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The Engineer Mine, Tagish Lake, British Columbia.

The Engineer mine is a Dana locality for classic, botryoidal "allemontite" (stibarsen and native arsenic). Several other minerals of interest to the collector are also found, including crystallized auriferous silver ("electrum"). The site is currently being mined for gold, but the operators are also setting aside specimens specifically for the collector market.

INTRODUCTION

The Engineer mine is located on the east shore of the Taku Arm of Tagish Lake, about 32 km (20 miles) west of Atlin, British Columbia. Whitehorse, Yukon, is about 137 km (85 miles) north. National Topographic Series Map Sheet 104 M/8E covers this area. Access to the mine is either by boat or float-equipped aircraft.

HISTORY

As with so many mines in British Columbia, the Engineer mine's history is one of high hopes and dreams, fancy financial footwork, success and disaster. The story began in 1899, when Charles A. Anderson, an engineer with the White Pass and Yukon Railway, paddled south along the eastern shore of Taku Arm. He found visible gold in large quartz veins in bluffs at the water's edge. Anderson staked the Hope claim on July 8, recorded it in Atlin, then returned with Henry C. Diers, another company engineer, to stake another twelve claims which became known as the Engineer Group. These men then organized the Engineer Mining Company of Skagway, Alaska, and began development work on the property, which continued for several years They also began construction of a small mill, but did not complete it. The Company's money had run out and the results had not been encouraging enough to attempt more fund-raising. As a result, the claims were allowed to lapse in 1906. A group of local men led by Edwin Brown restaked the claims, then in 1907 sold them to Captain James Alexander, John Dunham, Ben G. Nichol and K. Wawrecka of the Northern Partnership Syndicate.

The new owners began by prospecting the neighboring ground, which resulted in the staking of the Northern Partnership Numbers 1, 2, 3, 4 and 5 claims. The construction of the mill was also completed and several tons of high-grade ore were treated by amalgamation methods.

Minimal work was done between 1910 and 1912 due to pending litigation. After acquiring the interests of his partners, Captain Alexander continued more comprehensive and systematic prospecting and development than had been previously undertaken and, for the next 6 years, work continued sporadically. It slowed down when engineers and consultants visited during attempts to sell the mine. When asked about the origin of the mine's name Alexander was reported to have replied, "Because it has been 'engineered' to death!"

In 1918, Wayne Darlington, a well-known New York engineer, managed to secure an option on the mine from Alexander, with a total purchase price of $1,000,000. This option was passed on to the Mining Corporation of Canada. One of the Corporation's young engineers, George Randolph, was in British Columbia inspecting properties for option. Charles E. Watson, then manager of the MCC, also came to British Columbia to look over properties already optioned by Randolph. Watson had just joined Randolph at the Silver Creek property near Revelstoke when a wire was received to proceed immediately to the Engineer mine. Watson and Randolph joined Captain Alexander, his lady and C. S. Verril, an engineer representing Darlington, in Vancouver. They sailed for Skagway and then went on to visit the mine. The group was returning to Vancouver aboard the Canadian Pacific Railway steamer Princess Sophia, which had sailed from Skagway at midnight on October 26th, 1918. At 3:00 a.m., in a blinding snow storm, the steamer ran aground on the Vanderbilt Reef in the Lynn Canal. At dawn, the tide was low, leaving the boat high and dry on the reef. For more than a day the ship was perched atop the reef. It had been decided that if an attempt were made to bring the passengers ashore during the storm, many would surely perish. Just after dark on October 28th, the Princess Sophia finally plunged off the rocks, taking everyone on board into the icy depths. A pet dog was the only survivor (Greene, 1969).

For several years after Alexander's death, little work was done at the mine due to litigation regarding the ownership. It turned out that the woman accompanying Alexander in British Columbia was not his wife as people had assumed. Apparently Mrs. Alexander and their 16-year-old daughter were still living in England when they learned of his demise. Litigation arose when their claim as heirs was countered by a claim made by Alan Smith of Philadelphia. Smith claimed that he had grubstaked Alexander and the two had an agreement that in the event of the death of one partner, the other was to receive the deceased's share of the Engineer mine. The mine was held under bond by Ecla Copper Company, a Nevada mining corporation. Repair and development work done during this time was headed by Reggie Brooks, a long-time friend of Captain Alexander.

