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Matilda & House prospects, Dolomi Mountain, Prince of Wales Island, Ketchikan Mining District, Prince of Wales-Hyder Census Area, Alaska, USAi
Regional Level Types
Matilda & House prospectsGroup of Prospects
Dolomi MountainMountain
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° 8' 53'' North , 132° 3' 7'' West
Latitude & Longitude (decimal):
Type:
Group of Prospects
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Metlakatla1,405 (2017)30.4km
Ketchikan8,197 (2017)33.5km
Saxman417 (2017)34.6km
Mindat Locality ID:
198780
Long-form identifier:
mindat:1:2:198780:8
GUID (UUID V4):
0


Location: This site is arbitrarily plotted in the middle of James Lake, in the SE¼ sec. 31, T77S, R89E, about 1.4 km (4,400 feet) E of Dolomi Mountain. These prospects were briefly described by Brooks (1902), who did not give good locations, and they have not been described since. The Matilda claim is north of the Fortune (CR 205) claim, which is south of James Lake. The House claim is about a mile north of Dolomi. The Matilda and House claims are probably within 0.5 mile of James Lake.

Geology: The only published descriptions of the Matilda and House claims are by Brooks (1902). The deposit on the Matilda claim is a quartz vein 3 feet thick that strikes east and dips 60S. The vein is in sheared mica schist; it contains pyrite and 'is said to carry gold.' The deposit on the House claim is a quartz vein 1 to 2 feet thick that cuts marble. The vein, which is exposed in a small pit, strikes N15E and dips 30NW; it contains (minor?) pyrite, chalcopyrite, and tetrahedrite. The rocks in the Dolomi area are part of the Wales Group of Late Proterozoic and Cambrian age (Herreid, 1967). They are folded into a large dome centered over the eastern third of Paul Lake, and consist of several marble layers 200 to 1300 feet thick, interbedded with calcareous chlorite schist and marble.

Workings: Probably only surface pits.

Age: The vein is younger than the Late Proterozoic or Cambrian host rocks.

Commodities (Major) - Au; (Minor) - Cu, Sb

Development Status: None

Deposit Model: Low-sulfide, brecciated 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
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
'Tetrahedrite Subgroup'2.GB.05Cu6(Cu4C2+2)Sb4S12S
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 Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S
SbAntimony
Sb Tetrahedrite SubgroupCu6(Cu4C22+)Sb4S12S

Other Databases

Link to USGS - Alaska:CR196

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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