Virtual Museum ID: 19-RM26
Skarn is, rock(s) formed or altered by the interaction of magma, country rock, reactive fluids and heat are known as skarn.
Skarn or tactites are hard, coarse-grained metamorphic rocks that have been chemically altered by metasomatism(the chemical alteration of rock by hydrothermal and other fluids). Commonly forms around the edges of a magma body(or silicate rock) that intrudes into a carbonate layer composed of either dolomite or limestone. It consists mainly of Ca, Mg, Fe and/or Mn silicates which are free from or poor in water.
The information listed below relates to the current holding location or collection that the sample is from, and whether the item is viewable at that location or is part of a private collection. Coordinates are given as guides, and we remind you that collecting specimens from these locations is not allowed. Caution is advised visiting such sites and Below BC assumes no responsibility for any injuries or trespassing charges that may occur as a result of the viewer entering these sites.
Original Collection:Rossland Museum & Discovery Centre (RM)
Virtual Museum ID:19-RM26
Date Added to VM:2019-06-09
Sample Origin:SE of Salmo, B.C.
Specific Site:Dodger and Jersey Mine
Datum:11 (NAD 83)
Primary Mineral Formula:-
Advanced Geological Information
The following section provides geological data relating to the specimen or the site it was collected from, when available. Information has been obtained from various sources including private and government datasets but may not be up to date. Any geological time periods or ages listed often relate to the primary geology of the area, and may not be the actual date of an event such as mineral formation.
Geological Formation:Laib Formation
Geological Period:Lower Cambrian
Stratigraphic Age:510 to 541 Million Years Ago
Geological Terrane:Kootenay, Plutonic Rocks
The property lies on the summit between Sheep and Lost Creeks, about 13 kilometres southeast of Salmo. The early development work on the Emerald was done on a lead-zinc showing by J. Waldbesen and by Iron Mountain Ltd.; reference is made to this development in the Jersey (082FSW009).
After being inactive from about 1925 to 1940, the owners, Iron Mountain Ltd., increased their holdings from 17 to 41 claims and carried out exploration and a small amount of development for 3 years which led to the discovery of scheelite to the west of the principal lead-zinc showing early in 1942. Later in the year, scheelite ore was found on the Dodger (082FSW011) property to the east of the lead-zinc zone. At about the same time the Feeney (082FSW247) ore body, about 183 metres north of the Empire, was discovered.
In August 1942 the property was purchased by the Dominion Government who operated it through the Wartime Metals Corporation. A mill was built beside the Nelson-Nelway Highway and put into production in August 1943 but on September 10th an order was received to close down.
Early in 1947 the property was bought by Canadian Exploration Ltd. and production was resumed in June. Exploration for additional tungsten ore was extended to a study of the Jersey (082FSW009) showing which was dominantly zinc bearing and by the end of 1948 a considerable tonnage of lead-zinc ore had been proven on the Jersey. The tungsten operation was closed down and the mill converted to a lead-zinc operation for production from the Jersey.
Early in 1951 the Canadian Government bought back from the company the known Emerald tungsten orebodies and the partly developed Dodger (082FSW011). An agreement was made for Canadian Exploration Ltd. to build a tungsten mill and to mine tungsten ore on a fee basis. A 227 tonnes mill was built near the portal of the Emerald 3,800 level and put into production in December 1951. Further diamond drilling on company ground demonstrated the existence of a large tonnage of tungsten ore so the company agreed to buy the tungsten operation from the Government. The mill operated until the end of 1958. On the Emerald claim all ore was mined from above the 3,800 level main haulageway by open pitting and underground mining. An inclined shaft was put down to the 2,730 level and 9 levels established off this, the bottom one 344 metres vertically below the 3,800 level. All ore was mined out above this lowest level. A small orebody on the Feeney claim was mined out by 1955. The mining of the Dodger zone was completed in 1957.
Diamond drilling on the Invincible claim revealed a tungsten orebody 245 to 275 metres below the surface that is estimated to contain 350,000 tonnes grading 0.83 per cent tungstic oxide. The sinking of a 275-metre vertical shaft was begun but the project was abandoned in 1958 on completion of a sales contract with the United States General Services Administration. Work was resumed on the property in 1967. A geophysical survey was made of the Invincible claim (Lot 12084) and 394 metres of diamond drilling was done in 2 holes in the Tungsten King workings (082FSW034, 321, 322).
