Larson Exploration Prospect

Occurrence in Florence county in Wisconsin, United States with commodity Iron
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. Economic information about the deposit and operations
  15. Mining district
  16. Ownership information
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10082687
MRDS ID W062037
Record type Site
Current site name Larson Exploration Prospect

Geographic coordinates

Geographic coordinates: -88.34115, 45.90694 (WGS84)
Location accuracy 100(meters)
Relative position Acc Lat/Lon Is For The Main Entrance (Taken From Usbm Cd-Rom 9/95)., Acc Lat/Lon Is For The Main Entrance (Taken From Usbm Cd-Rom 9/95).

Site location context

Political divisions (FIPS codes)

Florence(county)

Wisconsin(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Florence West(quadrangle 1:24,000 scale)

Iron Mountain(quadrangle 1:100,000 scale)

Iron Mountain(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Menominee(hydrologic unit)

Northwestern Lake Michigan(hydrologic accounting unit)

Northwestern Lake Michigan(hydrologic subregion)

Great Lakes(hydrologic region)

Geographic areas

Country State County
United States Wisconsin Florence

Public Land Survey System information

Meridian Township Range Section Fraction State
40N 17W 35 W2 OF NW4 Wisconsin

Commodities

Commodity Importance
Iron Primary

Comments on the commodity information

  • MATERIAL WAS LEAN, NON-BESSEMER WITH A HIGH ALUMINA CONTENT.

Materials information

Materials Type of material
Goethite Ore
Hematite Ore
Magnetite Ore
Quartz Gangue

Alteration

  • (Local) Leaching Of Silica Or Replacement By Iron Oxides Or A Combination Of These Processes.

Mineral occurrence model information

Model code 241
USGS model code 34a
Deposit model name Superior Fe (BC name is Lake Superior & Rapitan types iron-formation)

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Chemical Sediment > Iron Formation
    Rock unit name Vulcan Iron Formation
    Rock description Vulcan Iron Formation
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Neoproterozoic

Nearby scientific data

(1) -88.34115, 45.90694

Economic information

Geologic structures

Type of structure Regional
Structure description Major Troughs Into Which Iron Fm. Has Slumped; Regional Trends Are E-W To Ne-Sw.

Ore body information

  • General form STRATABOUND
    Dip 50-55 N

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1849
Year of first production 1948
Year of last production 1948
Production years 1948

Mining district

District name Menominee Iron District

Ownership information

  • Type Operator
    Owner Jackson County Iron Co.

Comments on the production information

  • SAMPLE SHIPMENT WENT THROUGH THE PORT AT ESCANABA, MI. LAKE SUPERIOR IRON ORE ASSOCIATION, 1952, HAS PRODUCTION FIGURES FOR INDIVIDUAL MINES AND LEASES.

Comments on development

  • A SAMPLE SHIPMENT WAS MINED FROM AN OPEN CUT IN 1948. AS OF 1950 THE PROPERTY WAS ABANDONED. ; ECON.COM: IRON ORE WAS DISCOVERED IN DICKINSON COUNTY IN 1849; THE FIRST SHIPMENTS WERE MADE IN 1877, AND PRODUCTION CEASED IN 1959. IRON ORE WAS DISCOVERED IN IRON COUNTY IN 1851; THE FIRST SHIPMENTS WERE MADE IN 1882, AND PRODUCTION WAS CONTINUING IN 1966.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit VULCAN IRON FORMATION CONSISTS OF THINNLY BEDDED LAYERS OF MAGNETITE, MARTITE, AND SPECULARITE, ALTERNATING WITH QUARTZ-RICH LAYERS; MINOR LOW-IRON SILICATE MINERALS ARE PRESENT (DUTTON AND ZIMMER, 1968). THE FORMATION RANGES FROM 300-800 FT THICK.
Deposit THE GEOLOGY CONSISTS OF PRECAMBRIAN W CRYSTALLINE ROCKS OVERLAIN BY PRECAMBRIAN X SEDIMENTARY ROCKS. DURING PRECAMBRIAN X TIME, PRECAMBRIAN W ROCKS BLOCK FAULTED AND DIFFERENTIALLY RAISED; LOWERED; FORMING TROUGHS. PRECAMBRIAN X SEDIMENTS SLUMPED INTO THE TROUGHS. AT ABOUT THE SAME TIME, THE ENTIRE AREA WAS REGIONALLY THERMAL METAMORPHOSED. THIS AREA OF THE MENOMINEE DISTRICT IS IN THE CHLORITE AND BIOTITE ISOGRADS. ALTHOUGH BOTH THE VULCAN IRON FM. AND THE RIVERTON IRON FM. ARE PRECAMBRIAN X IN AGE, THE VULCAN IRON FM. IS THE OLDER. THE VULCAN IRON FM. IS PART OF THE MENOMINEE GROUP.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-OCT-95 Sutphin, David M. (Cannon, W. F.) U.S. Geological Survey
Updater 01-MAR-97 Sutphin, David M. U.S. Geological Survey
Editor 01-MAY-97 Mason Jr., G.T. U.S. Geological Survey

Beyond USGS

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