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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Unnamed Prospect (ARDF - IL046; east of head of Lake Fork of Paint River), Redoubt Mining District, Kenai Peninsula Borough, Alaska, USAi
Regional Level Types
Unnamed Prospect (ARDF - IL046; east of head of Lake Fork of Paint River)- not defined -
Redoubt Mining DistrictMining District
Kenai Peninsula BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
59° 14' 31'' North , 154° 29' 5'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Kokhanok170 (2015)27.5km
Newhalen182 (2017)58.0km
Mindat Locality ID:
202196
Long-form identifier:
mindat:1:2:202196:9
GUID (UUID V4):
0


Location: This prospect is at an elevation of about 1,600 feet, east of the head of Lake Fork and 1.35 miles west of hill 3169. The prospect is in the NW1/4 sec.10, T. 11 S., R. 31 W., Seward Meridian. The site corresponds to locality 17 of Detterman and Cobb (1972) and locality 17 of Reed (1967), and is accurate within about 0.5 mile.
Geology: The area of this prospect is underlain mainly by Jurassic, biotite-hornblende quartz diorite (Detterman and Reed, 1980). At the prospect, the quartz diorite intrudes hornblende gabbro (Reed, 1967). The prospect is a 100- to 150-foot-wide breccia zone in quartz diorite. The breccia is cut by a 0.5- to 2-foot-wide, malachite-stained fault zone and by many smaller, sulfide-rich, quartz(?) veins. The sulfides almost certainly include chalcopyrite and pyrite. Four of five grab samples of mineralized rock collected by Reed (1967) contained more than 0.5 percent copper. One grab sample assayed 11.9 parts per million (ppm) gold, 20 ppm silver, and more than 5,000 ppm copper. Selected sulfide-rich specimens from the mineralized fault zone yielded assays of more than 0.5 ounce of gold per ton (Reed, 1967; Cobb, 1976). The prospect was restaked in 1964, possibly for iron present as magnetite(?). A short, partly caved, adit found by Reed (1967) dates from an earlier period of exploration.
Workings: The prospect was explored by a short adit that was partly caved when visited by Reed (1967). The prospect area was restaked in 1964 during a flurry of exploration for iron on the Alaska Peninsula.
Age: Jurassic or younger.
Alteration: Oxidation of copper.

Commodities (Major) - Ag, Au, Cu; (Minor) - Fe?
Development Status: None
Deposit Model: Polymetallic vein? (Cox and Singer, 1986; model 22c).

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
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Malachite5.BA.10Cu2(CO3)(OH)2

List of minerals for each chemical element

HHydrogen
H MalachiteCu2(CO3)(OH)2
CCarbon
C MalachiteCu2(CO3)(OH)2
OOxygen
O MagnetiteFe2+Fe23+O4
O MalachiteCu2(CO3)(OH)2
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S PyriteFeS2
FeIron
Fe ChalcopyriteCuFeS2
Fe MagnetiteFe2+Fe23+O4
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:IL046

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.

References

Cobb, E.H., 1976, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Iliamna, Lake Clark, Lime Hills, and McGrath quadrangles, Alaska: U.S. Geological Survey Open-File Report 76-485, 101 p. Cobb, E.H., and Reed, B.L., 1981, Summaries of data on and lists of references to metallic and selected nonmetallic mineral occurrences in the Iliamna, Lake Clark, Lime Hills, and McGrath quadrangles, Alaska; Supplement to Open-File Report 76-485; Part A, Summaries to January 1, 1981: U.S. Geological Survey Open-File Report 81-1343-A, 25 p. Cobb, E.H., and Reed, B.L., 1981, Summaries of data on and lists of references to metallic and selected nonmetallic mineral occurrences in the Iliamna, Lake Clark, Lime Hills, and McGrath quadrangles, Alaska; Supplement to Open-File Report 76-485; Part B, Lists of references to Januray 1, 1981: U.S. Geological Survey Open-File Report 81-1343-B, 20 p. Detterman, R.L., and Cobb, E.H., 1972, Metallic mineral resources map of the Iliamna quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-364, 1 sheet, scale 1:250,000. Detterman, R.L., and Reed, B.L., 1980, Stratigraphy, structure, and economic geology of the Iliamna quadrangle, Alaska: U.S. Geological Survey Bulletin 1368-B, 86 p. MacKevett, E.M., Jr., and Holloway, C.D., 1977, Map showing metalliferous and selected non-metalliferous mineral deposits in the eastern part of southern Alaska: U.S. Geological Survey Open-File Report 77-169-A, 99 p., 1 sheet, scale 1:1,000,000. Reed, B.L., 1967, Results of stream sediment sampling and bedrock analyses in the eastern part of the Iliamna quadrangle, and at Kasna Creek, Lake Clark quadrangle, Alaska: U.S. Geological Survey Open-File Report 272, 18 p.
 
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