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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  02-Mar-2009 by Shea Sweene (SSW)

Summary Help Help

NMI 093L14 Au9
Name GLACIER GULCH (NORTH SIDE) Mining Division Omineca
BCGS Map 093L084
Status Past Producer NTS Map 093L14W
Latitude 054º 49' 48'' UTM 09 (NAD 83)
Longitude 127º 16' 56'' Northing 6077227
Easting 610342
Commodities Silver, Lead, Zinc, Gold, Copper Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Intermontane Terrane Stikine
Capsule Geology

The mineralization occurs near a fault contact with Lower Jurassic Hazelton Group volcanics of the Telkwa Formation and the Lower Cretaceous Skeena Group sediments. Fractures cut across the volcanic host rocks and mineralization occurs along silicified joints and bedding planes in the tuffs of the Hazelton Group as well as in quartz veins. The veins host occurrences of galena, sphalerite, pyrite and pyrrhotite. The dark green, fine-grained andesites lie in fault contact with the younger sediments comprised of rusty weathering quartzite, greywacke, slate and conglomerate. The basal sedimentary unit is comprised of a number of coal seams striking northwards and dipping 45 to 60 degrees east.

The main quartz vein, at 900 metres elevation, hosts dark sphalerite and minor amounts of arsenopyrite, pyrite, pyrrhotite, galena, and chalcopyrite accompanied by minor quartz gangue. The vein strikes 010 degrees and dips between 50 to 60 degrees west. The fissuring extends to the fault contact of the volcanic and sedimentary rocks. Samples collected by D. Lay in 1937 near the bottom of the shaft assayed 2.05 grams per tonne gold and 20.57 grams per tonne silver. Another sample collected by D. Lay, a 45.7 centimetre channel sample across the face of the drift assayed 6.86 grams per tonne gold, 233 grams per tonne silver, 2 per cent lead, and 5.4 per cent zinc (Minister of Mines Annual Report 1937, page C20).

In an open cut near the shaft a sphalerite vein 5 metres in length and 13 centimetres wide was exposed. Southwest of this vein is another vein consisting of equal parts of quartz and pyrrhotite with a little chalcopyrite. A 20 centimetre channel sample across the vein assayed 12.34 grams per tonne gold, 0.54 per cent copper, and nickel nil (Minister of Mines Annual Report 1938).

In another open cut, further southeast of the shaft, a vein was exposed consisting of solid sphalerite with 5 to 10 per cent quartz gangue, minor galena, pyrrhotite, and chalcopyrite.

Production data between the years 1933 to 1939 totalled 165 tonnes mined with 9,236 grams gold, 36,919 grams silver, 2400 kilo- grams lead, and 6,053 kilograms zinc.

Bibliography
EMPR AR 1926-131; 1927-137; 1928-163; 1930-140; 1933-97; 1934-
C5; 1935-C35,G48; 1936-G43; *1937-C20,33; 1938-B36-38; 1939-
55,58,70; 1940-41,43; 1941-41; 1950-100; 1958-10; 1959-17;
1961-19; 1962-16; 1963-26; 1964-51
EMPR ASS RPT 5041, 6480, 10370, 18236, 19569, 20797, 21743
EMPR EXPL 1975-E143; 1977-E97
EMPR FIELDWORK 1988, pp. 195-208
Kirkham, R.V., (1969): A Mineralogical and Geochemical Study of
the Zonal Distribution of Ores in the Hudson Bay Range, British
Columbia, Ph.D. Thesis, University of Wisconsin
EMPR GEM 1973-347; 1974-262
EMPR MAP 69-1
EMPR OF 1993-21; 1994-14
EMPR PF (Glacier Gulch Group)
EMPR PF Rimfire (Sirola, W.M. (1977-10-04): Re: Hudson Bay Mountain (Glacier Gulch) Molybdenum Prospect)
GSC BULL 270
GSC MAP 971A
GSC MEM *223, pp. 72,73
GSC OF 351
GSC P 44-23

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