Virtual Museum ID: 19-AME9

Specimen Summary

Bornite is an important copper ore mineral found in many different types of copper deposit. It is also known as peacock ore because of its iridescent purple-blue-green tarnish. Fresh bornite, however, is copper red. Bornite commonly occurs with other copper sulphide minerals such as chalcocite and weathers, or “oxidizes”, to malachite.

Chalcopyrite is the most common ore mineral for copper and is a sulphide of iron and copper. Chalco comes from the Greek word chalko, meaning copper. Chalcopyrite is commonly found in sulphide deposits in most ore-forming environments. A characteristic deep brass yellow colour and iridescent green-to-purple weathering surfaces distinguish chalcopyrite from gold and sulphides such as pyrite.

This sample comes from the Bethlehem copper porphyry deposit in the Central Interior. The deposit is about 15 km west of the small town of Logan Lake, and about 80 km southwest of Kamloops.

The Bethlehem deposit is one of the deposits that make up the Highland Valley Copper mine, which also includes the Lornex, Highmont and Valley deposits. Early prospectors found copper mineralization in the Highland Valley area in the late 1800s and started hand mining at the Snowstorm and Iona zones of the Bethlehem deposit in 1907, when a wagon trail was built to nearby Ashcroft and the Fraser Canyon railway line. Large-scale open pit mining started at Bethlehem in 1962 and continued until the early 1980s, when production shifted to the other deposits, which are still being mined today. The large Valley pit and operations are visible from a lookout on Highway 97C.

The main ore minerals at the Bethlehem deposit were bornite and chalcopyrite, as seen in this sample. The ore minerals are mainly in very narrow veins, often only a few millimetres wide. Chalcopyrite is also found as fine “disseminations”, or speckles, throughout the host granodiorite rock. Pyrite is also common at Bethlehem, mainly towards the outer edges of the deposit. The other ore mineral mined at Bethlehem was molybdenite, another sulphide mineral and the main ore for molybdenum, which also occurs in narrow veins with quartz.

From 1962 to 1982, production at the Bethlehem mine totalled 96,324,510 tonnes of ore that yielded 99,826,893 grams silver, 1,279,833 grams gold, 398,112,545 kilograms copper and 851,048 kilograms molybdenum.

Specimen Data


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.

Collection Details

Original Collection:

Association for Mineral Exploration (AME)

Sub Collection:


Collection ID:


Virtual Museum ID:



Date Added to VM:


Location Information

Sample Origin:

Highland Valley, B.C.

Specific Site:

Bethlehem Mine

UTM Easting:


UTM Northing:



10 (NAD 83)

Coordinate Accuracy:


Specimen Details

VM Category:


Primary Features:


Primary Mineral Formula:

Cu5FeS4 · MoS2

Primary Category:


Secondary Features:


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:

Guichon Creek batholith

Geological Period:

Late Triassic to Early Jurassic

Stratigraphic Age:

Geological Belt:


Geological Terrane:


Minfile ID:


Site Details:

The Valley deposit lies within the Late Triassic to Early Jurassic Guichon Creek batholith and is hosted by Bethsaida phase porphyritic quartz monzonite and granodiorite. Feldspar porphyry and quartz feldspar porphyry dykes 0.6 to 35 metres wide dip steeply eastward in the western and central areas, and northward in the southern area of the deposit. These dykes are cut by mineralized fractures and quartz veinlets, and have been dated at 204 Ma +/- 4 Ma. The Bethsaida granodiorite is also intruded by aplite dykes up to 30 centimetres wide, tan-coloured felsite dykes up to 4.5 metres wide, and three types of lamprophyre dykes (spessartite, hornblende vogesite, vogesite).

The most prominent structural features are the north trending, west dipping Lornex fault and the east trending Highland Valley fault. Faults and fractures in the deposit comprise four main sets. Quartz veinlets are subparallel to two of the earlier formed fault and fracture sets.

Silicic, potassic, phyllic, argillic and propylitic alteration are intimately associated. Stockworks of quartz veinlets 1 to 2 centimetres in width are common. Vuggy veinlets have envelopes of medium-grained sericite and/or potassic feldspar, and contain minor amounts of sericite, plagioclase, potassium feldspar, calcite, hematite, bornite, chalcopyrite, molybdenite, digenite and covellite. These veinlets are moderately abundant within the 0.3 per cent copper isopleth. An area of well-developed barren quartz veinlets, generally 0.5 to 1.3 millimetres wide, without alteration envelopes, occurs in the southeastern part of the deposit.

