Vote for your favorite mineral in #MinCup26! - Quartz vs. Asagiite
It's a classic vs a newbie as the most common named mineral in the crust Quartz is up against an exceedingly-rare sea foam-green mineral discovered just a few years ago Asagiite.
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Hillside; Silver King Prospect, Kantishna Mining District, Denali Borough, Alaska, USAi
Regional Level Types
Hillside; Silver King ProspectProspect
Kantishna Mining DistrictMining District
Denali BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 32' 18'' North , 150° 58' 40'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
197984
Long-form identifier:
mindat:1:2:197984:1
GUID (UUID V4):
0


The prospect is in Denali National Park and Preserve.
Location: The Hillside or Silver King (Cobb, 1980 [OFR 80-363]) prospect is at the northwest foot of Quigley Ridge about 0.15 mile south of the mouth of Friday Gulch. The location is between a shaft at an elevation of about 1800 feet and a cut along Moose Creek at an elevation of about 1550 feet. The location is approximate but probably is accurate within 1000 feet. The Hillside prospect is included with the Red Top mine (MM118) in location 7 of Cobb (1972 [MF 366]) and location 6 of MacKevett and Holloway (1977).
Geology: The country rock in the area of the Hillside or Silver King prospect is probably metafelsite of the lower Paleozoic Spruce Creek sequence (Thornsberry, McKee, and Salisbury, 1984, fig. K-2). The Hillside vein was discovered in a 40-foot shaft sunk just west of the west end line of the Red Top claim (MM118), and presumably is an extension of the Red Top vein. The vein is 5 to 6 feet thick and and consists of quartz containing galena, possibly chalcopyrite and tetrahedrite, and probably some silver and gold. A possible extension of this vein on the west side of Moose Creek was uncovered during ground sluicing, but the cut had sloughed by 1921 (Davis, 1923, p. 123). The prospect was in litigation when it was visited by Davis; one claimant called the claim the Hillside; the other called it the Silver King.
Workings: The deposit was explored during or before 1922 by a 40-foot shaft and by sluicing and other surface work.
Age: The deposit is assumed to be Eocene (see record MM091).

Commodities (Major) - Ag(?), Au(?); (Minor) - Cu, Pb
Development Status: Undetermined.
Deposit Model: Polymetallic vein (Cox and Singer, 1986; model 22c).

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

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


Mineral List


3 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcopyrite ?2.CB.10aCuFeS2
Galena2.CD.10PbS
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
FeIron
Fe ChalcopyriteCuFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:MM123

Other Regions, Features and Areas containing this locality


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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