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Unnamed Occurrence (ARDF - MH088; east of Maclaren Glacier), Valdez Creek Mining District, Matanuska-Susitna Borough, Alaska, USAi
Regional Level Types
Unnamed Occurrence (ARDF - MH088; east of Maclaren Glacier)- not defined -
Valdez Creek Mining DistrictMining District
Matanuska-Susitna BoroughBorough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 19' 24'' North , 146° 30' 3'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
201207
Long-form identifier:
mindat:1:2:201207:3
GUID (UUID V4):
0


Location: This occurrence is on the east side of the Maclaren Glacier valley at about 4,250 feet elevation, in the SE1/4 section 25, T. 19 S., R. 6 E., Fairbanks Meridian. The location is approximate; it corresponds to locality A6 of Kurtak and others (1992), who gave a range of elevation of between 4,000 and 4,500 feet. The location is probably accurate within a quarter of a mile.
Geology: The rocks near the occurrence are schist, argillite, and slate of late Paleozoic protolith age (Nokleberg and others, 1991). Quartz-ankerite veins about 0.2 foot wide cut across the metamorphic structure. Quartz veins, as much as 0.3 foot wide, in zones as much as 30 feet thick, parallel schistosity. Sulfides are sparse; the rocks are locally stained with malachite, suggesting that chalcopyrite occurs locally in the quartz-ankerite veins (Kurtak and others, 1992, p. 92). Quartz and quartz-ankerite veins contain small concentrations of metals. Of six total samples collected at the site, five contained from 2 to 3 parts per million (ppm) silver; a malachite-stained quartz-carbonate vein contained 276 ppm copper and 80 parts per billion (ppb) gold. Another quartz vein contained 185 ppb gold. Antimony is slightly enriched; three of the six samples contain from 20 to 45 ppm antimony (Kurtak and others, 1992).
Workings: There are no workings. The veins were discovered during U.S. Bureau of Mines study of the area (Kurtak and others, 1992).
Age: Late Paleozoic or younger; possibly related to Cretaceous regional metamorphism (Nokleberg and others, 1982).
Alteration: Oxidation of iron- and copper-bearing minerals.

Commodities (Major) - Ag, Au; (Minor) - Cu, Sb
Development Status: None
Deposit Model: Low-sulfide Au-quartz veins (Cox and Singer, 1986; model 36a).

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
Chalcopyrite ?2.CB.10aCuFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Ankerite5.AB.10Ca(Fe2+,Mg)(CO3)2
Malachite5.BA.10Cu2(CO3)(OH)2

List of minerals for each chemical element

HHydrogen
H MalachiteCu2(CO3)(OH)2
CCarbon
C AnkeriteCa(Fe2+,Mg)(CO3)2
C MalachiteCu2(CO3)(OH)2
OOxygen
O AnkeriteCa(Fe2+,Mg)(CO3)2
O MalachiteCu2(CO3)(OH)2
O QuartzSiO2
MgMagnesium
Mg AnkeriteCa(Fe2+,Mg)(CO3)2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
CaCalcium
Ca AnkeriteCa(Fe2+,Mg)(CO3)2
FeIron
Fe AnkeriteCa(Fe2+,Mg)(CO3)2
Fe ChalcopyriteCuFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:MH088

Other Regions, Features and Areas containing this locality

North AmericaContinent
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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