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Unnamed Prospects (ARDF - MC037; upper Roaring Creek), Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Unnamed Prospects (ARDF - MC037; upper Roaring Creek)- not defined -
Chistochina Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
61° 40' 59'' North , 143° 49' 51'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Mindat Locality ID:
202530
Long-form identifier:
mindat:1:2:202530:1
GUID (UUID V4):
c7d3e942-f3b7-461c-b1fc-d66057f8c532


The locality is in the Wrangell-Saint Elias National Park and Preserve.
Location: MacKevett and others (1978) identify several prospects in the upper valley of Roaring Creek. The location of this record is the more central of these prospects. It is at an elevation of about 4,900 feet, 3,700 feet northeast of elevation 7336 (Rock), and 2,400 feet east-northeast of the center of section 19, T. 2 S., R. 9 E. of the Copper River Meridian. This is locality 159 of MacKevett (1976) and locality 15 of MacKevett and others (1978). Cobb and MacKevett (1980) included these prospects under the name 'Roaring Cr.'.
Geology: The deposit at these prospects consist of thin veins that contain small amounts of chalcopyrite, bornite, chalcocite and malachite in Permian sedimentary rocks and Triassic gabbro (Moffit and Mertie, 1923; MacKevett, 1976). They veins were explored by short adits and open cuts. The widespread deposition of copper in Triassic greenstone and limestone of the area is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic or Early Cretaceous (MacKevett and others, 1997). Copper-bearing minerals were deposited in the underlying Nikolai Greenstone at about 112 Ma (Silberman and others, 1980).
Workings: The prospects were explored by short adits and open cuts that are now largely caved.
Age: Cretaceous? The widespread deposition of copper in Triassic greenstone and limestone of the area is thought to have accompanied regional deformation and low-grade metamorphism in the Late Jurassic or Early Cretaceous (MacKevett and others, 1997). Copper-bearing minerals were deposited in the underlying Nikolai Greenstone at about 112 Ma (Silberman and others, 1980).
Alteration: Oxidation.

Commodities (Major) - Cu
Development Status: None
Deposit Model: Basaltic Cu (Cox and Singer, 1986; model 23)

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
β“˜Chalcocite2.BA.05Cu2S
β“˜Bornite2.BA.15Cu5FeS4
β“˜Chalcopyrite2.CB.10aCuFeS2
Group 5 - Nitrates and Carbonates
β“˜Malachite5.BA.10Cu2(CO3)(OH)2

List of minerals for each chemical element

HHydrogen
Hβ“˜ MalachiteCu2(CO3)(OH)2
CCarbon
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ MalachiteCu2(CO3)(OH)2
SSulfur
Sβ“˜ BorniteCu5FeS4
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ ChalcociteCu2S
FeIron
Feβ“˜ BorniteCu5FeS4
Feβ“˜ ChalcopyriteCuFeS2
CuCopper
Cuβ“˜ BorniteCu5FeS4
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChalcociteCu2S
Cuβ“˜ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:MC037

Other Regions, Features and Areas containing this locality

North America
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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