The property was examined and bonded by Andrew Sostad for New York interests in the fall of 1923. Extensive work began again in 1924, when Engineer Gold Mines, Limited, was incorporated in the State of Delaware, with the British Columbia head office in Vancouver. With a capitalization of $1,000,000, the Company made the mine a major operation by building a power plant and transmission lines and installing a 50 tons-per-day concentrator near the 5th level portal. The concentrator was started in November of 1925 and within two months had milled 1,700 tons of ore yielding 1,814 ounces of gold and 843 ounces of silver. The high mining and milling rate outpaced the development of reserves and after the summer of 1926, having produced 7,757 ounces of gold that year, the mine and mill were shut down for the winter to let ore reserve development catch up. After a short period of milling during the summer of 1927, developed reserves were once again exhausted and the mine was closed. Exploration and development continued until 1931 when all work in the mine was ceased even though reserves had been established in the lower levels. Reggie Brooks stayed on as a caretaker for Engineer Gold Mines for the next two years. Although he was not a paid employee, he was permitted by the company to hand-mine the surface showings.

In 1934 the mine was sold at a Sheriff's sale to representatives of the Mining Corporation of Canada, Limited, for $25,000 cash in satisfaction of judgments against the mine: over $8,700 to a C. L. Hershman, over $4,000 to a Louis Schulz and $207,431.18 in favor of John G. Harris. In his memoirs, Reggie Brooks relates how the latter came to have a claim against the mine. Apparently, someone who knew Harris well had informed Brooks that the claim was transferred to Stewart Hamilton, then treasurer of Engineer Gold Mines in New York, by C. V. Bob, an earlier president of the company, in exchange for an estate in the West Indies which Hamilton had acquired. Hamilton, in turn, transferred the loan indebtedness to Jack Harris, his brother-in-law because, as an executive officer of the company, Hamilton could not very well sell the mine and satisfy his judgement for the debt.

The Mining Corporation of Canada made no attempt to reopen the mine. John E. Hammell arranged for an option on the mine from the Corporation in 1936. The engineer he had hoped would run the operation died after falling down a shaft at a gold mine in the Philippines, and Hammell consequently turned down the option. In May of 1944, Neil Forbes, Tommy Kirkwood and Pete Brandes of Atlin bought the mine from the Mining Corporation for $5,000 plus about $1,500 in back taxes. These miners highgraded the property off and on through the 1940's until 1952. Walter Sweet, also of Atlin, joined the group in 1945, after obtaining Pete Brandes' interest.

There has been no production from the mine since 1952, although several companies have made efforts to explore the property further. The property was bought by Tagish Gold Mines Limited in the early 1960's. Nu-Energy Resources Limited merged with Tagish Gold Mines in 1975 and in the same year conducted an exploration program. In 1979, Nu-Lady acquired the right to the property and continued exploration for the next couple of years. Total Erickson Resources Limited carried out magnetometer aerial and ground geophysical surveys in 1987 (Smith, 1990). The Engineer mine is presently being worked by Warren Arnholtz and Swede Martensson of Ampex Mining.

One story about the Engineer mine relates a curse put on the mine in its early days. The curse proclaims that "nothing but death and disaster would be the lot of Alexander and anyone else who had anything to do with the property" (Fairlie, 1940). Perhaps it is still in effect. With their operation shut down for the season, Warren and Swede were heading home across Tagish Lake in October of 1993 when a sudden storm capsized the boat. They, along with the boat's owner and captain, Rob Cumming, hung on for over an hour in the icy water before being rescued. Most of that season's gold lies at the bottom of the lake. The tale is not yet ended.

