Ontario Geological Survey
Permanent Link to this Record:
MDI42D14NW00002
Record Name(s) | Longworth Occurrence - 1917, Mud Vein - 1982, Tb 3250 - 1917 |
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Related Record Type | Simple |
Related Record(s) | |
Record Status | Discretionary Occurrence |
Date Created | 1980-Jan-11 |
Date Last Modified | 2022-May-06 |
Created By | |
Revised By |
Primary Commodities: Gold
Secondary Commodities: Silver, Lead
Township or Area: Pays Plat Lake Area
Latitude: 48° 59' 39.69" Longitude: -87° 19' .62"
UTM Zone: 16 Easting: 476823 Northing: 5426877 UTM Datum: NAD83
Resident Geologist District: Thunder Bay South
NTS Grid: 42D14NW, 42E03SW
Point Location Description: Map in Assessment file 42E03SE8252
Location Method: Data Compilation
Access Description: The property is located approximately 402 m east of Little Duck Lake and 804 m northeast of Bobbie Lake. The Little Duck Lake area is approximately 27 km north of Schreiber (claim map G-609). The property is accessible by aircraft to Big Duck Lake. Alternately, a diamond drill trail leads to the Big Duck Lake area from the Winston Lake Mine site.
1917: The occurrence was staked by W. Longworth. One-quarter interest in the property was transferred to S. Richardson and a second quarter to R. Matheson. 1918: One-quarter interest in the property was transferred to P. Longe. A total of 60 days of work was recorded. 1919: A total of 150 days of work was recorded. 1954: A HLEM survey was conducted for the Bathurst-Maritimes Group. 1960: Sampling of the property was done by the Keevil Mining Group. 1981: Noranda Exploration Company Limited performed a magnetometer survey over the property. 1982: IP, magnetometer and VLF-EM surveys, sampling and geological mapping were conducted by Noranda Exploration Company Limited. The occurrence was restaked by C. Dorvean for Corporation Falconbridge Copper. Diamond drilling, geophysical and geochemical surveys were conducted. Geochemical and airborne geophysical surveys were carried out. 1983: Geological sampling was conducted over the property.
Office File Number | Online Assessment File Identifier | Online Assessment File Directory |
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2.7632 | 42E03SE8252 | 42E03SE8252 |
2.5288 | 42D14NW0031 | 42D14NW0031 |
2.4624 | 42D14NW0029 | 42D14NW0029 |
2.4933 | 42D14NW0028 | 42D14NW0028 |
63.531 | 42D14NW0049 | 42D14NW0049 |
2.4146 | 42D14NW0033 | 42D14NW0033 |
Province: Superior
Subprovince: Wawa
Terrane: Wawa-Abitibi
Belt: Schreiber-Hemlo
Geological Age: Archean
Dec 07, 2005 (B Nelson) - Tanton (1920) first described the Longworth occurrence: 'on one of the Longworth claims a highly pyritiferous vein has been weathered to a depth of 12 feet and fine gold can be panned from the gossan. This is locally known as the Mud Vein though it does not occur in a fault plane. These veins range from less than a foot to about 15 feet in width and their walls are fairly distinct, though a narrower marginal zone of country rock is frequently found impregnated with quartz and pyrite. These deposits have the appearance of fissure fillings which have a minor amount of marginal replacements of country rock associated with them.'Hopkins (1922) writes that the circuitous vein which strikes northeast-southwest for 200 feet and dips from 60 to 80 degrees southeast occurs in hornblende schist and altered basic pillow lava. The vein is from one to three feet wide and consists of brown and yellow soft iron oxide carrying fragments of mica, pyrite and some galena and quartz. At depth the decomposed material will probably give way to calcite and pyrite etc. Similar decomposed material was noticed in the McQuaig, Fisher and other deposits.
Rock Type | Rank | Composition | Texture | Relationship | Schist-Unsubdivided | 1 | Hornblende | Host |
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Mafic pillowed flow | 2 | Pillowed | Host |
Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
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1 | Galena | Economic | Ore | ||||
2 | Pyrite | Economic | Ore | ||||
Quartz | Alteration | Silicification | 1 | Unknown | Disseminated |
Dec 07, 2005 (B Nelson) - The vein consists of brown and yellow soft iron oxide carrying fragments of mica, pyrite and some galena and quartz. Four chip samples, three at the northeast end; one near the southwest end, were taken across the exposed portion of the deposit by the Keevil Mining Group in September 1960. These samples indicate the gold content to be low. Wells (1984) reports that a grab sample (# TBS 538) taken by Corporation Falconbridge Copper returned 930 ppb Au.
Map - Nipigon-Schreiber, geological compilation series, Thunder Bay District
Publication Number: M2232 Scale: 1:253,440 Date: 1973
Author: Carter M.W., McIlwaine W.H., Wisbey P.A.
Publisher Name: Ontario Division of Mines
Location:
MonoMap - Mineral deposits of the Big Duck Lake area, District of Thunder Bay
Publication Number: R027 Page: 37 Date: 1997
Author: Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
File - Schreiber-Hemlo Resident Geologist Mineral Deposit Files, Thunder Bay office
Publication Number: Min Dep Date:
Author:
Publisher Name:
Location: Thunder Bay RGP
Map - Big Duck Lake area, District of Thunder Bay
Publication Number: M2023 Scale: 1:15,840 Date: 1997
Author: Pye E.G.
Publisher Name: Ontario Dept. of Mines
Location:
Mono - Gold deposits of Ontario, part 1, districts of Algoma, Cochrane, Kenora, Rainy River, and Thunder Bay
Publication Number: MDC013 Page: 300 Date: 1971
Author: Ferguson S.A., Groen H.A., Haynes R.
Publisher Name: Ontario Dept. of Mines and Northern Affairs
Location:
Mono - Mineral Occurrences in the Nipigon-Marathon Area, Volumes 1 and 2.
Publication Number: OFR5951 Page: 143-145 Date: 1996
Author: Schnieders B.R., Smyk M.C., Speed A.A., McKay D.B.
Publisher Name: Ontario Geological Survey
Location:
Part - Schreiber-Duck Lake area
Publication Number: ARV30-04.001 Page: 20 Date: 1998
Author: Hopkins P.E.
Publisher Name: Ontario Dept. of Mines
Location:
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