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Hercules Mine, Harquahala Mining District, La Paz County, Arizona, USAi
Regional Level Types
Hercules MineMine
Harquahala Mining DistrictMining District
La Paz CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
33° 46' 14'' North , 113° 32' 59'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Wenden728 (2011)5.8km
Salome1,530 (2011)6.1km
Vicksburg597 (2011)18.9km
Utting126 (2011)32.1km
Brenda676 (2011)37.9km
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 Elements

Mineral List


2 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrite
var. Gold-bearing Pyrite
2.EB.05aFeS2
2.EB.05aFeS2
Unclassified
'Limonite'-

List of minerals for each chemical element

SSulfur
S Pyrite var. Gold-bearing PyriteFeS2
S ChalcopyriteCuFeS2
S PyriteFeS2
FeIron
Fe Pyrite var. Gold-bearing PyriteFeS2
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2

Other Databases

Link to USGS MRDS:10027607

Other Regions, Features and Areas containing this locality

North America
North America PlateTectonic Plate
USA

This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.
 
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