South Filson Creek deposit

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

Geologic information

Identification information

Deposit ID 10048466
MRDS ID MP00053
Record type Site
Current site name South Filson Creek deposit
Alternate or previous names Filson Creek

Geographic coordinates

Geographic coordinates: -91.67378, 47.82167 (WGS84)
Elevation 457
Location accuracy 1000(meters)
Relative position ABOUT 1 MI NORTHWEST OF OMADAY LAKE, Est Estimated From Map And Description In Kuhns And Others, 1990

Site location context

Political divisions (FIPS codes)

Lake(county)

Minnesota(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Bogberry Lake(quadrangle 1:24,000 scale)

Ely(quadrangle 1:100,000 scale)

Two Harbors(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Rainy Headwaters(hydrologic unit)

Rainy(hydrologic accounting unit)

Rainy(hydrologic subregion)

Souris-Red-Rainy(hydrologic region)

Federal lands

Superior 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 Minnesota Lake

Public Land Survey System information

Meridian Township Range Section Fraction State
4th Principal 062N 011W 25 SE4 OF SW4 Minnesota

Comments on the location information

  • IN SUPERIOR NATIONAL FOREST

Commodities

Commodity Importance
Copper Primary
Nickel Critical Primary
Palladium Critical Secondary
Platinum Critical Secondary
Gold Secondary
Silver Secondary
Cobalt Critical Secondary

Comments on the commodity information

  • PT AND PD ARE CORRELATED WITH HIGH CU. SPERRYLITE IS ALWAYS ASSOCIATED WITH SERPENTINE AND IS A VERY LATE STAGE MINERAL. SEE KUHNS AND OTHERS (1990) FOR EXTENSIVE DISCUSSION OF PGE MINERALIZATION AND ANALYTICAL DATA

Materials information

Materials Type of material
Bornite Ore
Chalcocite Ore
Chalcopyrite Ore
Covellite Ore
Cubanite Ore
Digenite Ore
Galena Ore
Millerite Ore
Niccolite Ore
Pentlandite Ore
Pyrrhotite Ore
Sperrylite Ore
Sphalerite Ore
Biotite Gangue
Chlorite Gangue
Iddingsite Gangue
Ilmenite Gangue
Magnetite Gangue
Sericite Gangue
Serpentine Gangue
Stilpnomelane Gangue

Alteration

  • (Local) Serpentine/Mica Assemblage, Later Argillic Alteration, Localized Hematitic Alteration, Greenschist Facies Assemblage

Analytical data

Result CU:NI=3:1. CORE YIELDED UP TO 87.5 FT OF 1.24% CU+NI. MAXIMUM VALUES FROM HIGH-GRADE INTERSECTIONS OF 4 DRILL CORES ARE 1.35% CU, 0.36% NI, 1.1 PPM PT, 2.6 PPM PD, 31 PPB IR, 19 PPB OS, 78 PPB RH, 130 PPB RU, 370 PPB AU, 4.5 PPM AG. WEIGHTED AVERAGE OF COMBINED PT AND PD=651 PPB, OF AU=137 PPB. PD:PT=2:1, CU:NI=3:1 IN MINERALIZED ZONES. PD RANGES FROM 53-2600 PPB, PT FROM 25-1100 PPB, AU FROM <1-413 PPB, AG FROM 0.4-8.8 PPM, AND RH FROM <2-78 PPB

Mineral occurrence model information

Model code 9
USGS model code 5a
Deposit model name Duluth Cu-Ni-PGE

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Granitoid > Granite
    Rock unit name Giants Range Batholith
    Stratigraphic age (youngest) Neoarchean
    Stratigraphic age (youngest) Neoarchean
  • Host or associated Host
    Rock type Plutonic Rock > Mafic Intrusive Rock > Gabbro > Troctolite
    Rock unit name South Kawishiwi Intrusion
    Stratigraphic age (youngest) Mesoproterozoic
    Stratigraphic age (youngest) Mesoproterozoic

Nearby scientific data

(1) -91.67378, 47.82167

Economic information

Geologic structures

Type of structure Local
Structure name Faults
Type of structure Local
Structure name Brecciation

Ore body information

  • General form DISSEMINATED, DISCONTINUOUS VEINLETS

Controls for ore emplacement

  • Sulfide Distribution Controlled By Texture (Pegmatitic Zones) And Structure (Amount Of Fine-Grained Fractures). Overall Distribution Controlled By A Northwest-Trending Fracture Zone. Faults And Folds Were Responsible For Localizing Sulfide Mineralization As Well As For Providing Conduits For Later Syn- To Post-Magmatic Hydrothermal Fluids.

