Michigan-Utah Mine

Past Producer in Salt Lake county in Utah, United States with commodities Silver, Lead, Copper, Gold, Manganese, Zinc, Molybdenum
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. 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. Land status
  17. Production statistics
  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 10101913
MRDS ID D011945
Record type Site
Current site name Michigan-Utah Mine
Alternate or previous names Grizzly Tunnel, Cleave Tunnel, Topeka Tunnel, City Rocks Tunnel, Butte Mine, Black Bess Mine, Solitude Tunnel, Utah Mines Coalition, Lavina, Darlington, Regulator, Continental-Alta.

Geographic coordinates

Geographic coordinates: -111.61772, 40.59577 (WGS84)
Elevation 2877
Relative position 6010 FT N71 DEGREES W OF MT. MILLICENT

Site location context

Political divisions (FIPS codes)

Salt Lake(county)

Utah(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Brighton(quadrangle 1:24,000 scale)

Salt Lake City(quadrangle 1:100,000 scale)

Salt Lake City(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Jordan(hydrologic unit)

Jordan(hydrologic accounting unit)

Great Salt Lake(hydrologic subregion)

Great Basin(hydrologic region)

Federal lands

Uinta-Wasatch-Cache 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 Utah Salt Lake

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 002S 003E 33 NE OF SE OF SW Utah

Comments on the location information

  • UTM COORDINATES GIVE ABOVE ARE FOR PORTAL OF THE CLEAVE TUNNEL. COORDINATES FOR OTHER MAIN TUNNEL AS FOLLOWS, CITY ROCKS TUNNEL-4494020N, 448200E, ROLLINS TUNNEL-4494060N, 448250E, GRIZZLY TUNNEL-4494020N, 447810E ; INFO FROM LAND.ST :1983

Commodities

Commodity Importance
Silver Primary
Lead Primary
Copper Secondary
Gold Secondary
Manganese Critical Secondary
Zinc Critical Tertiary
Molybdenum Tertiary

Materials information

Materials Type of material
Argentite Ore
Chalcopyrite Ore
Galena Ore
Gold Ore
Malachite Ore
Smithsonite Ore
Sphalerite Ore
Wad Ore
Calcite Gangue
Quartz Gangue

Alteration

  • (Local) Bleaching, Minor Silicification, Calc-Silicates, Oxidation

Analytical data

Result ORE FROM ALL MINING DONE BETWEEN 1901 AND 1919 AVERAGED 52 CENTS/TON AU, 16.5 OZ/TON AG, 9.12% PB, AND 1.2% CU

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Rock unit name Alta Stock;Grizzly Dike-Alaskite
    Rock description Alta Stock;Grizzly Dike-Alaskite
    Stratigraphic age (youngest) Oligocene
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Maxfield Limestone;Fitchville Formation
    Rock description Maxfield Limestone;Fitchville Formation
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Dolomite

Nearby scientific data

(1) -111.61772, 40.59577

Economic information

Geologic structures

Type of structure Regional
Structure description Sevier Overthrust Belt, Cordilleran Hinge Line, Uinta-Cottonwood Arch
Type of structure Local
Structure description Grizzly Overthrust Zone, Northeast Striking Fissures

Ore body information

  • General form TABULAR
    Strike N60E
    Dip 80N
    Depth to top 0M
    Depth to bottom 365.76M
  • General form TABULAR
    Dip 80N
  • General form TABULAR
    Dip 80N

Controls for ore emplacement

  • Northeast Striking Fissures, Intersections Between Fissures And Favorable Beds, Proximity To Dikes

Comments on the geologic information

  • PALEOZOIC UNITS RANGE FROM CAMBRIAN TINTIC QUARTZITE TO DESERET LIMESTONE. ALTA STOCK LIES TO SOUTH. DIKES HAVE NORTHEASTERLY STRIKE. BEDDING ABOUT 20 TO 30 DEGREES TO EAST. GRIZZLY THRUST IS TROUGH-LIKE

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Medium
Significant No
Discovery year 1869
Year of first production 1870
Year of last production 1928

Mining district

District name Little Cottonwood District

Land status

Ownership category Private

Production statistics

  • Year 1919
    Period 1901-1919
    Material ORE
    Accuracy Estimate
    Description Cp_Grade: ^52 Cents/Ton Au, 16 Oz/Ton Ag, 9.12% Pb, 1.2% Cu
    Importance Item Commodity Group Amount recovered Grade Recovery percentage
    Ore Copper Copper 1wt-pct
    Ore Lead Lead 9wt-pct
    Ore Silver Silver 452g/mt

Comments on the production information

  • SEVERAL CARS OF HIGH GRADE MN ORE MARKETED DURING WWI. ORE TRANSPORTED BY AERIAL TRAMWAYS TO TANNERS FLAT AND THEN BY RAIL TO SALT LAKE VALLEY SMELTERS.

Workings at the site

  • Type of workings Underground
    Length 19812M

Comments on the workings information

  • TOTAL LENGTH REPORTED INCLUDES SOLITUDE, BUTTE, AND BLACK BESS WORKINGS. MAIN PORTALS ARE TOPEKA, CLEVE, CITY ROCKS, SOLITUDE, AND BUTTE FOR THE CITY ROCKS FISSURES AND THE GRIZZLY FOR THE GRIZZLY-LAVINIA FISSURES. MINOR WORKINGS INCLUDE 17 SHORT ADITS AND 7 SHORT SHAFTS. LARGER WORKINGS NOT MENTIONED BEFORE INCLUDE SEVEN ADITS, AVERAGING 1250 FT. IN DEPTH.

Comments on development

  • EARLY WORK ON BUTTE AND BLACK BESS MINES. LATER MINES WERE CONSOLIDATED AND THE CITY ROCK AND GRIZZLY-LAVINIA FISSURES WERE EXPLOITED

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit MOST PRODUCTION CAME FROM FISSURE DEPOSITS AND ASSOCIATED REPLACEMENT PODS. REPLACEMENTS FORMED AT INTERSECTIONS BETWEEN FAVORABLE LIMESTONE BEDS AND FISSURES. NUMEROUS FISSURES WERE MINED BUT MOST OF THE PRODUCTION CAME FROM THE CITY ROCKS AND GRIZZLY-LAVINIA FISSURE SYSTEMS. MINOR PRODUCTION CAME FROM CONTACT MAGNETITE-RICH, COPPER-BEARING REPLACEMENT BODIES NEAR DIKES. MOST FISSURES STRIKE N60E AND DIP STEEPLY TO THE NORTH. SOME REVERSAL OF DIPS SEEN ACROSS THE GRIZZLY THRUST FAULT.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1984 Shubat, Michael A. Utah Geological and Mineral Survey

Beyond USGS

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

External references