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Latitude & Longitude (WGS84):
46° 1' 5'' North , 112° 32' 6'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Butte34,190 (2011)1.6km
Walkerville700 (2017)1.8km
Butte-Silver Bow (Balance)33,525 (2013)16.0km
Warm Springs3,000 (2013)26.4km
Anaconda9,417 (2011)33.7km
Mindat Locality ID:
6050
Long-form identifier:
mindat:1:2:6050:2
GUID (UUID V4):
0
Other/historical names associated with this locality:
Stewart Mine


Located within the Butte National Landmark District, the Stewart (or Steward) is approximately 200 feet north of the intersection of North Main and Woolman Streets on the east side of the street. The headframe, main hoist house, and auxiliary hoist house remain on the Stewart mine site. The mine was one of the major mines on Butte Hill and had extensive surface facilities, most of which have been removed.

Erected in 1898, the headframe at West Stewart constitutes one of Butte's earliest examples of the larger headframes; the 126-foot headframe permitted the use of five-ton skips and a ten-foot diameter sheave wheel. The construction of this headframe resembles the one erected at the Original mine in 1902; the Gillette-Herzog Mfg. Co. of Minneapolis manufactured both headframes. The headframe was designed so ore could be shunted directly from ore cars via a tramway into loading bins, from which rail cars could be loaded. In later years the Anaconda Company abandoned this rail line and used trucks to haul ore to the Weed Concentrator (Harrier and Farnham 1930; Piper 1987).

With the exception of the Original mine, the Stewart has the only remaining brick hoist house on the Butte hill. This brick hoist house was built between 1891 and 1906. In 1906 Clark replaced the steam hoist with one operated with compressed air. This became common practice on the Butte hill during the first decade of the twentieth century, and this retrofit could be accomplished with several minor adjustments, which included enlarging the engine cylinders. The tower at the rear of the hoist house contains a steam line (Shovers 1984; Piper 1987; Sanborn 1891; 1900; 1914).

The auxiliary hoist house contained the Bowser steam hoist, which was converted to operate on compressed air early in the twentieth century. The steel tank and smokestack located adjacent to the auxiliary hoist house on the west served as an exhaust for the steam-powered hoisting engine. Clark erected this building sometime between 1891 and 1906 (Piper 1987; Sanborn 1891; 1900; 1914).

The Stewart mine (aka West Stewart or Steward) was one of Butte's deepest and most productive copper-silver mines from the late 1890s until its closure in 1973. Although large-scale development did not begin at the West Stewart until the turn of the century, the original mining claim was actually patented several decades earlier. On August 9, 1877, William A. Clark, John W. Steward, Samuel F. Larabie, and Clark's brother, Joseph, filed on 10 acres known as the Steward lode. The Stewart vein, rich in silver ore, branches both east and west of the original lode, encompassing the Gagnon, Original and Parrot mine sites. The Clark Brothers initially developed the Steward lode from the East Stewart shaft beginning in the 1880s, working the vein sporadically with 10 to 30 men and reaching a depth of 330 feet by 1894. The miners worked the 2-compartment shaft using a Ledgerwood steam hoist.

Within the next six years, the Stewart grew from a small, insignificant operation into one of Butte's premier copper-silver mines. By 1895 W. A. Clark and his brothers, J. Ross and Joseph, operated the Original and the Colusa-Parrot, both located along the Stewart vein .

The miners made great advances in the Stewart shaft during the last years of the nineteenth century, reaching a depth of 600 feet in 1895, 800 feet in 1898, and 1000 feet in 1900, and a powerful E. P. Allis hoisting engine replaced the old engine. By 1900 Clark employed 140 men in the mine.

The first years of the twentieth century marked noticeable changes both above and below ground at the Stewart. In 1898 the 126-foot-tall steel headframe replaced the wooden one over the 1,300-foot-deep, 3-compartment shaft. Connections were driven between the Stewart and the other Clark mines, the Nipper, Parrot, and Original. That same year work continued on a shaft several hundred feet to the west, a mine that came to be known as the West Stewart. Clark employed 114 men to work this mine, who in one year's time advanced the shaft 650 feet, creating a shaft 1,100 feet deep that was served by a compressed air Nordberg hoist.

By 1905 the number of miners working underground had risen to 235, and the shaft reached a depth of 1,900 feet. Tunnels were driven, connecting the West Stewart with the Clear Grit and the Mountain Con. Trammers at the West Stewart still relied on horses to move ore from the stope to the shaft, while some of the Amalgamated mines had already shifted to electric locomotives. By this time work in the East Stewart had subsided, and the shaft was relegated to serve as a ventilation shaft for the more productive West Stewart. Even with improved ventilation, the Stewart remained one of the two hottest mines on the Butte hill (the Belmont being the worst), with temperatures as high as 1300°F in certain deep-level stopes.

