Ontario Geological Survey
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MDI32D04SW00202
Record Name(s) | DDH KK-82-2 - 1982, Lampe - 1982, R. Montgomery - 1918, King Kirkland - 1918 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1995-May-15 |
Date Last Modified | 2023-Aug-16 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Lebel
Latitude: 48° 9' 27.31" Longitude: -79° 57' 12.47"
UTM Zone: 17 Easting: 577828.322 Northing: 5334344.941 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 32D04SW
Point Location Description: Diamond drill hole
Location Method: Based on Assessment
Access Description: The King Kirkland shaft is located southeast of the hamlet of King Kirkland. Gravel road access is gained by travelling south and then east on the most westerly street in the hamlet for approximately I km. At this point the roadway turns south toward the railway line and a snowmobile trail goes up a hill to the northeast. Follow the snowmobile trail for about 100 m. The shaft is cement capped and may be difficult to find. Drill hole KK-82-2 is located 110 m. north of the shaft.
1918 - The initial claims were staked following the discovery of gold on the property by R. Montgomery. 1920-1923 - King Kirkland Gold Mines Ltd. was formed in 1920. Extensive exploration in the next 3 years about 30 narrow quartz-carbonate veins were discovered on the property. An inclined shaft was sunk with development on the 90-foot and 400-foot levels. 1923 - Tonopah Mining Co. optioned the property, completed additional lateral work on the 400-foot level. The option was dropped and the mine closed at the end of 1923. 1936 - The company reorganized in 1936 as Kirkking Gold Mines Ltd. The workings were resampled and additional diamond drilling was completed. Sampling of the vein system did not return assays as expected from earlier underground sampling. The charter was surrendered in 1938 and the claims reverted back to King Kirkland Gold Mines Ltd. 1980-1983 - Lampe Resource Company Ltd. and propsectors Mike Leahy and Carl Forbes completed trenching and sampling, ground magenetics, VLF-EM and radiometric surveys, and diamond-drilled two holes. 2000 - Property optioned by Goldaur Resources Inc. stripped the overburden off the trace of the hole and sampled the zone on surface.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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KL-1562, 27 | 32D04NW0246 | 32D04NW0246 |
25, KL-1562 | 32D04NW0264 | 32D04NW0264 |
2.4035, KL-1562 | 32D04NW0252 | 32D04NW0252 |
2.3646, KL-1562 | 32D04NW0260 | 32D04NW0260 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Timiskaming
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Zeolite
Dec 07, 2005 (D Guidon) - The property is underlain by a grey, fine to medium grained rock, with phenocrysts up to 8 mm in diameter. The rock is mapped as 'porphyrite' by MacLean (1956). Two diamond drill holes from the property are stored at the Swastika drill core library (KL-1291 and KL-1292). Examination of the drill core shows that the rock is not consistently porphyritic. Rock fragments and possible bedding can be observed suggesting that, at least in part, the rock is sedimentary in origin.
Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz-Carbonate | Host |
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Porphyry-unsubdivided | 2 | Trachytic | Porphyritic, Bedded | Hanging Wall |
Dec 07, 2005 (D Guidon) - The property is underlain by a grey, fine to medium grained rock, with phenocrysts up to 8 mm in diameter. The rock is mapped as 'porphyrite' by MacLean (1956). Two diamond drill holes from the property are stored at the Swastika drill core library (KL-1291 and KL-1292). Examination of the drill core shows that the rock is not consistently porphyritic. Rock fragments and possible bedding can be observed suggesting that, at least in part, the rock is sedimentary in origin. Numerous quartz-carbonate veins were prospected on the property. Most are less than a few inches across but, in places, some are up to 6 feet in width. The majority are northeast-trending with a steep dip to the north. The rock, in the vicinity of the veins, is altered to a yellowish-green colour and a strong foliation is sometimes developed. Near the shaft, fuchsite fragments can be observed in the rock. Carbonate staining indicates the presence of Fe-dolomite as well as calcite.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Carbonate | Economic | Gangue | ||||
2 | Pyrite | Economic | Gangue | ||||
3 | Quartz | Economic | Gangue | ||||
4 | Sericite | Economic | Gangue | ||||
5 | Chalcopyrite | Economic | Gangue | ||||
Dolomite | Alteration | Carbonatization | 1 | Weak | Veins | ||
Quartz | Alteration | Sericitization | 2 | Weak | Veins | ||
Sericite | Alteration | Sericitization | 3 | Weak | Replacement |
Dec 07, 2005 (D Guidon) - Diamond drill hole KK-82-2 (core library number KL- 1291, MDI32D04SW00202), collared 500 feet north of the shaft, was drilled to the northwest and intersected 3 quartz-carbonate veins. The veins are identified as the No. 13, the No. I and a vein in-between (Hopkins, 1923). The rock has been altered by silica, sericite and chlorite development. Fine grained disseminated pyrite is present in concentration of about 4% and trace amounts of chalcopyrite have been observed. The alteration zone for the vein between the No. 13 and the No. 1 veins as observed in drill core extends from 109 to 156.5 feet down the drill hole. Sampling by Lampe Resources and Queenston of 22.2 feet of core over a 26.6 foot core length returned averaged assays 0.03 ounce ton gold. The remainder of the alteration zone remains unsampled.
