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Christmas and Enterprise Prospect (Whitney claims), Lemesurier Island, Chichagof Mining District (Chicagof Mining District), Hoonah-Angoon Census Area, Alaska, USAi
Regional Level Types
Christmas and Enterprise Prospect (Whitney claims)Prospect
Lemesurier IslandIsland
Chichagof Mining District (Chicagof Mining District)Mining District
Hoonah-Angoon Census AreaCensus Area
AlaskaState
USACountry

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Latitude & Longitude (WGS84):
58° 15' 28'' North , 136° 5' 48'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Gustavus434 (2017)27.2km
Mindat Locality ID:
196917
Long-form identifier:
mindat:1:2:196917:0
GUID (UUID V4):
0


Two patented claims, inactive for many years. Favorable area for skarn and porphyry-type molybdenum-copper deposits. The area is in Tongass National Forest, outside of Glacier Bay National Park and Preserve. It appears to be open for mineral location.

Location:
The prospect is about 50 feet above sea level near the southernmost point on Lemesurier Island, about 0. 2 mile west of triangulation station Gail. It is located accurately within about 0.1 mile. It is location 61 of Cobb (1972).

Geology:
Molybdenum and copper occur in contact-type deposits in marble of Paleozoic age that has been intruded by a granitic pluton of probable Cretaceous age. At the Whitney claims, a thirty-foot-wide zone along a contact between marble and granitic rock is mainly garnet-pyroxene tactite. A 78-foot adit driven in about 1916, started in tactite, cut through banded hornfels and quartzite, and ended in 'diorite'. Molybdenite occurs as fracture coatings and as disseminations in the tactite. Hornfels is developed locally and contains chalcopyrite. Local molybdenite-lined vugs or pockets in the tactite contain as much as several percent molybdenum.

Workings:
Surface exposures of molybdenite and chalcopyrite were explored in a 78-foot-long tunnel and 25-foot-crosscut, that were driven in about 1916. The occurrence was first reported by Knopf in 1912 and subsequently described in resource summaries by several researchers. It was visited by Reed in 1938, and in 1942, Smith summarized developments and also reported that Reed believed the prospect deserved more work.

Age:
Cretaceous or younger.

Alteration:
Development of hornfels and tactite.

Production:
Small test shipments made.

Commodities:
(Major) - Mo; (Minor) - Cu

Development Status:
None.

Deposit Model:
Contact metasomatic deposit, molybdenum skarn.

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
Chalcopyrite2.CB.10aCuFeS2
Molybdenite2.EA.30MoS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3

List of minerals for each chemical element

CCarbon
C CalciteCaCO3
OOxygen
O CalciteCaCO3
O QuartzSiO2
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S MolybdeniteMoS2
CaCalcium
Ca CalciteCaCO3
FeIron
Fe ChalcopyriteCuFeS2
CuCopper
Cu ChalcopyriteCuFeS2
MoMolybdenum
Mo MolybdeniteMoS2

Other Databases

Link to USGS - Alaska:MF079

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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