GEOLOGY

Several investigators made cursory observations in the Tagish Lake area from 1899 to the mid-1950's. A map of the area was drawn by R. L. Christie in 1957. The most significant work relevant to the Taku Arm (in particular, to the east of the lake) was done by Bultman (1979) and by the British Columbia Geological Survey (Mihalynuk and Mountjoy, 1990). The Engineer mine area was also studied as part of the Bennett Project conducted by the BC Geological Survey (Schroeter, 1986).

The Engineer mine claims are situated within the Whitehorse Trough, which is a synclinorium underlain by the Late Triassic Stuhini Group. The center of the trough is dominated by the Jurassic Laberge Group. The Whitehorse Trough is structurally controlled to the west by the Llewellyn Fault, which separates it from the Coast Plutonic Complex, and to the east by the Nahlin Fault which separates the trough from the Atlin terrane.

The orebodies of the Engineer mine are part of an epithermal vein system situated in the sedimentary rocks of the Inklin Formation. This formation is one of two comprising the Laberge group of rocks, which are a northwest-trending linear belt of Early Sinemurian to Late Pliensbachian muddy turbidites, graywackes and conglomerates (Johannson, 1993).

Several workers have made comments about the mineralization history, or aspects thereof (for example, Mihalynuk and Mountjoy, 1990, and Schroeter, 1986), but a more comprehensive hypothesis than the one presented in this article has not yet been put forward or tested. Smith (1990) points out that two types of mineralization exist: the low-grade, finely disseminated mineralization of the "shear zones" and "hubs," and that of the "erratically distributed pockets of high-grade gold ore that occur in the numerous narrow quartz veins throughout the property."

Two nearly vertically dipping and northwest-trending zones of dilatant quartz veins ("shear zones" in previous literature) cut the Inklin rocks. These have been interpreted as splays of the Llewellyn Fault system (Schroeter, 1986). Smith (1990) also compares the "shear zone" quartz veins with the type of quartz veins found in the California Motherlode belt on the basis of the presence of graphitic horizons parallel to the quartz zones. The last major motion along the Llewellyn Fault has been dated at about 132 Ma (million years) by potassium-argon dating of sericite from the fault zone (Mihalynuk, personal communication, 1993), and an early period of gold mineralization could have taken place during this time. Each of these zones hosts a large, oval stockwork or "hub" from which some subsidiary, though clearly epithermal, veins seem to radiate.

Schroeter (1986) suggests that "mineralization in the vicinity of Engineer Mountain and Bee Peak may be genetically related to a hydrothermal event associated with intrusive activity." Mihalynuk (personal communication, 1993) has obtained dates of 55 Ma and 62 Ma for the Sloko volcanics, which he feels are coeval with the Engineer Mountain plutons. An epithermal event associated with this activity could well have followed older structural weaknesses such as the "shear" zones and created offshoots. The distinct clastic nature of some of the electrum/roscoelite mineralization suggests that the epithermal event was at least a lengthy one, if not multi-episodic with earlier mineralization having been brecciated and redeposited by a later episode of the same event. Furthermore, a specimen of the epithermal material (in the University of British Columbia collection) exhibiting a slickensided surface with the gold smeared across it supports the idea of an extended or multi-episodic epithermal event. The feature is too small to suggest post-epithermal tectonic movement in the area, and no large-scale, post-mineralization faulting was observed by the author who visited the mine (MM).

MINERALS

Allemontite mixture of stibarsen + arsenic or antimony

The occurrence of "allemontite" at the Engineer mine was the first in Canada (Walker, 1921). Because allemontite is a discredited species, further description of the material is given under arsenic and stibarsen.

Ankerite Ca(Fe,Mg,Mn)(C[O.sub.3])

Ankerite occurs as fine-grained masses up to several centimeters in calcite veinlets in the cockscomb quartz/calcite veins.

