Ontario Geological Survey
Permanent Link to this Record:
MDI32D12SE00005
| Record Name(s) | Holt Mine - 2010, Holt-McDermott Mine - 1988, McDermott Occurrence - 1923, Barrick Resources Corp. - 1984, Camflo Mines Ltd. - 1980, American Barrick Resources Corp. - 1985, Bailey Claims - 1946 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Past Producing Mine With Reserves or Resources |
| Date Created | 1988-Jul-04 |
| Date Last Modified | 2023-Aug-16 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Holloway
Latitude: 48° 30' 47.7" Longitude: -79° 44' 23.87"
UTM Zone: 17 Easting: 593056 Northing: 5374115.01 UTM Datum: NAD83
Resident Geologist District: Kirkland Lake
NTS Grid: 32D12SE
Point Location Description: The shaft: 2.82 km south and 1.16 km east of the northwest corner of Holloway Township.
Location Method: Field Visit with GPS
Access Description: The vertical 3 compartment shaft is collared in the southeast part of patented claim no. 11535, with access provided from Highway 101 via a 750 m long gravel road.
1922-26: P. A. McDermott (McDermott Gold Mines Ltd.): discovery of gold in Holloway Twp.; overburden stripping;, McDermott Gold Mines Ltd. incorporated; trenching (10 trenches), pitting, DD-3-427.5 ft. 1946-47: Sylvanite Gold Mines - property acquisition. 1948-50: Sylvanite Gold Mines Ltd.: optioned McDermott Gold Mines claims; 11 DDH's (925 m) along 76 m strike. 1980-84: Camflo Mines Ltd.: acq'uired McDermott Gold Mines claims (via takeover of Wilanour Resources Ltd.); optioned McDermott Mines claims; geological, geochemical surveys., VLF, magnetometer surveys;IP survey stripping, blasted 1,500 lb bulk sample; 69 DDH; acquired additonal claims in area. 1984-85: Barrick Resources Corp. acquired McDermott Mine claims via amalgamation with Camflo Mines Ltd. work began on 3 comp. expl. shaft (to be sunk 1,200 ft); became American Barrick Resources Corp.; magnetometer survey. 1986-89:American Barrick Resources Ltd.: surface drilling; underground exploration on 150 and 350 m levels via exploration shaft; completed mine surface facility; ventilation raise bored to surface from 150 m level; commercial Au production begins; ventilation raise bored from surface to 350 m level; drift on 300 level driven to Three Star and Worvest claims; mine officially opened on August 9th; 2 drifts begun on 150 and 250 m levels to access Mattawasaga deposit (Mattawasaga claims); continued mining operations; acquired 35% interest (from Lenora Resources) in Worvest claims and in additional clasims in mine area; drifting on 150 and 250 m levels driven to access auriferous material on Canamax claims. 2004: Production ceases. 2004-2006: Newmont Mining: property purchased. Underground exploration was carried out. New reserves included with the Holloway Mine; property put on care and maintenance. 2007-present: St Andrew Goldfields Ltd.: amalgamated with Holloway Mining Ltd.; mine went into production in April 2011. The Holt Complex, consisting of Holt, Holloway and Taylor mines ceased production on April 2, 2020, as part of Kirkland Lake Gold's response to the COVID-19 pandemic, whilst continuing the strategic review of the Holt Complex.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| KL-0321/ 2.6826 | 32D12SW0307 | 32D12SW0307 |
| KL-0321/2.6368 | 32D12SW9335 | 32D12SW9335 |
| KL-1125/63.3804 | 32D12SW0312 | 32D12SW0312 |
| KL-0321/ 63.4007 /OM81-6-C-64 | 32D12SW0309 | 32D12SW0309 |
| KL-0102/63.4993/OM86-6-C-78 | 32D12SW0301 | 32D12SW0301 |
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Porcupine
Geological Age: Mesoarchean
Metamorphism Grade: Greenschist
Jul 28, 2016 (R Degagne) - Geological mapping indicates that the Holt-McDermott Mine orebodies are within or immediately marginal to the east striking Porcupine-Destor Fault Zone (PDFZ). Bedrock north of the PDFZ consists mainly of weakly metamorphosed (greenschist or lower metamorphic grade) and variably folded and faulted volcanic, volcaniclastic, sedimentary, and intrusive rock of the (Archean) Hunter Mine and Stoughton-Roquemaure Groups. Bedrock south of the PDFZ consists mainly of weakly metamorphosed (greenschist or lower facies) homoclinal north northeast striking, steeply south dipping, and south facing volcanic and interflow sedimentary rocks of the (Archean) Kinojevis Group. The PDFZ is a wide (at least 1 km in width according to Jensen structurally and lithologically complex domain which is characterized by variably altered (weakly metamorphosed) volcanic and sedimentary and intrusive rocks and their variably strained and altered products. Jensen and Langford termed this complex assemblage the Porcupine-Destor Complex. In addition to fault and/or shear bounded blocks of Hunter Mine Group, Stoughton-Roquemaure Group, and Kinojevis Group rocks, the Porcupine-Destor Complex is characterized at various places by the presence of alkalic intrusive and (weakly metamorphosed) extrusive rocks, (weakly metamorphosed) Timiskaming type metasedimentary rocks, and variably developed domains of metasomatism. Bedrock exposure within and immediately marginal to the PDFZ is scarce; most bedrock in the area is mantled by variable thicknesses of often complex.
