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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  13-Dec-1995 by Gilles J. Arseneau (GJA)

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NMI 082K3 Ag12
Name HILLSIDE Mining Division Slocan
BCGS Map 082K005
Status Past Producer NTS Map 082K03E
Latitude 050º 02' 32'' UTM 11 (NAD 83)
Longitude 117º 09' 33'' Northing 5543337
Easting 488603
Commodities Silver, Copper Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Quesnel
Capsule Geology

The Hillside occurrence is located west of Retallack and east of Jackson creek at 1190 metres elevation above sea level, in the Slocan Mining Division.

Regionally, the area lies on the western margin of the Kootenay Arc, in allochthonous rocks of the Quesnel Terrane. In the vicinity of the occurrence, the Quesnel Terrane is dominated by the Upper Triassic Slocan Group, a thick sequence of deformed and metamorphosed shale, argillite, siltstone, quartzite and minor limestone. Rocks of the Slocan Group are tightly and disharmonically folded. Early minor folds are tight to isoclinal with moderate east plunging, southeast inclined axial planes and younger folds are open, southwest plunging with subhorizontal axial planes. The sedimentary sequence has been regionally metamorphosed to lower greenschist facies.

South of the occurrence, the Slocan Group has been intruded by the Middle Jurassic Nelson intrusions which comprise at least six texturally and compositionally distinct phases ranging from diorite to lamprophyre. The most dominant phase is a medium to coarse grained potassium feldspar porphyritic granite. Several feldspar porphyritic granodiorite dikes, apparently related to the Nelson intrusions, also cut the sedimentary sequence near the occurrence (Paper 1989-5).

The property is underlain by thinly bedded calcareous argillite, shale and slate of the Slocan Group. Minor limestone and quartzite beds are also present. The sedimentary rocks strike northwest and dip southwest. A small granodiorite stock and several quartz porphyritic dikes cut the sedimentary sequence just west of the occurrence. The area is cut by east and northwest-trending faults.

On the Hillside property three small adits totalling about 180 metres explore a quartz vein that follows a northwest trending fault zone. The vein is narrow and dips southeast. Vein mineralogy is not know, but silver and copper were recovered from the occurrence in 1900.

Production from the vein yielded 13,654 grams of silver and 424 kilograms of copper from a total of 2 tonnes mined.

Bibliography
EMPR AR 1911-290; 1926-248; 1966-223
EMPR ASS RPT *9659
EMPR BC METAL MM01233
EMPR EXPL 1980-105
EMPR INDEX 3-200
EMPR P 1989-5
GSC MAP 273A; 1667
GSC MEM 173; *184, p. 223; 309
GSC OF 464
EMPR PFD 752813

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