McClure's Knob Magnetite Deposits

Occurrence in Ashe county in North Carolina, United States with commodity Iron
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. Links to other databases
  14. Bibliographic references
  15. General comments
  16. Reporter information

Geologic information

Identification information

Deposit ID 10026393
MRDS ID K004804
Record type Site
Current site name McClure's Knob Magnetite Deposits
Alternate or previous names Tolley Cut
Related records 10223778

Geographic coordinates

Geographic coordinates: -81.44232, 36.5348 (WGS84)
Relative position ABOUT 1.3 MILES W OF STATE RT. 16 BRIDGE OVER HELTON CREEK, AND JUST EAST OF DIRT ROAD OVER DIVIDE WEST OF KNOB.

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 APPROXIMATE; IT IS JUST NORTH OF MAIN SUMMIT OF MC CLURE'S KNOB, WHICH IS NOT NAMED ON MAP.

Commodities

Commodity Importance
Iron Primary

Comments on the commodity information

  • SAMPLE LOCALITIES ON MC CLURE'S KNOB ARE THE TOLLEY CUT, THE TUNNEL, BLEVIN'S FORGE, AN OUTCROP, AND PRICE OPENING. THE PHOSPHOROUS CONTENT OF THE MC CLURE'S KNOB ORES IS CONSIDERED AS HIGH, RANGING FROM 0.03 TO 1.12%.

Materials information

Materials Type of material
Magnetite Ore
Epidote Gangue
Hornblende Gangue

Analytical data

Result BAYLEY (1923) GIVES ANALYSES FOR SIX LOCALITIES AROUND THE KNOB
Result FINE, GRANULAR MAGNETITE ORE MIXED WITH HORNBLENDE FROM THE TOLLEY CUT CONTAINED 44.87% FE, 23.23% SIO2, 0.036% S, 0.053% P, AND A P:FE RATIO OF 0.118.

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) -81.44232, 36.5348

Economic information

Geologic structures

Type of structure Regional
Structure description Northeast

Ore body information

  • General form LENS, PINCH AND SWELL
    Thickness 0.91M

Comments on the geologic information

  • BAYLEY (1923) DESCRIBES THE HOST ROCK AS MICACEOUS SCHIST, HORNBLENDE SCHIST, AND GNEISS.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Significant No

Mining district

District name Poison Branch Belt Of Deposits

Comments on the workings information

  • WORKINGS INCLUDE A 500 - FOOT ADIT, AND SEVERAL TRENCHES AND PITS. LENSES OF MAGNETITE AS MUCH AS 3 FEET THICK WERE FOUND IN SOME OF THE OPENINGS. THE COUNTRY ROCK STRIKES N 50 E AND DIPS SOUTHEAST. BAYLEY (1923) STATES THAT THE MANY PITS AND EXPOSURES INDICATES THAT THE VEIN IS NEARLY CONTINUOUS OVER THE KNOB.

Comments on development

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

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.