| Rock Type | Rank | Composition | Texture | Relationship | Syenite | 1 | Intrudes |
|---|---|---|---|---|
| Mafic lava flow-unsubdivided | 2 | Tholeiitic Basalt; Cbz, Sil, Py, Lx | Fine-Grained To Aphanitic.; Sheared,Pillowed, Mass | Footwall |
| Mafic lava flow-unsubdivided | 3 | Tholeiitic Basalt; Cbz, Chl, Py | Fine-Grained To Aphanitic | Hanging Wall |
| Schist-Unsubdivided | 4 | Chl-Carb, Py, Qv, Au | Variably Banded | Host |
| Breccia-unsubdivided | 5 | Hem, Carb, Qv, Py, Au, +/-Ab | Microcrystalline | Host |
Jul 28, 2016 (R Degagne) - Footwall (tholeiitic) basalt is reported to be fine grained, chloritic, weakly silicified, and weakly carbonatized; to generally display undeformed primary volcanic textures; and, proximal to the anomalously auriferous Lower Transition Zone, to be leucoxenitic. It contains about 1% of finely disseminated pyrite. Unaltered footwall basalt grades or may be in sharp contact with chlorite-carbonate schist which is termed the Lower Transition Zone. The Lower Transition Zone is characteristically megascopically banded and consists of variably interlaminated chloritic domains and cream colored carbonate streaks and masses. It is also variably pyritic (average pyrite content typically increases from background levels (about 1%) distally to about 3% proximally to the Main Mineralized Zone), carbonate bearing (increasing from traces distally to as much as about 50% of megascopically visible carbonate proximal to the Main Mineralized Zone), and siliceous. The Main Mineralized Zone is in gradational contact with the Lower Transition Zone. The Main Mineralized Zone consists of a microcrystalline grey to pale purple colored (hematitic) siliceous breccia (the rock has been shattered) which contains(locally as much as 30%) pyrite as disseminations, localized along fractures, and as 1 cm size clots; and albite. The breccia has been recemented by less than 1 mm wide interfragment quartz veinlets. The Main Mineralized Zone grades with decreasing silica and increasing carbonate content into (hanging wall) Upper Transition Zone, which is similar to the Lower Transition Zone: a carbonate-chlorite schist which generally contains 1-3% of disseminated pyrite. Most ore is reported (Anderson 1989) to occur adjacent to the McKenna Fault, which often forms the structural hanging wall of the ore. The Upper Transition Zone grades into or is in sharp contact with relatively unaltered chloritic, carbonate-bearing, and weakly pyritic hanging wall (tholeiitic) basalt.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Chalcopyrite | Economic | Ore | ||||
| 3 | Pyrrhotite | Economic | Ore | ||||
| 5 | Specularite | Economic | Ore | ||||
| 6 | Magnetite | Economic | Ore | ||||
| 1 | Carbonate | Economic | Gangue | ||||
| 4 | Sericite | Economic | Gangue | ||||
| 5 | Albite | Economic | Gangue | ||||
| 7 | Feldspar | Economic | Gangue | ||||
| 9 | Rutile | Economic | Gangue | ||||
| 10 | Sphene | Economic | Gangue | ||||
| 11 | Apatite | Economic | Gangue | ||||
| Hematite | Alteration | Hematization | 1 | Medium | Replacement | ||
| Quartz | Alteration | Silicification | 2 | Medium | Veins | ||
| Pyrite | Alteration | Pyritic | 3 | Medium | Disseminated | ||
| Calcite | Alteration | Carbonatization | 4 | Medium | Replacement | ||
| Dolomite | Alteration | Carbonatization | 5 | Medium | Replacement | ||
| Albite | Alteration | Albitic | 6 | Medium | Replacement | ||
| Chlorite | Alteration | Chloritic | 7 | Unknown | Replacement |