On June 1, 1910, ownership transferred from W. A. Clark to the ACM Co. During the last months of Clark's dominion, ore hoisting was transferred from the Stewart to the Original mine. Six months later hoisting resumed at the Stewart, and ore mined at the Little Minah and the Clear Grit was hoisted through the Stewart shaft. In 1911 the ACM found a vein of high-grade ore on the 2,300-foot level and set their workforce of 479 men to the task of drifting in both directions from the shaft along the vein. By 1912 miners at the Stewart reached a depth of 2,500 feet using a hoisting system of three double-decked cages and 7-ton ore skips. The same year fire ravaged workings at the 1,700-foot level, but damage was confined to that single level, and work continued in stopes above and below. Although copper production fell off at the end of World War I, by 1920 the Stewart shaft reached a depth of 3,633 feet, making it ACM's deepest Butte mine.

During the next two decades low metal prices, strikes, and a nationwide economic depression temporarily halted mining at the Stewart mine. World War II demands for copper reactivated the Stewart, and for the next 20 years, the Stewart was a major producer. After the war, copper continued to be hoisted through the modern Kelley shaft located to the northeast. Miners connected the Stewart underground to the Kelley on the 3000-foot level so that ore mined in the Stewart could be raised through the Kelley, taking advantage of its larger skips and more powerful hoisting engine. Even after A. C. M. halted block caving in 1955 and turned to pit mining, miners continued to extract copper ore selectively in the Stewart underground until 1973, when underground operations ceased. Some experimental mining occurred in the Stewart until 1980. The Stewart shaft eventually reached a depth of 4,400 feet, making it one of Butte's longest operating and deepest copper mines (Shovers 1987).


Ref.: Rocks & Min.: 16:247.; Ore Deposits at Butte, Montana, R. H. Sales, 1914; Guidebook for the Butte Field Meeting of the Society Of Economic Geologists, 1973.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


37 valid minerals.

Detailed Mineral List:

Aikinite
Formula: CuPbBiS3
Albite
Formula: Na(AlSi3O8)
Albite var. Oligoclase
Formula: (Na,Ca)[Al(Si,Al)Si2O8]
Andalusite
Formula: Al2(SiO4)O
Anhydrite
Formula: CaSO4
Ankerite
Formula: Ca(Fe2+,Mg)(CO3)2
'Apatite'
Formula: Ca5(PO4)3A
Baryte
Formula: BaSO4
Betekhtinite
Formula: Pb2(Cu,Fe)22-24S15
'Biotite'
Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Bornite
Formula: Cu5FeS4
Description: The Stewart is probably most famous for the bornite and tennatite specimens found there. I have one very interesting specimen consisting of a single needle of betekthinite to 1.5cm included within a translucent, doubly terminated calcite scalenohedron to
Calcite
Formula: CaCO3
Description: The Stewart is probably most famous for the bornite and tennatite specimens found there. I have one very interesting specimen consisting of a single needle of betekthinite to 1.5cm included within a translucent, doubly terminated calcite scalenohedron to
Chalcocite
Formula: Cu2S
Chalcopyrite
Formula: CuFeS2
'Chlorite Group'
Colusite
Formula: Cu13VAs3S16
Corundum
Formula: Al2O3
Corundum var. Sapphire
Formula: Al2O3
Covellite
Formula: CuS
Digenite
Formula: Cu9S5
Dolomite
Formula: CaMg(CO3)2
Enargite
Formula: Cu3AsS4
Fluorite
Formula: CaF2
Galena
Formula: PbS
Hinsdalite
Formula: PbAl3(PO4)(SO4)(OH)6
References:
Hübnerite
Formula: MnWO4
Magnetite
Formula: Fe2+Fe3+2O4
Molybdenite
Formula: MoS2
Muscovite
Formula: KAl2(AlSi3O10)(OH)2
Muscovite var. Sericite
Formula: KAl2(AlSi3O10)(OH)2
Native Silver
Formula: Ag
Orthoclase
Formula: K(AlSi3O8)
Pyrite
Formula: FeS2
Description: The Stewart is probably most famous for the bornite and tennatite specimens found there. I have one very interesting specimen consisting of a single needle of betekthinite to 1.5cm included within a translucent, doubly terminated calcite scalenohedron to
Quartz
Formula: SiO2
Description: The Stewart is probably most famous for the bornite and tennatite specimens found there. I have one very interesting specimen consisting of a single needle of betekthinite to 1.5cm included within a translucent, doubly terminated calcite scalenohedron to
Rhodochrosite
Formula: MnCO3
Scheelite
Formula: Ca(WO4)
Siderite
Formula: FeCO3
Sphalerite
Formula: ZnS
Stromeyerite
Formula: AgCuS
'Tennantite Subgroup'
Formula: Cu6(Cu4C2+2)As4S12S
Description: The Stewart is probably most famous for the bornite and tennatite specimens found there. I have one very interesting specimen consisting of a single needle of betekthinite to 1.5cm included within a translucent, doubly terminated calcite scalenohedron to
'Tetrahedrite Subgroup'
Formula: Cu6(Cu4C2+2)Sb4S12S
Titanite
Formula: CaTiO(SiO4)
Uraninite ?
Formula: UO2
Wittichenite
Formula: Cu3BiS3
Wurtzite
Formula: (Zn,Fe)S
References:
Daniel J. Evanich CollectionIdentification: Visual Identification

