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File Created: 16-Sep-1989 by Peter S. Fischl (PSF)
Last Edit:  31-Aug-2007 by Sarah Meredith-Jones (SMJ)

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NMI 082E1 Lst1
Name FIFE LIMESTONE, CHRISTINA LAKE, GRAND FORKS Mining Division Greenwood
BCGS Map 082E009
Status Past Producer NTS Map 082E01E
Latitude 049º 04' 18'' UTM 11 (NAD 83)
Longitude 118º 12' 25'' Northing 5436124
Easting 411849
Commodities Limestone Deposit Types R09 : Limestone
Tectonic Belt Omineca Terrane Quesnel
Capsule Geology

A vertically dipping bed of limestone outcrops along Highway 3 on Christina Lake, 0.8 kilometres north of the Fife cut off road and continues north-northeast up the hillside for at least 3.2 kilometres. The limestone has been correlated with the Pennsylvanian to Permian Mount Roberts Formation or (according to the Geological Survey of Canada Open File 1969) an Ordovician to Devonian unnamed unit. The bed thickens from 27 metres along the highway to 240 metres, 1.5 kilometres northeast.

The bed contains medium to fine grained, bluish grey to white, banded limestone that is intensely fractured and sheared. Nodules and lenses of blue chert and streaks of rusty and siliceous limestone contaminate this deposit. The siliceous limestone is more common near the contacts with the enclosing volcanics. Contorted mafic dykes intrude the limestone. Two samples analyzed as follows (in per cent):

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Sample A Sample B

CaO 52.78 51.0

MgO 0.30 0.3

Insolubles 4.64 -

SiO2 - 6.5

R2O3 0.20 -

Al2O3 - 0.1

Fe2O3 0.17 0.3

MnO 0.02 -

P2O5 0.016 -

Sulphur 0.02 -

Ig. Loss 41.94 41.5

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Sample A was taken across a 27.4 metre wide face of the southern quarry on the east side of the C.P. Railway track (Minister of Mines Annual Report 1959, p. 173, Sample 6). Sample B is a representative analysis of the limestone quarried in the early 1940's (CANMET Report 811, p. 197).

Limestone was produced from four major quarries and several smaller quarries and glory holes on both sides of the C.P. Railway, 0.8 to 1.6 kilometres north of Fife, between 1911 and 1957. A total of 1.6 million tonnes of limestone were quarried during this time. The limestone was used entirely for flux at Cominco's smelter in Trail.

Bibliography
EMPR AR 1913-27; 1914-28; 1915-33; 1916-31; 1918-205; 1919-163; 1920-
155; 1921-180; 1922-171; 1923-180; 1924-164; 1925-194; 1926-206;
1927-226; 1928-236; 1930-228,423; 1931-239; 1932-286; 1935-G52;
1936-D58; 1938-D41; 1939-A112; 1940-A98; 1941-A93; 1942-A91;
1943-A86; 1944-A82; 1945-132; 1946-206; 1947-218; 1948-189; 1949-
257; 1950-225; 1951-222; 1952-260; 1953-192; 1954-182; 1955-94;
1956-152; 1957-87; *1959-173
EMPR OF 1992-18, pp. 116, 117
GSC MAP 6-1957
GSC OF 481; 1969
CANMET RPT 452, Vol. 5, p. 148,149; *811, Part 5, pp. 196-197
EMPR PFD 1036, 1255, 752810

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