In the west-central part of the deposit, potassium feldspar is associated with vein sericite in some replacement zones, as veinlet envelopes along fractures, and disseminated in quartz veinlets. Hydrothermal biotite occurs in small amounts. Flaky sericite and quartz, both as replacement zones and as envelopes around quartz veinlets, constitute the most common type of alteration associated with copper mineralization. Strong phyllic alteration coincides with the 0.5 per cent copper isopleth. Phyllic alteration is closely associated with pervasive argillization, which is strongest where fractures are most closely-spaced. Feldspars are altered to sericite, kaolinite, quartz and calcite. The phyllic-argillic zone grades outward to a peripheral zone of weak to moderate propylitization, characterized by clay, sericite, epidote, clinozoisite and calcite replacing plagioclase, and chlorite and epidote replacing biotite. The age of hydrothermal alteration is approximately 191 Ma.

At the Valley deposit, gypsum is interpreted to be secondary and post-ore. It is commonly fibrous and white to orange but locally it forms large platy crystals or may be massive. Anhydrite, which is also present, provide indirect evidence for the secondary nature of the gypsum. It is apparently the same age as and associated with sericitic and potassic alteration. Quartz-gypsum veins and quartz-potash feldspar veins in which gypsum fills interstices provide more direct evidence for its secondary nature. Gypsum is believed to have formed at the expense of anhydrite which was deposited from the ore-forming fluids. Gypsum veins are common in the lower portion of the orebody (Open File 1991-15).

Sulphides occur chiefly as disseminations in quartz veinlets, and in phyllic (bornite) and potassic (chalcopyrite) alteration zones. Mineralization includes bornite and chalcopyrite, with minor digenite, covellite, pyrite, pyrrhotite, molybdenite, sphalerite and galena. The oxide zone averages 4.5 metres in thickness, and contains limonite, malachite, pyrolusite, digenite, native copper, and tenorite(?).

Production from the Lornex mine (092ISW045) was combined with the Valley operations in 1987.

Highland Valley Copper was created in mid-1986 by bringing together the Highland Valley mining operations of Lornex Mining Corporation Ltd. and Cominco Ltd. into a new single entity, structured as a partnership.

On the south side of the valley was the Lornex mine which started mining in 1972. In 1981, the Lornex concentrator had been expanded to become one of the largest in the industry.

On the north side was Bethlehem Copper (092ISE001) which started mining in 1963. In 1981, this operation was absorbed by Cominco who already owned the Valley orebody (092ISW012) located west of the Lornex pit on the south side of the valley. Mining of the original Bethlehem Copper pits ceased in 1982.

The Highmont mill on the south side of the valley was acquired in 1988 when Highmont Mining Company joined the partnership. This mill had been closed down in 1984 when the Highmont deposit (092ISE013) became uneconomical.

Lornex Mining Corporation Ltd. was wound up at the end of 1988 with the result that Rio Algom Limited, Teck Corporation and Highmont Mining Company obtained direct participation in the cash flow from the partnership. Today's participation in the cash flow is:


50. per cent-Cominco Ltd.

33.6 per cent-Rio Algom Limited

13.9 per cent-Teck Corporation (including 2.5 per cent from Highmont)

2.5 per cent-Highmont Mining Company (excluding Teck's 2.5 per cent)


Highland Valley Copper operates two distinct mines, the Valley mine and the Lornex mine, and between the two has measured and indicated ore reserves of 761 million tonnes of 0.408 per cent copper and 0.0072 molybdenum. The ore reserves of each mine are: Valley mine - 627 million tonnes at 0.418 per cent copper and 0.0056 per cent molybdenum; Lornex mine - 135 million tonnes at 0.364 per cent copper and 0.0144 per cent molybdenum. The individual mine reserves are calculated at an equivalent cutoff grade of 0.25 per cent copper using a molybdenum multiplying factor of 3.5 (CIM Bulletin July/August 1992, pages 73,74).

Mining is carried out in the two mines simultaneously at a proportion of 80 per cent in the Valley mine and 20 per cent in the Lornex mine, and the ratio is projected to remain much the same over mine life. Based on current plans, the property has a life of approximately 18 years at conservative metal prices and an average stripping ratio of 0.8 (CIM Bulletin July/August 1992, pages 71-73).

Published reserves at January 1, 1995 were 539.7 million tonnes grading 0.42 per cent copper and 0.0073 per cent molybdenum. The mine life is estimated to be about fourteen more years (Information Circular 1995-9, page 6).

In 1995, with Explore B.C. Program support, Highland Valley Copper carried out 197 line kilometres of high-powered induced polarization surveys for very deep penetration, and drilled 1701 metres in 4 holes. This work was done on the Lornex SW Extension, Roscoe Lake and JA zones. No anomalies of merit were detected in Lornex SW Extension, and Roscoe Lake gave only limited encouragement. IP work on the JA zone detected an anomaly extending to the south, well beyond the limits of known mineralization, and another anomaly 2000 by 1500 metres in size at the east end of the grid. Both anomalies warrant drill testing (Explore B.C. Program 95/96 - M80).