Comments on the geologic information

  • SOUTH FILSON CREEK AREA IS CHARACTERIZED GEOPHYSICALLY BE A WELL-DEFINED NORTHEAST-TRENDING MAGNETIC LOW, WHICH COULD BE INTERPRETED AS A MAJOR STRUCTURE OR A NORMAL TROCTOLITE BETWEEN TWO HIGHLY MAGNETIC TROCTOLITES. LATE SYENITE DIKES WERE INJECTED INTO SOME OF THE SHEARED SERPENTINITE FRACTURES

Economic information about the deposit and operations

Development status Prospect
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1967
Discoverer Hanna Mining Co.

Mining district

District name Western Margin Duluth Complex

Land status

Ownership category National Forest

Ownership information

  • Type Operator
    Owner American Copper And Nickel Co.
    First year 1989
  • Type Owner
    Owner U.S. Forest Service
    First year 1989

Comments on the reserve resource information

  • BASED ON 1989 PRICES FOR 7 COMMODITIES, THERE ARE NO ORE RESERVES IN THE AREA STUDIED BY KUHNS AND OTHERS (1990). HOWEVER, FURTHER DRILLING IN THE AREA COULD REVEAL RESOURCES NOT CURRENTLY KNOWN

Comments on the workings information

  • DRILL HOLES ONLY AND SURFACE SAMPLING

Comments on development

  • 24 DRILL HOLES INDICATE SPORADIC MINERALIZATION OF LOW TO MODERATE GRADE

Reference information

Bibliographic references

  • Analytical Data

    KUHNS AND OTHERS, 1990; MORTON AND HAUCK, 1989; HAUCK AND BARNES, 1989

  • Deposit

    KUHNS, M.J.P., HAUCK, S.A., AND BARNES, R.J., 1990, ORIGIN AND OCCURRENCE OF PLATINUM GROUP ELEMENTS, GOLD AND SILVER IN THE SOUTH FILSON CREEK COPPER-NICKEL MINERAL DEPOSIT, LAKE COUNTY, MINNESOTA: NATURAL RESOURCES RESEARCH INSTITUTE TECHNICAL REPORT NRRI/GMIN-TR-89-15, 60 P.

  • Deposit

    MORTON, PENELOPE, AND HAUCK, S.A., 1989, PRECIOUS METALS IN THE COPPER-NICKEL DEPOSITS OF THE DULUTH COMPLEX, IN MOREY, G.B., ED., WORKSHOP ON THE APPLICABILITY OF GOLD AND PLATINUM-GROUP-ELEMENT MODELS IN MINNESOTA: MINNESOTA GEOLOGICAL SURVEY INFORMATION CIRCULAR 30, P. 47-48.

  • Deposit

    HAUCK, S.A., AND BARNES, R.J., 1989, PRECIOUS METALS (PT-PD-AU-AG) IN THREE COPPER-NICKEL DEPOSITS IN THE DULUTH COMPLEX: NATURAL RESOURCES RESEARCH INSTITUTE, CENTER FOR APPLIED RESEARCH AND TECHNOLOGY DEVELOPMENT, TECHNICAL SUMMARY REPORT NRRI/GMIN-TSR-89-1, 19 P.

General comments

Subject category Comment text
Deposit DEPOSIT IS ABOUT 2200 FT ABOVE BASAL CONTACT OF DULUTH COMPLEX, ONE OF THE SO-CALLED CLOUD ZONE DEPOSITS. THERE WERE LIKELY TWO EPISODES OF MINERALIZATION, A PRIMARY STAGE AND A HYDROTHERMAL STAGE. THE HYDROTHERMAL STAGE IS SPATIALLY ASSOCIATED WITH HIGHLY SERPENTINIZED FRACTURES IN A PROPOSED NORTHEAST-TRENDING FAULT ZONE. SECONDARY SULFIDES FORMED MICROVEINLETS RELATED TO THE FRACTURING. PT AND PD HAVE HIGHER CONCENTRATIONS IN THE SECONDARY SULFIDE STAGE AND CORRELATE WITH HIGH SULFUR VALUES. ZONES OF SECONDARY MINERALIZATION ARE <1-90 FT THICK
Deposit Discovery Year: LATE 1960'S

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-93 Peterson, Jocelyn A. U.S. Geological Survey
Editor 24-FEB-05 Woodruff, L.G. U.S. Geological Survey

Beyond USGS

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