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Jim Creek Occurrence, Anchorage Mining District, Matanuska-Susitna Borough, Alaska, USAi
Regional Level Types
Jim Creek OccurrenceOccurrence
Anchorage Mining DistrictMining District
Matanuska-Susitna BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
61° 34' 11'' North , 148° 48' 0'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Lazy Mountain1,479 (2011)9.9km
Butte3,246 (2011)12.7km
Knik River744 (2011)13.6km
Palmer6,788 (2017)17.0km
Farm Loop1,028 (2011)19.7km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Mat-Su Rock and Mineral ClubPalmer, Alaska17km
Mindat Locality ID:
198221
Long-form identifier:
mindat:1:2:198221:6
GUID (UUID V4):
0


Location: Prospect is located 1.5 mile downstream from the headwaters of Jim Creek at a point roughly 1,500 ft north of the creek . Location accurate within 1 mile. Locality 45 of Cobb (1972), and locality 34 of MacKevett and Holloway (1977).
Geology: Heavily silicified greenstone is cut by a vein that averages 1 ft thick. The vein strikes N 80 W, and is approximately vertical. The vein is composed of 40 percent chalcopyrite, 40 percent pyrrhotite, 15 percent sphalerite, and 5 percent calcite; and assays show 15.08 percent Cu, 2.95 percent Zn, 1.75 oz/ton Ag, and trace Au. The greenstone on both sides of the sulfide vein has been replaced by quartz and calcite, and cut by very thin arsenopyrite veins. Assays of replaced wall rock show 0.41 oz/ton Ag and 0.04 percent Cu. An alaskite dike runs approximately 500 ft upslope the sulfide vein prospect and slate outcrops 50 ft downhill from prospect (Landes, 1927).
Workings: The vein is composed of 40 percent chalcopyrite, 40 percent pyrrhotite, 15 percent sphalerite, and 5 percent calcite; and assays show 15.08 percent Cu, 2.95 percent Zn, 1.75 oz/ton Ag, and trace amounts of Au. Assays of replaced wall rock show 0.41 oz/ton Ag and 0.04 percent Cu (Landes, 1927).
Age: Mesozoic or younger
Alteration: Calcite and quartz replacement of greenstone at periphery of sulfide vein.

Commodities (Major) - Ag, Cu, Zn; (Minor) - Au
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


6 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
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3

List of minerals for each chemical element

CCarbon
C CalciteCaCO3
OOxygen
O CalciteCaCO3
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ArsenopyriteFeAsS
S ChalcopyriteCuFeS2
S PyrrhotiteFe1-xS
S SphaleriteZnS
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ArsenopyriteFeAsS
Fe ChalcopyriteCuFeS2
Fe PyrrhotiteFe1-xS
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS
AsArsenic
As ArsenopyriteFeAsS

Other Databases

Link to USGS - Alaska:AN087

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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