Jul 28, 2016 (A Wilson) - Assays from the 1926 diamond drilling program returned values of 0.255 oz/t Au over 8.2 m and 0.12 oz/t Au over 5.1 m. Assays from the Sylvanite Gold Mines Ltd. 1948-50 diamond drilling program returned values ranging from 0.12-0.36 oz Au / ton across 1.0 - 2.9 m in 8 holes. Assays from the1949 diamond drilling program completed by Sylvanite Gold Mines returned assays ranging from $1.90 Au over 40 ft (drill hole S5) to $4.13 Au over 30 ft (drill hole S2) Native gold in mineralized zones at the Holt Mine occurs as fine grains spatially associated with pyrite, typically located in fractures, on grain boundaries, or encapsulated in pyrite grains. Microscopically, gold grain distribution can be clustered, however, assays do not reveal erratic or "nuggety" gold concentrations. Gold values in mineralized zones die out laterally, over several metres within the envelope of altered rock. There is generally a fairly sharp boundary on the hanging-wall side, but a more gradational lessening of values on the footwall side. This is particularly evident in Zone 4 and less evident in Zone 6 where the contacts of the mineralization are generally sharp with the surrounding mafic volcanic rocks.
Dec 07, 2005 (R Degagne) - Pyrite and gold contents in both the Transitional Alteration and Main Silicified Zones are reported to correlate directly with albite content, with the highest pyrite contents (locally as much as 30%) and gold tenors (assays greater that 2 ounces of gold per ton have been documented) associated with honey colored albitic domains within the Main Mineralized Zone. Nonalbitic, generally pale purple colored siliceous breccia of the Main Mineralized Zone in most places averages no more than 0.01-0.06 ounce of gold per ton (Workman 1985, 1986). The greatest gold tenors are reported to occur within the Main Mineralized Zone not within domains of maximum silica content, but rather marginal to these where redeposition of gold from the auriferous siliceous breccia which was mobilized by carbonate depositing fluids took place. Additional anomalous gold tenors on the McDermott and adjacent claims are reported (Workman 1985) to include: 1. those associated with a purple/grey to green colored fine grained zoned feldspar phyric rock which has been affected by brecciation and Main Mineralized Zone type alteration and which is mineralized with abundant visible gold. 2. 0.1-0.3 mm size grains of native gold associated with foliation parallel quartz veinlets within chlorite-carbonate schist.
Jul 28, 2016 (R Degagne) - Re-evaluation of the Holt-McDermott deposit by American Barrick Resources in late 1985 led to the conclusion that the gold mineralization is hosted by altered intermediate dikes near and within a splay of the PDFZ rather than by interflow sedimentary material (Workman 1985, 1986). According to this model, the carbonate-chlorite schist which envelops the Main Mineralized Zone as the Upper and Lower Transitional Alteration Zones is interpreted as sheared and variably carbonatized diorite dike material and host tholeiitic basalt. The dike material is believed to have been intruded into a splay of the PDFZ and subsequently plastically strained along with some basaltic host rock. This was followed by a second quartz dioritic intrusive event within the splay (deformation zone). Subsequent tectonism is believed to have resulted in multiple events characterized by brittle straining of quartz dioritic dike material, with each event accompanied by pervasive and penetrative silicification, hematization, sulfidation (as pyrite), albitization, gold deposition, and by quartz stringer formation. The final significant hydrothermal regime to which the deformation zone was subjected is manifested now by pervasive and widespread carbonatization (dolomitization proximal to and calcite alteration distal to the Main Mineralized Zone) and was accompanied by limited gold remobilization (Workman 1985, 1986).
| Rank | Classification |
|---|---|
| 1 | Hydrothermal |
| Rank | Characteristic |
|---|---|
| 1 | Breccia |
| 3 | Disseminated |
| 2 | Vein |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular | 76 | 60 |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular | 76 | 76 |
Date: Feb 18, 1997
Geologist: R Degagne
Notes: Visited in 1984 and 1985 by A. C. Bath (OFR 5735, V.1, OGS, 1990).
