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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  23-Nov-1995 by Craig H.B. Leitch (CHBL)

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NMI 082F2 Au1
Name VIRGINIA (L.6887), OHIO (L.5962), VIRGINIA, BAYONNE, MAY 1, YVONNE Mining Division Nelson
BCGS Map 082F016
Status Past Producer NTS Map 082F02W
Latitude 049º 09' 12'' UTM 11 (NAD 83)
Longitude 116º 57' 28'' Northing 5444502
Easting 503079
Commodities Gold, Silver Deposit Types I01 : Au-quartz veins
I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Ancestral North America
Capsule Geology

There appears to be some confusion regarding the location of the Virginia; at least three separate but reasonably close locations are indicated by the map on page E10 of the Minister of Mines Annual Report for 1937. First, there is a symbol with the name Virginia, just east of Arkansas Lake; second, the Virginia Crown grant (Lot 6887); and third, the Crown grant Ohio (Lot 5962) assigned to the Virginia in MINFILE, both on the map and on the data sheet, from which recorded production has come. To add to the confusion, the Geological Survey of Canada National Mineral Inventory lists the Virgina as a sub-name for the North Wind property (082FSE049).

The property is located between elevations of 1830 to 2137 metres on the west side of John Bull Mountain, on the Summit Creek watershed some 24 kilometres east-southeast of Salmo. The Echo group of claims (082FSE031) lies to the southeast and the Bayonne group (082FSE030) lies to the east. See Bayonne for exploration details.

There is general consensus among the references consulted that the showings consist of a fracture, slip surface or fracture zone, varying along its length from 0.3 to 1 metre wide, in places filled with leached, honeycombed quartz up to 0.6 metre thick, and variably gossanous. Sheared rusty granodiorite adjoins the fissure in places, which is hosted in granodiorite of the Mine stock, part of the Nelson intrusions of Middle Jurassic age. Gossan and crushed granitic material contain traces of gold; however, recorded production in 1936 and 1938 of 19 tonnes averaged 19.5 grams per tonne gold and 30.8 grams per tonne silver.

The fracture system strikes 105 to 100 degrees and dips 72-85 degrees to the north; it has been exposed over a strike length of 100 metres. Geochemical and physical work (mapping, trenching) was performed over this and adjoining ground by Goldrich Resources in 1987.

Bibliography
EMPR AR 1904-131; 1909-276; 1915-171; 1934-E26; 1937-E10, E45; 1938- A36,E42
EMPR ASS RPT 16846, 20982, 24448, 24450, 25387, 25472, 25742
EMPR BC METAL MM01087
EMPR FIELDWORK 1994, pp. 135-155
EMPR INDEX 3-217
EMPR PF (Typewritten special report by H. Sargent: see Minister of Mines Annual Report 1937, Part E, page 45)
GSC MAP 603A
GSC MEM 228, p. 83
GSC OF 929; 2721
EMPR PFD 2586, 600200

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