Liberty Mine (Silver Hill Mine), Black Mountains, Mohave County, Arizona, USAi
| Regional Level Types | |
|---|---|
| Liberty Mine (Silver Hill Mine) | Mine |
| Black Mountains | Mountain Range |
| Mohave County | County |
| Arizona | State |
| USA | Country |
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Latitude & Longitude (WGS84):
35° 41' 15'' North , 114° 32' 10'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| White Hills | 323 (2011) | 13.7km |
| Dolan Springs | 2,033 (2011) | 26.0km |
| Boulder City | 15,551 (2017) | 42.0km |
| Searchlight | 539 (2011) | 42.6km |
| Chloride | 271 (2011) | 43.0km |
Other/historical names associated with this locality:
Sunbeam group
A former Pb-Ag-Zn-Au-Cu-Mo occurrence/mine located in the NW¼NE¼SE¼ sec. 4, T23N, R18W, G&SRM, about ½ mile SW of Chloride, on Bureau of Land Management administered land. Owned by S. Seger, Arizona (1947). Operated by R. P. M. Davis (1977). Produced during the period 1901-1948. The USGS MRDS database stated accuracy for this locality is 500 meters.
Mineralization is a polymetallic deposit hosted in schist. The ore body is shoots and lenses that strike N10W and dip 45E at a width of 9.14 meters. The mineralization is associated with a Late Cretaceous porphyry intrusion. Associated rocks include Neoproterozoic granite. Local rocks include Early Proterozoic granitic rocks.
Regional geologic structures include Precambrian schistosity at N30E. Late Cretaceous veins, fissures, and dikes striking NW to NNW regionally.
Workings include unspecified surface and underground openings.
SILVER HILL VEIN.
The Silver Hill vein is located on Silver Hill, a prominent elongated ridge just southwest of Chloride and rising about 150 feet above it. It extends southward nearly to the railroad station. The ridge trends about north and south, is about three-fourths of a mile long and one-eighth of a mile broad, and is composed almost wholly of dark amphibolite schist. A coarse granitic rock appears to be intruded in its western base, and it is locally traversed by dikes and stringers of the garnet-bearing aplitic granite and also by a coarse pegmatitic granite. The schist dips about 60° E. and is cut by a well-marked sheeting that dips about 35° W.
As shown by openings and croppings, the northern or main half of the ridge is traversed longitudinally just west of the crest by a well-marked vein or mineral zone, varying from 2 to 12 feet or more in width, whose croppings, hardly rising above the surface, consist of brownish, yellowish, or greenish stained quartz, and seemingly altered dike material which in places is calcareous and brecciated. The foot wall consists of a bowldery or brecciated schist.
The vein strikes N. 7° W. and dips steeply east. It is opened at intervals along its extent by five or six inclined shafts, some of which attain a maximum depth of about 100 feet. The work was done mostly in pioneer times, as this was among the first veins worked in the district. The ore contains silver, lead, and gold and is reported to carry about 2 ounces of gold to the ton, but the principal production is stated to be a small amount of lead.
The Silver Hill vein is located on Silver Hill, a prominent elongated ridge just southwest of Chloride and rising about 150 feet above it. It extends southward nearly to the railroad station. The ridge trends about north and south, is about three-fourths of a mile long and one-eighth of a mile broad, and is composed almost wholly of dark amphibolite schist. A coarse granitic rock appears to be intruded in its western base, and it is locally traversed by dikes and stringers of the garnet-bearing aplitic granite and also by a coarse pegmatitic granite. The schist dips about 60° E. and is cut by a well-marked sheeting that dips about 35° W.
As shown by openings and croppings, the northern or main half of the ridge is traversed longitudinally just west of the crest by a well-marked vein or mineral zone, varying from 2 to 12 feet or more in width, whose croppings, hardly rising above the surface, consist of brownish, yellowish, or greenish stained quartz, and seemingly altered dike material which in places is calcareous and brecciated. The foot wall consists of a bowldery or brecciated schist.
The vein strikes N. 7° W. and dips steeply east. It is opened at intervals along its extent by five or six inclined shafts, some of which attain a maximum depth of about 100 feet. The work was done mostly in pioneer times, as this was among the first veins worked in the district. The ore contains silver, lead, and gold and is reported to carry about 2 ounces of gold to the ton, but the principal production is stated to be a small amount of lead.
Mineralization is a polymetallic deposit hosted in schist. The ore body is shoots and lenses that strike N10W and dip 45E at a width of 9.14 meters. The mineralization is associated with a Late Cretaceous porphyry intrusion. Associated rocks include Neoproterozoic granite. Local rocks include Early Proterozoic granitic rocks.
Regional geologic structures include Precambrian schistosity at N30E. Late Cretaceous veins, fissures, and dikes striking NW to NNW regionally.
Workings include unspecified surface and underground openings.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsCommodity List
This is a list of exploitable or exploited mineral commodities recorded at this locality.Mineral List
5 valid minerals.
Rock Types Recorded
Select Rock List Type
Alphabetical List Tree DiagramDetailed Mineral List:
| ⓘ Calcite Formula: CaCO3 |
| ⓘ Galena Formula: PbS |
| ⓘ 'Limonite' |
| ⓘ Molybdenite Formula: MoS2 |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Molybdenite | 2.EA.30 | MoS2 |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Calcite | 5.AB.05 | CaCO3 |
| Unclassified | |||
| ⓘ | 'Limonite' | - | |
List of minerals for each chemical element
| C | Carbon | |
|---|---|---|
| C | ⓘ Calcite | CaCO3 |
| O | Oxygen | |
| O | ⓘ Calcite | CaCO3 |
| O | ⓘ Quartz | SiO2 |
| Si | Silicon | |
| Si | ⓘ Quartz | SiO2 |
| S | Sulfur | |
| S | ⓘ Galena | PbS |
| S | ⓘ Molybdenite | MoS2 |
| S | ⓘ Pyrite | FeS2 |
| Ca | Calcium | |
| Ca | ⓘ Calcite | CaCO3 |
| Fe | Iron | |
| Fe | ⓘ Pyrite | FeS2 |
| Mo | Molybdenum | |
| Mo | ⓘ Molybdenite | MoS2 |
| Pb | Lead | |
| Pb | ⓘ Galena | PbS |
Other Databases
| Link to USGS MRDS: | 10027811 |
|---|
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
USA
- Mojave DesertDesert
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