Francis Magnetite Mine and Henninger Prospects

Past Producer in Ashe county in North Carolina, United States with commodities Iron, Manganese
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Commodities
  6. Materials information
  7. Host and associated rocks
  8. Nearby scientific data
  9. Geologic structures
  10. Ore body information
  11. Economic information about the deposit and operations
  12. Mining district
  13. Ownership information
  14. Links to other databases
  15. Bibliographic references
  16. General comments
  17. Reporter information

Geologic information

Identification information

Deposit ID 10026390
MRDS ID K004800
Record type Site
Current site name Francis Magnetite Mine and Henninger Prospects
Alternate or previous names French Mine

Geographic coordinates

Geographic coordinates: -81.4876, 36.50036 (WGS84)
Relative position 0.9 MILE SSW OF LITTLE PINEY CHURCH, JUST NORTH OF DIRT ROAD ON RIDGE JUST WEST OF PINEY CREEK.

Site location context

Political divisions (FIPS codes)

Ashe(county)

North Carolina(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Grassy Creek(quadrangle 1:24,000 scale)

Wytheville(quadrangle 1:100,000 scale)

Winston-Salem(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Upper New(hydrologic unit)

Kanawha(hydrologic accounting unit)

Kanawha(hydrologic subregion)

Ohio(hydrologic region)

Geographic areas

Country State County
United States North Carolina Ashe

Comments on the location information

  • LOCATION IS VERY APPROXIMATE. HENNINGER PROSPECTS ARE 600 FEET TO THE WEST; LAT-LONG VALUES FROM THE NATIONAL ATLAS ARE FOR THE LOCATION APPROXIMATELY 0.9 MILES SSW OF LITTLE PINEY CHURCH

Commodities

Commodity Importance
Iron Primary
Manganese Critical Tertiary

Materials information

Materials Type of material
Magnetite Ore

Analytical data

Result NITZE (IN BAYLEY, 1923) NOTES THAT ORE CARRIES AN EXCESSIVE AMOUNT OF MOISTURE
Result ANALYSIS OF FLOAT ORE FROM SLOPE: 27.23% FE, 3.49% SIO2, 5.22% MN, 0.058% P, 42.60% H2O, P:FE RATIO 0.213

Host and associated rocks

  • Host or associated Associated
    Rock type Metamorphic Rock > Gneiss
    Rock unit name Cranberry Gneiss: Augen Gneiss And Porphyritic Gneiss (Rankin, Espenshade, And Neuman, 1972)
    Rock description Cranberry Gneiss: Augen Gneiss And Porphyritic Gneiss (Rankin, Espenshade, And Neuman, 1972)
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Neoproterozoic
    Stratigraphic age (youngest) Neoproterozoic
  • Host or associated Host
    Rock type Metamorphic Rock > Gneiss

Nearby scientific data

(1) -81.4876, 36.50036

Economic information

Geologic structures

Type of structure Regional
Structure description Northeast

Ore body information

  • General form LENS, PINCH AND SWELL

Comments on the geologic information

  • NITZE (IN BAYLEY, 1923) DESCRIBES THE ORE AS SOFT AND MANGANIFEROUS ON THE OUTCROP, CONTAINING SCATTERED GRAINS OF HARD MAGNETITE. GRANULAR MAGNETITE ORE WAS FOUND ON THE NEIGHBORING HENNINGER PROPERTY.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Significant No

Mining district

District name Poison Branch Belt Of Deposits

Ownership information

  • Type Owner
    Owner Francis, Robert

Comments on the workings information

  • THE ORE ZONE IS 10 FEET IN WIDTH AND THINS OVER A SHORT DISTANCE. THE MAIN CUT IS ABOUT 250 FEET ABOVE THE CREEK; A CAVED TUNNEL 75 FEET IN LENGTH HAD BEEN DRIVEN AT THE ROADSIDE. BAYLEY (1923) SAYS THAT VERY LITTLE IS KNOWN ABOUT THE TWO SMALL CUTS ON THE HENNINGER PROPERTY TO THE WEST.

Comments on development

  • ECON.COM: THE MAGNETITE IS EASILY SEPARATED FROM GANGUE AND IS EXCEPTIONALLY LOW IN PHOSPHOROUS AND SULFUR.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit ACCORDING TO BAYLEY (1923), THE POISON BRANCH BELT IS A CONTINUOUS SERIES OF DEPOSITS, WITH EACH DEPOSIT COMPRISED OF A NUMBER OF NEARLY PARALLEL, CLOSELY SPACED VEINS. COMMERCIAL PORTIONS OF THE ORE BODIES ARE "...IN THE FORM OF VEINS OR DIKES OF RICH MAGNETITE THAT CUT MASSES OF LEANER ORE. THE LEAN ORE COMPRISES THE LENSES." BAYLEY DOES NOT DESCRIBE THE HOST ROCK, BUT IT IS PRESUMED TO BE CRANBERRY GNEISS, AS SHOWN ON THE GEOLOGIC MAP (RANKIN, ESPENSHADE, AND NEUMAN, 1972). ; INFO.SRC : 1 PUB LIT

Reporter information

Type Date Name Affiliation Comment
Reporter 01-NOV-1975 Hale, Robin C. U.S. Geological Survey

Beyond USGS

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