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Holt | 2019 | Proven + Probable Reserve | 5987755 | OFR6375, p.6 | Gold 4.00 g/t | |
| Holt | 2019 | Measured + Indicated Resource | 8545117 | OFR6375, p.6 | Gold 4.20 g/t | |
| Holt | 2019 | Inferred Mineral Resource | 10027726 | OFR6375, p.6 | Gold 4.40 g/t | |
| Holt | 2018 | Measured + Indicated Resource | 7587209 | OFR6367, p.6 | Gold 4.06 g/t | |
| Holt | 2018 | Proven + Probable Reserve | 3957298 | OFR6367, p.6 | Gold 4.28 g/t | |
| Holt | 2018 | Inferred Mineral Resource | 9394999 | OFR6367, p.6 | Gold 4.70 g/t | |
| Holt | 2014 | Inferred Mineral Resource | 7866000 | Press Release February 12, 2015 | 1,181,000 oz Au | Gold 4.67 g/t |
| Holt | 2014 | Measured Mineral Resource | 3702000 | Press Release February 12, 2015 | 473,000 oz Au | Gold 3.97 g/t |
| Holt Mine | 2014 | Proven Mineral Reserve | 1452000 | Press Release February 12, 2015 | 181,000 oz Au | Gold 4.26 g/t |
| Holt | 2014 | Indicated Mineral Resource | 3861000 | Press Release February 12, 2015 | 485,000 oz Au | Gold 3.90 g/t |
| Holt | 2014 | Probable Mineral Reserve | 2414000 | Press Release February 12, 2015 | 392,000 oz Au | Gold 5.05 g/t |
| Year | Tonnes | Commodities | Reference | Comment |
|---|---|---|---|---|
| 2020 | 237347 |
Gold 29391 Ounces |
OFR6375 p.6 | 29,391 ozs Au produced from 237,347 tons grading 4.25 g/t Au. The Holt Complex includes the Holt Mine, Taylor Mine and Holloway Mine, which all feed the Holt Mill. |
| 2019 | 853528 |
Gold 113952 Ounces |
St Andrew Goldfields Ltd. press release January 9, 2020. | 113,952 ounces produced from 853,528 tons grading 4.4 g/t in 2019. The Holt Complex includes the Holt Mine, Taylor Mine and Holloway Mine, which all feed the Holt Mill. |
| 2018 | 471819 |
Gold 67770 Ounces |
St Andrew Goldfields Ltd. press release January 8, 2019. | 67,770 ounces produced from 471,819 tons grading 4.7 g/t in 2018. |
| 2017 | 462987 |
Gold 66677 Ounces |
St Andrew Goldfields Ltd. press release January 11, 2018. | 66,677 ounces produced from 462,987 tons grading 4.7 g/t in 2017. |
| 2016 | 416048 |
Gold 57086 Ounces |
St Andrew Goldfields Ltd. press release January 9, 2017. | 57,086 ounces produced from 416,048 tons grading 4.52 g/t in 2016. |
| 2015 | 426614 |
Gold 63048 Ounces |
St Andrew Goldfields Ltd. press release January 8, 2016. | 63 048 ounces produced from 470 261 tons grading 4.17 g/t in 2015. |
| 2014 | 8780443 |
Gold 1409473 Grams |
OFR6305, p. 7 | 968782 tons @ 0.152 oz/’t Au |
| 2013 | 8338336 |
Gold 1409473 Grams |
OFR6295, p. 2 | 9191442 tons @ 0.153 oz/t Au |
| 2012 | 316486 |
Gold 50445 Ounces |
OFR6287 | |
| 2011 | 232330 |
Gold 32376 Ounces |
OFR 6275 | |
| 2004 | 357431 |
Gold 1697566 Grams |
OGS OFR 6150, p.25 | 394 000 ton s at 0.139 opt Au (54 578 ounces) |
| 2003 | 459856 |
Gold 2784228 Grams |
OFR 6131 | 89515 OZ FROM 506905 TONS |
| 2002 | 471491 |
Gold 2599255 Grams |
OGS OFR 6114, P.20 | |
| 2001 | 450537 |
Gold 2599535 Grams |
OGS OFR 6083, P.24 | |
| 2000 | 486496 |
Gold 5931806 Grams |
OFR 6051, P.29 | |
| 1999 | 503061 |
Gold 3361695 Grams |
OGS OFR 6007, P.20 | |
| 1998 | 497122 |
Gold 4179654 Grams |
OGS OFR 5991, P. 22 | |
| 1997 | 418646 |
Gold 3622746 Grams |
OGS OFR 5973, P.17 | |
| 1996 | 215260 |
Gold 1155263 Grams |
OGS OFR 5958, P. 7-3 | |
| 1995 | 382470 |
Gold 2064929 Grams |
OGS OFR 5943 P. 171 | |
| 1994 | 3674098 |
Gold 1859988 Grams |
OGS OFR 5921 P.151 | |
| 1993 | 199145 |
Gold 1997434 Grams |
OGS OFR 5892 P.154 | |
