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Spirit Mountain Prospect, Nizina Mining District, Valdez-Cordova Census Area, Alaska, USAi
Regional Level Types
Spirit Mountain ProspectProspect
Nizina Mining DistrictMining District
Valdez-Cordova Census AreaCensus Area
AlaskaState
USACountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
61° 18' 20'' North , 144° 15' 50'' West
Latitude & Longitude (decimal):
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Chitina126 (2017)25.1km
Mindat Locality ID:
200104
Long-form identifier:
mindat:1:2:200104:6
GUID (UUID V4):
817c4f89-9931-47a9-86e5-5fc2fb532f27


This prospect is in Wrangell-St. Elias National Park.
Location: This prospect is on the west side of upper Canyon Creek valley about 1.8 miles southwest of the west end of summit Lake and nine-tenths of a mile southeast of elevation 5,990. It is at an elevation of 4,000 feet near center of the east boundary of section 35, T. 6 S., R. 6 E., of the Copper River Meridian. This prospect is probably located to within one-quarter mile. It is locality 61 of Cobb and Matson (1972) and locality 52 of Winkler and others (1981 [OFR 80-892-B]).
Geology: Mafic and ultramafic sill-like bodies that intrude metasedimentary rocks of the Haley Creek terrane contain disseminations and segregations of bravoite, chalcopyrite, pentlandite, pyrite, pyrrhotite, and sphalerite (Kingston and Miller, 1945; Herried, 1970; Winkler and others, 1981 [OFR 80-892-B]; Winkler and others, 1981
Workings: This prospect was explored by a large open cut, numerous test pits, and a 50-foot long adit (Moffit, 1914; Pierce, 1946).
Age: Not known; the protolith ages of metasedimentary and metaplutonic rocks in the Haley Creek terrane are not known but much deformation and recrystallization probably occurred in the mid-Cretaceous or younger (Winkler and others, 1981 [OFR 80-892-A]).
Alteration: The ultramafic host rocks are extensively altered to various assemblages of antigorite, chlorite, epidote, hornblende, limonite, magnetite, serpentine, tremolite, and talc.
Reserves: One mineralized body is 200 feet long, 1 inch to 22 feet thick, and exposed over 150 feet vertically. Another mineralized body is 45 feet long; it is 3 feet thick at the surface, but it pinches down to a 6-inch thickness within 10 feet of the surface (Kingston and Miller, 1945). The resource in these two bodies is 6,500 tons of material that contains 0.22 to 7.61 percent nickel and 0.12 to 1.56 percent copper (Kingston and Miller, 1945, p. 56).

Commodities (Major) - Cu, Ni; (Minor) - Ag, Co, PGE, Zn
Development Status: None
Deposit Model: Duluth Cu-Ni-PGE? (Cox and Singer, 1986; model 5a)

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


10 valid minerals.

Detailed Mineral List:

Antigorite
Formula: Mg3(Si2O5)(OH)4
Chalcopyrite
Formula: CuFeS2
'Chlorite Group'
Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
'Hornblende Root Name Group'
Formula: ◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
'Limonite'
Magnetite
Formula: Fe2+Fe3+2O4
Pentlandite
Formula: (NixFey)Σ9S8
Pyrite
Formula: FeS2
Pyrite var. Bravoite
Formula: (Fe,Ni)S2
Pyrrhotite
Formula: Fe1-xS
'Serpentine Subgroup'
Formula: D3[Si2O5](OH)4
Sphalerite
Formula: ZnS
Talc
Formula: Mg3Si4O10(OH)2
Tremolite
Formula: ◻Ca2Mg5(Si8O22)(OH)2

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
Pentlandite2.BB.15(NixFey)Σ9S8
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
Pyrite
var. Bravoite
2.EB.05a(Fe,Ni)S2
2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Group 9 - Silicates
Epidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Tremolite9.DE.10◻Ca2Mg5(Si8O22)(OH)2
Talc9.EC.05Mg3Si4O10(OH)2
Antigorite9.ED.15Mg3(Si2O5)(OH)4
Unclassified
'Chlorite Group'-
'Limonite'-
'Hornblende Root Name Group'-◻Ca2(Z2+4Z3+)(AlSi7O22)(OH,F,Cl)2
'Serpentine Subgroup'-D3[Si2O5](OH)4

List of minerals for each chemical element

HHydrogen
H AntigoriteMg3(Si2O5)(OH)4
H Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
H TalcMg3Si4O10(OH)2
H Tremolite◻Ca2Mg5(Si8O22)(OH)2
H Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
H Serpentine SubgroupD3[Si2O5](OH)4
OOxygen
O AntigoriteMg3(Si2O5)(OH)4
O Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
O MagnetiteFe2+Fe23+O4
O TalcMg3Si4O10(OH)2
O Tremolite◻Ca2Mg5(Si8O22)(OH)2
O Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
O Serpentine SubgroupD3[Si2O5](OH)4
FFluorine
F Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
MgMagnesium
Mg AntigoriteMg3(Si2O5)(OH)4
Mg TalcMg3Si4O10(OH)2
Mg Tremolite◻Ca2Mg5(Si8O22)(OH)2
AlAluminium
Al Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Al Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
SiSilicon
Si AntigoriteMg3(Si2O5)(OH)4
Si Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Si TalcMg3Si4O10(OH)2
Si Tremolite◻Ca2Mg5(Si8O22)(OH)2
Si Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
Si Serpentine SubgroupD3[Si2O5](OH)4
SSulfur
S Pyrite var. Bravoite(Fe,Ni)S2
S ChalcopyriteCuFeS2
S Pentlandite(NixFey)Σ9S8
S PyriteFeS2
S PyrrhotiteFe1-xS
S SphaleriteZnS
ClChlorine
Cl Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
CaCalcium
Ca Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Ca Tremolite◻Ca2Mg5(Si8O22)(OH)2
Ca Hornblende Root Name Group◻Ca2(Z42+Z3+)(AlSi7O22)(OH,F,Cl)2
FeIron
Fe Pyrite var. Bravoite(Fe,Ni)S2
Fe ChalcopyriteCuFeS2
Fe Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Fe MagnetiteFe2+Fe23+O4
Fe Pentlandite(NixFey)Σ9S8
Fe PyriteFeS2
Fe PyrrhotiteFe1-xS
NiNickel
Ni Pyrite var. Bravoite(Fe,Ni)S2
Ni Pentlandite(NixFey)Σ9S8
CuCopper
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS

Other Databases

Link to USGS - Alaska:VA080

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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