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Unnamed Occurrence (ARDF - SR257; east side of Knight Island), Prince William Sound Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - SR257; east side of Knight Island)- not defined -
Prince William Sound Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
60° 17' 2'' North , 147° 42' 28'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201734
Long-form identifier:
mindat:1:2:201734:4
GUID (UUID V4):
0


Location: The occurrence is located near tidewater, about 3 miles southwest of the mouth of Marsha Bay. It is in the NW1/4 section 10, T. 2 N., R. 10 E., of the Seward Meridian. This is location 141 of MacKevett and Holloway (1977), location 239 of Cobb and Tysdal (1980), and location S-41 of Jansons and others (1984). This location is accurate to within a quarter of a mile.
Geology: The country rock is slate, graywacke, and greenstone of the Orca Group of early Teriary age (Nelson and others, 1985). Greenstone encloses slate lenses less than 50 feet long and more than 20 feet wide. These lenses contain as much as 1 percent chalcopyrite. A 25-foot-wide tuffaceous zone in the greenstone contains as much as 5 percent chalcopyrite (Kurtak and Jeske, 1986). A greenstone-slate breccia zone with a quartz matrix contained a trace of chalcopyrite. Tysdal (1978 [MF-880-A]) reported one mineralized zone, 7.5 meters wide and 9 meters long, containing quartz, chalcopyrite, pyrrhotite, and sphalerite. A 20-foot-wide random chip sample of a 20-foot-wide mineralized slate lens contained 480 ppm copper and 580 ppm zinc. A 25-foot-wide random chip sample of the tuffaceous zone contained 0.24 percent copper and 1.1 percent zinc (Kurtak and Jeske, 1986). The greenstone-slate breccia zone was not sampled.
Workings: A 20-foot-wide random chip sample of the mineralized slate unit contained 480 ppm copper and 580 ppm zinc. A 25-foot-wide random chip sample of the tuffaceous zone contained 0.24 percent copper and 1.1 percent zinc (Kurtak and Jeske, 1986). The greenstone-slate breccia zone was not sampled. No workings or improvements are reported.
Age: Tertiary or younger; the occurrence is in rocks of the Orca Group of Tertiary age.
Alteration: Greenstone is altered basalt.

Commodities (Major) - Cu, Zn
Development Status: None
Deposit Model: Besshi massive sulfide (Cox and Singer, 1986; model 24b)

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


4 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
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 PyrrhotiteFe1-xS
S SphaleriteZnS
FeIron
Fe ChalcopyriteCuFeS2
Fe PyrrhotiteFe1-xS
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS

Other Databases

Link to USGS - Alaska:SR257

Other Regions, Features and Areas containing this locality

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.

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