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Granite Creek Mine, Potosi Mining District, Osgood Mountains, Humboldt County, Nevada, USAi
Regional Level Types
Granite Creek MineMine
Potosi Mining DistrictMining District
Osgood MountainsMountain Range
Humboldt CountyCounty
NevadaState
USACountry

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Latitude & Longitude (WGS84):
41° 8' 11'' North , 117° 16' 34'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Golconda214 (2011)27.1km
Winnemucca7,887 (2017)42.6km
Paradise Valley109 (2011)45.2km
Battle Mountain3,635 (2011)62.0km
Mindat Locality ID:
59659
Long-form identifier:
mindat:1:2:59659:1
GUID (UUID V4):
b620ce1d-eda3-4a20-9597-035139fac2c2


Secs. 29 & 30 T38N R42E. Tactite.
Structure: Folds, Faults

Alteration: Contact Metamorphism

Deposit: Scheelite is irregularly distributed and is entirely absent from much of the tactite. Where the contact is about parallel to the strike of the limestone, the tungsten mineralization is more nearly uniform throughout the whole mass of tactite. Where the contact is at an angle to the strike of sedimentary beds, the tactite bodies and the ore zones within them are more irregular and may pitch in the direction of the dip of -the beds. The largest and most continuous tactite orebody is a-t the eastern end of the property. The main layer has been traced for 230 ft on the surface where its width ranges from 5 to- 25 ft. On the lower adit level it is 200 ft long. The average- width is between 15 and 20 ft and the tungsten content is r- ather uniformly about 0.6 % wo3, which was diluted somewhat - in mining. Occurrence of scheelite was known for some time before ore was mined in 1942. Mainly underground workings, from 1942 to 1944 and from 1950 to 1955. The property is estimated to have about 42,200 tons ore at 0.45% wo3 reserves. Main production was from the main tactite body at the east end of the orebody. Workings consist of 2 adits connected to 2 glory holes; pits and trenches. ; info.src : 1 pub lit; 2 unpub rept

Deposit type: W skarn

Geology: Main tactite body lay in keel & lower part of trough-like structure, very variable in size and shape the contact is generally east-west with numerous irregularities. Irregular and discontinuous tactite bodies occur along the contact for over 2200 ft.

Rock formation(s): Osgood Mtns. Stock
Preble Formation;Preble Formation;Preble Formation;Preble Formation


Ore(s): Tactite At Limestone/Granodiorite Contact

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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.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
β“˜Chalcopyrite2.CB.10aCuFeS2
β“˜Molybdenite2.EA.30MoS2
β“˜Pyrite2.EB.05aFeS2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
β“˜Scheelite7.GA.05Ca(WO4)

List of minerals for each chemical element

OOxygen
Oβ“˜ ScheeliteCa(WO4)
SSulfur
Sβ“˜ ChalcopyriteCuFeS2
Sβ“˜ MolybdeniteMoS2
Sβ“˜ PyriteFeS2
CaCalcium
Caβ“˜ ScheeliteCa(WO4)
FeIron
Feβ“˜ ChalcopyriteCuFeS2
Feβ“˜ PyriteFeS2
CuCopper
Cuβ“˜ ChalcopyriteCuFeS2
MoMolybdenum
Moβ“˜ MolybdeniteMoS2
WTungsten
Wβ“˜ ScheeliteCa(WO4)

Other Databases

Link to USGS MRDS:10045079

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