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Big Banana Mine (Maude claim; Big Banana Nos. 1-2-3 claims), Baboquivari Mining District, Baboquivari Mountains, Pima County, Arizona, USAi
Regional Level Types
Big Banana Mine (Maude claim; Big Banana Nos. 1-2-3 claims)Mine
Baboquivari Mining DistrictMining District
Baboquivari MountainsMountain Range
Pima CountyCounty
ArizonaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
31° 54' 30'' North , 111° 39' 20'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Ali Chukson132 (2011)13.6km
Topawa299 (2011)19.2km
Sells2,495 (2011)21.3km
South Komelik111 (2011)23.5km
Cowlic135 (2011)33.4km
Mindat Locality ID:
35371
Long-form identifier:
mindat:1:2:35371:0
GUID (UUID V4):
0


Ref.: Dale, V.B., Stewart, L.A., and McKinney, W.A. (1960), Tungsten deposits of Cochise, Pima, and Santa Cruz Counties., Arizona, U.S. Bureau of Mines Report of Investigation 5650: 67-69.

Keith, Stanton B. (1974), Arizona Bureau of Geology & Mineral Technology, Geological Survey Branch Bull. 189, Index of Mining Properties in Pima County, Arizona: 108 (Table 4).

Phillips, K.A. (1987), Arizona Industrial Minerals, 2nd. Edition, Arizona Department of Mines & Minerals Mineral Report 4, 185 pp.

MRDS database Dep. ID file #10039471, MRDS ID #M050133; and, Dep. ID file #10186505, MAS ID #0040190118.

A former small surface and underground W-Cu-Mo-Fluorspar mine located in North-central sec. 32, T.17S., R.7E. (protracted), on the west side of the Baboquivari Mountains and 1.5 miles SE of San Juan Spring. Discovered in 1954 by Mr. William H. Coplan. Produced 1954 and 1955-1957 ?. Owned at times, or in part, by Coplen; C.G. Glasscock; and the Tideland Oil Co.

Mineralization is a replacement deposit of spotty scheelite with skarn minerals, pyrite and fluorite in narrow en echalon shoots in a strongly fractured zone cutting Laramide metamorphic quartzite adjacent to altered intrusive rhyolite. The mineralized zone strikes S15E and is 1,000 feet or more in length. The host rock unit is the Ali Molina Formation. Ore control was tensional shears in a major NW-striking fault zone. Hydrothermal alteration has affected scheelite lenses.

Workings included tunnels and open cuts. The lower cut produced some ore; the middle cut produced considerable ore; the upper cut produced ore in 1957; the main adit, which was lowest, was mostly in barren rock. The workings are 60.96 meters deep and 304.8 meters long. Produced about 20,000 pounds of tungsten concentrates in 1955 and 1956.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


6 valid minerals.

Detailed Mineral List:

Chalcopyrite
Formula: CuFeS2
Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Fluorite
Formula: CaF2
'Garnet Group'
Formula: X3Z2(SiO4)3
Molybdenite
Formula: MoS2
Pyrite
Formula: FeS2
Scheelite
Formula: Ca(WO4)

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Molybdenite2.EA.30MoS2
Pyrite2.EB.05aFeS2
Group 3 - Halides
Fluorite3.AB.25CaF2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Scheelite7.GA.05Ca(WO4)
Group 9 - Silicates
Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Unclassified
'Garnet Group'-X3Z2(SiO4)3

List of minerals for each chemical element

HHydrogen
H Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
OOxygen
O Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
O ScheeliteCa(WO4)
O Garnet GroupX3Z2(SiO4)3
FFluorine
F FluoriteCaF2
AlAluminium
Al Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SiSilicon
Si Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Si Garnet GroupX3Z2(SiO4)3
SSulfur
S ChalcopyriteCuFeS2
S MolybdeniteMoS2
S PyriteFeS2
CaCalcium
Ca Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Ca FluoriteCaF2
Ca ScheeliteCa(WO4)
FeIron
Fe ChalcopyriteCuFeS2
Fe Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
MoMolybdenum
Mo MolybdeniteMoS2
WTungsten
W ScheeliteCa(WO4)

Other Databases

Link to USGS MRDS:10039471

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