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Veta Prospect, Mallard Bay, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi
Regional Level Types
Veta ProspectProspect
Mallard BayBay
Prince of Wales IslandIsland
Ketchikan Mining DistrictMining District
Prince of Wales-Hyder Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
54° 47' 5'' North , 132° 1' 26'' West
Latitude & Longitude (decimal):
KΓΆppen climate type:
Nearest Settlements:
PlacePopulationDistance
Metlakatla1,405 (2017)47.7km
Mindat Locality ID:
202777
Long-form identifier:
mindat:1:2:202777:0
GUID (UUID V4):
3dee80c3-6c76-469c-8afd-846d915daecc


Location: The Veta prospect is about 0.2 mile northwest of the head of Mallard Bay, and about 0.2 mile south of the center of section 6, T. 82 S, R. 90 E. (The Veta prospect is often included with the Polson and Ickis prospects (DE039) in early reports).
Geology: The rocks in the area are Silurian or Ordovician quartz monzonite, syenite, and quartz diorite that are part of a batholith that makes up the southeastern tip of Prince of Wales Island (Gehrels, 1992). There are several prominent northwest-trending faults near the prospect. The workings consist of two flooded vertical shafts, one 30 feet deep and the other 78 feet deep, and about 78 feet of drifts and crosscuts (Knopf, 1910; MacKevett, 1963; Maas and others, 1991). The working are in fine-grained diorite along a fault zone about 3 feet wide that strikes N50W and dips 80NE. The fault zone and its wallrocks are pervasively altered to secondary iron minerals and clay. Quartz veins in the fault contain pyrite and chalcopyrite, along with less-abundant bornite, malachite(?), chrysocolla, and hematite. The sulfides are also disseminated through the wall rocks. Maas and others (1991) collected several samples from rubble crop and dumps that contained 1,833 parts per million (ppm) to 6.41 percent copper, 5.6 to 25.7 ppm silver, and 94 to 7,258 parts per billion gold.
Workings: The workings consist of two flooded vertical shafts, one 30 feet deep and the other 78 feet deep, and about 78 feet of drifts and crosscuts.
Age: The vein cuts Silurian or Ordovician granitic rocks.
Alteration: Pervasive alteration of the fault zone and granitic wall rocks to secondary iron oxides and clay minerals.

Commodities (Major) - Ag, Au, Cu
Development Status: None
Deposit Model: Quartz vein with copper, gold, and silver values. (Cox and Singer, 1986; model

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


7 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Bornite2.BA.15Cu5FeS4
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
β“˜Hematite4.CB.05Fe2O3
β“˜Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
β“˜Malachite5.BA.10Cu2(CO3)(OH)2
Group 9 - Silicates
β“˜Chrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 Β· nH2O, x < 1

List of minerals for each chemical element

HHydrogen
Hβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hβ“˜ MalachiteCu2(CO3)(OH)2
CCarbon
Cβ“˜ MalachiteCu2(CO3)(OH)2
OOxygen
Oβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oβ“˜ HematiteFe2O3
Oβ“˜ MalachiteCu2(CO3)(OH)2
Oβ“˜ QuartzSiO2
AlAluminium
Alβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
SiSilicon
Siβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siβ“˜ QuartzSiO2
SSulfur
Sβ“˜ BorniteCu5FeS4
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ PyriteFeS2
FeIron
Feβ“˜ BorniteCu5FeS4
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ HematiteFe2O3
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ BorniteCu5FeS4
Cuβ“˜ ChalcopyriteCuFeS2
Cuβ“˜ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuβ“˜ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS - Alaska:DE040

Other Regions, Features and Areas containing this locality


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