Hercules Mine, Harquahala Mining District, La Paz County, Arizona, USAi
Regional Level Types | |
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Hercules Mine | Mine |
Harquahala Mining District | Mining District |
La Paz County | County |
Arizona | State |
USA | Country |
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Latitude & Longitude (WGS84):
33° 46' 14'' North , 113° 32' 59'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Mindat Locality ID:
33504
Long-form identifier:
mindat:1:2:33504:2
GUID (UUID V4):
8469c9ce-2470-4a64-902c-b87aa8022af3
‡Ref.: Bancroft, H. (1911), Reconnaissance of the ore deposits in northern Yuma County, Arizona, USGS Bull. 451: 109-110.
Wilson, E.D., Cunningham, J.B., and Butler, G.M. (1934), Arizona Lode Gold Mines and Gold Mining (revised 1967), Arizona Bureau of Mines Bull. 137: 132.
Keith, Stanton B. (1978) State of Arizona Bureau of Geology and Mineral Technology, Geological Survey Branch Bull. 192, Index of Mining Properties in Yuma County, Arizona: 153 (Table 4).
U.S. Bureau of Mines - Arizona Bureau of Geology and Mineral Technology production file data.
Arizona Bureau of Mines file data.
MRDS database Dep. ID file #10027607, MRDS ID #M003502; and, Dep. ID #10138037, MAS ID #0040120262.
A former surface and underground Au-Ag-Cu-Fe mine located in South-central (center S½) sec. 18, T5N, R12W, 5 miles by road SE of Salome and 4 miles S of Wenden, on state land. Owned at times, or in part, by the Hercules Gold Mining Co. (1934); Mr. John R. Shanley; McDonald; Mr. Tom Rogers & Mr. Leo Farrington; Mr. J.J. Rogers; Cline & Hurtz; and Mr. J.B. Sharp.
Mineralization is gold and silver ores with local copper, in brecciated, discontinuous, lenticular, banded, quartz-jasper fissure veins cemented by limonite from the oxidation of auriferous pyrite and chalcopyrite in a shear zone. Wall rock is a Precambrian quartz diorite gneiss intruded by quartz diorite dikes and overlain by Precambrian calcareous schist. The vein, as exposed in the East shaft, strikes S.75ºW. and dips 60ºN. and is 8 to 24 inches (20 to 60 cm) wide. It contains abundant limonite. Post-mineralization faulting occurred along both the dip and the strike of the veins.
Mineralization occurs along an overthrust fault that places Precambrian metamorphics over Paleozoic-Mesozoic sediments. Mineralization locally is associated with micro-diorite dikes 20 to 20 MY in age.
Workings include an two shallow inclined shafts, adits, and open cut operations. This mine was worked prior to 1900 and sporadically from 1934 through 1050. It produced a total of some 2,670 tons of ore and siliceous gold flux averaging about 0.25 oz. Au/T and 0.27 oz. Ag/T plus 1¼ tons of copper.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
ⓘ Chalcopyrite Formula: CuFeS2 |
ⓘ 'Limonite' Description: Abundant |
ⓘ Pyrite Formula: FeS2 |
ⓘ Pyrite var. Gold-bearing Pyrite Formula: FeS2 |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
ⓘ | Pyrite var. Gold-bearing Pyrite | 2.EB.05a | FeS2 |
ⓘ | 2.EB.05a | FeS2 | |
Unclassified | |||
ⓘ | 'Limonite' | - |
List of minerals for each chemical element
S | Sulfur | |
---|---|---|
S | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
S | ⓘ Chalcopyrite | CuFeS2 |
S | ⓘ Pyrite | FeS2 |
Fe | Iron | |
Fe | ⓘ Pyrite var. Gold-bearing Pyrite | FeS2 |
Fe | ⓘ Chalcopyrite | CuFeS2 |
Fe | ⓘ Pyrite | FeS2 |
Cu | Copper | |
Cu | ⓘ Chalcopyrite | CuFeS2 |
Other Databases
Link to USGS MRDS: | 10027607 |
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Other Regions, Features and Areas containing this locality
North America
- Sonoran DesertDesert
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
USA
- Arizona
- Harquahala MountainsMountain Range
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