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Ontario Geological Survey
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MDI42A11SE00002
| Record Name(s) | Hoyle Pond Mine - 1986 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Producing Mine |
| Date Created | 1986-Dec-30 |
| Date Last Modified | 2024-Jul-05 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Hoyle
Latitude: 48° 33' 4.76" Longitude: -81° 6' 28.16"
UTM Zone: 17 Easting: 492043 Northing: 5377586 UTM Datum: NAD83
Resident Geologist District: Timmins
NTS Grid: 42A11SE
Point Location Description: Main shaft located in Lot 4, conc.1
Location Method: Data Compilation
Access Description: Access to the Kinross Gold Corp. security gatehouse is via a gravel road that proceeds northwards from the end of Florence Street in Porcupine, Ontario. Once past the gatehouse, one proceeds eastwards along a gravel road located on the mine property past the Owl Creek open pit, over the Kidd Creek railroad tracks, and then onward to the headframe.
1969: Texas Gulf Sulphur Company - DD-1.1980-94: Kidd Creek Mines Ltd./Falconbridge Gold Corporation - DD-11,100 m; collaring of decline, underground exploration, bulk sampling; mining. 1994:Kinross Gold Corporation /Porcupine Joint Venture- property acquired; mining. 2006: Goldcorp - property acquired; mining
Province: Superior
Subprovince: Abitibi
Terrane: Wawa-Abitibi
Belt: Abitibi
Tectonic Assemblage: Tisdale
Geological Age: Neoarchean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Mar 15, 2016 (R Pressacco) - All of the stratigraphic units at the Hoyle Pond Mine and the 1060 Zone (with the exception of the younger diabase dikes) have been affected by deformation events which are manifested as strong cleavage fabrics, lineations, and folds. Rhys recognized two main stages of deformation, with 2 weak, overprinting crenulation cleavages. Very little physical evidence is present to document the first deformational event (D1), aside from the observation that the symmetric distribution of the Mg-tholeiitic volcanic rocks and clastic sediments about a core of ultramafic volcanic rocks suggests the presence of an anticlinal fold with a closure in the 1060 Zone area. Evidence for the second phase of deformation (D2) includes a steeply north dipping, northeasterly trending slaty cleavage that forms the main cleavage which is visible in the mine. It is developed throughout the Hoyle Pond Mine with variable intensity and has consistent strikes in the 240-255 deg. range. In the 1060 Zone area, the S2 cleavage cuts across the ultramafic/mafic contacts in the core of the Hoyle Anticline. The S2 cleavage is defined by a strong preferred orientation of platy minerals (chlorite and sericite), and flattening of pillows and other marker features. An elongation lineation (L2) that plunges steeply to the north-northeast on foliation surfaces is observed in various lithologies in the mine. Younger structural features present in the mine area include a crenulation cleavage (S3), kink banding (S4), minor brittle faults, and calcite-filled joints. The S3 crenulation cleavage is only locally developed, dips shallowly to the west and southwest, and is axial planar to rare, open minor folds of S2 foliation which have amplitudes of less than 0.5 metres.
| Rock Type | Rank | Composition | Texture | Relationship | Mafic pillowed flow | 1 | Mg-Tholeiitic Basalt | Pillowed, Amygdaloidal, Variolitic,,Massive | Host |
|---|---|---|---|---|
| Vein | 2 | Quartz | Host | |
| Ultramafic lava flow-unsubdivided | 3 | Komatiite | Massive, Pillowed, Polysutured | Near |
| Siltstone | 4 | Graphitic | Interbedded With Greywacke | Near |
Mar 15, 2016 (A Wilson) - The Hoyle Pond Mine occurs within the Tisdale Assemblage, 4.5 m north of the Destor-Porcupine Fault. The mine occurs in a sequence of south-facing 065º striking, steeply north-dipping, magnesium-rich tholeiitic basealts.
