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Latitude & Longitude (WGS84):
55° 37' 45'' North , 132° 1' 30'' West
Latitude & Longitude (decimal):
Type:
Group of Prospects
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Thorne Bay483 (2017)31.8km
Ketchikan8,197 (2017)39.8km
Saxman417 (2017)43.9km
Mindat Locality ID:
198001
Long-form identifier:
mindat:1:2:198001:4
GUID (UUID V4):
0


Location: This site is about at the center of three old prospects with similar geology--the Alexander, Hoffman, and Melville--in an area of about one-quarter square mile. The site is about 2.2 miles north-northwest of the mouth of Smugglers Creek, near the center of the NE1/4 section 14, T. 72 S., R. 87 E.

Geology: This site consist of a group of three neighboring prospects--Alexander, Hoffman, and Melville--that date from before WWI and have similar geology (Wright and Wright, 1908). At the Alexander prospect, a 45-foot tunnel exposes a quartz vein 6 inches to 3 feet wide that strikes north and dips 45W; it intersects the schistosity of folded greenstone and slate. At the Hoffman prospect, an irregular quartz vein about 5 feet thick strikes N5W and dips steeply west. It is exposed in a 21-foot tunnel in faulted greenstone and schist. Minor pyrite occurs in the quartz vein and in the wallrock. At the Melville prospect, a quartz vein cuts folded and faulted slate and greenstone. A little ore was mined from a short tunnel and treated in an arrastre. The deposit at the Melville prospect is unusual in the Helm Bay district because it contains arsenopyrite rather than pyrite in the quartz vein and wallrock. There is no indication of any exploration on any of these prospects since before WWI. The best of several recent samples of these prospects contained 2,642 parts per billion gold across 5 inches of mineralization (Bittenbender and others, 1993; Maas and others, 1995). The rocks in the area consist of metamorphosed andesite, basalt, agglomerate, and tuff, and minor flysch, shale, and phyllite. Eberlein and others (1983) and Brew (1996) consider them to be Paleozoic or Mesozoic in age; Gehrels and Berg (1992) tentatively mapped them as Jurassic or Cretaceous.

Workings: Each of these three prospects was explored by short adits, the longest 45 feet long, that were driven prior to 1908.

Age: The quartz veins cut country rocks that may be as young as Cretaceous or as old as Paleozoic.

Production: No production from the Alexander and Hofman prospects; the Melville produced a small amount of ore prior to 1908 that was treated in a local arrastre.

Reserves: None.

Commodities (Major) - Au

Development Status: Yes; small

Deposit Model: Low-sulfide 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


3 valid minerals.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Pyrite2.EB.05aFeS2
Arsenopyrite2.EB.20FeAsS
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2

List of minerals for each chemical element

OOxygen
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ArsenopyriteFeAsS
S PyriteFeS2
FeIron
Fe ArsenopyriteFeAsS
Fe PyriteFeS2
AsArsenic
As ArsenopyriteFeAsS

Other Databases

Link to USGS - Alaska:CR077

Other Regions, Features and Areas containing this locality

North America
North America PlateTectonic Plate

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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