Ford Mine

Past Producer in Madison county in Missouri, 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. Host and associated rocks
  9. Nearby scientific data
  10. Ore body information
  11. Economic information about the deposit and operations
  12. Mining district
  13. Ownership information
  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 10101472
MRDS ID D003732
Record type Site
Current site name Ford Mine
Alternate or previous names Ford Bank

Geographic coordinates

Geographic coordinates: -90.21649, 37.5209 (WGS84)
Relative position TWO MILES NORTHWEST OF CORNWALL

Site location context

Political divisions (FIPS codes)

Madison(county)

Missouri(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Higdon(quadrangle 1:24,000 scale)

Farmington(quadrangle 1:100,000 scale)

Rolla(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Whitewater(hydrologic unit)

Upper Mississippi-Meramec(hydrologic accounting unit)

Upper Mississippi-Kaskaskia-Meramec(hydrologic subregion)

Upper Mississippi(hydrologic region)

Geographic areas

Country State County
United States Missouri Madison

Public Land Survey System information

Meridian Township Range Section Fraction State
5th Principal 007E 033N 25 S2 OF NE Missouri

Comments on the location information

  • SITUATED ON THE SOUTH SLOPE OF A HILL, S1/2NE1/4 SECTION 25

Commodities

Commodity Importance
Iron Primary

Materials information

Materials Type of material
Marcasite Ore
Clay Gangue

Host and associated rocks

  • Host or associated Host
    Rock type Unconsolidated Deposit > Clay, Mud
    Rock unit name Bonneterre
    Rock description Bonneterre
    Stratigraphic age (youngest) Late Cambrian
    Stratigraphic age (youngest) Late Cambrian
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
  • Host or associated Host
    Rock type Sedimentary Rock > Chemical Sediment > Chert

Nearby scientific data

(1) -90.21649, 37.5209

Economic information

Ore body information

  • General form IRREGULAR LAYER
    Thickness 9.14M
    Length 457.2M
    Width 152.4M
    Depth to top 0M
    Depth to bottom 9.14M

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No

Mining district

District name Southeast Missouri

Ownership information

  • Type Owner
    Owner C. H. Gregoyre ( 1912 )

Comments on the production information

  • SEVERAL THOUSAND TONS HAVE BEEN SHIPPED FROM THIS MINE PRIOR TO 1910.

Workings at the site

  • Type of workings Surface/Underground
    Overall depth 9.14M
    Overall length 70.1M
    Overall width 15.24M

Comments on the workings information

  • PIT AND SHAFT. DIMENSIONS OF WORKINGS ARE FOR THE PIT ONLY.

Comments on development

  • ECON.COM: THE DEPOSIT HAS APPARENTLY BEEN WORKED OUT. EXTENT AND DEPTH OF THE MARCASITE VEINS ARE UNKNOWN.

Reference information

Bibliographic references

  • Deposit

    CRANE, G. W., 1912 , THE IRON ORES OF MISSOURI: MISSOURI BUREAU OF MINES AND GEOLOGY, 2ND SER., V. 10 , P. 267 .

  • Deposit

    NASON, FRANK L., 1892 , A REPORT ON THE IRON ORES OF MISSOURI: MISSOURI GEOLOGICAL SURVEY, 1ST SER., V. 2 , P. 246 - 247 .

General comments

Subject category Comment text
Deposit AERIAL EXTENT OF ORE IS BASED ON SURFACE ORE. THICKNESS IS FOR THE LIMONITE ORE RESTING ON LIMESTONE. IT CONSISTS OF IRREGULARLY MIXED MASSES OF YELLOW AND REDDISH BROWN, POROUS LIMONITE, FREQUENTLY IN BOTRYOIDAL AND MAMMILLARY FORMS. THE BEST AND HARDEST ORE IS IN THE UPPER PART OF THE DEPOSIT. THE ORE OCCASIONALLY PASSES INTO A PURE YELLOW OCHER, IN SOME PLACES, BECOME CLAYISH WITH SEAMS OF BROWN AND RED CLAY. THE THICKNESS OF THE DEPOSIT IS VARIABLE AND IRREGULAR. REDDISH BROWN CLAY RESTS ON TOP OF THE DEPOSIT. THE LIMESTONE CONTAINS NUMEROUS SEAMS AND JOINTS CEMENTED WITH MARCASITE

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1979 Sherwood, Liz U.S. Geological Survey

Beyond USGS

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