Dec 07, 2005 (R Pressacco) - The property scale geology of the Hoyle Pond Mine and 1060 Zone area is relatively straightforward. An easterly trending, steeply north dipping band of Mg- and Fe-tholeiitic mafic volcanic rocks and ultramafic volcanic rocks is flanked both north and south by clastic metasedimentary rocks containing minor amounts of intercalated graphic argillite. The ultramafic volcanic rocks are situated in the central portions on this band, mostly to the west of section 101750E on the mine grid, such that a thin interval of Mg-tholeiite mafic volcanic rocks is present between them and the flaking sedimentary rocks. Some Fe-tholeiites have been documented along the southern sedimentary contact by Downes et. al. (1984). The overall easterly trend is maintained throughout the property except in the immediate vicinity of the Hoyle Pond shaft where the Mg-tholeiites are observed to take on an overall Z-shape as a result of either tight folding or a system of northeasterly trending faults / shears. The sediments are composed of a mixture of carbonaceous argillites and greywackes which become increasingly more argillaceous near the mafic contacts. The argillites exhibit a compositional banding defined by alternating 1 - 2 mm thick dark and light coloured argillaceous layers. Karelse (1985) determined that these sediments were fine grained turbidites on the basis of preserved Bouma cycles. The sediments contain trace amounts of porphyroblastic and nodular pyrite, and have a pronounced fabric defined by closely spaced fracture cleavage and flattening of the pyrite nodules. In the northern sediments, the intensity of the fabric increases southwards towards the volcanic contact. Rapid changes in facing directions are observed along the strike length of both the northern and southern sediments, suggesting tight folding.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Arsenopyrite | Economic | Ore | ||||
| 3 | Pyrite | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| 2 | Carbonate | Economic | Gangue | ||||
| 3 | Chlorite | Economic | Gangue | ||||
| 4 | Sericite | Economic | Gangue | ||||
| 5 | Tourmaline | Economic | Gangue | ||||
| 6 | Albite | Economic | Gangue | ||||
| 7 | Sphalerite | Economic | Gangue | ||||
| 8 | Chalcopyrite | Economic | Gangue | ||||
| 9 | Scheelite | Economic | Gangue | ||||
| Carbonate | Alteration | Calcitization | 1 | Strong | Replacement | ||
| Sericite | Alteration | Unknown | 2 | Strong | Replacement | ||
| Chlorite | Alteration | Unknown | 3 | Medium | Replacement |
Apr 19, 2016 (A Wilson) - Most of the gold is structurally controlled and occurs in three predominant forms. Most of the gold at Hoyle Pond is hosted along the selvages of quartz veins and wall rocks or in stylolitic fracturs within quartz veins and is commonly accompanied by hydromuscovite. Gold associated with amorphous carbon occurs as refractory ore. Chlorite, sericite-carbonate alteration and silicification in the form of quartz veins and stringers accompany the gold mineralization. Sulphide mineralization is generally less than 5%. A distinctive type of alteration referred to as grey zones by the mine geologists is diagnostic of gold mineralization at the Owl Creek, Hoyle Pond and to a lesser extent at the Bell Creek mines. Amorphous carbon accompanied by enrichments in silica, calcium, potassium, iron, arsenic and gold form sharply bounded to diffuse alteration zones which are the primary exploration targets in the southern part of the township. The discovery hole at the Hoyle Pond Mine was drilled by Texas Gulf Sulphur Company Inc. in 1969 with hole DDH 69-17 intersecting 6.5 g / t Au / 3.0m (0.18 oz / ton / 9.8ft). Subsequent drill programs in 1980 and 1982 outlined a deposit containing 199 600 tonnes grading 15.1 g / t Au (97 670 oz Au).
Mar 15, 2016 (R Pressacco) - At least two, and possibly three generations of auriferous quartz veins are observed in the Main Zone and 1060 Zone area (Rhys 1996). While all of the rock types in the mine form hosts to the aurferous veins except the diabase dikes, the veins are most abundant, thickest, and most continuous within the basaltic units. The three vein types are: Grey Quartz Veins: These early grey quartz>albite +/- tourmaline + carbonate + hydromica (hydromuscovite) + carbon veins are commonly surrounded by 'grey zone' alteration halos (Rye 1987). These veins are commonly ribboned with dark grey bands of tourmaline, carbon and carbonate that are either discrete aggregates of these minerals, or are pervasively disseminated throughout the quartz. The bands commonly contain, or are spatially associated with, coarse native gold. The banding may represent cyclic opening of the veins in a crack-seal fashion. The veins vary from <0.1m to 3 metres in thickness, but are thicker where later generations of quartz have further dilated the vein. Grey quartz veins are commonly folded and boudinaged by the S2 cleavage. White Quartz Veins: These veins are of intermediate age, and consist of white, milky quartz that contains <1 to 3% ribbons and bands of chlorite, muscovite, carbonate and pyrite that are commonly ribboned in texture. This type of quartz further dilates the older grey quartz veins, often brecciating them. The result is composite veins that contain brecciated fragments of grey quartz, or locally banded areas of grey quartz that are separated by the younger white quartz. In the 1060 Zone area, 0.5-3% disseminated pyrite occurs in the wall rocks to this type of vein. Gold is typically finer grained than in the grey quartz, and is often associated with the pyrite.
