Lyle Mine

Occurrence in Koochiching county in Minnesota, United States with commodity Gold
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. Host and associated rocks
  9. Nearby scientific data
  10. Geologic structures
  11. Controls for ore emplacement
  12. Economic information about the deposit and operations
  13. Mining district
  14. Workings at the site
  15. Links to other databases
  16. Bibliographic references
  17. General comments
  18. Reporter information

Geologic information

Identification information

Deposit ID 10082801
MRDS ID W062151
Record type Site
Current site name Lyle Mine

Geographic coordinates

Geographic coordinates: -93.11745, 48.61972 (WGS84)
Elevation 338
Location accuracy 100(meters)
Relative position LOCATED AT THE NORTH TIP OF DRYWEED ISLAND OF RAINY LAKE, IN NOYAGEURS NATIONAL PARK, ABOUT 12 MILES EAST OF FORT FRANCES, ONTARIO, CANADA., Acc Location Taken From 1:50,000 Scale Map, Acc Location Taken From 1:50,000 Scale Map

Site location context

Political divisions (FIPS codes)

Koochiching(county)

Minnesota(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Cranberry Bay(quadrangle 1:24,000 scale)

International Falls(quadrangle 1:100,000 scale)

International Falls(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Rainy Lake(hydrologic unit)

Rainy(hydrologic accounting unit)

Rainy(hydrologic subregion)

Souris-Red-Rainy(hydrologic region)

Federal lands

Voyageurs National Park(National Park)

National Park NPS(Type of land area)

NPS(Federal land areas administered by NPS)

Geographic areas

Country State County
United States Minnesota Koochiching

Public Land Survey System information

Meridian Township Range Section Fraction State
71N 22W 23 SE4 Minnesota

Comments on the location information

  • PLOTTED ON MAP I-1927.

Commodities

Commodity Importance
Gold Primary

Materials information

Materials Type of material
Gold Ore
Apatite Gangue
Feldspar Gangue
Pyrite Gangue
Quartz Gangue
Tourmaline Gangue

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Schist
    Rock unit name Seine Series
    Stratigraphic age (youngest) Neoarchean
    Stratigraphic age (youngest) Neoarchean

Nearby scientific data

(1) -93.11745, 48.61972

Economic information

Geologic structures

Type of structure Regional
Structure description In The Quetico Subprovince Of The Superior Province. The Rainy Lake Area Lies Within A Dextral Wrench (Shear) Zone Bounded On The North By The Quetico Fault And On The South By The Rainy Lake-Seine River Fault.

Controls for ore emplacement

  • Sims And Day (1992) Note That The Fundamental Regional Control On Gold Deposits In The Superior Province Is Transcurrent And Oblique Slip-Shear Deformation Zones That Formed In Late Archean Time.

Comments on the geologic information

  • NEAR THE LITTLE AMERICAN MINE, THERE IS A SERIES OF LESS EXPLORED PROPSECTS OF SIMILAR QUARTZ VEINS AND OVERLAPPING LENSES; THE LYLE MINE IS ONE OF THOSE PROSPECTS. MAP I-1927 SHOWS THE HOST ROCK TO BE LATE ARCHEAN TECTONITE--MYLONITE, PHYLLONITE, SCHIST, AND CATACLASITE.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Rainy Lake

Workings at the site

  • Type of workings Underground
    Name of workings LYLE MINE SHAFT
    Overall depth 30.48M

Comments on the workings information

  • IN 1895, THE "MINE" HAD A 100-FT SHAFT.

Comments on development

  • EXPLORATION FOR GOLD DEPOSITS IN THE REGION HAS BEEN HAMPERED BY A GENERALLY THIN, DISCONTINUOUS MANTLE OF PLEISTOCENE GLACIAL DEPOSITS. ; ECON.COM: THE GOLD VALUES MUST HAVE BEEN LOW, BECAUSE THE WORK WAS SOON ABANDONED. GOLD MINES IN THE CANADIAN PART OF THE RAINY LAKE DISTRICT HAD PRODUCED MORE THAN ONE MILLION DOLLARS WORTH OF GOLD BY 1937, MOSTLY FROM HYPOTHERMAL VEINS LIKE THE ONE AT THE LITTLE AMERICAN MINE AND AT OTHER MINES IN THE AREA.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit GROUT (1937) CLASSIFIED THE VEIN AT LYLE AS BEING OF HYPOTHERMAL ORIGIN. THE WALLROCK AT LYLE IS LIKE THAT AT THE LITTLE AMERICAN MINE. CARD AND OTHERS (1989) DISTINGUISHED TWO TYPES OF GOLD DEPOSITS IN THE SUPERIOR PROVINCE OF CANADA: (1) SULFIDE SCHIST DEPOSITS, AND (2) EPIGENETIC VEIN DEPOSITS. THE LARGE HEMLO DEPOSIT IN CANADA IS BELIEVED TO BE AN EPIGENETIC VEIN DEPOSIT. SULFIDE SCHIST DEPOSITS ARE LESS COMMON AND LESS PRODUCTIVE THAN EPIGENETIC VEIN DEPOSITS.
Deposit THE OCCURRENCE OF LARGE GOLD DEPOSITS IN CANADA SUGGESTS THAT THE GREENSTONE-GRANITE TERRANES OF MINNESOTA ARE FAVORABLE FOR THE OCCURRENCE OF IMPORTANT GOLD DEPOSITS.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-DEC-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.