Little Bell Shaft

Past Producer in Summit county in Utah, United States with commodities Lead, Silver, Copper, Zinc, 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. 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. Ownership information
  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 10101914
MRDS ID D011998
Record type Site
Current site name Little Bell Shaft
Alternate or previous names Daly West Group, United Park City Mines, Little Bell Mine, Park Utah Consolidated Mines
Related records 10179563

Geographic coordinates

Geographic coordinates: -111.50911, 40.61105 (WGS84)
Elevation 2612
Relative position 1500 FT N 47 E FROM USLM 7

Site location context

Political divisions (FIPS codes)

Summit(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)

Upper Weber(hydrologic unit)

Weber(hydrologic accounting unit)

Great Salt Lake(hydrologic subregion)

Great Basin(hydrologic region)

Geographic areas

Country State County
United States Utah Summit

Public Land Survey System information

Meridian Township Range Section Fraction State
Salt Lake 002S 004E 28 SW OF SW OF SW Utah

Comments on the location information

  • INFO FROM LAND.ST :1983

Commodities

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

Materials information

Materials Type of material
Anglesite Ore
Cuprite Ore
Galena Ore
Gold Ore
Sphalerite Ore
Tetrahedrite Ore
Calcite Gangue
Quartz Gangue
Pyrite Unknown

Alteration

  • (Local) Oxidation

Analytical data

Result 21% PB, 76 OZ/TON AG, .05 OZ/TON AU, 2.25% CU

Host and associated rocks

  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Rock unit name Weber Quartzite;Park City Formation
    Rock description Weber Quartzite;Park City Formation
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone

Nearby scientific data

(1) -111.50911, 40.61105

Economic information

Geologic structures

Type of structure Local
Structure description East-West Striking Faults
Type of structure Regional
Structure description Uinta-Cottonwood Arch, Sevier Overthrust Belt, Park City Anticline

Ore body information

  • General form TABULAR
    Strike N 90 E
    Dip 90 S
    Depth to top 91.44M

Controls for ore emplacement

  • East-West Striking Faults

Comments on the geologic information

  • BEDDING DIPS 20 TO 30 DEGREES TO THE NORTHWEST

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1880
Year of first production 1906

Mining district

District name Park City District

Land status

Ownership category Private

Ownership information

  • Type Owner
    Owner United Park City Mines Co.

Workings at the site

  • Type of workings Underground
    Length 1036.32M
    Overall depth 243.84M

Comments on the workings information

  • AS OF 1912 THE SHAFT WAS 753 FT DEEP WITH LEVELS AT DEPTHS OF 100,200, 300, AND 500 FT. THE 100 FT LEVEL EXTENDS 200 FT SOUTH, THE 200 FT LEVEL EXTENDS 400 FT NORTH AND NORTHWEST, THE 300 FT LEVEL EXTENDS 900 FT SOUTH, AND THE 500 FT LEVEL HAS ABOUT 1100 FT OF WORKINGS EXTENDING NORTH, WEST AND SOUTHWEST FROM THE SHAFT. THE 300 FT LEVEL OF THIS MINE CONNECTS WITH THE 200 FT LEVEL OF THE QUINCY MINE

Comments on development

  • CLAIMS LOCATED IN 1880 AND TUNNEL DRIVEN AT CREEK LEVEL. IN 1901 SYSTEMATIC EXPLORATION WAS BEGUN AS THE RICH DALY WEST AND QUINCY ORES WERE DISCOVERED. LITTLE BELL SHAFT WAS STARTED IN 1901. RICH LEAD ORE STRUCK IN 1906 AND 1909-1910. NEW DISCOVERIES OF ORE MADE IN 1911-1912. PROPERTY CONSOLIDATED WITH PARK UTAH CONSOLIDATED MINES IN 1920 AND WITH UNITED PARK CITY MINES IN 1953

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit ORE FOUND IN THREE EAST-WEST STRIKING FRACTURE ZONES WHICH DIP VERTICALLY. THE NORTHLY ZONE IS NEARLY BARREN AND THE MIDDLE ZONE MOST PRODUCTIVE. THE SOUTHERN ZONE MAY MERGE WITH THE MIDDLE ZONE AT DEPTH. ORE WAS HIT AT THE 300 FT AND 500 FT LEVELS. ORE GENERALLY OCCURS ALONG THE FAULT CONTACT BETWEEN QUARTZITE AND LIMESTONE
Deposit AMOUNT OF ORE PRODUCED IS UNREPORTED BUT SAID TO BE RELATIVELY SMALL ; INFO.SRC : 1 PUB LIT

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