Mar 15, 2016 (R Pressacco) - In brief, the 'grey zone' style of alteration is closely associated with many of the gold-bearing quartz veins at Hoyle Pond and typically occurs as asymmetrical alteration selvages around a central quartz vein. In places 'grey zone' alteration does exist without the presence of a quartz vein, and while elevated gold values may be present in the altered zones, the alteration zones alone do not usually constitute ore. The grey alteration zones are recognized chiefly through a variation in the colour of the host rocks from a light green - grey in unaltered host rocks, through a light grey colour on the outer margins of the zones, to a dark grey to black colour as the central portions of the zones are approached. For the most part the alteration zones occur as bands, isolated pods, and at times as anastomosing three dimensional networks which surround lenses of less altered Mg-tholeiites. They trend generally towards an azimuth of 0608 and dip vertically. The zones can reach strike lengths on the order of 500m, and vary rapidly in width from 0.5m to 20m or more along strike or down dip. For the most part however, the intensity of alteration increases inwards toward a central core. The margin of an alteration zone is marked first by a subtle colour change from a buff green colour to a grey-green basalt and a noticeable increase in foliation intensity occurring over approximately a 1m interval. These marginal areas lack significant pyrite mineralization or brecciation. Toward the center of the alteration zone, the rock becomes perceptibly darker in colour and becomes enriched in 1 - 5 mm sized grains of recrystallized pyrite in roughly 2 - 5% overall abundance. A fine network of 1 - 2 mm wide carbonaceous fractures and randomly oriented carbonate stringers also become increasingly common, causing a fine brecciation of the host volcanic rocks.
| Rank | Classification |
|---|---|
| 1 | Hydrothermal |
| Rank | Characteristic |
|---|---|
| 1 | Vein |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular |
| Shape | Length | Thickness | Depth | Strike | Dip | Plunge | Trend | Age | Reference |
|---|---|---|---|---|---|---|---|---|---|
| Irregular |
Date: Jan 07, 1999
Geologist: R Pressacco
Notes: Gold mineralization on the Kinross land holdings in Hoyle-Whitney-Matheson Twps area occurs in close association to quartz veins with associated wall rock alteration halos. To date, the known mineralization occurs as a number of vein swarms located in several areas such as: the Bell Creek Deposit (past producer), the Blackhawk (Vogel) Zone, the Owl Creek Deposit (past producer), the Owl Creek East Zones (350 Zone and 950 Zone), the Hoyle Pond Deposit (in production), the 1060 Zone (in production), and the Sediment Zone. At the Hoyle Pond Mine, the Main Zone includes a series of veins that strike in a general east to northeast direction. At least 7 of these veins have been of economic significance (7, 10, 12, 13, 14, 16, and 17 veins). The 1060 Zone at Hoyle Pond consists of at least 5 main vein structures (1060, B1, B2, B3, A, and Porphyry Veins).
