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Pika Canyon Prospect, Southeast Fairbanks Census Area, Alaska, USAi
Regional Level Types
Pika Canyon ProspectProspect
Southeast Fairbanks Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
63° 49' 47'' North , 141° 24' 35'' West
Latitude & Longitude (decimal):
Köppen climate type:
Mindat Locality ID:
199389
Long-form identifier:
mindat:1:2:199389:2
GUID (UUID V4):
0


Pika Canyon prospect is sometimes called Pitka Canyon, but Pitka is a misspelling of the name.
Location: The Pika Canyon prospect is located in sections 29, 30, 31, and 32, T.24 N., R. 21 E., of the Copper River Meridian, it covers about 2 square miles. It is location 7 of Singer and others (1976), and location 12 of Eberlein and others (1977). It lies directly west of the Fishhook prospect (TC009) and 3 miles south of Liberty Creek. The location is accurate to within 1/2 mile.
Geology: The geology at Pika Canyon consists of three main units: Precambrian or early Paleozoic gneiss and schist, Paleozoic phyllite and schist, and Tertiary mafic to felsic volcanic rocks. Many NE-trending faults as well as intense folding dominate the area (Gill, 1977). During 1974-1976, soil, rock chip, and stream-sediment sampling were conducted on the prospect by Cities Services Mineral Corp., as well as a ground magnetic survey on a 200- by 500-foot grid (Gill, 1977, p. 2). The soil samples showed anomalous values for copper, zoned in a pattern typical of porphyry-copper deposits in the southwest U.S. (Gill, 1977, p. 87). Pyrite, chalcopyrite, and possibly sphalerite were found in float samples (Gill, 1977). The alteration at Pika Canyon is patchy and somewhat irregular, but generally occurs in somewhat concentric zones of potassic, phyllic, and propylitic alteration (Gill, 1977, p. 86).
Workings: During 1974-1976, soil, rock chip, and stream-sediment sampling were conducted on the prospect, as well as a ground magnetic survey on a 200- by 500-foot grid (Gill, 1977, p. 2).
Age: Tertiary?
Alteration: The alteration at Pika Canyon is patchy and somewhat irregular, but generally occurs in somewhat concentric zones of potassic, phyllic, and propylitic alteration (Gill, 1977, p. 86).

Commodities (Major) - Cu
Development Status: None
Deposit Model: Porphyry Cu deposit (Cox and Singer, 1986; model 21a)

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
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Group 5 - Nitrates and Carbonates
Malachite5.BA.10Cu2(CO3)(OH)2

List of minerals for each chemical element

HHydrogen
H MalachiteCu2(CO3)(OH)2
CCarbon
C MalachiteCu2(CO3)(OH)2
OOxygen
O MalachiteCu2(CO3)(OH)2
SSulfur
S ChalcopyriteCuFeS2
S PyriteFeS2
S SphaleriteZnS
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu MalachiteCu2(CO3)(OH)2
ZnZinc
Zn SphaleriteZnS

Other Databases

Link to USGS - Alaska:TC023

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate
USA

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References

 
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