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Homestake Mine, Hyder Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi
Regional Level Types
Homestake MineMine
Hyder Mining DistrictMining District
Prince of Wales-Hyder Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
56° 4' 29'' North , 130° 10' 8'' West
Latitude & Longitude (decimal):
Type:
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Stewart496 (2013)19.1km
Mindat Locality ID:
198028
Long-form identifier:
mindat:1:2:198028:1
GUID (UUID V4):
03eb172b-6f45-4b2d-a0cb-4bd39cfbd3d6


Property originally staked in 1923
Location: The Homestake mine is in Section 7 at about 3500 feet elevation on a south-facing mountainside approximately 0.3 mile east of upper Ibex Creek (Elliott and Koch, 1981, p. 14, loc. 51). The location is probably accurate within a quarter of a mile.
Geology: The country rock in the area of the Homestake mine is Triassic Texas Creek Granodiorite, which regionally underlies and locally intrudes pelitic metasedimentary and subordinate andesitic metavolcanic strata of the Jurassic or older Mesozoic Hazelton Group; and the Eocene Hyder Quartz Monzonite, which intrudes the Hazelton and Texas Creek rocks (Smith, 1977, Koch, 1996). The deposit consists of a quartz fissure vein 4-5.5 feet thick in Texas Creek Granodiorite (Buddington, 1925, p. 88-89). The vein was traced in outcrop for about 250 feet. The mineralized parts of the vein contain bands of solid sulfide up to 4 feet thick consisting mainly of argentiferous 'steel' galena, accompanied by pyrite, chalcopyrite, and a little sphalerite. The granodiorite hanging wall of the vein contains stringers of tetrahedrite. So-called 'steel' galena resembles augen gneiss with eyes of granulated pyrite in flow-banded galena; this texture indicates that the mineral deposit was subjected to intense stress since its formation (Buddington and Chapin, 1929, p. 320). A 9.5-ton test shipment of sorted ore sent to a smelter in 1925 contained 50% Pb, 0.7% Zn, 22.87 oz Ag per ton, and 0.29 oz Au per ton (Buddington, 1929, p. 95; Cobb, 1978, p. 39). Lead-isotope studies of galena from the Homestake mine (Maas and others, 1929, p. 229-248) indicate that the deposit is Eocene in age, contemporaneous with emplacement of the Hyder Quartz Monzonite.
Workings: A 25-foot crosscut adit is reported to have cut the vein 35 feet below its outcrop (Buddington, 1926, p. 53).
Age: Lead-isotope studies of galena from the Homestake mine (Maas and others, 1929, p. 229-248) indicate that the deposit is Eocene in age, contemporaneous with emplacement of the Hyder Quartz Monzonite.

Commodities (Major) - Ag, Au, Cu, Pb, Zn
Development Status: Yes; small
Deposit Model: Polymetallic veins

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


5 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Sphalerite2.CB.05aZnS
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Galena2.CD.10PbS
β“˜Pyrite2.EB.05aFeS2
β“˜'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
β“˜Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
Oβ“˜ QuartzSiO2
SiSilicon
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ GalenaPbS
Sβ“˜ PyriteFeS2
Sβ“˜ SphaleriteZnS
Sβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
ZnZinc
Znβ“˜ SphaleriteZnS
SbAntimony
Sbβ“˜ Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
PbLead
Pbβ“˜ GalenaPbS

Other Databases

Link to USGS - Alaska:BC051

Other Regions, Features and Areas containing this locality

North America
North America PlateTectonic Plate

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.

References

 
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