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Hoyle Pond Mine | 2001 | Recoverable | 920538 | OFR 6082, P. 15 | Gold 13.75 g/t | |
| Hoyle Pond Mine | 2000 | Recoverable | 1195271 | OFR 6050 P. 15 | Gold 11.8 Grams | |
| Hoyle Pond Mine | 1999 | Recoverable | 3594000 | KINROSS GOLD CORPORATION, TIMMINS OPERATIONS, VISITOR'S HANDBOOK 07/18/00 | INCLUDES 2.4 MILLION TONNES @ 2.5 G/T AU FROM THE OWL CREEK DEPOSIT | Gold 5.5 Grams |
| Hoyle Pond Mine | 1998 | Recoverable | 3154000 | KINROSS GOLD CORPORATION, TIMMINS OPERATIONS, VISITOR'S HANDBOOK 07/18/00 | Gold 9.08 Grams | |
| Hoyle Pond Mine | 1997 | Recoverable | 4602126 | OFR 5985 | Gold 11.07 Grams | |
| Hoyle Pond Mine | 1996 | Recoverable | 4245903 | OFR 5985 | Gold 13.8 Grams | |
| Hoyle Pond Mine | 1995 | Recoverable | 1163889 | OFR 5985 | Gold 15.46 Grams | |
| Hoyle Pond Mine | 1994 | Recoverable | 260000 | OFR 5985 | Gold 15.07 Grams | |
| Hoyle Pond Mine | 1993 | Recoverable | 225644 | OFR 5985 | Gold 17.3 Grams | |
| Hoyle Pond Mine | 1992 | Recoverable | 184640 | OFR 5985 | Gold 14.6 Grams | |
| Hoyle Pond Mine | 1991 | Recoverable | 254009 | OFR 5985 | Gold 15.4 Grams | |
| Hoyle Pond Mine | 1990 | Recoverable | 291367 | OFR 5985 | Gold 16.9 Grams | |
| Hoyle Pond Mine | 1989 | Recoverable | 335624 | OFR 5985 | Gold 16.2 Grams | |
| Hoyle Pond Mine | 1988 | Recoverable | 382900 | OFR 5985 | Gold 16.5 Grams | |
| Hoyle Pond Mine | 1987 | Recoverable | 407000 | OFR 5985 | Gold 19.5 Grams | |
| Hoyle Pond Mine | 1986 | Recoverable | 437000 | OFR 5985 | Gold 23.1 Grams | |
| Hoyle Pond Mine | 1985 | Recoverable | 199637 | OFR 5985 | Gold 15.1 Grams |
| Year | Tonnes | Commodities | Reference | Comment |
|---|---|---|---|---|
| 2023 | 221654 |
Gold 50162 Ounces |
OFR6410, p.6 | 7.61 g/t Au |
| 2022 | 200297 |
Gold 42141 Ounces |
OFR6402, p.6 | 7.07 g/t Au |
| 2021 | 309688 |
Gold 72448 Ounces |
OFR6384, p.7 | 7.84 g/t Au |
| 2020 | 327160 |
Gold 94986 Ounces |
OFR6374, p.7 | Head grade of 9.667 g/t, recovery 93.4%, recovered ounces: 94986 oz. |
| 2019 | 352318 |
Gold 122083 Ounces |
OFR6366, p.8 | Head grade of 10.778 g/t, recovery 96.81% recovered ounces: 118195 oz. |
| 2018 | 404005 |
Gold 141425 Ounces |
OFR6354, p.9 | Grade of 11.4 g/t Au |
| 2017 | 412528 |
Gold 159896 Ounces |
OFR 6339, p.8 | |
| 2016 | 367358 |
Gold 157760 Ounces |
OFR6327, p.7 | Grade of 14.16 g/t gold |
| 2015 | 362300 |
Gold 274300 Ounces |
OFR6317, p.9 | production was 274300 oz |
| 2014 | 321500 |
Gold 300000 Ounces |
OFR 6304, p. 3 | production was 300 000 oz |
| 2013 | 348987 |
Gold 155464 Ounces |
OFR 6294, p. 12 | production was 155 464 oz |
| 2012 | 306388 |
Gold 128699 Ounces |
OFR 6284, p. 10 | production was 128 699 oz |
| 2011 | 314957 |
Gold 141202 Ounces |
OFR 6284, p. 10 | production was 141 202 oz |
| 2010 | 327208 |
Gold 118244 Ounces |
OFR 6284, p. 10 | production was 118 244 oz |
| 2009 | 334126 |
Gold 125516 Ounces |
