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Clipper; Cutter; Bendingo Prospects, Karta River Wilderness, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi
Regional Level Types
Clipper; Cutter; Bendingo ProspectsGroup of Prospects
Karta River WildernessWilderness Area
Prince of Wales IslandIsland
Ketchikan Mining DistrictMining District
Prince of Wales-Hyder Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
55° 31' 49'' North , 132° 40' 26'' West
Latitude & Longitude (decimal):
Type:
Group of Prospects
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Hollis112 (2011)3.8km
Thorne Bay483 (2017)19.9km
Klawock765 (2017)26.6km
Craig1,248 (2017)30.5km
Hydaburg391 (2017)37.2km
Mindat Locality ID:
196958
Long-form identifier:
mindat:1:2:196958:3
GUID (UUID V4):
0


These prospect are now in the Karta River Wilderness Area which is closed to exploration and mining.
Location: The only published location of the Clipper and Cutter prospects is on a small-scale map in Wright and Wright (1908). For this record, they are presumed to be 0.2 mile northeast of Granite Mountain and about 0.4 mile north-northeast of the center of section 20, T. 73 S., R. 84 E. The location of the Bendingo prospect is even more speculative; for lack of better information, it is grouped with the Clipper and Cutter prospects.
Geology: The deposit on the Cutter claim is a quartz vein with gold and sulfides (Wright and Wright, 1908). The sulfides are unspecified but the vein reportedly is similar to veins at the Flagstaff Mine (CR043) that contain chalcopyrite, galena, and pyrite. The quartz vein on the Clipper claim is 8 to 18 inches wide in an altered and decomposed diabase dike in granite (Wright and Wright, 1908). The Clipper vein was explored with surface stripping and short test adits. The deposit on the Bendingo claim is a quartz vein in granite; it contains free gold and sulfides, and is similar to the veins at the Flagstaff Mine. The rocks in the vicinity of these prospects are part of a large granodiorite-quartz diorite stock (Sainsbury, 1961; Eberlein and others, 1983; Brew, 1996). Early workers considered it to be Mesozoic or Cretaceous, but recent radiometric dating indicates that it is Devonian (S.M. Karl, oral communication, 2003).
Workings: Various combinations of surface stripping and short adits.
Age: Unknown, other than that the veins are in Devonian granitic rocks.

Commodities (Major) - Ag, Au, Cu, Pb
Development Status: None
Deposit Model: Gold-quartz vein (Cox and Singer, 1986; model 36a).

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


5 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
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S GalenaPbS
S PyriteFeS2
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
AuGold
Au Native GoldAu
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:CR036

Other Regions, Features and Areas containing this locality


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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