| 1992 | 411270 |
Gold 1440869 Grams |
OGS MP 161 P.273 | |
| 1991 | 594404 |
Gold 1888853 Grams |
OGS MP 158 P.261 | |
| 1990 | 973827 |
Gold 3810736 Grams |
OGS MP 158 P.267, OGS MP 147, P.257 (DIFFERENCE BETWEEN PRODUCTION) | PRODUCTION FOR 1989 AND 1990 |
| 1988 | 219071 |
Gold 676090 Grams |
AMERICAN BARRICK RESOURCES CORP., ANNUAL REPORT, 1988 (OFR 5735, V.1, P.416) |
File - Resident Geologist files KL-0178, KL-0321 (OM83-6-C-34), KL-1808
Publication Number: Date:
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Map - North part of the Township of Holloway, District of Cochrane, Ontario
Publication Number: M1953-04 Date: 1997
Author: Satterly J., Hogg N.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological series, Quaternary geology of the Magusi River area, Cochrane and Timiskaming districts
Publication Number: P2483 Scale: 1:50,000 Date: 1982
Author: Baker C.L., Steele K.G., Seaman A.A.
Publisher Name: Ontario Geological Survey
Location:
Book - Canadian Mining Journal 1987,Vol 108 No 7,p. 31-36
Publication Number: CMJ V108 Page: 31-36 Date: 1987
Author:
Publisher Name: Canadian Mining Journal
Location: Kirkland Lake RGP
Map - Part of the Lightning River area, District of Cochrane, Ontario
Publication Number: ARM34A Scale: 1:63,360 Date: 1998
Author: Gledhill T.L.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geological series, Precambrian geology of the Magusi River area, Cochrane and Timiskaming districts
Publication Number: P2434 Scale: 1:63,360 Date: 1982
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Book - Northern Miner 83-12-22, Camflo Mines, p.1,19
Publication Number: NMINER Date: 1983
Author:
Publisher Name: Northern Miner
Location: Kirkland Lake RGP
Map - Geological series, Precambrian geology of the Lightning River area, Cochrane District
Publication Number: P2433 Scale: 1:63,360 Date: 1982
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Book - Northern Miner 85-02-21, Barrick, p A1, A2
Publication Number: NMINER Date: 1985
Author:
Publisher Name: Northern Miner
Location: Kirkland Lake RGP
Map - Geological series, Precambrian geology of the Lightning River area, Cochrane District
Publication Number: P2433 Scale: 1:63,360 Date: 1982
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Precambrian geology of the Lightning Mountain area, Lightning River area, Cochrane District
Publication Number: P2432 Scale: 1:15,840 Date: 1982
Author: Jensen L.S.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of the north half of Holloway Township
Publication Number: ARV62-07 Page: Part 7, p. 29-30 Date: 1997
Author: Satterly J.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Geophysical/geochemical series, Matheson-Black River area, Harker Township, airborne electromagnetic survey, total intensity magnetic survey, District of Cochrane
Publication Number: M80599 Scale: 1:20,000 Date: 1984
Author: Questor Surveys Ltd.
Publisher Name: Ontario Geological Survey
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 131 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Folio - Holloway Township, District of Cochrane
Publication Number: GDIF272 Date: 1997
Author: Kirkland Lake RGO
Publisher Name: Ontario Geological Survey
Location:
Map - Geophysical/geochemical series, Matheson-Black River area, Holloway Township, airborne electromagnetic survey, total intensity magnetic survey, District of Cochrane
Publication Number: M80600 Scale: 1:20,000 Date: 1984
Author: Questor Surveys Ltd.
