Germania Mine, Turquoise Mining District (Courtland-Gleeson Mining District), Cochise County, Arizona, USAi
| Regional Level Types | |
|---|---|
| Germania Mine | Mine |
| Turquoise Mining District (Courtland-Gleeson Mining District) | Mining District |
| Cochise County | County |
| Arizona | State |
| USA | Country |
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Latitude & Longitude (WGS84):
31° 46' 26'' North , 109° 48' 24'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
Local clubs are the best way to get access to collecting localities
| Club | Location | Distance |
|---|---|---|
| Sunsites Gem and Mineral Club | Pearce, Arizona | 15km |
Mindat Locality ID:
33010
Long-form identifier:
mindat:1:2:33010:8
GUID (UUID V4):
dbd49a96-66d9-40a6-9b5d-714a80584217
A former small underground Cu-Ag-Au-Gemstone mine located in the SW ¼ sec. 16, T.19S., R.25E. (Pearce 15 minute topo map), 1/2 mile SE of Turquoise Mountain, and approximately 1/4 mile north of Courtland. Produced 1909-1940. Owned at times, or in part, by the Calumet & Arizona Mining Co. and the Phelps Dodge Corp. Operators including Charles Gerdes, Calumet Arizona, Gerdes & McDonald, and F.E. Laymon.
Mineralization is irregular, oxidized, blanket-like copper ores in thrust fault breccia between Bolsa Quartzite above, and Carboniferous Abrigo Limestone below. Thickness of the overthrust material is about 100 feet. Some ore is in the limestone. Ore concentration was oxidation. In some areas, Abrigo Limestone underlies Bolsa Quartzite in the overlying plate. The thickness of the overthrust material about 100 feet.
Local structures include an overthrust of Bolsa Quartzite over Paleozoic rocks.
Workings include a shaft(s). Workings are 1,493.52 meters long by 152.4 meters deep. Average of 15 feet thick drifts on the 145, 215, 260, 275, 300, and 500 foot levels. Mineralization pinched out at depth. Workings adjoin the Maid of Sunshine & the Mary shaft sunk in 1909.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Calcite Formula: CaCO3 References: |
| ⓘ Chrysocolla Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| ⓘ Cuprite Formula: Cu2O |
| ⓘ Hematite Formula: Fe2O3 References: |
| ⓘ Hematite var. Specularite Formula: Fe2O3 References: |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 4 - Oxides and Hydroxides | |||
|---|---|---|---|
| ⓘ | Cuprite | 4.AA.10 | Cu2O |
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | var. Specularite | 4.CB.05 | Fe2O3 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 9 - Silicates | |||
| ⓘ | Chrysocolla | 9.ED.20 | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| O | ⓘ Cuprite | Cu2O |
| O | ⓘ Hematite | Fe2O3 |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Hematite var. Specularite | Fe2O3 |
| Al | Aluminium | |
| Al | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Si | Silicon | |
| Si | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Hematite var. Specularite | Fe2O3 |
| Cu | Copper | |
| Cu | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Cu | ⓘ Cuprite | Cu2O |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
Other Databases
| Link to USGS MRDS: | 10088876 |
|---|
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
- Pedregosa BasinBasin
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References
