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Ontario Geological Survey
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MDI52P10SW00007
| Record Name(s) | Howells Lake Prospect - 1977, New Jersey Zinc - 1985, Canadian Nickel - 1985 |
|---|---|
| Related Record Type | Partial |
| Related Record(s) | |
| Record Status | Developed Prospect With Reported Reserves or Resources |
| Date Created | 1985-Jul-24 |
| Date Last Modified | 2024-Jun-13 |
| Created By | |
| Revised By |
Primary Commodities: Antimony, Gold
Township or Area: Snowdrift Lake Area
Latitude: 51° 34' 23.13" Longitude: -88° 47' 21.64"
UTM Zone: 16 Easting: 376000.001 Northing: 5715074.998 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52P10SW
Point Location Description: Diamond drill hole
Location Method: Data Compilation
Access Description: Located approximately 95 km due east of Pickle Lake at Howells Lake, which is just west of Miminiska Lake. Accessible by boat along the Albany River system form the Forth Hope First Nation, located about 50 km to the east. Alternatively, direct access may be obtained via float plane form Pickle Lake.
1971: 2 ddh - Conwest Exploration Company Ltd. 1977: AM - New Jersey Zinc Exploration Company (Canada) Ltd. 1978; 5 ddh - New Jersey Zinc Exploration Company (Canada) Ltd. 1979: AM and ddh program - New Jersey Zinc Exploration Company (Canada) Ltd. 1980: AEM and VLF-EM - New Jersey Zinc Exploration Company. 1984: ddh - Felmont Oil Corporation. 1986: 20 ddh - by MPH Consulting Ltd for Barque Resources Ltd.
| Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
|---|---|---|
| 2.30150 | 20000000511 | 20000000511 |
| 2.33717 | 20000002029 | 20000002029 |
| 2.2759 | 52P06NE9615 | 52P06NE9615 |
| 2.3057 | 52P09NE0017 | 52P09NE0017 |
| 2.3707 | 52P10NE0028 | 52P10NE0028 |
| 17 | 52P10SW0042 | 52P10SW0042 |
| 14 | 52P10SW0014 | 52P10SW0014 |
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Miminiska-Fort Hope
Geological Age: Neoarchean
Oct 11, 2006 (Mark Puumala) - The geology of the Miminiska Peninsula area was mapped by Wallace (1981), who identified three major supracrustal rock sequences. These include two mafic metavolcanic-dominated sequences and one metasedimentary rock-dominated sequence. The oldest of these units is interpreted to be a thick, predominantly mafic metavolcanic sequence that is found in the southern portion of the Miminiska Peninsula and the area immediately south of Miminiska Lake. These mafic metavolcanic rocks have in turn been interpreted to be overlain by a metasedimentary rock sequence that is dominated by wacke and mudstone, but also contains significant thicknesses of banded iron formation. The metasedimentary sequence is overlain to the north by a second mafic-metavolcanic rock-dominated sequence. A significant unit of felsic to intermediate pyroclastic rocks has also been mapped in the western portion of this area (southeast of Howells Lake). This unit is located immediately south of the metasedimentary sequence west of Miminiska Lake, but is enclosed within the metasedimentary rocks further to the east. This area is bounded to the northwest by felsic intrusive rocks of the Troutfly Lake Batholith. Stratigraphic units in the vicinity of Howells Lake generally strike approximately northeast, with steep, near-vertical dip. Further to the northeast, towards Keezhik Creek, stratigraphy strikes in a more easterly orientation. Wallace (1981) indicates that foliation is generally oriented sub-parallel to the primary sedimentary bedding and igneous flow contact features. Foliation and shearing are noted by Clark (2005) to be most prominent in tuffaceous mafic metavolcanic layers. Wallace (1981b) mapped a number of northeast-trending faults and lineaments in this area. More recent maps (e.g., McKay 2004) illustrate a northeast-striking fault that parallels the metavolcanic/metasedimentary rock contact in the vicinity of Howells Lake. This structure appears to be related to many of the gold and antimony/gold occurrences in this area.
| Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Near |
|---|---|---|---|---|
| Schist-Unsubdivided | 2 | Graphitic | Near | |
| Porphyry-unsubdivided | 3 | Near | ||
| Vein | 4 | Quartz | Host |
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Chalcopyrite | Economic | Ore | ||||
| 2 | Magnetite | Economic | Ore | ||||
| 3 | Pyrite | Economic | Ore | ||||
| 4 | Pyrrhotite | Economic | Ore | ||||
| 5 | Stibnite | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| Carbonate | Alteration | Carbonatization | 1 | Unknown | Disseminated |
Oct 11, 2006 (Mark Puumala) - The Howells Lake prospect is located in close proximity to a contact between metasedimentary and metavolcanic rock units that has been interpreted as a fault (northeast-striking) on a geological compilation map prepared by McKay (2004). The occurrence of possible economic mineralization in this area was first reported by Prest (1939), who noted the presence of pyrite-mineralized porphyry intrusions and massive stibnite float on a small island in the northeastern portion of Howell's Lake. An unpublished property visit report prepared by John Scott in 1977 that is available in the Thunder Bay North Resident Geologist's Office Mineral Deposit Files indicates that economic mineralization at this location consists primarily of stibnite and gold, with minor galena, sphalerite, silver and tetrahedrite. Mineralization occurs primarily in quartz veins, with some also present in the host rocks. The quartz veins are described as being approximately perpendicular to an unconformity between the volcanic and sedimentary rocks. The presence of an unconformity at this location had been interpreted by New Jersey Zinc (holder of the claim group at the time). This contact may be equivalent to the fault interpreted by McKay (2004). Patterson et al. (1986) report the presence of an extensive zone of carbonate alteration associated with a nearby quartz porphyry intrusion, and shearing and quartz veining at the contact between mafic metavolcanic rocks and graphitic schist. The quartz veining is indicated to be associated with green mica, pyrite and stibnite. Patterson et al. (1986) also report that Homestake Mineral Development had defined two mineralization zones with the following mineral resource estimates. Western zone: 83,000 tons grading 1.37% Sb and 0.07 oz/ton Au. Eastern zone: 660,000 tons grading 3.1% Sb and with erratic Au grades.
Dec 07, 2005 (C Salo) - Carbonate alteration is associated with porphyry intrusion.
| Rank | Classification |
|---|---|
| 1 | Vein |
| Rank | Characteristic |
|---|---|
| 2 | Sheared |
| 1 | Vein |
| Zone | Year | Category | Tonnes | Reference | Comments | Commodities |
|---|---|---|---|---|---|---|
| Western Zone | 1986 | Inferred Mineral Resource | 83000 | Patterson et al. 1986. | 1.37% Sb, 0.07 oz/ton Au | Antimony 1.37 %, Gold 0.07 oz/T |
| Eastern Zone | 1986 | Inferred Mineral Resource | 660000 | Patterson et al. 1986. | 3.1% Sb with erratic Au | Antimony 3.1 % |
Map - Keezhik-Miminiska lakes area, District of Kenora (Patricia Portion), Ontario
Publication Number: ARM48E Scale: 1:63,360 Date: 1997
Author: Prest V.K.
Publisher Name: Ontario Dept. of Mines
Location:
Map - Miminiska Peninsula, Kenora and Thunder Bay districts
Publication Number: M2416 Scale: 1:31,680 Date: 1979
Author: Wallace H.
Publisher Name: Ontario Geological Survey
Location:
Mono - Mineral Occurrences and Prospects in the Fort Hope-Winisk Area
Publication Number: OFR5926 Date: 1995
Author: Mason J.K., White G.D.
Publisher Name: Ontario Geological Survey
Location:
Map - Ontario geological map, west central sheet
Publication Number: M2199 Scale: 1:1,013,760 Date: 1970
Author: Ayres L.D., Lumbers S.B., Milne V.G., Robeson D.W.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Article - Beardmore-Geraldton Resident Geologist's District - 1988
Publication Number: MP142.006 Page: 111-132 Date: 1997
Author: Mason J.K., White G.D., Speed A.A., Gaudino S.
Publisher Name: Ontario Geological Survey
Location:
Map - Fort Hope-Lansdowne House sheet, geological compilation series, Cochrane, Kenora, and Thunder Bay districts
Publication Number: M2237 Scale: 1:253,440 Date: 1972
Author: Thurston P.C., Carter M.W., Riley R.A.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Article - Thunder Bay Resident Geologist's area, North Central Region
Publication Number: MP134.004 Date: 1997
Author: Patterson G.C., Scott J.F., Mason J.K., Schnieders B.R., MacTavish A.D., Dutka R.J., Kennedy M.C., White G.D., Hinz P.
Publisher Name: Ontario Geological Survey
Location:
Article - 1982 report of the Thunder Bay Resident Geologist
Publication Number: MP107.004 Date: 1997
Author: Patterson G.C., Mason J.K., Schnieders B.R.
Publisher Name: Ontario Geological Survey
Location:
Part - Geology of the Keezhik-Miminiska lakes area
Publication Number: ARV48-06 Date: 1998
Author: Prest V.K.
Publisher Name: Ontario Dept. of Mines
Location:
File - Resident Geologist MDI files: The Howells Lake Au-Sb Deposits, New Jersey Zinc
Publication Number: Date: 1977
Author: Scott, J.F.
Publisher Name:
Location: Thunder Bay RGP
Mono - Operation Fort Hope
Publication Number: MP042 Date: 1970
Author: Thurston P.C., Carter M.W.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
MonoMap - Geology of the Opikeigan Lake area, District of Kenora (Patricia Portion)
Publication Number: R185 Date: 1978
Author: Wallace H.
Publisher Name: Ontario Geological Survey
Location:
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