Spruce Road deposit

Prospect in Lake county in Minnesota, United States with commodities Copper, Nickel, Platinum, Palladium, Cobalt, Gold, Silver, PGE
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. Mineral occurrence model information
  9. Host and associated rocks
  10. Nearby scientific data
  11. Geologic structures
  12. Ore body information
  13. Controls for ore emplacement
  14. Economic information about the deposit and operations
  15. Mining district
  16. Ownership information
  17. Reserves and resources
  18. Workings at the site
  19. Links to other databases
  20. Bibliographic references
  21. General comments
  22. Reporter information

Geologic information

Identification information

Deposit ID 10038935
MRDS ID M046425
Record type Site
Current site name Spruce Road deposit
Alternate or previous names Spruce Open Pit Inco, Spruce Mine, Inco Prospect, Ely Spruce, Ely Nickel Copper

Comments on the site names

  • This record has combined information from original MRDS records W000707 and W800356. The site name in the other records was the Ely Nickel Copper Deposit.

Geographic coordinates

Geographic coordinates: -91.681, 47.82972 (WGS84)

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 24,25 Minnesota

Comments on the location information

  • SE of Ely, MN. 3.3 miles NE of Highway 1. The location is accurate using Hauck and others (1997) map blown up to 1:24,000.

Commodities

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

Comments on the commodity information

  • PGE MINERALIZATION IS KNOWN TO OCCUR ONLY ALONG THE WESTERN CONTACT OF THE 1.1 GA DULUTH COMPLEX. PASTERIS (1984, 1985) RECOGNIZED FIVE VARIETIES OF OXIDES IN THE BABBITT AND SPRUCE ROAD DEPOSITS: 1) SPINEL AND ILMENITE RODS IN PLAGIOCLASE; 2) INDIVIDUAL ILMENITE GRAINS; 3) INDIVIDUAL MAGNETITE GRAINS; 4) GRANULAR (COMPOSITE?) ILMENITE-MAGNETITE; AND 5) LAMELLAR ILMENITE IN MAGNETITE. OTHER MINERALS FOUND INCLUDE MACKINAWITE, VALLERITE, VIOLARITE, TALNAKHITE, AND ULVOSPINEL.

Materials information

Materials Type of material
Bornite Ore
Bravoite Ore
Chalcocite Ore
Copper Ore
Cuprite Ore
Digenite Ore
Galena Ore
Magnetite Ore
Pentlandite Ore
Pyrite Ore
Sphalerite Ore
Tenorite Ore
Troilite Ore
Olivine Gangue
Plagioclase Gangue
Pyroxene Gangue
Pyrrhotite Unknown

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 Host
    Rock type Plutonic Rock > Mafic Intrusive Rock
    Rock unit name Duluth Complex
    Rock description Duluth Complex
    Stratigraphic age (youngest) Mesoproterozoic
  • Host or associated Host
    Rock type Plutonic Rock > Mafic Intrusive Rock > Gabbro > Troctolite
    Rock unit name South Kawishiwi Intrusion
    Rock description South Kawishiwi Intrusion
    Stratigraphic age (youngest) Mesoproterozoic
  • Host or associated Associated
    Rock type Plutonic Rock > Granitoid > Granite
    Rock unit name Giants Range Batholith
    Rock description Giants Range Batholith
    Stratigraphic age (youngest) Archean
  • Host or associated Associated
    Rock type Sedimentary Rock > Chemical Sediment > Iron Formation
    Rock unit name Biwabik Formation
    Rock description Biwabik Formation
    Stratigraphic age (youngest) Paleoproterozoic
  • Host or associated Associated
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Argillite
    Rock unit name Virginia Formation
    Rock description Virginia Formation
    Stratigraphic age (youngest) Paleoproterozoic

Nearby scientific data

(1) -91.681, 47.82972

Economic information

Geologic structures

Type of structure Regional
Structure description Several Ne-Trending Normal Faults Parallel The Midcontinent Rift System Near The Margin. These Faults Formed During The Opening Of The Rift And Controlled Emplacement Of The Troctolitic And Late Intrusions.

Ore body information

  • General form TABULAR - LENS
    Thickness 91.44M
  • General form TABULAR - LENS

Controls for ore emplacement

  • 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

  • THE DULUTH COMPLEX IS A LARGE, COMPOSITE THOLEIITIC MAFIC INTRUSION THAT WAS EMPLACED INTO COMAGMATIC FLOOD BASALTS ALONG A PORTION OF THE MIDDLE PROTEROZOIC (1.1 GA, KEWEENAWAN) MIDCONTINENT RIFT SYSTEM. IN THE SOUTH KAWISHIWI INTRUSION, SULFIDES FORM A DISCREET ZONE UNDERLYING SULFIDE-FREE ROCKS. MOST SULFIDES OCCUR INTERSTITIALLY BETWEEN EUHEDRAL OLIVINE OR PLAGIOCLASE OR ARE INCLUDED IN THE RIMS OF SILICATES. THE SULFIDES FORMED AFTER MOST SILICATES HAD ACCUMULATED. HOST ROCK TYPE IS THE SPRUCE BRECCIA FACIES OF THE BASAL ZONE OF THE KAWISHIWI INTRUSION, A MEDIUM-COARSE GRAINED TROCTOLITE.

