Mammoth Mine, Silver Bell Mining District, Silver Bell Mountains, Pima County, Arizona, USAi
Regional Level Types | |
---|---|
Mammoth Mine | Mine |
Silver Bell Mining District | Mining District |
Silver Bell Mountains | Mountain Range |
Pima County | County |
Arizona | State |
USA | Country |
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Latitude & Longitude (WGS84):
32° 24' 51'' North , 111° 31' 45'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Avra Valley | 6,050 (2011) | 20.2km |
Nelson | 259 (2011) | 24.4km |
Red Rock | 169 (2011) | 26.2km |
Picture Rocks | 9,563 (2011) | 27.6km |
Marana | 41,315 (2017) | 28.6km |
Mindat Locality ID:
36340
Long-form identifier:
mindat:1:2:36340:7
GUID (UUID V4):
c145b98e-c255-4cab-849b-3ef028563505
Other/historical names associated with this locality:
Old Boot Mine; Imperial Mine; Union Mine; Southern Beauty Mine; Page Mine
β‘Ref.: Stewart, C.A. (1912) The geology and ore deposits of the Silverbell mining district, Arizona, AIME Bull. 65: 455-505 (AIME Transactions, Vol. 43: 240-290.
University of Arizona Bull. 41 (1916-17), Mineralogy of Useful Minerals in Arizona: 29.
Richard, K.E. & Courtright, J.H. (1954), Structure & Mineralization at Silver Bell, Arizona, Mining Engineering, Vol. 6(11): 1095-1099 (AIME Transactions, 1954 - Vol. 199 (1955)).
Galbraith, F.W. & D.J. Brennan (1959), Minerals of Arizona: 43.
Richard, K.E. & Courtright, J.H. (1966), Structure & Mineralization at Silver Bell, Arizona, in Titley, S.R. and Hicks, C.L., eds., Geology of the porphyry copper deposits, southwestern North America: 157-163 (University of Arizona Press).
Elevatorski, E.A. (1971), Arizona Fluorspar, Arizona Department of Mineral Resources, U.S. Bureau of Mines Report of Investigation 5651: 33.
Keith, Stanton B. (1974), Arizona Bureau of Geology & Mineral Technology, Geological Survey Branch Bull. 189, Index of Mining Properties in Pima County, Arizona: 143 (Table 4).
Elevatorski, E.A. (1971), Arizona Fluorspar, Arizona Department of Mineral Resources, U.S. Bureau of Mines Report of Investigation 5651: 49.
Phillips, K.A. (1987), Arizona Industrial Minerals, 2nd. Edition, Arizona Department of Mines & Minerals Mineral Report 4, 185 pp.
Peirce, H. Wesley (1990), Arizona Geological Survey Industrial Minerals card file.
Mining World, Vol. 36: 1104-1107, 1147-1150.
Niemuth, N.J. & K.A. Phillips (1992), Copper Oxide Resources, Arizona Department of Mines & Mineral Resources Open File Report 92-10: 12 (Table 1).
Arizona Bureau of Mines file data.
MRDS database Dep. ID file #10039686, MRDS ID #M050652; and, Dep. ID #10210633, MAS ID #0040190306.
A former small underground Cu-Ag-Pb-Zn-Mo-Au-Baryte-Fluorspar mine located in the NE ΒΌ sec. 4 T.12S., R.8E. (Vaca Hills 15 minute topo map), 2Β½ miles NW of Silver Bell. First produced 1865. Owned at times, or in part, by the Huachuca Mining & Smelting Co.; Pima County Mining & Smelting Co.; Silver Bell Mining Co.; Albert Steinfeld Co.; Imperial Copper Co.; and the American Smelting & Refining Co. (ASARCO).
Mineralization is copper, and minor lead and zinc, carbonates and sulfides in fissure veins and irregular disseminations in pyrometasomatic deposits in garnetized or altered Paleozoic limestone blocks engulfed in Laramide dacite porphyry and monzonite intrusives, along a major fault zone. Alteration was hydrothermal metasomatism. Tactite present.
Local structures include a major fault zone.
Prospected and worked from the 1870's to 1931 as an underground mine. Over 1,000,000 tons of ore were produced, averaging better than 3% Cu and about 1 oz. Ag/T with minor Pb, Zn & Au.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
β Azurite Formula: Cu3(CO3)2(OH)2 References: |
β Baryte Formula: BaSO4 |
β Bornite Formula: Cu5FeS4 References: |
β Chalcopyrite Formula: CuFeS2 |
β Cuprite Formula: Cu2O References: |
β Fluorite Formula: CaF2 Colour: Green |
β Galena Formula: PbS References: |
β 'Garnet Group' Formula: X3Z2(SiO4)3 |
β 'Limonite' References: |
β Malachite Formula: Cu2(CO3)(OH)2 References: |
β Sphalerite Formula: ZnS References: |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
β | Bornite | 2.BA.15 | Cu5FeS4 |
β | Sphalerite | 2.CB.05a | ZnS |
β | Chalcopyrite | 2.CB.10a | CuFeS2 |
β | Galena | 2.CD.10 | PbS |
Group 3 - Halides | |||
β | Fluorite | 3.AB.25 | CaF2 |
Group 4 - Oxides and Hydroxides | |||
β | Cuprite | 4.AA.10 | Cu2O |
Group 5 - Nitrates and Carbonates | |||
β | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
β | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
β | Baryte | 7.AD.35 | BaSO4 |
Unclassified | |||
β | 'Limonite' | - | |
β | 'Garnet Group' | - | X3Z2(SiO4)3 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | β Azurite | Cu3(CO3)2(OH)2 |
H | β Malachite | Cu2(CO3)(OH)2 |
C | Carbon | |
C | β Azurite | Cu3(CO3)2(OH)2 |
C | β Malachite | Cu2(CO3)(OH)2 |
O | Oxygen | |
O | β Azurite | Cu3(CO3)2(OH)2 |
O | β Baryte | BaSO4 |
O | β Cuprite | Cu2O |
O | β Malachite | Cu2(CO3)(OH)2 |
O | β Garnet Group | X3Z2(SiO4)3 |
F | Fluorine | |
F | β Fluorite | CaF2 |
Si | Silicon | |
Si | β Garnet Group | X3Z2(SiO4)3 |
S | Sulfur | |
S | β Baryte | BaSO4 |
S | β Bornite | Cu5FeS4 |
S | β Chalcopyrite | CuFeS2 |
S | β Galena | PbS |
S | β Sphalerite | ZnS |
Ca | Calcium | |
Ca | β Fluorite | CaF2 |
Fe | Iron | |
Fe | β Bornite | Cu5FeS4 |
Fe | β Chalcopyrite | CuFeS2 |
Cu | Copper | |
Cu | β Azurite | Cu3(CO3)2(OH)2 |
Cu | β Bornite | Cu5FeS4 |
Cu | β Chalcopyrite | CuFeS2 |
Cu | β Cuprite | Cu2O |
Cu | β Malachite | Cu2(CO3)(OH)2 |
Zn | Zinc | |
Zn | β Sphalerite | ZnS |
Ba | Barium | |
Ba | β Baryte | BaSO4 |
Pb | Lead | |
Pb | β Galena | PbS |
Other Databases
Link to USGS MRDS: | 10039686 |
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Other Regions, Features and Areas containing this locality
Mexico
- Sierra Madre OccidentalMountain Range
North America
- Sonoran DesertDesert
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mazatzal DomainDomain
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