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Greek Boy; Rusty Lode Prospect, Juneau Mining District, Juneau, Alaska, USAi
Regional Level Types
Greek Boy; Rusty Lode ProspectProspect
Juneau Mining DistrictMining District
JuneauCity Borough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
58° 51' 30'' North , 134° 59' 56'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Mud Bay212 (2011)39.8km
Haines1,713 (2015)49.1km
Mindat Locality ID:
197807
Long-form identifier:
mindat:1:2:197807:3
GUID (UUID V4):
39b85d39-3296-4648-821a-0b944cf133ba


Location: The Greek Boy prospect is at an elevation of 200 feet, about 4 miles north of the mouth of the Berners River where it empties into Berners Bay, 2 miles northeast of the Jualin mine (JU044), and 4 miles due east of the Kensington mine (JU029). It is in the SE1/4 section 1, T. 35 S., R. 62 E. of the Copper River Meridian. The location is accurate. There are several open cuts 1 mile north-northwest of the Greek Boy that have been considered part of the Greek Boy prospect (Redman and others, 1989), but due to the large distance from the main workings they are described separately (ARDF JU023).
Geology: The Greek Boy deposit was discovered prior to 1889 and developed by 3 adits and a winze totaling 1,287 feet (Redman and others, 1989). Roehm (1938 [PE 112-14]) describes the deposit as a more or less continuous stringer lode in a narrow schist band 8 to 20 feet wide that is along the contact of quartz diorite gneiss and metabasalt. The contact varies in strike from N 26-40 W and dips slightly off vertical to the southwest; it can be traced across the entire length of the claims. Roehm (1938 [PE 112-14]) reports gold values up to 4.1 ppm over 6 feet. U.S. Bureau of Mines samples contain up to 0.4 ppm gold (Redman and others, 1989). Roehm calculated a resource of 100,400 tons of ore that contain 0.05 ounce of gold per ton for the Greek Boy deposit. The Greek Boy prospect is in the Berners Bay district at the north end of the Juneau Gold Belt. The district is characterized by a series of structurally-controlled, mesothermal gold-bearing quartz veins. Most of the veins are in Early Cretaceous (105 Ma) Jualin Diorite, which intrudes Mesozoic (Upper Triassic) metabasalt. The age of mineralization in the Berners Bay district is about 55 Ma, the same as the other mesothermal gold vein deposits in the Juneau Gold Belt (Goldfarb and others, 1997).
Workings: The Greek Boy deposit was discovered prior to 1889 and developed by 3 adits and a winze totaling 1,287 feet (Redman and others, 1989).
Age: The age of mineralization in the Berners Bay district is about 55 Ma, the same as the other mesothermal gold-quartz-vein deposits in the Juneau Gold Belt (Goldfarb and others, 1997).
Reserves: Roehm (1938 [PE 112-14]) calculated a resource for the Greek Boy prospect of 100,400 tons of ore that contain 0.05 ounce of gold per ton.

Commodities (Major) - Ag, Au, Cu
Development Status: None
Deposit Model: Low-sulfide Au-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 1 - Elements
Gold1.AA.05Au
Group 2 - Sulphides and Sulfosalts
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 PyriteFeS2
FeIron
Fe PyriteFeS2
AuGold
Au GoldAu

Other Databases

Link to USGS - Alaska:JU035

Other Regions, Features and Areas containing this locality

North America
North America PlateTectonic Plate

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References

 
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