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File Created: 24-Jul-1985 by BC Geological Survey (BCGS)
Last Edit:  04-Jan-1996 by Gilles J. Arseneau (GJA)

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NMI 082F14 Pb13
Name JENNIE LIND (L.1806), READ (L.1247), TENDER FOOT (L.1248), CARNATION, REED, ROBERTSON (L.1808) Mining Division Slocan
BCGS Map 082F094
Status Past Producer NTS Map 082F14W
Latitude 049º 57' 50'' UTM 11 (NAD 83)
Longitude 117º 16' 50'' Northing 5534653
Easting 479878
Commodities Silver, Lead, Zinc, Gold Deposit Types I05 : Polymetallic veins Ag-Pb-Zn+/-Au
Tectonic Belt Omineca Terrane Quesnel
Capsule Geology

The Jennie Lind property is situated on the south side of Carpenter Creek, between Idaho and Selkirk peaks at 1950 metres elevation above sea level in the Slocan Mining Division. The property includes the Jennie Lind, Read and Tender Foot Crown grants (Lots 1806, 1247 and 1248 respectively). The underground workings are on the Jennie Lind claim.

The initial discoveries and development work were at the higher elevations, on the Read, Robertson and Jennie Lind claims on the west side of the ridge, and on the Carnation (082FNW048) and Tenderfoot claims on the east side. Later work was at lower elevations on the east side of the ridge on the Violet & Violet Fr. claims, and in a crosscut adit driven from the adjoining Minniehaha (082FNW048) property.

The Read, Robertson & Tenderfoot claims, owned by W.M. Robertson and associates, were under bond in 1892 to the London Mercantile Association, and in 1893 to J.A. Finch and associates. The Jenny Lind claim was owned by Paul & Chas. Anderson of Silverton. They reported a small shipment of ore in 1895. The Carnation claim, owned by D.D. Mann was under development from 1895 or earlier. Crown-grants were issued in 1897 as follows: the Carnation (Lot 575) to D.D. Mann, the Read (Lot 1247) and Tenderfoot (Lot 1248) to E.E. Evans, the Jennie Lind (Lot 1806) and Robertson (Lot 1808) to The West Kootenay (B.C.) Exploring and Mining Company, Limited. In 1904 the Robertson and Jennie Lind claims were held as part of the adjacent Wakefield property (82FNW059) which was under lease to The Anglo-Slocan Syndicate Limited. The Read and Tenderfoot claims were worked in 1906 by M.S. Davys who shipped a small amount of ore.

During the period 1917 to the mid 1920's claims on the east side of the ridge, including the Carnation, Violet (Lot 3168) and Violet Fr. (Lot 3170) were held by G.W. Clark & associates under bond from A.R. Mann and others. During that period considerable development work was done in Nos. 2 and 3 adits. The Victoria Syndicate, Limited, of London, acquired an option on the property in 1925. Development work was carried out on both sides of the ridge, mainly in No. 2 drift adit which was driven southwesterly for 853.4 metres through the mountain to the Jennie Lind claim. A raise was driven to the old Read workings. A 3048-metre tramline was installed at the west portal of No. 2 adit at an elevation of 1967 metres. The syndicate dropped the option in 1928 and work was resumed by G.W. Clark. In January 1929 A.R. Mann & associates incorporated Carnation Silver Lead Mines, Limited to acquire the 17 claims and fractions. The claims were electrically prospected for one month by The Radiore Company of Canada, Limited. Underground work began in August in No. 3 adit on the east side of the ridge. Operations ceased in 1930.

Early exploration on the Jennie Lind and Read claims on the west side of the ridge was carried out in a series of 8 or more short adits and open cuts. On the east side of the ridge, to 1930, the main lode (Carnation lode) had been partly explored on and close to the northeast corner of the Carnation claim by 3 adits and a 6-metre shaft. A 36.5-metre drift adit was driven on the "D" vein at the 1996-metre elevation about 183 metres northwest of No. 2 adit; the latter as mentioned earlier, had been driven through the mountain at the 1966 metre elevation. A third adit, begun in 1929 at the 1920 metre elevation, was driven as a crosscut for 45.7 metres northwesterly to the lode, which was drifted on southwesterly for about 122 metres.

