Picket Pin

Occurrence in Sweet Grass county in Montana, United States with commodities Platinum, Palladium, Copper, Nickel, Cobalt, Iridium, Gold, Arsenic, Antimony
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Alteration
  8. Host and associated rocks
  9. Nearby scientific data
  10. Geologic structures
  11. Ore body information
  12. Controls for ore emplacement
  13. Economic information about the deposit and operations
  14. Mining district
  15. Land status
  16. Ownership information
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10048501
MRDS ID MP00090
Record type Site
Current site name Picket Pin

Geographic coordinates

Geographic coordinates: -110.05108, 45.44936 (WGS84)
Elevation 3048
Relative position AT THE SUMMIT OF PICKET PIN MOUNTAIN

Site location context

Political divisions (FIPS codes)

Sweet Grass(county)

Montana(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Picket Pin Mountain(quadrangle 1:24,000 scale)

Gardiner(quadrangle 1:100,000 scale)

Bozeman(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Stillwater(hydrologic unit)

Upper Yellowstone(hydrologic accounting unit)

Upper Yellowstone(hydrologic subregion)

Missouri(hydrologic region)

Federal lands

Custer Gallatin National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Geographic areas

Country State County
United States Montana Sweet Grass

Comments on the location information

  • UNSURVEYED. IN CUSTER AND GALLATIN NATIONAL FORESTS. LOCATION GIVEN IS SUMMIT OF PICKET PIN MOUNTAIN; HOWEVER, DEPOSIT IS TRACEABLE ALONG STRIKE FOR 22 KM

Commodities

Commodity Importance
Platinum Critical Primary
Palladium Critical Primary
Copper Secondary
Nickel Critical Secondary
Cobalt Critical Tertiary
Iridium Critical Tertiary
Gold Tertiary
Arsenic Critical Tertiary
Antimony Critical Tertiary

Materials information

Materials Type of material
Chalcopyrite Ore
Pentlandite Ore
Pyrite Ore
Pyrrhotite Ore
Sperrylite Ore
Apatite Gangue
Calcite Gangue
Chlorite Gangue
Graphite Gangue
Magnetite Gangue
Plagioclase Gangue
Quartz Gangue
Talc Gangue

Alteration

  • (Local) Plagioclase Is Altered To Clinozoisite-Epidote, Pyroxene To Chlorite-Calcite-(Talc)- Magnetite-Quartz, Pyrrhotite To Pyrite

Analytical data

Result 6.1% NI, 14.6% CU, 0.2% CO, 1.4 PPM IR, 35 PPM PT, 44 PPM PD, 3.6 PPM AU IN SULFIDE-RICH SAMPLE (BOUDREAU AND MCCALLUM). 0.58% CU, 0.21% NI, 2.5 PPM PT (+IR, RU, RH), 2.5 PPM PD, 0.22 PPM AU (HOWLAND AND OTHERS). OZ/TON VALUES CONVERTED TO PPM

Host and associated rocks

  • Host or associated Host
    Rock type Plutonic Rock > Mafic Intrusive Rock > Anorthosite
    Stratigraphic age (youngest) Neoarchean
    Stratigraphic age (youngest) Early Cretaceous

Nearby scientific data

(1) -110.05108, 45.44936

Economic information

Geologic structures

Type of structure Regional
Structure description The Stillwater Complex Is Exposed Along The Northern Margin Of The Beartooth Uplift, One Of Several Laramide Basement-Cored Ranges That Make Up The Rocky Mountain Foreland Of South-Central Montana (Foose And Others, 1961: Kulik And Schmidt, 1988)
Type of structure Local
Structure description Cross Faults Offset Sulfide Bearing Zone

Ore body information

  • General form LENSES, PODS, PIPES, DISSEMINATED
    Strike NW
    Dip MODERATELY TO STEEPLY NORTH
    Thickness 150M
    Length 22000M
    Depth to top 0M

Controls for ore emplacement

  • Crystallization Processes Within Anorthosite

Comments on the geologic information

  • MINERALIZING FLUIDS WERE SILICA AND ALKALI RICH WITH HCL AND HF. A LACK OF FE AND TI OXIDES INDICATES THE SULFIDES FORMED AT HIGHER SULFUR FUGACITIES. AGE OF STILLWATER COMPLEX IS 2,705 +/- 4 MA BASED ON U-PB SYSTEMATICS ON ZIRCON-BADDELEYITE (PREMO AND OTHERS, 1990)

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Medium
Significant No
Discovery year 1936

Mining district

District name In Stillwater Complex

Land status

Ownership category National Forest

Ownership information

  • Type Operator
    Owner Anaconda Co.
    First year 1980

Comments on the workings information

  • SAMPLING ONLY

Comments on development

  • PRESENCE OF MINERALIZATION WAS KNOWN FROM NEAR HEAD OF NORTH FORK PICKET PIN CREEK IN 1930'S. SOIL GEOCHEMICAL SAMPLING PROGRAM IN 1968 DEFINED AREA OF MINERALIZATION AROUND PICKET PIN.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit SULFIDE ZONE IS STRATIFIED WITHIN UPPER 150 M OF ANORTHOSITE SUBZONE II AND CAN EXTEND UP TO TROCTOLITE BUT GENERALLY ENDS ABOUT 10 M FROM TOP OF ANORTHOSITE WHERE THERE IS A DISTINCT TEXTURAL CHANGE. MINERALIZING SOLUTIONS PERCOLATED UPWARD DURING SOLIDIFICATION OF ANORTHOSITE. HOWLAND AND OTHERS NOTED THAT THE SULFIDES ARE INTERSTITIAL TO SILICATES AND PARTLY REPLACE THEM. DEPOSIT HAS HIGHER CU AND LOWER NI THAN J-M REEF; UNPUBLISHED MODEL NAME: PICKET PIN MINERALIZATION.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-SEP-1991 Peterson, Jocelyn A. U.S. Geological Survey

Beyond USGS

Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.

Operator history (post-MRDS)

MRDS records operators as of each record's last update (≤ 2019). Some of the operators listed here have since changed hands or dissolved:

Curated by qvyshift.com from publicly-reported M&A activity (SEC filings, press releases, USGS Mineral Yearbooks). Not authoritative — verify against primary sources before relying on it. The MSHA panel above is the current authoritative source for actively-permitted mines.