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File Created: 13-May-1991 by Garry J. Payie (GJP)
Last Edit:  07-May-2007 by Nicole Robinson (NR)

Summary Help Help

NMI
Name JOHN, MAGNUSON Mining Division Trail Creek
BCGS Map 082F013
Status Prospect NTS Map 082F04E
Latitude 049º 07' 32'' UTM 11 (NAD 83)
Longitude 117º 32' 28'' Northing 5441554
Easting 460521
Commodities Silver, Zinc, Lead Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Quesnel
Capsule Geology

The John showing is underlain by sediments of the Lower Jurassic Elise Formation, Rossland Group. The host rocks consist of thin- bedded limestones and argillites lying above massive limestone. The bedding strikes 153 degrees and dips 40 degrees to the southwest.

Workings, consisting of a pit and an 18-metre long adit, explore a fissure which varies from a crack to 0.45 metres in width. Pyrite is reported to be the main visible mineral. The fissure is vertical and strikes 100 degrees. In 1954, a shipment consisting of 7.2 tonnes of "development rock" was made to the Trail smelter. The ore produced 404 grams of silver, 79 kilograms of lead and 145 kilograms of zinc (Minister of Mines Annual Report 1954, page 153).

Bibliography
EMPR AR *1954-50,123
EMPR BC METAL MM01021
EMPR BULL 74; 109
EMPR FIELDWORK 1987, pp. 19-30; 1988, pp. 33-43; 1989, pp. 11-27;
1990, pp. 9-31
EMPR OF 1988-1; 1989-11; 1990-8; 1990-9; 1991-2; 1991-16
GSC MAP 1090A; 1091A; 1504A
GSC MEM 77; 308
GSC OF 1195
GSC P 62-5; 79-26
GCNL #68 (Apr. 6), 1992

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