British Columbia Ministry of Energy, Mines and Natural Gas and Responsible for Housing
News | The Premier Online | Ministries & Organizations | Job Opportunities | Main Index

MINFILE Home page  ARIS Home page  MINFILE Search page  Property File Search
Help Help
File Created: 29-Jul-1996 by Keith J. Mountjoy (KJM)
Last Edit:  21-Jul-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name GRANITE (L.1585), BANNER (L.1586) Mining Division Greenwood, Osoyoos
BCGS Map 082E014
Status Past Producer NTS Map 082E03E
Latitude 049º 06' 03'' UTM 11 (NAD 83)
Longitude 119º 12' 27'' Northing 5441012
Easting 338870
Commodities Gold, Silver, Copper, Lead, Zinc Deposit Types I01 : Au-quartz veins
Tectonic Belt Omineca Terrane Quesnel
Capsule Geology

The Granite occurrence is located at 1204 metres elevation 6.5 kilometres east of McKinney Creek and south of Baldy Mountain. The Cariboo-Amelia occurrence (082ESW020) is located 4.5 kilometres to the northeast and Bridesville, British Columbia is located 8 kilometres to the south-southeast.

Work was reported on the Banner and Granite claims as early as 1899. At this time they were owned and operated by Camp McKinney Mines. A substantial amount of work was reported and a 5-stamp mill was reported to have run for some time with very satisfactory results. No records could be found, however, concerning the length of time, the amount of ore that was processed, or the recovered grades. It is thought that most of the mill ore was supplied from the Banner claim. Recent work on the Granite and Banner claims has been conducted in 1981 by the Rock Creek Joint Venture Syndicate, 1985 by A. Dupras, 1986 by Gold Hill Syndicate and in 1987 under option to Wapiti Exploration Inc. During 2008 through 2012, Grizzly Discoveries Inc. completed programs of geochemical (rock, stream sediment and soil) sampling, geological mapping and airborne and ground geophysical surveys on the Dayton-Sidley area of the Greenwood Property.

Lithologies underlying the Granite occurrence consists of biotite granodiorite of the Middle Jurassic Nelson intrusions. The dominant fractures strike 032 degrees. For a more detailed description of the surrounding geology refer to the Cariboo-Amelia occurrence.

On the Granite claim, it is reported that a quartz vein carried chalcopyrite, galena, pyrite and minor sphalerite. The vein is 140 centimetres wide and strikes 290 to 330 degrees in the main shaft. The vein has been traced 41 metres north to a second shallower shaft in granodiorite hostrock. In 1985, a sample was taken from 4.6 metres deep in the main shaft. This sample (582060) yielded 8.2 grams per tonne gold (Assessment Report 14609).

On the Banner claim, another quartz vein is hosted in granodiorite. Three samples were taken by the Rock Creek Joint Venture Syndicate in 1981. The best sample, a 60-centimetre chip across the vein, yielded 0.24 gram per tonne gold and 2.81 grams per tonne silver (Assessment Report 12389).

Bibliography
EMPR AR *1899-773; 1900-990
EMPR ASS RPT *9896, *12389, *14609, 16168, 16975
EMPR BULL 6, p. 6
EMPR MR MAP 7 (1934)
EMPR OF 1989-5
GSC MAP 538A; 539A; 37-21; 15-1961; 1738A
GSC OF 481; 637; 1505A; 1565A; 1969
Basque, G. (1992): Ghost Towns and Mining Camps of the Boundary Camp,
pp. 12-22
Dufresne, M. (2013-11-10): Technical Report for the Greenwood Gold Project
Dufresne, M. (2013-11-25): Technical Report for the Greenwood Gold Project
EMPR PFD 800471

COPYRIGHT | DISCLAIMER | PRIVACY | ACCESSIBILITY