Ontario Geological Survey
Permanent Link to this Record:
MDI000000001777
Record Name(s) | Point Showing - 1946 |
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Related Record Type | |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 2014-Oct-16 |
Date Last Modified | 2022-Feb-23 |
Created By | |
Revised By |
Primary Commodities: Gold
Township or Area: Garden Lake Area
Latitude: 49° 32' 4.61" Longitude: -89° 47' 55.54"
UTM Zone: 16 Easting: 297504 Northing: 5490653 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 52H12SW
Point Location Description: Trench location from map P3422
Location Method: Data Compilation
Access Description: This occurrence is located adjacent to Garden Lake and can be accessed by boat. Access to the north shore of Garden Lake can be achieved by travelling approximately 7.5 km southwest along Grew Road from the intersection of Highway 811. Then proceed south for approximately 4 km along a secondary logging road.
1946: Prospecting, sampling, geological mapping and diamond drilling by Little Long Lac Gold Mines Ltd. 1987-89: Airborne and ground geophysical surveys, geological mapping and outcrop stripping by Garden Lake Resources. The showing is currently located within the boundaries of the Garden Pakashkan Conservation reserve and is no longer open for staking.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.17987 | 52H12SE2001 | 52H12SE2001 |
63.2983 | 52H12SE0011 | 52H12SE0011 |
2.13306 | 52H12SW9180 | 52H12SW9180 |
14 | 52H12SW0018 | 52H12SW0018 |
63.6337 | 52H12SW0019 | 52H12SW0019 |
63.5295 | 52H12SW0010 | 52H12SW0010 |
2.11717 | 52H12SW0011 | 52H12SW0011 |
2.10886 | 52H12SW0012 | 52H12SW0012 |
Province: Superior
Subprovince: Wabigoon
Belt: Beardmore-Geraldton
Geological Age: Archean
Oct 21, 2014 (Mark Puumala) - The following geological description is excerpted from Hart (2000). The main rock types in the trenches are basaltic flows and pillowed flows intruded by porphyritic felsic dykes. In some cases the dykes intrude at a shallow angle to the bedding. The basalts are variably sheared, ranging from undeformed pillowed flows on the south to intensely sheared banded chloritic units on the north, in the GLDZ. The intensely sheared units are very strongly iron carbonate altered. The dykes are also highly deformed within the GLDZ, moderately carbonatized, with quartz veining containing minor tourmaline and 1 to 2% pyrite. Quartz veining with tourmaline was not observed elsewhere in the belt. A sample of the quartz veining with tourmaline contained no detectable gold (sample365; Table 3).
Rock Type | Rank | Composition | Texture | Relationship | Mafic lava flow-unsubdivided | 1 | Basalt |
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Porphyry-unsubdivided | 2 | Porphyritic Felsic Dyke |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Pyrite | Economic | Ore | ||||
2 | Galena | Economic | Ore | ||||
1 | Tourmaline | Economic | Gangue |
Oct 21, 2014 (Mark Puumala) - The following discussion of mineralization at the Point Showing is excerpted from Hart (2000 OFR6037). Little Long Lac Mines Gold Ltd. conducted the initial exploration of the gold showing located on the point situated along the south east shore of Garden Lake, west of the Bluff showing (Phelan, 1946). The gold bearing units at the Point showing are described as being quartz filled shear zones in an arkose with coarse cubic pyrite and galena. The best grab sample returned 0.22 oz Au/t, but could not be duplicated by additional sampling or a single diamond drill hole with a length of 194 m. A sample by C. Bumbu in 1984 assayed of 8.5 g Au/t across 3 m in pyritized and cherty buff coloured carbonate rocks (Junnila, 1989). A grab sample during a property visit by Garden Lake Resources returned 23.3 g Au/t. The IP survey identified a string of anomalies located under the lake, north of the Point showing. These results lead to a program of power stripping in 11 areas, geological mapping and collection of 52 samples for assay. The rocks in the trenches were described as a 600 m thick succession of, from north to south, chlorite schist / mafic tuff, sedimentary carbonate-chlorite schist, chlorite schist, and pillowed flows. This succession youngs to the south, with foliations trending south west. Numerous small quartz-carbonate veins parallel to foliation generally contain 1% pyrite. Assays from the sampling program averaged 0.03 g Au/t, and re-sampling of the original trench could not confirm the previously reported gold value. The showing was visited by the Resident Geologist.s staff in 1989, before the stripping was conducted by Garden Lake Resources (Lavigne et al., 1990). The rocks were described as a sheared, buff tan coloured, sericitized feldspar porphyry with relict feldspar crystals and pyrite cubes up to 0.5 cm. A sample of this material assayed 630 ppb Au.
Rank | Classification |
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1 | Lode (Gold) |
MonoMap - Precambrian Geology, Garden Lake Area
Publication Number: OFR6037 Scale: Date: 2000
Author: Hart T.R.
Publisher Name: Ontario Geological Survey
Location:
Mono - Garden-Obonga Lake Area High Density Lake Sediment and Water Geochemical Survey, Northwestern Ontario
Publication Number: OFR6009 Scale: Date: 2000
Author: Jackson J.E., Dyer R.D.
Publisher Name: Ontario Geological Survey
Location:
MonoMap - Geology of the Garden Lake area, District of Thunder Bay
Publication Number: R025 Scale: Date: 1997
Author: Milne V.G.
Publisher Name: Ontario Dept. of Mines
Location:
Data - Ontario Airborne Geophysical Surveys, Magnetic and Electromagnetic Data, Garden-Obonga Area
Publication Number: GDS1105 Scale: Date: 2000
Author: Ontario Geological Survey
Publisher Name: Ontario Geological Survey
Location:
Map - Precambrian Geology, Garden Lake Greenstone Belt (West Half)
Publication Number: P3422 Scale: 1:20,000 Date: 2000
Author: Hart T.R.
Publisher Name: Ontario Geological Survey
Location:
Map - Garden Lake area, Thunder Bay District
Publication Number: M2058 Scale: 1:63,360 Date: 1997
Author: Milne V.G.
Publisher Name: Ontario Dept. of Mines
Location:
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