Economic information about the deposit and operations

Development status Prospect
Commodity type Metallic
Significant Yes
Discovery year 1955
Discoverer International Nickel Company

Mining district

District name Western Margin Duluth Complex

Ownership information

  • Type Owner-Operator
    Owner International Nickel Co. Of Canada, Ltd. (Inco)

Comments on the ownership information

  • The deposit was discovered by geophysical anomaly and localized by drilling by INCO.

Reserves and resources

  • Type In-situ
    Estimate year 1973
    Total resources 12390mt commodity
    Commodity Subtype Grade units Group Importance Year
    Nickel nickel 0.21 wt-pct Nickel Major 1973
  • Type In-situ
    Estimate year 1973
    Total resources 37760mt commodity
    Commodity Subtype Grade units Group Importance Year
    Copper copper 0.64 wt-pct Copper Major 1973
  • Type In-situ
    Estimate year 1973
    Total resources 2360mt commodity
    Commodity Subtype Grade units Group Importance Year
    Cobalt cobalt 0.04 wt-pct Cobalt Minor 1973
  • Type In-situ
    Estimate year 1973
    Total resources 5900000mt ore

Comments on the reserve resource information

  • ALONG THE WESTERN MARGIN OF THE DULUTH COMPLEX, THE CU-NI SULFIDE RESOURCES ARE ESTIMATED AT 4.4 BILLION TONS OF 0.66 PERCENT CU WITH A CU:NI RATIO OF 3.3:1 (HAUCK AND OTHERS, 1997). OTHER MINERALIZED BODIES NEAR THE BASE OF THE DULUTH GABBRO HAVE BEEN EXPLORED NORTHEAST OF THE ELY AREA. TWO LARGE DEPOSITS, TOTALING SEVERAL HUNDRED MILLION TONS OF MATERIAL, ARE REPORTED TO AVERAGE 0.75% CU AND 0.25% NI.
  • EST BY MINN. GEOLOGICAL SURVEY FOR BASAL ZONE OF COMPLEX

Workings at the site

  • Type of workings Surface
    Area 218.538HA
    Overall length 2000M
    Overall width 1200M

Comments on the workings information

  • POTENTIAL AND PLANNED MINE - IF IT CAN GET PAST ENVIRONMENTAL LAWS AS OF 1975 - THICKNESS VARIES FROM 50 - 300 FT. AN OPEN PIT MINE IS PLANNED WHICH WILL FOLLOW THE MINERALIZED ZONE DOWN TO A MAXIMUM PIT DEPTH OF 304 M.

Comments on development

  • DEPOSIT DISCOVERED BY GEOPHYSICAL ANOMALY, AND LOCALIZED BY DRILLING

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DISCOVERED IN 1948 NEAR BASE OF DULUTH GABBRO COMPLEX IN LAKE COUNTY, 10 MILES SE OF ELY, MINN. THE COMPLEX IS A HUGE LOPOLITHIC STRATIFORM INTRUSIVE, EXTENDING FOR 150 MILES NE FROM DULUTH, WITH MAXIMUM THICKNESS 50,000 FEET. GABBRO, ANORTHOSITE, AND GRANOPHYRE ARE THE MAIN ROCK TYPES IN THIS HIGHLY DIFFERENTIATED LAYERED PLUTON, BUT PERIDOTITE AND NORITE LAYERS ARE PRESENT IN THE LOWER PART. GRADE SAMPLES RANGE FROM 0.32% CU, AND 0.13% NI, TO 1.12% CU AND 0.38% NI. CORNWALL, 1966, INDICATES A SULFIDE DEPOSIT OF 100,000-200,000 TONS OF CONTAINED NICKEL.: UPDATE BY GLENN L. SHAFFER-1/75, RESERVES AND POTENTIAL RESOURCES, GEOLOGIC DESCRIPTION. FURTHER UPDATE ON 7/75 TO SAME FIELDS
Deposit The deposit is made up of stratiform magmatic sulfide segregatioons that are disseminated in layers and lenses.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-1975 Page, Norman U.S. Geological Survey
Updater 25-JUL-1996 Sutphin, D.M. U.S. Geological Survey
Editor 05-JAN-1997 Mason, Jr., G.T. U.S. Geological Survey
Reporter 01-AUG-1972 Coury, Anny U.S. Geological Survey
Updater 07-JAN-1975 Shaffer, Glenn L. U.S. Geological Survey
Editor 25-NOV-2003 Woodruff, Laurel G. U.S. Geological Survey Work done in Filemaker
Editor 24-FEB-2005 Woodruff, L.G. U.S. Geological Survey

Beyond USGS

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