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Unnamed Prospect (ARDF - SI189; north shore of Warm Springs Bay), Chichagof Mining District (Chicagof Mining District), Sitka, Alaska, USAi
Regional Level Types
Unnamed Prospect (ARDF - SI189; north shore of Warm Springs Bay)- not defined -
Chichagof Mining District (Chicagof Mining District)Mining District
SitkaCity Borough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
57° 5' 35'' North , 134° 48' 36'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Angoon456 (2017)47.6km
Mindat Locality ID:
202402
Long-form identifier:
mindat:1:2:202402:1
GUID (UUID V4):
aec0ae4c-9cc3-44ed-bef5-8ec576abbf06


Some of the deposit is probably within the townsite of Baranof that is private land. However, most of it is within the Tongass National Forest.
Location: This prospect is plotted near the site of Manleyville (which is shown on the 1:63,360-scale U.S. Geological Survey topographic map) on the north side of Warm Springs Bay. The prospect covers an area of about a square mile north of Manleyville. The occurrence is at the northeast corner of sec. 19, T. 55 S., R. 67 E. It is location P-113 of Bittenbender and others (1999) and MAS no. 0021140154 (U.S. Bureau of Land Management, 2002). The location is accurate.
Geology: This prospect is a porphyry copper deposit about a square mile in area that was first identified and staked by El Paso Natural Gas company in 1973. There apparently has been little or no further work by private industry but Bittenbender and others (1999) of the U.S. Bureau of Mines sampled extensively in the area. The rocks in the area are mostly part of a large Tertiary batholith that consists mainly of hornblende-biotite tonalite with subordinate hornblende-biotite granodiorite and garnet-muscovite-biotite trondhjemite (Loney and others, 1975). The northern part of the mineralized area borders on or extends into a mass of Triassic and Jurassic schist and gneiss about 3 miles long and 2 miles wide within the batholith. The deposit consists of: 1) disseminated sulfides in silicified tonalite; 2) pyrite and chalcopyrite at the edges of granodiorite inclusions; and 3) quartz veinlets with pyrite, chalcopyrite, and sphalerite in the tonalite. The mineralization is extensive but relatively low grade. Bittenbender and others (1999) collected 74 samples over the deposit; 20 representative samples of the deposit average 600 parts per million (ppm) copper and 85 ppm molybdenum. Samples of the quartz veinlets with sulfides gave higher values, the highest of which were 9,000 ppm copper, 1,650 ppm molybdenum, and 544 ppm bismuth. Gold and silver values were below detection or negligible in all samples.
Workings: Apparently only surface sampling.
Age: Tertiary or younger based on the age of the granodiorite host rocks.
Alteration: The granodiorite host rock is silicified and cut by quartz veinlets.

Commodities (Major) - Cu, Mo, Zn; (Minor) - Bi
Development Status: None
Deposit Model: Porphyry copper.

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 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S PyriteFeS2
S SphaleriteZnS
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS

Other Databases

Link to USGS - Alaska:SI189

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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