Drilling during 1968 on the Invincible (082FSW218) showing totalled 2875 metres. Development work was begun in 1969 and production began in mid-October 1970. The Emerald tungsten mill was rehabilitated to handle about 454 tonnes per day. Ore reserves at the end of 1970 from three separate zones totalled 435,500 tonnes averaging 0.65 per cent W03. Initial production was from the rehabilitated Dodger workings since the Invincible ore zone had not been reached. The Invincible drift was advanced to 1310 metres during the year; the orebody was developed by a decline trackless haulageway. Mill capacity was increased to around 544 tonnes per day during 1971. The company name was changed in 1972 to Canex Placer Limited. Ore reserves were exhausted and the mine closed in August 1973, and in 1977, Canex's assets were acquired by Placer Development Limited. In 1979, Mentor Exploration and Development Co., Limited optioned the property from Placer. In 1980, they diamond drilled 4504 metres in 11 holes plus one wedged hole. The best intersection was 0.36 per cent W03 over 1.07 metres.
The Emerald Tungsten zone is located on the west side of the Emerald Stock granite of the Middle to Late Jurassic Nelson Intrusions. The zone occurs within the Lower Cambrian Laib Formation along the contact of the Reeves Member limestone with the Emerald Member argillite as well as on the limestone-granite contact.
The strata strike about 020 degrees and dip between 45 and 70 degrees east; many of the beds are actually overturned. The granite appears at the surface as a north trending elongate stock. West of the stock are argillite and skarn bands of the Truman Member (Laib Formation), which forms an isoclinal anticline overturned to the west. The Reeves limestone is on the west limb of this anticline, and dips 25 to 70 degrees east, terminating at depth against granite. It is succeeded on the west by the Emerald argillite that also dips east. Both the Emerald and nearby Feeney (082FSW247) ore zones are transected by the Granite fault; drilling, east and north of the fault, located the Invincible (082FSW218) tungsten zone at the same stratigraphic horizon.
Within the deposit four distinct types of mineralization can be recognized: sulphide, "greisen", skarn, and quartz ores. The sulphide-type consists of irregularly shaped "replacement" bodies in limestone and dolomite, consisting of pyrrhotite, calcite, biotite and scheelite. Locally quartz, pyrite, molybdenite and chalcopyrite may be present. The "greisen"-type of ore is in altered granite and extends as much as 12 metres into the granite from the contact with the limestone. The ore consists of potash feldspar, in some places completely kaolinized, abundant quartz, sericite, pyrite, tourmaline and scheelite. Locally, calcite or ankerite, apatite, pyrrhotite or molybdenite may be present. The skarn-type of ore, ocurring mainly at or near the contact of limestone and argillite, consists of garnet, diopside, calcite and quartz with small amounts of pyrrhotite, pyrite, scheelite and molybdenite. The quartz-type ore, which in many places grades into greisen, is silicified limestone intersected by numerous veins of quartz containing abundant ankerite, large crystals of scheelite, a few flakes of molybdenite, and orange-fluorescing crystals of apatite. Near the veins are found disseminated scheelite and pyrite with some pyrrhotite and tremolite. Also reported are native bismuth, arsenopyrite, gold, tellurides, cassiterite, vesuvianite, fluorite, and wollastonite (G. Ray, 1995).
Scheelite is the main tungsten mineral but minor powellite and wolframite have also been reported. Most of the scheelite occurs as fine, disseminated grains in lenticular skarn zones which extend an average of about 5 to 6 metres from the granite contact along the limestone-argillite contact. Grades are 0.5 to 1.5 per cent WO3.
The Emerald Tungsten mine was worked in 1943, 1947 to 1949 (inclusive) and again from 1951 to 1958 (inclusive). Production to the end of 1957 amounted to 597,100 tonnes of ore (Bulletin 41, page 119). Production for the Emerald deposit, combined with that of the Feeney (082FSW247) and Dodger (082FSW011) deposits, is recorded with the production statistics of the Jersey mine (082FSW009).
During 2014, Margaux Resources Ltd. conducted a two-phase drilling program on the East Emerald target area that produced 6318.6 metres of core over 35 drill holes (Assessment Report 35243). Drilling confirmed and expanded on historic reports of contained tungsten. The tungsten-bearing zones consist of several mostly parallel skarn bands in argillite or limestone beds that dip moderately to the east. Assessment Report 35243 reports mostly on work completed in 2014, however also includes indicated and inferred resource grades from 2008 for the East Emerald and Emerald Mine areas. An indicated resource of 256,000 tonnes grading 0.19 per cent WO3 and an inferred resource of 1,122,000 tonnes grading 0.28 per cent WO3 are reported (Assessment Report 35243).