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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  25-Sep-1995 by Gilles J. Arseneau (GJA)

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NMI 082K2,7 Pb1
Name LAVINA (L.3784), IRON CAP (L.3785), RUTHIE BELL (L.3786), ST. JOSEPH (L.3787), BUTE FR. (L.3789), GIANT Mining Division Slocan
BCGS Map 082K026
Status Past Producer NTS Map 082K02W
Latitude 050º 14' 48'' UTM 11 (NAD 83)
Longitude 116º 53' 37'' Northing 5566062
Easting 507585
Commodities Silver, Lead, Zinc Deposit Types E12 : Mississippi Valley-type Pb-Zn
E13 : Irish-type carbonate-hosted Zn-Pb
Tectonic Belt Omineca Terrane Kootenay, Ancestral North America
Capsule Geology

The Lavina prospect is situated near the peak of Mount Lavina in the Slocan Mining Division. The property consists of five Crown grants, Lot 3785 (Iron Cap), Lot 3786 (Ruthie Bell), Lot 3787 (St. Joseph), Lot 3789 (Bute Fraction) and Lot 3784 (Lavina). The main workings are on Crown grant Lot 3784.

Regionally, the area lies within the Kootenay Arc near the margins of the Ancestral North American Terrane. The Kootenay Arc is a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Eocambrian Hamill Group, the Lower Cambrian Badshot Formation, and the lower Paleozoic Lardeau Group. The volcano-sedimentary sequence is intruded by numerous Ordovician, Devonian and Mississippian granitoid plutons. The rocks have undergone regional metamorphism to middle or upper greenschist facies (Paper 1993-1).

The occurrence is in limestone and dolomite of the Lower Cambrian Badshot Formation on the eastern limb of the Duncan anticline (Geological Survey of Canada Map 1326A). The formation strikes northwest and dips between 35 and 60 degrees to the east. The main workings consist of two interconnecting adits on the north slope of Lavina Ridge. Mineralization within the workings consisted of a series of lenticular quartz and calcite veins less than 10 centimetres wide containing fine to medium-grained galena and cerussite. The ore was best developed in the limestone below a narrow band of dark grey biotite schist.

Two hundred and twenty-nine tonnes of ore were mined from this property to produce 276,754 grams of silver, 124,340 kilograms of lead and 2335 kilograms of zinc.

Bibliography
EMPR AR 1897-528; 1899-597,694,708; 1900-850,986; 1902-151; 1903-140; 1904-161,198; 1906-143; 1917-155,188; 1918-162; 1924-190; 1925-235; 1926-268; 1927-283
EMPR BC METAL MM01268
EMPR BULL *49, pp. 75-76
EMPR FIELDWORK 1992, pp. 9-16
EMPR GEM 1972-72
EMPR GEOS MAP 1995-1
EMPR INDEX 3-203
EMPR PF (82KSE General File - Geology map by P. Billingsley, 1958)
EMR MP CORPFILE (Embassy Petroleum Ltd.)
GSC MAP 1929-2; 235A; 1326A
GSC MEM 161, pp. 26,105-108; 369
Pope, A.J. (1989): The Tectonics and Mineralization of the Toby- Horsethief Creek Area, Purcell Mountains, Southeast British Columbia, Canada, unpublished Ph.D. Thesis, University of London, England
EMPR PFD 810270

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