Antimony Sb

The occurrence of native antimony at the Engineer mine is first mentioned by Thomson (1937) and Walker (1921). It occurs as lumpy nodules up to 5 cm wide in cockscomb quartz. These specimens are quite different from the banded, colloform "allemontite" in that they appear homogeneous. A polished cut through a specimen in the University of British Columbia collection does not show banding like that in similarly cut "allemontite." Native antimony has also been found as rhombohedral crystals to 2 mm in calcite veinlets on level 5 of the "E" vein.

Arsenic As

Native arsenic occurs as bright silvery bands interlayered with stibarsen ("allemontite"). After being collected and exposed to air, these bands soon alter to a sooty black color. Reniform masses up to 30 cm wide are the largest known. The surface of these aggregates can vary from being smooth to pimply to drusy with crystals up to 1 mm visible. [See also stibarsen.]

Arsenopyrite FeAsS

Arsenopyrite occurs as euhedral prisms associated with the roscoelite/electrum nodules and as freestanding crystals in quartz vugs of the calcite/quartz veins. Crystals up to 5 mm are known. Some interesting arsenopyrite crystals with a coating of lollingite and more tiny, irridescent arsenopyrite crystals sprinkled over the lollingite also occur in the quartz vugs. The arsenopyrite samples analyzed contain 0.55 to 4.49 % antimony. Values for iron remain fairly constant, whereas the sulfur and, to a lesser degree, the arsenic values fluctuate correspondingly with the antimony values. This suggests that the antimony is substituting for sulfur and possibly arsenic in the structure.
Table 1. Five analyses of various zones within an arsenopyrite
crystal. Analysis #6 was made on the lighter grey core of the
arsenopyrite crystal seen on the far right, center of BSE photo 3.
See also BSE photo 2.

                              1        2       3        5        6

Weight %

Concentration

Fe                        35.08    35.74    35.66    35.71    32.98
S                         19.53    21.20    20.82    20.95    16.60
As                        43.52    41.70    43.09    40.79    41.23
Sb                         2.51     2.12     1.26     3.38     9.49
TOTAL                    100.64   100.76   100.83   100.83   100.30

Normalized Atomic
Concentration

Fe                        34.16    34.13    34.09    34.29    34.01
S                         33.13    35.26    34.66    35.03    29.81
As                        31.59    29.68    30.70    29.19    31.69
Sb                         1.12     0.93     0.55     1.49     4.49
TOTAL                    100.00   100.00   100.00   100.00   100.00


Berthierite Fe[Sb.sub.2]S

Berthierite was identified by X-ray analysis in a sample collected by the British Columbia Geological Survey. It occurs as fine needles up to 1 cm long in a quartz-lined vug (Schroeter, 1986).

Bismuth Bi

Bismuth was first mentioned from the Engineer mine by Cairnes (1911), but no analyses or documentation of specimens were given. No bismuth was detected in any samples analyzed by the current authors.

Calaverite Au[Te.sub.2]

[See under Tellurides.]

Calcite CaC[O.sub.3]

Calcite is a gangue mineral in the epithermal, vuggy quartz veins. Aesthetic rhombs and blades up to several centimeters in size and coated with iron oxides are found in the vugs of many of the same veins. Clear, colorless prisms with rhombic terminations also occur throughout the mine.

Chalcopyrite CuFe[S.sub.2]

Chalcopyrite was reported to occur in a quartz vug in the quartz/calcite veins (B.C. Mines Annual Report, 1927). This is the only mention of any copper-beating mineral occurring in this mine.

Fluorite Ca[F.sub.2]

Fluorite occurs as pale green masses and small, clear, colorless cubes in the epithermal veins. The cubes (up to 1 mm on an edge) are associated with arsenopyrite and calcite crystals in quartz-lined vugs.

Gold Au

[See under Silver.]
Table 2. Five analyses of different points within a lollingite
overgrowth on an arsenopyrite crystal. See BSE photos 2 and 3.

