Mineral Deposit Inventory for Ontario

Ministry of Energy, Northern Development and Mines

Permanent Link to this Record: MDI52C13NW00004

Deposit: MDI52C13NW00004

General

Mineral Deposit Identification
Deposit Name(s) 404 Road - 1982
Related Deposit Type None
Deposit Status occurrence
Date Created 1987-May-07
Date Last Modified 2019-Nov-26
Created By Q Unknown
Revised By T Pettigrew

Commodities

Primary Commodities: granite (building stones)

Location

Township or Area: Rowe

Latitude: 48° 57' 55"    Longitude: -93° 59' 11.71"

UTM Zone: 15    Easting: 427789   Northing: 5424065    UTM Datum: NAD83

Resident Geologist District: Kenora

NTS Grid: 52C13NW, 52D16NE

Point Location Description: Map on p. 33 of MDC027

Location Method: data compilation

Source Map: OGS 1975, MAP 2325 OFF LAKE-BURDITT LAKE

Sources Map Scale: 1:50 000

Access Description: Eastern part of Rowe Township, on the north side of Road 404

Exploration and Mining History

There is no recorded bedrock extraction, but several small gravel pits are present. No assessment reports were found on file.

Geology

Province: Superior

Subprovince: Wabigoon

Intrusion: Sabskong Batholith

Geological Age: Archean   

Mineral Deposit Lithology

Lithology Data
Rock Type Rank Composition Texture Relationship
felsic intrusive 1 granite is

Mineralization

Deposit Mineralization and Alteration
Rank Mineral Name Class Economic Mineral Type Alteration Mineral Type Alteration Ranking Alteration Intensity Habit Description
1 biotite economic gangue

Mineralization Comments

11/26/2019 (T Pettigrew) - The area examined comprises light pinkish grey, medium-grained biotite 'granite'. There are three predominant joint sets: 120-145/85 E 3 m or more apart; 030/85 E 1.5 m or more apart; and 080-090/85 S. The outcrop surface is lichen-covered but does not appear to have great textural variations. There is a slight foliation trending 315 degrees in the western outcrops and only a few small knots in evidence. Aplite dikes 5 to 30 cm wide locally cut the granite. The dikes are usually several metres apart. The colour of the granite varies from light pink-grey to grey-brown; the grey-brown shade is predominant. Colour changes are gradational over distances of 50 to 100 m (Storey, 1986).

References

Publication - Building and Ornamental Stone Inventory in the Districts of Kenora and Rainy River, p. 32-33

Publication Number: MDC027    Date: 1986

Author: Storey, C.C.

Publisher Name: OGS


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Ministry Contact Information

For detailed information regarding this mineral deposit please contact the Kenora Resident Geologist District Office