 11. They are arranged en echelon and tend to pinch and swell along the strike, alternately appearing as stringers in a narrow shear zone and then swelling to 2 and 3 feet for short distances. The quartz is milky and very brittle with a scattered mineralization of pyrite, chalcopyrite, galena and a considerable amount of fine native gold. The gold is most prominent along minute fractures in the quartz, appearing as a film on the fracture faces. (Gold at $34.98 per ounce, 1937 price). No. 10 vein average $18.88 (0.54 ounce per ton Au) over an average width of 1.13 feet for a length of 130 feet. No. 9 vein includes a 100 foot section which averaged $8.96 (0.26 ounce per ton Au) over 1.17 ft. and a second section 70 feet in length which showed negligible values. No. 8 vein averaged $5.34 (0.15 ounce per ton Au) over 1.47 feet over a length of 110 feet. (Resident Geologist's Files, Schreiber Hemlo District, Thunder Bay) In 1973, a one ton bulk sample of quartz was collected from the shaft dump and milled by W. Acker at the Hays Lake Mine. The sample was reported to indicate 0.50 ounce per ton Au.
Dec 07, 2005 (B Nelson) - Resident Geologist personnel obtained an assay result of 0.90 oz/ton Au from a sample containing visible gold along sericite seams (No. 10 Vein).
Date: Feb 18, 1997
Geologist: B Nelson
Notes: Resident Geologist personnel visited the property June 18, 1985; July 9, 1985; September 25, 1985; August 19, 1986; August 3 | 9, 1988; October 18, 1989; July 11, 1990; November 7, 1990; May 22, 1991; July 10, 1992; July 14, 1992; August 6, 1992; June 17, 1993. Sampling by Resident Geologist personnel returned values including the following: 0.70 oz/ton Au, 0.88 oz/ton Ag from the head frame dump (crack seal veins, py, gn, cp). 0.94 oz/ton Au, 0.72 oz/ton Ag from the #10 vein. 0.90 oz/ton Au from the #10 vein (selected grab sample, V.G. along sericite seams). 1.09 oz/ton Au, 0.18 oz/ton Ag, from underground at the McKenna-McCann, 5 feet east (quartz vein). 0.67 oz/ton Au, 0.20 oz/ton Ag, from underground at the McKenna-McCann, 40 feet east (quartz vein).
Year | Tonnes | Commodities | Reference | Comment |
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1937 | 24 |
Gold 22.68 Ounces |
OFR 5951, p. 381 | A 27.3 ton bulk sample was shipped to the Little Long Lac Mill. 9.6 tons from the No. 8 vein indicated 0.57 opt Au, 12.7 tons from the No. 9 vein indicated 0.91 opt Au, and 5 tons from the No. 10 vein indicated 1.13 opt Au giving 22.68 ounces of gold from the 27.3 t milled. |
Map - Nipigon-Schreiber, geological compilation series, Thunder Bay District
Publication Number: M2232 Scale: 1:253,440 Date: 1973
Author: Carter M.W., McIlwaine W.H., Wisbey P.A.
Publisher Name: Ontario Division of Mines
Location:
Map - Schreiber-Duck Lake area, District of Thunder Bay
Publication Number: ARM30A Scale: 1:63,360 Date: 1998
Author: Hopkins P.E., Tanton T.L.
Publisher Name: Ontario Dept. of Mines
Location:
Part - The southwestern part of the Schreiber area
Publication Number: ARV47-09.001 Page: 23-25 Date: 1998
Author: Harcourt G.A.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Schreiber area, District of Thunder Bay, Ontario
Publication Number: ARM47J Scale: 1:31,680 Date: 1997
Author: Bartley M.W., Harcourt G.A.
Publisher Name: Ontario Dept. of Mines
Location:
File - Resident Geologist Mineral Deposit Files
Publication Number: Min Dep Date:
Author:
Publisher Name:
Location: Thunder Bay RGP
Map - Geological series, Precambrian geology of the Terrace Bay area, west sheet, Thunder Bay District
Publication Number: P2417 Scale: 1:15,840 Date: 1981
Author: Carter M.W.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral Occurrences in the Nipigon-Marathon Area, Volumes 1 and 2.
Publication Number: OFR5951 Page: 372-385 Date: 1996
Author: Schnieders B.R., Smyk M.C., Speed A.A., McKay D.B.
Publisher Name: Ontario Geological Survey
Location:
Mono - Geology of Schreiber-Terrace Bay area, District of Thunder Bay
Publication Number: OFR5692 Page: 125-127 Date: 1988
Author: Carter M.W.
Publisher Name: Ontario Geological Survey
Location:
Article - Schreiber-Hemlo Resident Geologist's District - 1990
Publication Number: MP152.007 Date: 1997
Author: Schnieders B.R., Smyk M.C., Hinz P.
Publisher Name: Ontario Geological Survey
Location:
Compend - Report of Activities 1992, Resident Geologists
Publication Number: MP161 Page: 132-133 Date: 1993
Author: Fenwick K.G., Pitts A.E., Newsome J.W.
Publisher Name: Ontario Geological Survey
Location:
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