Analysis                      8        9      10       12       13

Weight %
Concentration

Fe                        28.50    28.16   29.36    28.84    28.72
S                          1.17     0.84    4.49     2.16     1.96
As                        67.72    67.92   62.31    66.27    66.76
Sb                         2.56     2.42    3.67     2.53     2.26
TOTAL                     99.95    99.34   99.83    99.80    99.70

Normalized Atomic
Concentration

Fe                        34.66    34.61   34.42    34.68    34.63
S                          2.47     1.79    9.17     4.53     4.12
As                        61.42    62.24   54.45    59.40    60.00
Sb                         1.43     1.36    1.97     1.39     1.25
TOTAL                     99.98   100.00  100.01   100.00   100.00


Lollingite Fe[As.sub.2]

Lollingite was identified as a coating and as tiny crystals on arsenopyrite crystals in quartz vugs. These coated arsenopyrite crystals have a bizarre, spiky appearance and could be considered as lollingite encrustation pseudomorphs after arsenopyrite with some smaller arsenopyrite and pyrite crystals sprinkled on the lollingite. Electron microprobe analyses showed the presence of 1.26 to 1.97% antimony.

Pyrite Fe[S.sub.2]

Pyrite occurs as cubes and pyritohedrons up to 2 mm in small quantities near and along the vein/country rock contacts. These are probably the result of country rock alteration and scavenging as the hydrothermal fluids were intruding. Pyrite was also found as extremely small (5-10 microns) crystals on lollingite/arsenopyrite crystals. Sulfide mineralization is very poor throughout the mine.

Pyrrhotite [Fe.sub.1-x]S (x = 0-0.17)

Massive pyrrhotite occurs intimately associated with the arborescent electrum and roscoelite, and as small blebs and streaks in clasts of the sedimentary host rocks within the quartz/calcite veins. As with other sulfides, pyrrhotite is a very minor constituent in the veins.

Quartz Si[O.sub.2]

Quartz is the main gangue mineral in the Engineer vein system. Most is of a drusy, "cockscomb" habit and while not really notable on its own, often provides a beautiful matrix for other, more "collectible" species. Of interest to the collector, though, are the drusy quartz pseudomorphs after calcite and the pseudomorphous specimens in which the calcite has been replaced by quartz producing "quartz pseudomorphs after pseudomorphs after calcite."

Roscoelite K[(V,Al,Mg).sub.2](Al[Si.sub.3])[O.sub.10][(OH).sub.2]

Dark green to black roscoelite occurs as a radiating, micaceous coating (up to several millimeters thick) surrounding electrum in the epithermal veins. This association is sometimes enclosed in calcite which can be etched away to reveal the arborescent nature of the electrum and roscoelite. All green micaceous minerals analyzed by the authors have been identified as roscoelite. No chromium was found in any sample. References to "mariposite" in previous literature are probably references to the roscoelite due to their similar appearance and because mariposite is perhaps more commonly associated with gold veins.

Siderite FeC[O.sub.3]

Siderite was identified as dark brown, earthy or sparry masses and as paler brown, crusty crystal aggregates up to several centimeters in diameter. It is associated with clear, colorless calcite in quartz vugs.

Silver (Auriferous) (Ag,Au)

Highly auriferous silver (40-42% Au) occurs as dendritic crystals, plates and wires in the quartz/calcite veins. Auriferous silver from the "E," Double Decker and adjacent veins is most often enclosed in roscoelite. This association is found as distinct clasts and as irregular nodules, both up to several tens of centimeters in size. Auriferous silver occurs alone in cockscomb quartz, particularly in the Shaft and Governor veins. A number of superbly crystallized specimens, ranging in size from micromounts to miniatures (5 cm), were collected from the Governor vein during the 1994 season. Habits of these crystals vary from centimeter-sized single sheets (flattened octahedra) to millimeter-scale, highly modified cuboctahedra. The sheet-like crystals commonly have raised, triangular growth hillocks on them. Quartz crystals often "pierce" the sheet-like crystals, which then have overgrowths of more equant crystals collaring the quartz. This is the first noted occurrence of well-crystallized auriferous silver ("electrum") in Canada. (Note: the "E" vein is also referred to as the "Engineer" or "No. 8" vein.)
Table 3. Analyses of two silver samples. Copper and mercury were
analyzed for but were not detected.

