Skene Mine

Past Producer in Jo Daviess county in Illinois, United States with commodities Lead, Zinc
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. Economic information about the deposit and operations
  14. Mining district
  15. Ownership information
  16. Workings at the site
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10106500
MRDS ID W800208
Record type Site
Current site name Skene Mine

Geographic coordinates

Geographic coordinates: -90.23678, 42.29807 (WGS84)

Site location context

Political divisions (FIPS codes)

Jo Daviess(county)

Illinois(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Elizabeth(quadrangle 1:24,000 scale)

Dubuque South(quadrangle 1:100,000 scale)

Dubuque(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Apple-Plum(hydrologic unit)

Upper Mississippi-Maquoketa-Plum(hydrologic accounting unit)

Upper Mississippi-Maquoketa-Plum(hydrologic subregion)

Upper Mississippi(hydrologic region)

Geographic areas

Country State County
United States Illinois Jo Daviess

Public Land Survey System information

Meridian Township Range Section Fraction State
27N 2E 25 SW CORNER OF NW OF SW Illinois

Commodities

Commodity Importance
Lead Primary
Zinc Critical Tertiary

Materials information

Materials Type of material
Galena Ore
Sphalerite Ore
Calcite Gangue
Dolomite Gangue
Pyrite Gangue
Quartz Gangue

Alteration

  • (Local) Leaching, Silicification, Dolomitization

Mineral occurrence model information

Model code 224
USGS model code 32a
Deposit model name Mississippi Valley, S.E. Missouri Pb-Zn
Mark3 model number 42

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Dolomite
    Rock unit name Prosser Cherty Member
    Rock description Prosser Cherty Member
    Stratigraphic age (youngest) Middle Ordovician
    Stratigraphic age (youngest) Middle Ordovician

Nearby scientific data

(1) -90.23678, 42.29807

Economic information

Geologic structures

Type of structure Regional
Structure description Southeast Of Wisconsin Dome And On The Gentle West Limb Of Wisconsin Arch. To The South Is Illinois Basin And To The West And Southwest Is Forest City Basin. A Few Minles South O Fthe Zinc-Lead District Is Westward-Trending Savanna-Sabula Anticline. Regional Strike Is N 85 W And The Dip Is South.
Type of structure Local
Structure description N 83 E Trending Crevice

Comments on the geologic information

  • THE PROSER IS A MEMBER OF THE GALENA DOLOMITE.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Significant No
Discovery year 1901
Discoverer Charles Ashmore
Year of first production 1901
Year of last production 1907

Mining district

District name Upper Mississippi Valley

Ownership information

  • Type Operator
    Owner George Skene (To ; Elizabeth Mining And Milling Co. (1902 To
    Last year 1907

Workings at the site

  • Type of workings Underground
    Name of workings ORE BODY
    Overall depth 96M

Comments on the workings information

  • THE SOUTH PITCH WAS OPENED FOR OVER 1,000 FT. THE MINE IS BELOW THE PERMANENT WATER LEVEL. SKENE WAS FORMERLY A LARGE AND IMPORTANT LEAD MINE. IN 1944, THE USBM DRILL A SERIES OF FIVE HOLES TO SEE IF A DEPOSIT OF LEAD AND EXISTED AT GREATER DEPTH. THESE HOLES CUT MINERALIZED PITH-TYPE FRACTURES, BUT THE LEAD AND ZINC DEPOSITS ARE SMALL AND LEAN. LEAD MINERAL ARE MORE COMMON THAN ZINC.

Comments on development

  • ECON.COM: SHUT DOWN IN 1907 BECAUSE OF A FALL IN THE PRICE OF LEAD AND THE HIGH COST OF MINING.

Reference information

Bibliographic references

  • Deposit

    HEYL, A.V., AGNEW, A.F., LYONS, E.J., AND BEHRE, C.H., JR., 1959, THE GEOLOGY OF THE UPPER MISSISSIPPI VALLEY ZINC-LEAD DISTRICT: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 309, 310 P.

  • Deposit

    BAIN, H.F., 1905, ZINC AND LEAD DEPOSITS OF NORTHWESTERN ILLINOIS: U.S. GEOLOGICAL SURVEY BULLETIN 246, 56 P.

  • Deposit

    COX, G.H., 1914, LEAD AND ZINC DEPOSITS OF NORTHWESTERN ILLINOIS: ILLINOIS GEOLOGICAL SURVEY BULLETIN 21, 120 P.

  • Production

    COX, 1914, P. 59

General comments

Subject category Comment text
Deposit THE UPPER MISSISSIPPI VALLEY ZINC-LEAD DISTRICT LIES WITHIN THE SO-CALLED DRIFTLESS AREA WHERE NO MANTLE OF GLACIAL DRIFT IS PRESENT TO OBSCURE THE ROCK EXPOSURES. NATURAL CAVES ARE COMMON IN THE DISTRICT.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1994 Hedgman, Cheryl (Cannon, W.F.) U.S. Geological Survey
Updater 01-MAY-1996 Sutphin, David M. U.S. Geological Survey
Editor 01-MAY-1997 Mason Jr., G.T. U.S. Geological Survey

Beyond USGS

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