Publisher Name: Ontario Geological Survey
Location:
Map - Township of Harker, District of Cochrane, Ontario
Publication Number: M1951-04 Date: 1997
Author: Satterly J., Hogg N.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Mineral occurrences, deposits, and mines of the Black River-Matheson area
Publication Number: OFR5735 Page: 412-487 Date: 1990
Author: Bath A.C.
Publisher Name: Ontario Geological Survey
Location:
Map - Geological series, Quaternary geology, Lightning River area, District of Cochrane
Publication Number: P2734 Scale: 1:50,000 Date: 1985
Author: Vagners U.J., Courtney S.J.
Publisher Name: Ontario Geological Survey
Location:
Mono - Archean lode gold deposits in Ontario
Publication Number: MP139 Date: 1988
Author: Colvine A.C., Fyon J.A., Heather K.B., Marmont S., Smith P.M., Troop D.G.
Publisher Name: Ontario Geological Survey
Location:
Part - Lightning River gold area (District of Cochrane)
Publication Number: ARV34-06.004 Page: 96 Date: 1998
Author: Gledhill T.L.
Publisher Name: Ontario Dept. of Mines
Location:
Compend - Report of activities, 1987, Resident Geologists
Publication Number: MP138 Page: 251275 Date: 1988
Author: Kustra C.R.
Publisher Name: Ontario Geological Survey
Location:
Compend - Report of activities, 1986, Regional and Resident Geologists
Publication Number: MP134 Page: 175-218 Date: 1987
Author: Kustra C.R.
Publisher Name: Ontario Geological Survey
Location:
Part - Lightning River gold area
Publication Number: ARV33-03.004 Page: 41-49 Date: 1998
Author: Knight C.W.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology and petrogenesis of the Archean Abitibi belt in the Kirkland Lake area, Ontario
Publication Number: MP123 Date: 1985
Author: Jensen L.S., Langford F.F.
Publisher Name: Ontario Geological Survey
Location:
Compend - Report of activities, 1988, Resident Geologists
Publication Number: MP142 Page: 267-300 Date: 1989
Author: Fenwick K.G., Giblin P.E., Pitts A.E.
Publisher Name: Ontario Geological Survey
Location:
Compend - Summary of field work and other activities, 1986
Publication Number: MP132 Page: 404-407 Date: 1986
Author: Thurston P.C., White O.L., Barlow R.B., Cherry M.E., Colvine A.C.
Publisher Name: Ontario Geological Survey
Location:
Book - Geology of the McDermott Gold Deposit, K. L. Area, NE Ontario; In: Proceedings Volume: Gold 86 Symposium, Toronto, Canada, 1986, p. 184-190
Publication Number: Gold86 Page: 184-190 Date: 1986
Author: Workman, A.W.
Publisher Name:
Location:
File - Res/Reg Property Visit KL #207
Publication Number: PV-207 Date: 1901
Author:
Publisher Name:
Location: Kirkland Lake RGP office
File - Res/Reg Property Visit KL #250
Publication Number: PV-250 Date: 1901
Author:
Publisher Name:
Location: Kirkland Lake RGP office
Mono - Report of Activities 2019, Resident Geologist Program, Kirkland Lake Regional Resident Geologist Report: Kirkland Lake and Sudbury Districts
Publication Number: OFR6367 Page: 6 Date: 2020
Author: Chadwick P.J., Péloquin A.S., Suma-Momoh J., Daniels C.M., Hinz S., Kennedy C.A., Streit L., Todd R.M.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2020, Resident Geologist Program, Kirkland Lake Regional Resident Geologist Report: Kirkland Lake and Sudbury Districts
Publication Number: OFR6375 Page: 6 Date: 2021
Author: Chadwick P.J., Péloquin A.S., Suma-Momoh J., Daniels C.M., Hinz S.L.K., Dorland G., Patterson C., Todd R.M.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geological Synthesis of the Highway 101 Area, East of Matheson, Ontario
Publication Number: OFR6091 Page: 85 Date: 2003
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology of the Highway 101 Area, East of Matheson, Ontario
Publication Number: M2676 Scale: 1:50,000 Date: 2003
Author: Berger B.R., Luinstra B., Ropchan J.C.
Publisher Name: Ontario Geological Survey
Location:
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