OFR 6264, p. 10 | production was 125 516 oz |
| 2008 | 333596 |
Gold 114986 Ounces |
OFR 6235, p. 17 | production was 114 986 oz |
| 2007 | 361534 |
Gold 133336 Ounces |
OFR 6219, p. 16 | production was 133 336 oz |
| 2006 | 369252 |
Gold 130654 Ounces |
OFR 6203, p. 16 | 130 654 oz Au |
| 2005 | 402971 |
Gold 146581 Ounces |
OFR 6183, p. 16 | production was 146 581 oz |
| 2003 | 374463 |
Gold 135018 Ounces |
OFR 6130, p. 15 | production was 135018 oz |
| 2002 | 454000 |
Gold 157287 Ounces |
OFR 6113, p. 17 | production was 157 287 oz |
| 2001 | 443892 |
Gold 156261 Ounces |
OFR 6082 p. 12 | production was 156,261 oz |
| 2000 | 460576 |
Gold 140036 Ounces |
OFR 6050 p.15 | production was 140,036 oz |
| 1999 | 419108 |
Gold 136709 Ounces |
Kinross Gold Corporation, Timmins Operations, Visitor's Handbook 07/18/00 | 136,709 ounces |
| 1998 | 416156 |
Gold 158593 Ounces |
Kinross Gold Corporation, Timmins Operations, Visitor's Handbook 07/18/00 | 158,593 ounces |
| 1997 | 469177 |
Gold 174317 Ounces |
OFR 5985 | 174 317 oz Au |
| 1996 | 377752 |
Gold 160967 Ounces |
OFR 5985 | 160 967 oz Au |
| 1995 | 178653 |
Gold 91661 Ounces |
OFR 5985 | 91 661 oz Au |
| 1994 | 97369 |
Gold 55170 Ounces |
OFR 5985 | 55170 oz Au |
| 1993 | 77368 |
Gold 47092 Ounces |
OFR 5985 | 47 092 oz Au |
| 1992 | 109234 |
Gold 58564 Ounces |
OFR 5985 | 58 564 oz Au |
| 1991 | 106859 |
Gold 54118 Ounces |
OFR 5985 | 54 118 oz Au |
| 1990 | 114995 |
Gold 64573 Ounces |
OFR 5985 | 64 573 oz Au |
| 1989 | 109995 |
Gold 58540 Ounces |
OFR 5985 | 58 540 oz Au |
| 1988 | 97223 |
Gold 51358 Ounces |
OFR 5985 | 51 358 oz Au |
| 1987 | 100690 |
Gold 47212 Ounces |
OFR 5985 | 47,212 oz Au |
| 1986 | 83596 |
Gold 56898 Ounces |
OFR 5985 | 56 898 oz Au |
| 1985 | 64400 |
Gold 27000 Ounces |
OFR 5985 | 27 000 oz Au |
File - Resident Geologist file T-3357
Publication Number: Date:
Author:
Publisher Name:
Location: Timmins RGP office
Map - Geological Compilation of the Timmins Area, Abitibi Greenstone Belt
Publication Number: P3379 Scale: 1:100,000 Date: 1998
Author: Ayer J.A., Trowell N.F.
Publisher Name:
Location:
Mono - Report of Activities 2018, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6354 Date: 2019
Author: van Hees E., Bousquet P., Bustard A., Pressacco R.E., Daniels C.M., Fudge S.P., Walker J., Streit L., Wang L., Sword P., Patterson C.
Publisher Name: Ontario Geological Survey
Location:
Book - Northern Miner, 80-07-31, Texasgulf, p. 2
Publication Number: NMINER Date: 1980
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Map - Timmins data series, Hoyle Township, District of Cochrane
Publication Number: P2088 Scale: 1:15,840 Date: 1980
Author: Hunt D.S., Maharaj D.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2020, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6374 Date: 2021
Author: Azadbakht Z., Bousquet P., Zammit K., Daniels C.M., Hinz S.L.K., Sword P., Boucher C., Dorland G., Patterson C.