                              ENG2-M12      ENG3-M10

Weight %
Concentration

Au                              57.04        54.27
Ag                              42.02        43.96
Sb                               0.92         1.13

TOTAL                           99.98        99.36

Normalized Atomic
Concentration

Au                              42.17        39.80
Ag                              56.73        58.87
Sb                               1.10         1.33
TOTAL                          100.00       100.00


Stibarsen SbAs

Stibarsen occurs with arsenic as an intimate, layered mixture ("allemontite") which forms reniform masses up to 30 cm in breadth. Analyses of the layers have shown them not to be pure stibarsen interlayered with pure arsenic, as one might intuitively guess by looking at a polished sample. Most layers are some mixture of both minerals with the layer boundaries generally being defined by changes in grain size. Occasionally, a layer of relatively pure stibarsen or arsenic occurs, but this seems to be the exception. Most of this material was found in the upper levels of the mine and discarded during hand-cobbing of the ore. It is still being found on the fifth level (Bonanza Shoot) of the "E" vein.

Stibnite [Sb.sub.2][S.sub.3]

Gwillim (1900) notes that the Engineer orebody "carries values in free gold, also some stibnite." However, no Engineer mine stibnite specimens are currently known, and it is suggested that the usage of "stibnite" may be synonymous with "antimony (stibnium)." Most of the work done at the time would have been in the allemontite-rich upper levels, and this source of antimony would have been the most obvious.

Tellurides

Telluride occurrences at the Engineer mine were first mentioned by Gwillim (1900). However, he states that none were found in the Geological Survey of Canada's samples. All other references to tellurides date back to this first document, which is at best secondhand, unsubstantiated information. Calaverite was first mentioned by Cairnes (1911), who referred to Gwillim's "gold telluride" as "telluride, apparently calaverite." The 1900 report of the Minister of Mines quotes from a prospectus from the Engineer Mining Company of Skagway that indicates the presence of tellurides. It is further explained in the report that the Provincial Assayer did not find any tellurium in any of the samples. These samples were selected by the Company as representative of those which had been giving unfavorable fire assay results, due the "great presence of tellurides" compared to cyanide tests performed after the ore had been roasted. It is our opinion that the roasting effect was probably due to the presence of arsenic which, like tellurium, volatilizes readily upon roasting.

CONCLUSIONS

The occurrence of several minerals for which there is no physical evidence in the form of analyses or specimens would suggest that they were originally misidentified. These minerals include native bismuth, stibnite and tellurides, reports of the occurrence of which have unfortunately persisted in the literature.

Two distinct periods of mineralization are seen in the Engineer mine orebodies. The first produced low-grade dilation veins and may well have been related to Cretaceous movement along the Llewellyn Fault. The second period was clearly an epithermal event, possibly related to Tertiary magmatic activity, during which mineralizing fluids followed pre-existing structural weaknesses. Clastic textures of some of the gold/roscoelite mineralization, and minor faulting within the epithermal veins makes it apparent that more than a single episode was involved in this event. Most of the minerals of interest, ore as well as specimens, were emplaced during this period.

COLLECTING

The Engineer mine is currently being worked for gold by Ampex Mining. The operators, Warren Arnholtz and Swede Martensson, are setting aside material for the specimen market. It may also be worthwhile, from a collector's point of view, to sift through the 100-level dump material for "allemontite." A few nice pieces were found by one of us (MM) within a few hours of combing the surface of the dump.

ACKNOWLEDGMENTS

We thank Warren Arnholtz and Swede Martensson for their information, specimens, access to the property and exemplary northern hospitality. Discussions with Gary Johannson, Tom Schroeter and Mitch Mihalynuk are much appreciated, as were the review and comments on the initial draft by Joe Nagel. Thanks also go to George Robinson for providing specimen information, and to Jeff Scovil for photographing the C.M.N. specimen.