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Native Silver1.AA.05Ag
Group 2 - Sulphides and Sulfosalts
Chalcocite2.BA.05Cu2S
Digenite2.BA.10Cu9S5
Bornite2.BA.15Cu5FeS4
Stromeyerite2.BA.40AgCuS
Betekhtinite2.BE.05Pb2(Cu,Fe)22-24S15
Covellite2.CA.05aCuS
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Colusite2.CB.30Cu13VAs3S16
Wurtzite2.CB.45(Zn,Fe)S
Galena2.CD.10PbS
Molybdenite2.EA.30MoS2
Pyrite2.EB.05aFeS2
Wittichenite2.GA.20Cu3BiS3
'Tennantite Subgroup'2.GB.05Cu6(Cu4C2+2)As4S12S
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Aikinite2.HB.05aCuPbBiS3
Enargite2.KA.05Cu3AsS4
Group 3 - Halides
Fluorite3.AB.25CaF2
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Corundum4.CB.05Al2O3
var. Sapphire4.CB.05Al2O3
Quartz4.DA.05SiO2
Hübnerite4.DB.30MnWO4
Uraninite ?4.DL.05UO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Rhodochrosite5.AB.05MnCO3
Siderite5.AB.05FeCO3
Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
Dolomite5.AB.10CaMg(CO3)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Anhydrite7.AD.30CaSO4
Baryte7.AD.35BaSO4
Scheelite7.GA.05Ca(WO4)
Group 8 - Phosphates, Arsenates and Vanadates
Hinsdalite8.BL.05PbAl3(PO4)(SO4)(OH)6
Group 9 - Silicates
Andalusite9.AF.10Al2(SiO4)O
Titanite9.AG.15CaTiO(SiO4)
Muscovite9.EC.15KAl2(AlSi3O10)(OH)2
var. Sericite9.EC.15KAl2(AlSi3O10)(OH)2
Orthoclase9.FA.30K(AlSi3O8)
Albite9.FA.35Na(AlSi3O8)
var. Oligoclase9.FA.35(Na,Ca)[Al(Si,Al)Si2O8]
Unclassified
'Biotite'-K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
'Chlorite Group'-
'Apatite'-Ca5(PO4)3A