Kelowna Exploration Company, Limited in 1939 optioned the Carnation and adjacent claims and began an extensive geological survey. The option on the Carnation was given up in 1940 but control of the adjacent claims was retained. In August 1945 the company purchased the Carnation group of 14 Crown-granted claims and fractions. In 1948 the old No. 3 adit at 1920 metres elevation was reopened. In 1949 a new low level adit at elevation 1670 metres was begun at the south edge of the Western Fr. claim of the Minniehaha property, and a second, 1670-metre east adit, was driven the following year. Two crosscuts were driven across the lode in the old 1920-metre adit and a new adit (1859 metres) was driven westerly for 166 metres after the lode had been uncovered at that level by stripping. The new low-level 1670-metre adit was driven in search of the downward extension of the Carnation lode exposed in the 1920 adit, 243.8 metres above. The new adit was driven 70 metres southwesterly into the hill, then 420.6 metres in a south 7-degree west direction through the adjacent Evening claim (082FNW049). Two mineralized lodes, about 122 metres apart, were encountered. The first, probably related to the Minniehaha lode, was drifted on for 103.6 metres in the 1670 main adit and for 97.5 metres in the 1670 east adit. The second lode (Carnation lode) was drifted on westerly for about 548.6 metres to a point down dip from the upper levels and a crosscut was driven 100.5 metres into the hangingwall. The company name was changed in 1951 to Kelowna Mines Hedley Limited. The results of the exploration work were disappointing and operations ceased in June 1951.

Silver Standard Mines Limited, in 1961, acquired an option on 59 claims from Oil Participations Incorporated who had acquired the claims from Kelowna Mines when that company was dissolved in 1958. Drilling was done to test the Carnation lode 122 metres below the 1670 level. Subsequent exploration was on claims down dip to the east (see Silvana (82FNW050)). Silmonac Mines Limited was incorporated in 1963 to acquire the property. The company name was changed in 1977 to Silvana Mines Inc.

Regionally, the area lies on the western margin of the Kootenay Arc, in allochthonous rocks of the Quesnel Terrane. In the vicinity of the occurrence, the Quesnel Terrane is dominated by very fine grained clastic sedimentary rocks of the Upper Triassic Slocan Group that include locally weakly metamorphosed argillite, quartzite, limestone and some tuffaceous rocks. These sedimentary rocks are intruded by dikes, sills and stocks of varied composition and origin. Permian and/or Triassic Kaslo Group metamorphosed volcanic rocks occur to the north of the Slocan Group rocks. Middle Jurassic Nelson intrusions are immediately south of the Slocan Group and are inferred to be the source of granitic to pegmatitic sills and dikes found in the area. The Nelson intrusions comprise at least six texturally and compositionally distinct phases ranging from diorite to lamprophyre. The most dominant phase is a medium to coarse grained potassium- feldspar porphyritic granite (Paper 1989-5).

The occurrence is hosted by predominantly interbedded black argillite and medium to dark grey quartzite and argillaceous quartzite of the Slocan Group. Argillaceous limestone, limestone and slate are also found in varying proportions in the sequence. The sedimentary rocks have been folded, fractured, faulted and regionally metamorphosed to greenschist facies. The regional northwest trending asymmetric Slocan syncline is thought to be Middle Jurassic and is the first recognizable deformation in the sequence. Several fault structures are evident and host vein mineralization. Later stage normal and thrust faults and shearing have chopped, deformed and remobilized the veins and mineralization. Horizontal displacement can be several metres to over 90 metres. Drag features are also present.

The vein exposed on the Jennie property is part of a vein system that has been traced to the east through the Carnation (082FNW048) and Silvana (082FNW050) and may extend as far east as the Ruth-Hope property (082FNW052). The vein has been explored with eight short adits on the Jennie Lind property. It is about a metre wide and contains mostly crushed rock cemented by coarse calcite and quartz. The ore consists of brecciated galena and sphalerite cemented by the gangue minerals. A sample of vein material from the dump in 1926 assayed 0.68 gram per tonne gold, 1900 grams per tonne silver, 17.2 per cent lead and 14.8 per cent zinc (Minister of Mines Annual Report 1926).

Production from the Jennie Lind in 1895 and in 1906 yielded 301,264 grams of silver and 31,497 kilograms of lead from 61 tonnes mined. Some production may be included with Carnation (082FNW048).

Bibliography
EMPR AR 1893-1058; 1896-37,67; 1897-534,573; 1904-175; 1906-249; 1921-135; *1926-250
EMPR BC METAL MM00510
EMPR BULL 29, p. 71
EMPR INDEX 3-201,210
EMPR P 1989-5
EMPR PF (See 082FNW, General - Geological plans of the Silverton area, B.C. Department of Mines, 1966; Geological compilation and structural map of the Sandon area, Kelowna Exploration; Starr, C.C. (1937): Report on Geology, in 082FNW180))
EMR MP CORPFILE (Kelowna Mines-Hedley Ltd.)
GSC MAP 273A; 1091A; 1667
GSC MEM 173, p. 13; *184, pp. 28-30, 158; 308, p. 146
GSC SUM RPT 1916, pp. 56-57

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