Mineral Hill Mine group, Planet, Santa Maria Mining District (Planet Mining District; Swansea Mining District; Bill Williams Mining District), Buckskin Mountains, La Paz County, Arizona, USAi
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Latitude & Longitude (WGS84):
34° 13' 54'' North , 114° 0' 45'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Parker Strip | 662 (2011) | 17.1km |
| Cienega Springs | 1,798 (2011) | 20.1km |
| Bluewater | 725 (2011) | 24.2km |
| Bluewater | 172 (2011) | 24.6km |
| Parker | 3,046 (2017) | 27.0km |
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 |
|---|---|---|
| Lake Havasu Gem & Mineral Society | Lake Havasu City, Arizona | 40km |
Other/historical names associated with this locality:
Continental Mine
A former underground Cu-Fe-Ag-Au (Be) mine located in sec. 3, in the SE¼ sec. 2, NE¼ & East-central sec. 10, & NW¼ sec. 11, T10N, R17W, 2.5 miles from Planet and 20 miles N of Bouse, on private land. First produced in 1900 and closed in 1970. Owned by various small operators; R.A. DeLano Co.; Arizona Ranch & Metals Co.; and the Powdered Metals Corp.
Mineralization is irregular ore bodies with secondary copper minerals in fractures, small veins, and disseminated in irregular replacement lenses of specular hematite, often massive and thick, in metamorphosed folded and faulted Paleozoic limestone and limy shale overlying Precambrian gneiss. The ore zone was 670.56 meters long, 91.44 meters wide, with a depth to top of 0 meters, and is 22.86 meters thick. The mineralization is associated with low-angle detachment faulting. Orebodies are within and immediately above the flinty, chloritic, micro-brecciated detachment surface. Limestone replacement by hematite with supergene enrichment followed by hydrothermal copper fracture filling. Ore concentration was supergene enrichment.
The strata which form Mineral Hill are undoubtedly continuous with those resting on the gneiss in the vicinity of the Planet Mine, and both series were probably lifted and deformed at the same time. In general the dip varies from 30° to 50° SW due to folding and faulting.
Workings include a shaft 150 feet deep and 4 tunnels, one of which is 400 feet long; also several open cuts, to a depth of 12.19 meters. worked sporadically from the early 1900's through 1970 for Cu, Au & Fe. Additionally, there has been considerable exploratory drilling. Total production would be close to 1,000,000 tons of ore averaging about 1.7% Cu with minor amounts of gold and silver.
A character sample contained 38.1% Fe, 0.1% Mn, 0.1% titania, 5.55% Cu, 0.07% P, 0.36% S, and 27.6% SiO2. Spectrographic analysis indicated the presence of 1 to 10% Al, Ca, & Cu; 0.1 to 1.0% Mg, Mn, Ti, 0.01 to 0.1% Co, Ni and 0.001 to 0.01% U.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Azurite Formula: Cu3(CO3)2(OH)2 |
| ⓘ Bornite Formula: Cu5FeS4 |
| ⓘ Brochantite Formula: Cu4(SO4)(OH)6 |
| ⓘ Calcite Formula: CaCO3 Habit: Scalenohedral crystals to 1 cm long. Colour: White Description: Occurs as crystals on hematite and chrysocolla. |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Chrysocolla Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| ⓘ Hematite Formula: Fe2O3 |
| ⓘ Hematite var. Specularite Formula: Fe2O3 |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
| ⓘ Pyrite Formula: FeS2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Hematite | 4.CB.05 | Fe2O3 |
| ⓘ | var. Specularite | 4.CB.05 | Fe2O3 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Brochantite | 7.BB.25 | Cu4(SO4)(OH)6 |
| 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 | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| H | ⓘ Brochantite | Cu4(SO4)(OH)6 |
| H | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | Carbon | |
| C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| C | ⓘ Calcite | CaCO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | Oxygen | |
| O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| O | ⓘ Brochantite | Cu4(SO4)(OH)6 |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| 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 |
| S | Sulfur | |
| S | ⓘ Bornite | Cu5FeS4 |
| S | ⓘ Brochantite | Cu4(SO4)(OH)6 |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Pyrite | FeS2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Bornite | Cu5FeS4 |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hematite | Fe2O3 |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Hematite var. Specularite | Fe2O3 |
| Cu | Copper | |
| Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
| Cu | ⓘ Bornite | Cu5FeS4 |
| Cu | ⓘ Brochantite | Cu4(SO4)(OH)6 |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
Other Databases
| Link to USGS MRDS: | 10027722 |
|---|
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Southern Basin and RangeWide Rift
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