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

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Latitude & Longitude (WGS84):
61° 37' 2'' North , 144° 8' 38'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Chitina126 (2017)19.3km
Mindat Locality ID:
196776
Long-form identifier:
mindat:1:2:196776:3
GUID (UUID V4):
0


This prospect is within the Wrangell-St. Elias National Park.
Location: This prospect is located near lower Benito Creek; it is at an elevation of 2,600 feet in the SE1/4 section 9, T. 3 S., R. 7 E., of the Copper River Meridian. This prospect is approximately located, perhaps to within 1 mile. It is locality 74 of Cobb and Matson (1972) and locality 59 of Winkler and others (1981 [OFR 80-892-B]). Cobb (1979 [OFR 79-1241]) incuded this prospect under the name 'Elliot Cr.'.
Geology: Quartz-calcite veins in mafic intrusive and metavolcanic rocks of the Paleozoic Skolai Group contain bornite, chalcopyrite, arsenopyrite, pyrite, and free gold. Secondary minerals include local malachite and azurite stains. The principal vein is 2 to 3 feet wide, strikes northwest, and dips steeply to the southeast (Moffit, 1921; Moffit and Mertie, 1923, p. 142-143). This vein has been traced over a distance of about 600 feet by five shallow holes and several open cuts produced by sluicing. It is extensively oxidized and gossanous at the surface. Other veins are present nearby, one of which may contain specular hematite. The Skolai Group is locally intruded by mafic to intermediate Jurassic plutons in this area. The veins postdate the Paleozoic Skolai Group and appear to postdate the Late Jurassic or Early Cretaceous deformation and metamorphism in the region (Winkler and others, 1981[OFR 80-892-A; MacKevett and others, 1997).
Workings: The principal vein at this prospect has been traced over a distance of about 600 feet by five shallow holes and several open cuts produced by sluicing.
Age: The veins postdate the Paleozoic Skolai Group and appear to postdate the Late Jurassic or Early Cretaceous deformation and metamorphism in the region (Winkler and others, 1981[OFR 80-892-B]; MacKevett and others, 1997).
Alteration: Oxidized; extensive development of iron oxides near the surface.

Commodities (Major) - Ag, Au, Cu
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
Native Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Arsenopyrite2.EB.20FeAsS
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 ArsenopyriteFeAsS
S ChalcopyriteCuFeS2
S PyriteFeS2
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ArsenopyriteFeAsS
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
AsArsenic
As ArsenopyriteFeAsS
AuGold
Au Native GoldAu

Other Databases

Link to USGS - Alaska:VA026

Other Regions, Features and Areas containing this locality

North AmericaContinent
North America PlateTectonic Plate

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