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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  22-Jul-2020 by Karl A. Flower (KAF)

Summary Help Help

NMI
Name TWO BROTHERS (L.2005), PRESIDENT (L.2006) Mining Division Revelstoke, Slocan
BCGS Map 082K045
Status Showing NTS Map 082K06E
Latitude 050º 25' 04'' UTM 11 (NAD 83)
Longitude 117º 00' 11'' Northing 5585083
Easting 499783
Commodities Copper, Silver Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Kootenay, Ancestral North America
Capsule Geology

The Two Brothers occurrence is located on Gallop Creek, west of Duncan Lake, in the Slocan Mining Division. The showing is situated on Reverted Crown grant Lot 2005 which is part of a contiguous group of three Reverted Crown grants and two fractional Crown grants (Lots 2005 to 2009) (see President, 082KSE012).

Regionally, the area lies within the Selkirk Mountains of southeastern British Columbia. The occurrence is within the Kootenay Arc, a curving belt of highly deformed metasedimentary and metavolcanic rocks which includes the Upper Proterozoic Horsethief Creek Group, the Upper Proterozoic to Lower Cambrian Hamill Group, the Lower Cambrian Badshot Formation, and the Paleozoic Lardeau and Milford groups. The volcano-sedimentary sequence is intruded by numerous Paleozoic to Mesozoic granitoid plutons.

The property is underlain by quartzite, limestone and volcanic rocks of the Index Formation of the Lardeau Group. The quartzite is locally brecciated and chloritic within north-trending shears. A 2-metre chip sample across a mineralized shear on Lot 2007 (President Fr.) (082KSE012) assayed 260 grams silver (Assessment Report 9480). Ore minerals within the shear consist of argentite and sphalerite.

In 1970, trenching work on the Two Brothers Reverted Crown grant uncovered a 3.5 metre wide area of quartz veining within altered limestone. This mineralization consists of mariposite, pyrite and tetrahedrite occurring as stringers in narrow quartz veins. The veins carried only low silver values (Exploration in British Columbia 1977).

Work History

In the 1890’s, mineralized float was identified in the area.

In 1970, a program of stripping and trenching was reportedly performed on the area. In 1976, Precambrian Shield Resources Ltd. option the property from Consolidated Boundary Exploration Ltd. and a lone diamond drill hole was completed. In 1980, Cominco completed a program of soil sampling and trenching.

In 2011, the area was examined by Moose Mountain Technical Services on the behalf of Rainbow Resources Inc. as the Big Strike property.

Bibliography
EMPR AR 1898-1084,1190,1192; 1903-244; 1924-368; *1925-236; 1926-269;
1928-310
EMPR ASS RPT 6282, *9480
EMPR BULL 49
EMPR EXPL 1976-E47; *1977-E65; 1978-E77; 1980-114,115
EMPR GEM 1969-336, Fig. 41#79; 1970-462; 1971-424
EMPR GEOS MAP 1995-1
EMPR P 1993-1, pp. 9-16
EMPR PF (See President, 082KSE012 - Canadian Superior Exploration
Ltd., Field notes and assay results)
GSC BULL 193
GSC MAP 1326A
GSC MEM 161; 369
GCNL #213, 1979
Morris, R.J. (2012-03-27): Property of Merit Report– West Kootenay Properties – Big Strike Project

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