List of minerals for each chemical element

HHydrogen
H BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
H HinsdalitePbAl3(PO4)(SO4)(OH)6
H MuscoviteKAl2(AlSi3O10)(OH)2
H Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CCarbon
C AnkeriteCa(Fe2+,Mg)(CO3)2
C CalciteCaCO3
C DolomiteCaMg(CO3)2
C RhodochrositeMnCO3
C SideriteFeCO3
OOxygen
O AlbiteNa(AlSi3O8)
O AndalusiteAl2(SiO4)O
O AnhydriteCaSO4
O AnkeriteCa(Fe2+,Mg)(CO3)2
O BaryteBaSO4
O BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
O CalciteCaCO3
O CorundumAl2O3
O DolomiteCaMg(CO3)2
O HinsdalitePbAl3(PO4)(SO4)(OH)6
O HübneriteMnWO4
O MagnetiteFe2+Fe23+O4
O MuscoviteKAl2(AlSi3O10)(OH)2
O Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
O OrthoclaseK(AlSi3O8)
O QuartzSiO2
O RhodochrositeMnCO3
O Corundum var. SapphireAl2O3
O ScheeliteCa(WO4)
O SideriteFeCO3
O TitaniteCaTiO(SiO4)
O UraniniteUO2
O Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
O ApatiteCa5(PO4)3A
FFluorine
F BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
F FluoriteCaF2
NaSodium
Na AlbiteNa(AlSi3O8)
Na Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
MgMagnesium
Mg AnkeriteCa(Fe2+,Mg)(CO3)2
Mg BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Mg DolomiteCaMg(CO3)2
AlAluminium
Al AlbiteNa(AlSi3O8)
Al AndalusiteAl2(SiO4)O
Al BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Al CorundumAl2O3
Al HinsdalitePbAl3(PO4)(SO4)(OH)6
Al MuscoviteKAl2(AlSi3O10)(OH)2
Al Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Al OrthoclaseK(AlSi3O8)
Al Corundum var. SapphireAl2O3
Al Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
SiSilicon
Si AlbiteNa(AlSi3O8)
Si AndalusiteAl2(SiO4)O
Si BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Si MuscoviteKAl2(AlSi3O10)(OH)2
Si Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Si OrthoclaseK(AlSi3O8)
Si QuartzSiO2
Si TitaniteCaTiO(SiO4)
Si Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
PPhosphorus
P HinsdalitePbAl3(PO4)(SO4)(OH)6
P ApatiteCa5(PO4)3A
SSulfur
S AikiniteCuPbBiS3
S AnhydriteCaSO4
S BaryteBaSO4
S BetekhtinitePb2(Cu,Fe)22-24S15
S BorniteCu5FeS4
S ChalcopyriteCuFeS2
S ChalcociteCu2S
S ColusiteCu13VAs3S16
S CovelliteCuS
S DigeniteCu9S5
S EnargiteCu3AsS4
S GalenaPbS
S HinsdalitePbAl3(PO4)(SO4)(OH)6
S MolybdeniteMoS2
S PyriteFeS2
S SphaleriteZnS
S StromeyeriteAgCuS
S Tennantite SubgroupCu6(Cu4C22+)As4S12S
S Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
S WitticheniteCu3BiS3
S Wurtzite(Zn,Fe)S
KPotassium
K BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
K MuscoviteKAl2(AlSi3O10)(OH)2
K OrthoclaseK(AlSi3O8)
K Muscovite var. SericiteKAl2(AlSi3O10)(OH)2
CaCalcium
Ca AnhydriteCaSO4
Ca AnkeriteCa(Fe2+,Mg)(CO3)2
Ca CalciteCaCO3
Ca DolomiteCaMg(CO3)2
Ca FluoriteCaF2
Ca Albite var. Oligoclase(Na,Ca)[Al(Si,Al)Si2O8]
Ca ScheeliteCa(WO4)
Ca TitaniteCaTiO(SiO4)
Ca ApatiteCa5(PO4)3A
TiTitanium
Ti BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Ti TitaniteCaTiO(SiO4)
VVanadium
V ColusiteCu13VAs3S16
MnManganese
Mn HübneriteMnWO4
Mn RhodochrositeMnCO3
FeIron
Fe AnkeriteCa(Fe2+,Mg)(CO3)2
Fe BetekhtinitePb2(Cu,Fe)22-24S15
Fe BiotiteK(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2
Fe BorniteCu5FeS4
Fe ChalcopyriteCuFeS2
Fe MagnetiteFe2+Fe23+O4
Fe PyriteFeS2
Fe SideriteFeCO3
Fe Wurtzite(Zn,Fe)S
CuCopper
Cu AikiniteCuPbBiS3
Cu BetekhtinitePb2(Cu,Fe)22-24S15
Cu BorniteCu5FeS4
Cu ChalcopyriteCuFeS2
Cu ChalcociteCu2S
Cu ColusiteCu13VAs3S16
Cu CovelliteCuS
Cu DigeniteCu9S5
Cu EnargiteCu3AsS4
Cu StromeyeriteAgCuS
Cu Tennantite SubgroupCu6(Cu4C22+)As4S12S
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
Cu WitticheniteCu3BiS3
ZnZinc
Zn SphaleriteZnS
Zn Wurtzite(Zn,Fe)S
AsArsenic
As ColusiteCu13VAs3S16
As EnargiteCu3AsS4
As Tennantite SubgroupCu6(Cu4C22+)As4S12S
MoMolybdenum
Mo MolybdeniteMoS2
AgSilver
Ag Native SilverAg
Ag StromeyeriteAgCuS
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
BaBarium
Ba BaryteBaSO4
WTungsten
W HübneriteMnWO4
W ScheeliteCa(WO4)
PbLead
Pb AikiniteCuPbBiS3
Pb BetekhtinitePb2(Cu,Fe)22-24S15
Pb GalenaPbS
Pb HinsdalitePbAl3(PO4)(SO4)(OH)6
BiBismuth
Bi AikiniteCuPbBiS3
Bi WitticheniteCu3BiS3
UUranium
U UraniniteUO2

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate
USA

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