REFERENCES

ANONYMOUS (1900-1953) Annual Reports 1899-1952, British Columbia Ministry of Mines.

ANONYMOUS (1901) Geological Survey of Canada, Annual Report 1900, 55A.

BULTMAN, T. R. (1979) Geology and Tectonic History of the Whitehorse Trough West of Atlin, British Columbia. Unpublished PhD thesis, Yale University.

CAIRNES, D. D. (1911) Canadian tellurium-containing ores, Journal of the Canadian Mining Institute, 14, 185-202.

CAIRNES, D. D. (1913) Portions of the Atlin District, British Columbia, Geological Survey of Canada, Memoir 37, 74-99.

CHRISTIE, R. L. (1957) Bennett, British Columbia. Geological Survey of Canada, Map 19-1957 with descriptive notes.

COOKE, H. C. (1946) Canadian Lode Gold Areas (summary account). Geological Survey of Canada, Economic Geology Series, 15, 13-14.

DAUGHTRY, K. L., and IKONA, C. K. (1975) Report on the Engineer Gold Mine, Atlin Mining Division, British Columbia. Private report for the Nu-Energy Development Corporation.

FAIRLIE, M. F. (1940) Notes on the Engineer Mine, Atlin, B.C.

GREENE, R. (1969) Personality Ships of British Columbia. Marine Tapestry Publications Limited, West Vancouver, B.C.

GUNNING, M. H. (1988) British Columbia Ministry of Energy, Mines and Petroleum Resources, Exploration in British Columbia 1987, B83-B87.

GWILLIM, J. C. (1900) Geological Survey of Canada, Annual Report 1899, 45B.

JAMES, H. T. (1928) Northwestern mineral survey district (no. 1). British Columbia Ministry of Mines, Annual Report 1927, C112-C114.

JOHANNSON, G. G. (1993) Preliminary report on the stratigraphy, sedimentology, and biochronology of the Inklin Formation in the Atlin Lake area, northern British Columbia; in Current Research, Part A; Geological Survey of Canada, Paper 93-1A, 37-42.

KURTZ, J. P., and HAUFF, P. L. (1987) Geological Society of America, Rocky Mountain Section, 40th annual meeting, Abstracts with Programs 19 (5), 288.

MIHALYNUK, M. G., and MOUNTJOY, K. J. (1990) Geology of the Tagish Lake Area (104M/8, 9E). British Columbia Ministry of Energy, Mines and Petroleum Resources, Geological Fieldwork 1989, Paper 1990-1, 181-196.

MIHALYNUK, M. G., and ROUSE, J. N. (1988) Preliminary geology of the Tutshi Lake area, northwestern British Columbia (104M/15). British Columbia Ministry of Energy, Mines and Petroleum Resources. Geological Fieldwork 1987, Paper 1988-1, 217-231.

POST, J. L., and BURNETT, J. L. (1985) Roscoelite type locality; gold and vanadium near Coloma, El Dorado County, California. California Geology, 38 (5), 99-102.

SABINA, A. P. (1992) Rocks and minerals for the collector - Alaska Highway: Dawson Creek British Columbia to Yukon/Alaska border. Geological Survey of Canada, Miscellaneous Report 50.

SCHROETER, T. G. (1986) Bennett Project. British Columbia Ministry of Energy, Mines and Petroleum Resources, Geological Fieldwork 1985, Paper 1986-1, 184-189.

SMITH, F. M. (1990) Report on the Engineer gold mine and nearby claims, Atlin mining division, British Columbia. Private report for Gentry Resources Limited.

THOMSON, E. (1937) A review of the occurrence of tellurides in Canada. University of Toronto Studies, Geological Series 40 (1936-1937), 95-101.

WALKER, T. L. (1921) "Allemontite" from Atlin, B.C. American Mineralogist, 6, 97-99.
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Author:Mauthner, Mark H.F.; Groat, Lee A.; Raudsepp, Mati
Publication:The Mineralogical Record
Date:Jul 1, 1996
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