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Unnamed Prospect (ARDF - NB009; northwest head of Caribou Creek), Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Unnamed Prospect (ARDF - NB009; northwest head of Caribou Creek)- not defined -
Chistochina Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
62° 37' 14'' North , 143° 27' 0'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Mentasta Lake112 (2011)37.1km
Mindat Locality ID:
202305
Long-form identifier:
mindat:1:2:202305:5
GUID (UUID V4):
0


The prospect is in the Wrangell-St. Elias National Preserve.
Location: This prospect is in the headwaters of an unnamed north tributary to Caribou Creek. It is an an elevation of about 4,800 feet, 3,200 feet northwest of elevation 5620, and 3,000 feet south-southeast of elevation 6240. The site is in the NE1/4 of section 25, T. 10 N., R.10 E. of the Copper River Meridian. This is locality 1 of Richter and Schmoll (1973), locality 5 of Richter and others (1975), and National Park Service locality WRST-2 (unpublished data). It is located to within a few hundred feet.
Geology: Gold occurs in 1/4- to 2 -inch-thick stringers of quartz, calcite, pyrite, galena, and sphalerite that are localized in a zone 6 to 12 inches wide that cuts dioritized volcanic rocks. An adit was driven N 65 E to crosscut the zone which is near an 8-foot-wide trachyte dike that strikes N 55 W and dips 45 NE (Moffit, 1954). The volcanic rocks are part of the Pennsylvanian-Permian Tetelna Volcanics that are intruded by a diorite gneiss complex within 500 feet of the prospect (Matson and Richter, 1971 [OFR 71-204]; Richter and Schmoll, 1973; Richter, 1976). K/Ar ages from the diorite complex indicate that it is Early Jurassic or older (Richter. Lanphere, and Matson, 1975).
Workings: An adit was driven N 65 E to crosscut the mineralized zone. It was caved by the early 1950s (Moffit, 1954).
Age: Early Jurassic or younger? This prospect is in the border zone of a large diorite complex that is Early Jurassic or older (Richter, Lanphere, and Matson, 1975).

Commodities (Major) - Au, Pb, Zn
Development Status: Undetermined.
Deposit Model: Polymetallic veins (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 1 - Elements
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
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 GalenaPbS
S PyriteFeS2
S SphaleriteZnS
CaCalcium
Ca CalciteCaCO3
FeIron
Fe PyriteFeS2
ZnZinc
Zn SphaleriteZnS
AuGold
Au GoldAu
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:NB009

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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