British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 16-Aug-1990 by Garry J. Payie (GJP)
Last Edit:  18-Mar-2026 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name POLY Mining Division Victoria
BCGS Map 092B081
Status Showing NTS Map 092B13W
Latitude 048º 52' 03'' UTM 10 (NAD 83)
Longitude 123º 55' 01'' Northing 5413132
Easting 432755
Commodities Copper, Silver, Zinc, Rhodonite, Gold Deposit Types Q02 : Rhodonite
Tectonic Belt Insular Terrane Wrangell
Capsule Geology

The Poly occurrence is located between Chipman and Solly creeks, approximately 3 kilometres north of the Chemainus River.

Regionally, the area is underlain by chert, siliceous argillite and siliciclastic rocks of the Mississippian to Pennsylvanian Fourth Lake Formation (Buttle Lake Group) and volcaniclastic rocks of the Middle to Upper Devonian Mclaughlin Ridge Formation (Sicker Group). These rocks are intruded by granodiorite and quartz diorite of the Early to Middle Jurassic Island Plutonic Suite and gabbroic to dioritic rocks of the Triassic Mount Hall Gabbro. Undivided sedimentary rocks of the Upper Cretaceous Nanaimo Group locally overlay the previous units.

Locally, argillite interbedded with a foliated tuff strikes west-northwest with a moderate dip to the north. Foliation has the same strike but has a steep northerly dip. The argillite contains finely disseminated pyrite and minor chalcopyrite. Limonite staining occurs locally. Rhodonite is also reported in the area.

Work History

In 1985 and 1986, E. Specogna completed programs of prospecting, rock sampling and four diamond drill holes, totalling 20.7 metres. In 1985, a rock sample (P2) of fresh rhodonite, taken approximately 500 metres to the southeast of the plotted location of the occurrence, assayed 0.14 gram per tonne gold (Assessment Report 14919).

Also at this time, Abermin Corp. and Laramide Resources conducted a program of geological mapping, trenching, rock sampling and diamond drilling to continue testing the Coronation Zone (MINFILE 092B 129) and other reconnaissance targets on the Lara property including the Poly occurrence area.

In 1987, Canamin Resources completed a program of geological mapping and geochemical sampling. Samples from the occurrence assayed up to 1.0 gram per tonne silver and 0.056 per cent zinc (Assessment Report 16906).

In 2023 and 2024, Nova Pacific Metals Corp. conducted a three-dimensional interpretation of a previous completed airborne magnetic survey on the Coronation trend of the Lara property, including the Poly occurrence area.

Bibliography
EMPR ASS RPT *14919, 15737, 15823, *16906, 42881
EMPR BULL 37
EMPR COMM FILE (Sargent, H. (1956): Manganese Occurrences in
British Columbia; Leaming, S.F. (1966): Rhodonite in British
Columbia, The Canadian Rockhound; Danner, W.R. (1975): Gem
Materials of British Columbia, Montana Bureau of Mines and
Geology, Special Publication 74)
EMPR FIELDWORK 1982, p. 46; 1987, pp. 81-91
EMPR OF 1988-8
EMPR PFD 680535
GSC MAP 42A; 1386A; 1553A
GSC MEM 13; 96
GSC OF 463; 701; 821
GSC P 72-44; 72-53; 75-1A, p. 23; 79-30
Cowley, P. (1979): Correlation of Rhodenite Deposits on Vancouver
Island and Saltspring Island, British Columbia, Unpublished B.Sc.
Thesis, University of British Columbia

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY