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Blue Bird Prospect, Chistochina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Blue Bird ProspectProspect
Chistochina Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
61° 39' 42'' North , 144° 1' 51'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Chitina126 (2017)27.0km
Mindat Locality ID:
196548
Long-form identifier:
mindat:1:2:196548:6
GUID (UUID V4):
0


This prospect is within the Wrangell-St. Elias National Park.
Location: This prospect is on the crest of the divide between the upper Middle Fork and East Fork Copper Creek (Val Alstine and Black, 1946, plate 30); it is at an elevation of about 5,300 feet nearly in the center of the S1/2 section 30, T. 2 S., R. 8 E., of the Copper River Meridian. This prospect is approximately located, probably to within one-quarter mile. It is included in locality 72 of Cobb and Matson (1972) and locality 58 of Winkler and others (1981 [OFR 80-892-B]).
Geology: Triassic Nikolai Greenstone is cut by shear zones that contain calcite-epidote veinlets and small amounts of pyrite, bornite, and enargite. These sulfides are also disseminated in small grains (Van Alstine and Black, 1946). This prospect was explored by two open cuts, and about 100 pounds of hand-sorted bornite and enargite were left near each cut. A polished section of this material showed covellite inclusions in enargite. Chalcocite occurs on the borders of bornite grains, as veinlets in bornite, and as irregular patches replacing bornite (Van Alstine and Black, 1946). The copper mineralization is believed to be related to the regional mineralizing event that produced the rich Kennecott copper deposits in the McCarthy quadrangle (MacKevett and others, 1997).
Workings: Van Alstine and Black (1946) reported that two open cuts explored this prospect.
Age: The copper mineralization is believed to be related to the mineralizing event that produced the rich Kennecott copper deposits in the McCarthy quadrangle to the east (MacKevett and others, 1997). This event is interpreted to have accompanied Late Jurassic or Early Cretaceous deformation and metamorphism (MacKevett and others, 1997, p. 88).

Commodities (Major) - Au, Cu
Development Status: None
Deposit Model: Veins, disseminations, and fracture fillings in greenstone; probably related to

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


8 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Chalcocite2.BA.05Cu2S
Bornite2.BA.15Cu5FeS4
Covellite2.CA.05aCuS
Chalcopyrite2.CB.10aCuFeS2
Enargite2.KA.05Cu3AsS4
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Malachite5.BA.10Cu2(CO3)(OH)2
Group 9 - Silicates
Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)

List of minerals for each chemical element

HHydrogen
H Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
H MalachiteCu2(CO3)(OH)2
CCarbon
C CalciteCaCO3
C MalachiteCu2(CO3)(OH)2
OOxygen
O CalciteCaCO3
O Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
O MalachiteCu2(CO3)(OH)2
AlAluminium
Al Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SiSilicon
Si Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SSulfur
S BorniteCu5FeS4
S ChalcopyriteCuFeS2
S ChalcociteCu2S
S CovelliteCuS
S EnargiteCu3AsS4
CaCalcium
Ca CalciteCaCO3
Ca Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
FeIron
Fe BorniteCu5FeS4
Fe ChalcopyriteCuFeS2
Fe Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
CuCopper
Cu BorniteCu5FeS4
Cu ChalcopyriteCuFeS2
Cu ChalcociteCu2S
Cu CovelliteCuS
Cu EnargiteCu3AsS4
Cu MalachiteCu2(CO3)(OH)2
AsArsenic
As EnargiteCu3AsS4

Other Databases

Link to USGS - Alaska:VA038

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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