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Inspiration Point; Inspiration Mine Prospect, Skagway Mining District, Skagway, Alaska, USAi
Regional Level Types
Inspiration Point; Inspiration Mine ProspectProspect
Skagway Mining DistrictMining District
SkagwayCity Borough
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
59° 36' 0'' North , 135° 9' 36'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Skagway920 (2015)18.0km
Haines1,713 (2015)43.6km
Mud Bay212 (2011)50.4km
Mindat Locality ID:
198143
Long-form identifier:
mindat:1:2:198143:1
GUID (UUID V4):
9b8ae6dd-7e59-4080-8a87-7e7643c716d4


Location: This location corresponds to map location 52 of Gilbert and others (1990) and the location in Clough (1989 [BOM, v. 2, sec. C]), referred to as the Inspiration Mine. It is in the south-central part of section 23, T. 26 S., R. 60 E. of the Copper River Meridian. However, Cobb (1972 [MF 424]) shows this prospect on the White Pass-Yukon railroad about 0.6 miles south of the Alaska-Canada border and Gilbert and others (1990) located an Inspiration Mine at the 3,400 foot elevation near the west-central edge of section 26, T. 26 S., R. 60 E..
Geology: According to Clough (1989 [BOM, v. 2, sec. C]), the Inspiration Mine was probably discovered in the mid-1920's and was intermittently worked until its abandonment in the late 1930's. An 18-ton trial shipment of ore reportedly assayed 7.65% lead, 6.2% zinc, and 3.05 ounces of silver per ton. Local prospectors apparently restaked the property in 1988. The upper level of workings includes an inclined shaft, a vertical shaft, an open-cut, and a 165-foot adit. There is another adit about 200 feet below the upper level of workings. Mineralization occurs in skarn zones developed along sheared limestone within the Clifton Granite. At this locality, the Clifton Granite is actually a diorite. Mineralization is confined to the skarn zones and is not found in the diorite. This is probably the same as location 52 of Gilbert and others (1990) who described skarn, garnet skarn, diorite, and sheared diorite. Skarn samples contain up to 1,500 ppm copper, 7,200 ppm lead, and 24,000 ppm zinc. U-Pb zircon dates of 48 Ma for the Clifton Granite establish a maximum age for the mineralization (Clough, 1991 [BOM, v. 2, sec. C]; Gilbert and others, 1990).
Workings: Exploratory work was done annually from about 1926 to 1932 (Berg and Cobb, 1967).
Age: U-Pb zircon dates of 48 Ma for the Clifton Granite establish a maximum age for the deposit (Clough, 1991 [BOM, v. 2, sec. C); Gilbert and others, 1990).
Alteration: Skarn peripheral to a diorite intrusion.
Production: According to Clough (1991 [BOM, v. 2, sec. C], the Inspiration Mine was probably discovered in the mid-1920's and was intermittently worked until its abandonment in the late 1930's. An upper level of workings includes an inclined shaft, a vertical shaft, an open-cut, and a 165-foot adit. There is another adit about 200 feet below the upper level of workings. An 18-ton trial shipment of ore reportedly assayed 7.65% lead, 6.2% zinc, and 3.05 ounces of silver per ton. Local prospectors apparently restaked the property in 1988.

Commodities (Major) - Ag, Pb; (Minor) - Au, Cu, Zn
Development Status: Yes; small
Deposit Model: Skarn, contact metasomatic (Cox and Singer, 1986; model 18a or 19a).

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Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


1 valid mineral.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Galena2.CD.10PbS

List of minerals for each chemical element

SSulfur
S GalenaPbS
PbLead
Pb GalenaPbS

Other Databases

Link to USGS - Alaska:SK073

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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

Berg, H.C., 1984, Regional geologic summary, metallogenesis, and mineral resources of southeastern Alaska: U.S. Geological Survey Open-file Report 84-572, 298 p., 1 plate, scale 1:600,000. Berg, H.C., and Cobb, E.H., 1967, Metalliferous lode deposits of Alaska: U.S. Geological Survey Bulletin 1246, 254 p. Clough, A.H., and Redman, E.C., 1991, Bureau of Mines mineral investigations in the Juneau mining district, Alaska, 1984-1988, Volume 2, Detailed mine, prospect, and mineral occurrence descriptions, Section C, West Lynn Canal subarea: U.S. Bureau of Mines of Mines Special Publication, 44 p. Cobb, E.H., 1972, Metallic mineral resources map of the Skagway quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map MF-424, 1 sheet, scale 1:250,000. Cobb, E.H., 1978, Summary of references to mineral occurrences (other than mineral fuels and construction materials) in the Mt. Fairweather and Skagway quadrangles, Alaska: U.S. Geological Survey Open-File Report 78-316, 123 p. Gilbert, W.G., Clough, A.H., Burns, L.E., Kline, J.T., Redman, E.C., and Fogels, E.J., 1990, Reconnaissance geology and geochemistry of the northeast Skagway quadrangle, Alaska: Alaska Division of Geological and Geophysical Surveys Report of Investigations 90-5, 2 sheets, scale 1:125,000. Herbert, C.F., and Race, W.H., 1964, Geochemical investigations of selected areas in southeastern Alaska, 1964: Alaska Division of Mines and Minerals Geochemical Report 1, 75 p. Smith, P.S., 1929, Mineral industry of Alaska in 1926: U.S. Geological Survey Bulletin 797, p. 1-50. Smith, P.S., 1930, Mineral industry of Alaska in 1927: U.S. Geological Survey Bulletin 810-A, p. 1-64.
 
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