Dec 07, 2005 (D Guidon) - Numerous quartz-carbonate veins were prospected on the property. Most are less than a few inches across but, in places, some are up to 6 feet in width. The majority are northeast-trending with a steep dip to the north. The rock, in the vicinity of the veins, is altered to a yellowish-green colour and a strong foliation is sometimes developed. Near the shaft, fuchsite fragments can be observed in the rock. Carbonate staining indicates the presence of Fe-dolomite as well as calcite.
Commodity | Analytical Method | Digestion Method | Result | Unit | Limit | Qualifier |
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Antimony | Unknown | BDL | ||||
Arsenic | Unknown | 124 | ppm | |||
Arsenic | Unknown | 145 | ppm | |||
Barium | Unknown | 1053 | ppm | |||
Barium | Unknown | 1104 | ppm | |||
Bismuth | Unknown | BDL | ||||
Bismuth | Unknown | BDL | ||||
Chromium | Unknown | 280 | ppm | |||
Chromium | Unknown | 217 | ppm | |||
Copper | Unknown | BDL | ||||
Copper | Unknown | BDL | ||||
Gold | Unknown | 12 | ppb | |||
Gold | Unknown | 1143 | ppb | |||
Gold | Unknown | 246 | ppb | |||
Lead | Unknown | 57 | ppm | |||
Molybdenum | Unknown | BDL | ||||
Molybdenum | Unknown | BDL | ||||
Nickel | Unknown | 77 | ppm | |||
Nickel | Unknown | 46 | ppm | |||
Selenium | Unknown | BDL | ||||
Silver | Unknown | BDL | ||||
Silver | Unknown | BDL | ||||
Tin | Unknown | BDL | ||||
Tungsten | Unknown | BDL | ||||
Zinc | Unknown | 79 | ppm | |||
Zinc | Unknown | 85 | ppm |
Rank | Characteristic |
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1 | Vein |
Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
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Unknown | 150 | 255 |
Date: Jul 26, 1999
Geologist: D Guidon
Notes: Property visited July 28, 1994 and KK-82-2 examined October 23, 1996. All information suggests that drill hole KK-82-2 is the only hole to test vein systems north of the shaft. Although possibly the least interesting of the veins, the No. 13 vein has a strike length of at least 500 feet. The most interesting of the 3 veins intersected by drilling is the intervening one between the No. I and No. 13 veins, which has an alteration zone over a 47 foot core length. The western extension of this system would be under King Lake. An old assay plan found in assessment file KL- 1426 for the long cross-cut on the 400-foot level shows a zone averaging 0.04 ounce per ton -old over a distance of 93 feet. This assaying was done in the 1920's and check assays from other parts of the mine sampled by Kirkking in the 1930's were disappointing. The zone is approximately on strike with the systems intersected in hole KK-82-2. Property visited July 25, 2000. Quickly looked at the exposure in the trench. Rock didn't look different from the drill core. No samples collected or photos taken. It is my understanding that the assays were similar to that obtained in the core.
File - Resident Geologist file KL-1426
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - Township of Lebel, District of Timiskaming, Ontario
Publication Number: ARM53A Scale: 1:12,000 Date: 1997
Author: MacLean A., Hogg N.
Publisher Name: Ontario Dept. of Mines
Location:
Core - Drill Core Library KL1291
Publication Number: DCL KL1291 Date: 1982
Author:
Publisher Name:
Location:
Part - Lebel and Gauthier townships (area between Kirkland and Larder lakes)
Publication Number: ARV32-04.002 Page: 70-72 Date: 1997
Author: Hopkins P.E.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Mineral resources and mining properties in the Kirkland Lake-Larder Lake area
Publication Number: MDC003 Page: 36-37 Date: 1964
Author: Savage W.S.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Geology of Lebel Township, District of Timiskaming
Publication Number: OFR5211 Page: 72-74 Date: 1976
Author: Lovell H.L.
Publisher Name: Ontario Division of Mines
Location:
Mono - Gold deposits of Ontario, part 2, part of District of Cochrane, districts of Muskoka, Nipissing, Parry Sound, Sudbury, Timiskaming, and counties of southern Ontario
Publication Number: MDC018 Page: 145 Date: 1979
Author: Gordon J.B., Lovell H.L., de Grijs J.W., Davie R.F.
Publisher Name: Ontario Geological Survey
Location:
Mono - Preliminary report on the Timmins-Kirkland Lake area, gold deposits file
Publication Number: OFR5467 Page: G0193 Date: 1983
Author: Hodgson C.J.
Publisher Name: Ontario Geological Survey
Location:
File - Res/Reg Property Visit Report KL#20
Publication Number: PV 20 Date: 1982
Author: Lovell, H.L.
Publisher Name:
Location: Kirkland Lake RGP office
Mono - Geology Of Lebel Township
Publication Number: B150 Date: 1998
Author:
Publisher Name:
Location:
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