Reserves estimated by the partnership as of January 1, 1996, were 504 million tonnes grading 0.42 per cent copper, 4.8 grams per tonne silver, 0.032 gram per tonne gold and 0.0076 per cent molybdnum (Information Circular 1997-1, page 8). In order to reach the credit limit for gold production, small amounts of gold from the Snip mine were added to the concentrate.

Reserves were estimated, as of January 1, 1997, at 495 million tonnes grading 0.42 per cent copper and 0.006 per cent molybdenum. Mining takes place in the Valley (95 per cent) and Lornex (5 per cent) pits (Information Circular 1998-1, page 8; Northern Miner, April 28, 1997).

A possible resource of 200 million tonnes grading 0.4 per cent copper at depth (beneath the current Valley pit design) was identified as a result of exploration in 1995. This resource was further examined in 1996 and resulted in the indentification of 350 million tonnes grading 0.384 per cent copper (Information Circular 1997-1; Northern Miner, April 28, 1997).

At the end of 1996, mine plans called for another 200 metres in depth in the Valley pit to the 2008. In addition, the partnership may consider mining the remaining 120 million tonnes grading 0.33 per cent copper estimated to exist in the Lornex pit (Information Circular 1997-1, page 8).

Ore reserves remaining at the beginning of 1998 are 457.1 million tonnes grading 0.419 per cent copper and 0.0085 per cent molybdenum (Exploration in BC 1997, page 34).

Ore reserves at the beginning of 1999 are 416.8 million tonnes grading 0.418 per cent copper and 0.0087 per cent molybdenum (Lorne Bond, pers. comm.; Exploration and Mining in BC 1998, page 60).

Highland Valley Copper suspended mining on May 15, 1999; they resumed August 30, 1999.

Ore reserves at the beginning of 2000 are 387 million tonnes grading 0.42 per cent copper and 0.008 per cent molybdenum (Information Circular 2001-1, page 6).

Ore reserves at the beginning of 2002 were 292.5 million tonnes proven and 52.6 milltion tonnes probable, totalling 345.1 million tonnes, grading 0.41 per cent copper (Teck Cominco Annual Report 2001).

At November 24, 2003 Highland Valley Copper contained approximately 296,000,000 tonnes of reserves grading 0.42 per cent copper (, November 24, 2003). The molybdenum grade is reported to be 0.007 per cent (The Northern Miner, December 15, 2003).

Mineral reserves as of December 31, 2005 are 260,200,000 tonnes in the Proven reserve category grading 0.43 per cent copper and 0.008 per cent molybdenum; 58,500,000 tonnes in the Probable reserve category grading 0.44 per cent copper and 0.007 per cent molybdenum; and 318,700,000 tonnes Total combined reserve grading 0.43 per cent copper and 0.008 per cent molybdenum (TeckCominco Annual Report 2005).

In September 2005, Highland Valley announced that mine life would be extended by five years to 2013. Very late in the year, Teck Cominco also announced that it is considering building a modern hydrometallurgical refinery on site. Most ore comes from the Valley pit, augmented by a small amount from the Lornex pit. Following a successful 300,000 tonne bulk sample test, the Highmont East pit, closed since the mid-1980s, was re-opened in the fall of 2005 to take advantage of higher molybdenum prices. In addition, exploration drilling was conducted nearby in the Highmont South area and results are being evaluated.

Teck completed a new life of mine plan which extended the mine life until 2027.

Reserves and Resources as of December 31, 2014 were:

(Teck Annual Information Form, March 2, 2015)


Category Amount (tonnes) Cu (%) Mo (%)

Proven 375,000,000 0.34 0.007

Probable 232,800,000 0.24 0.009


Proven & Probable 608,000,000 0.30 0.008

Measured 395,300,000 0.32 0.009

Indicated 612,900,000 0.22 0.011

Inferred 303,000,000 0.20 0.009

Calculated at 0.11 per cent Cu equivalent cut-off


Reserves and Resources as of December 31, 2017 were:

(Teck Annual Information Form, March 2, 2015)


Category Amount (tonnes) Cu (%) Mo (%)

Proven 372,100,000 0.32 0.007

Probable 217,400,000 0.27 0.009


Proven & Probable 589,500,000 0.30 0.007

Measured 488,400,000 0.31 0.009

Indicated 822,600,000 0.23 0.009

Inferred 382,400,000 0.23 0.007

Calculated at 0.10 per cent Cu equivalent cut-off.


Production for 2018 (system currently will not accept)

Teck Annual Information Form February 26, 2018

Mined: 112,037,000 tonnes

Milled: 51,888,000 tonnes

Cu: 100,800,000 kilograms

Mo 3,950,000 kilograms

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