Publisher Name: Ontario Geological Survey
Location:
Book - Northern Miner, 80-10-23, Texasgulf, p. 1,2
Publication Number: NMINER Date: 1980
Author:
Publisher Name: Northern Miner
Location: Timmins RGO
Mono - Report of Activities 2022, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6402 Page: 7 Date: 2023
Author: Azadbakht Z., Krukowski M., Maity B.K., Bousquet P., Daniels C.M., Hinz S.L.K., Adrianwalla C.J., Dorland G., Sabiri N., Patterson C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2019, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6366 Date: 2020
Author: van Hees E., Bousquet P., Suma-Momoh J., Daniels C.M., Hinz S.L.K., Boucher C., Sword P., Wang L., Fudge S.P., Millette A., Patterson C.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist area, Northern Region
Publication Number: MP128.006 Page: 167 Date: 1997
Author: Luhta L.E., Sangster P.J., Ireland J.C.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2023, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6410 Page: 6 Date: 2024
Author: D'Angelo V., Krukowski M., Maity B.K., Bousquet P., Daniels C.M., Hinz S.L.K., Meyer G., Sabiri N., Swiercz J., Adrianwalla C.J.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1988
Publication Number: MP142.012 Date: 1997
Author: Luhta L.E., Sangster P.J., Draper D.M., Ireland J.C., Bradshaw M.P., Hamblin C.D.
Publisher Name: Ontario Geological Survey
Location:
Article - Timmins Resident Geologist's District - 1989
Publication Number: MP147.012 Date: 1997
Author: Luhta L.E., Sangster P.J., Ireland J.C., Hamblin C.D., Bradshaw M.P.
Publisher Name: Ontario Geological Survey
Location:
Book - Core Library TI3343-44
Publication Number: core lib Date: 2001
Author:
Publisher Name:
Location: Timmins RGO
Mono - Report of Activities 2016, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6327 Date: 2017
Author: van Hees E., Bousquet P., Pace A., Daniels C.M., Wilson A.C., Samuel A., Walmsley J.
Publisher Name: Ontario Geological Survey
Location:
Book - Geological Setting of Gold Depositsin the Porcupine Gold Camp
Publication Number: Brisbin Date: 1998
Author: Brisbin, Dan
Publisher Name: Queen's University
Location: Timmins RGO
Book - A free carbon- and carbonate-bearing alteration zone associated with the Hoyle Pond gold occurrence, Ontario, Canada; In: Gold �82: The geology, geochemistry and genesis of gold deposits
Publication Number: Gold '82 Date: 1984
Author: Downes, M.J., Hodges, D.J., and Derweduwen, J.,
Publisher Name:
Location:
Book - Geology of Hoyle Pond; Unpublished Kidd Creek Mines Ltd. Internal Rpt.
Publication Number: Karelse Date: 1985
Author: Karelse, P.
Publisher Name: Kidd Creek Mines Ltd. Internal Report
Location:
Thesis - Geology and Geochemistry of the Hoyle Pond Gold Deposit, Timmins, Ontario
Publication Number: MSc Thesis Date: 1987
Author: Rye, K.
Publisher Name: University of Western Ontario
Location:
Mono - Special Project: Timmins Ore Deposit Descriptions
Publication Number: OFR5985 Date: 1999
Author: Pressacco R.E.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2000, Resident Geologist Program, Timmins Regional Resident Geologist Program: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6050 Date: 2001
Author: Atkinson B.T., Hailstone M.H., Seim G.Wm., Wilson A.C., Draper D.M., Farrow D.G., Hope P., Debicki R.L., Yule G.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Report of Activities 2001, Resident Geologist Program, Regional Land Use Geologist Report: Northwestern, Northeastern and Southern Ontario
Publication Number: OFR6085 Date: 2002
Author: Debicki R.L., Drost A.P., Rowell D.J., Yule G.R.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Precambrian Geology, Hoyle and Gowan Townships
Publication Number: R299 Page: 28, 32-34 Date: 1998
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology, Hoyle Township
Publication Number: M2532 Scale: 1:20,000 Date: 1998
Author: Berger B.R.
Publisher Name: Ontario Geological Survey
Location:
Book - Geology and Ore Deposits of the Timmins District, Ontario, Field Trip Guidebook 8th IAGOD Symposium, Hoyle Pond Mine, p. 114-123
Publication Number: Date: 1998
Author: R.J. Labine
Publisher Name: DEMR
Location: Timmiins RGO
Mono - Report of Activities 2017, Resident Geologist Program, Timmins Regional Resident Geologist Report: Timmins and Sault Ste. Marie Districts
Publication Number: OFR6339 Date: 2018
Author: van Hees E., Pace A., Bustard A., Gomwe T.S., Bousquet P., Daniels C.M., Wilson A.C., Streit L., Sword P., Patterson C., Fudge S.P.
Publisher Name: Ontario Geological Survey
Location:
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