GeologyOntario has moved. You will be redirected to the new site in 10 seconds. If you are not immediately redirected please follow the below link to the new GeologyOntario platform. For assistance please contact us.
Ontario Geological Survey
Permanent Link to this Record:
MDI52I08NE00009
Record Name(s) | Falcon Lake West - 1955, Motsen Claim Group - 1955 |
---|---|
Related Record Type | Partial |
Related Record(s) | |
Record Status | Occurrence |
Date Created | 1980-Apr-29 |
Date Last Modified | 2023-Aug-03 |
Created By | |
Revised By |
Primary Commodities: Lithium, Tantalum, Beryllium, Rubidium
Secondary Commodities: Cesium, Niobium
Township or Area: Falcon Lake Area
Latitude: 50° 28' 27.01" Longitude: -88° 9' .07"
UTM Zone: 16 Easting: 418396 Northing: 5591985 UTM Datum: NAD83
Resident Geologist District: Thunder Bay North
NTS Grid: 52I08NE
Point Location Description: Li occurrence west of Falcon Lake
Location Method: Data Compilation
Access Description: The Falcon Lake pegmatite area is located approximately 85 km ENE of Armstrong. It can be accessed by tertiary road.
1955: Mimz Syndicated conducted prospecting and discovered the showing. 1956: British Canadian Lithium Mines Limited conducted mapping and drilled 9 DDH. 1979: Cominco Limited carried out geochemistry, sampling. 2009: Canadian Orebodies conducted mapping, sampling, trenching and soil sampling. 2010: Canadian Orebodies drilled 3 DDH totalling 263.1 m. 2016: Argonaut Resources drilled 6 DDH totalling 534 m. 2023: Battery Age Minerals optioned the property from FE Battery Metals Corp. and drilled 30 DDH totalling 2642 m.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
---|---|---|
63A.313 | 52I08NE0012 | 52I08NE0012 |
12 | 52I08NE0009 | 52I08NE0009 |
2.3207 | 52I08NE0006 | 52I08NE0006 |
2.3957 | 52I08NE0007 | 52I08NE0007 |
2.53483 | 20000009257 | 20000009257 |
2.57187 | 20000013878 | 20000013878 |
2.46925 | 20000005990 | 20000005990 |
Province: Superior
Subprovince: Wabigoon
Belt: Caribou Lake
Geological Age: Archean
Rock Type | Rank | Composition | Texture | Relationship | Amphibolite | 1 | Schistose | Contains |
---|---|---|---|---|
Pegmatite | 2 | Is |
Mar 07, 2014 (A Wilson) - The exposed pegmatite body strikes N10OE and can be followed in outcrops for about 100 feet. Diamond drilling showed the pegmatite to be a lens-shaped mass, 300 to 400 feet long and up to about 70 feet thick, with a dip of 70O-80OE. The exposed pegmatite body cuts thinly layered schistose amphibolite striking N75OE and dipping steeply south. The second pegmatite body found in the West "area" lies east of, and parallel to, the first body.
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
---|---|---|---|---|---|---|---|
1 | Spodumene | Economic | Ore | ||||
2 | Feldspar | Economic | Gangue | ||||
3 | Quartz | Economic | Gangue | ||||
4 | Albite | Economic | Gangue | ||||
5 | Tourmaline | Economic | Gangue | ||||
6 | Beryl | Economic | Gangue | ||||
7 | Apatite | Economic | Gangue |
Mar 07, 2014 (A Wilson) - One drillhole cut the lens at a depth of 190 feet. The hole intersected 60 feet of pegmatite, of which 35 feet was found to average better than l.0% Li20. A second drillhole cut the lens at a depth of 250 feet. It intersected 75 feet of pegmatite. In this case, though, only 10 feet was found to average better l.0% Li20. One drillhole returned an intersection of 1.29% Li20 over 13.7 ft. and 1.09% Li20 over 36 ft. at a vertical depth of 70 ft. The pegmatite contains spodumene as unoriented prismatic crystals, mostly 3 to 6 inches and ranging up to about 12 inches in length, associated with potash feldspar, quartz, albite, and muscovite, together with accessory amounts of apatite and black tourmaline. In outcrop, the spodumene is characteristically pale-grey or pale-green and has a high lithia content. But, in the cores from the diamond-drillholes much of the spodumene was found to be dark-green or black and highly altered. As elsewhere in the area, this alteration is due mainly to a pseudomorphic replacement of the spodumene by muscovite or sericite. The second pegmatite body found in the west area lies east of, and parallel to, the first body. Two diamond-drillholes were collared in it; in a third hole, in which both contacts were intersected, a true width of over 35 feet was indicated. This pegmatite body was found to average over l.0% Li2O and to be the most important of the several occurrences found near Falcon Lake. It is similar in character to the exposed pegmatite and may be of greater lateral extent.
Apr 10, 2019 (Therese Pettigrew) - Results from the 2010 drill program included assays up to 1.52% Li2O, 68.6 ppm Ta2O5, 214.7 ppm Be, 377.9 ppm Cs, 79.9 ppm Nb, and 3477.1 ppm Rb (Assessment report 20000009257). Results from the 2016 drill program included assays up to 1.95% Li2O and 306 ppm Ta2O5 (Assessment report 20000013878). DDH 23FL-001 returned 1.37% Li2O over 27.6 m from 16.65 m depth (Battery Age Minerals ASX release July 26, 2023).
Rank | Classification |
---|---|
1 | Pegmatite |
Mono - Pegmatite mineral resources of Ontario
Publication Number: IMR021 Page: 48, 51 Date: 1997
Author: Hewitt D.F.
Publisher Name: Ontario Dept. of Mines
Location:
MonoMap - Geology of the Crescent Lake area, District of Thunder Bay
Publication Number: R055 Page: 53-56 Date: 1968
Author: Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
Publication - Geology of Canadian Lithium Deposits; Geological Survey of Canada, Economic Geology Report 21
Publication Number: Econ Geol 21 Page: 61-62 Date: 1965
Author: Mulligan, R.
Publisher Name: Geological Survey o
Location: https://doi.org/10.4095/102454
Mono - Industrial minerals of northern Ontario-supplement 1
Publication Number: OFR5388 Page: 192-193 Date: 1982
Author: Vos M.A., Abolins T., Smith V.
Publisher Name: Ontario Geological Survey
Location:
Map - Crescent Lake area, Thunder Bay District
Publication Number: M2100 Date: 1997
Author: Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
We are continuously updating our assessment file / technical report information. If you notice errors in the data, please contact us.
Please review our Terms of Use agreement for this data product.
For detailed information regarding this mineral record please contact the Thunder Bay North Resident Geologist District Office