J.W. Cooper Prospect

Occurrence in Cherokee 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. Alteration
  8. Host and associated rocks
  9. Nearby scientific data
  10. Ore body information
  11. Controls for ore emplacement
  12. Economic information about the deposit and operations
  13. Mining district
  14. Ownership information
  15. Links to other databases
  16. Bibliographic references
  17. General comments
  18. Reporter information

Geologic information

Identification information

Deposit ID 10026108
MRDS ID K002578
Record type Site
Current site name J.W. Cooper Prospect
Related records 10256863

Geographic coordinates

Geographic coordinates: -83.9324, 35.07511 (WGS84)
Relative position 0.8 MILE NORTHWEST OF ANDREWS DAM, ON THE WEST SIDE OF CALHOUN BRANCH

Site location context

Political divisions (FIPS codes)

Cherokee(county)

North Carolina(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Peachtree(quadrangle 1:24,000 scale)

Fontana Lake(quadrangle 1:100,000 scale)

Knoxville(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Hiwassee(hydrologic unit)

Middle Tennessee-Hiwassee(hydrologic accounting unit)

Middle Tennessee-Hiwassee(hydrologic subregion)

Tennessee(hydrologic region)

Geographic areas

Country State County
United States North Carolina Cherokee

Comments on the location information

  • LOCATION IS APPROXIMATE

Commodities

Commodity Importance
Iron Primary
Manganese Critical Primary

Materials information

Materials Type of material
Goethite Ore
Limonite Ore

Alteration

  • (Local) Weathering Of Iron-Bearing Minerals To Form Limonite

Analytical data

Result USBM ANALYSIS, GRAB SAMPLE: 54.5% FE
Result 5.2% SI
Result 0.08% S
Result AND 0.70% P

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Rock unit name Metadiorite; Precambrian; Dark-Green, Locally Porphyritic, Pyroxenite And Amphibolite. Van Horn (1948, P. 15) Terms These Rocks Metadiorite Because He Considers Them To Be Metamorphosed Diorites That Have Lost Their Feldspar And Quartz Through Metamorphism
    Rock description Metadiorite; Precambrian; Dark-Green, Locally Porphyritic, Pyroxenite And Amphibolite. Van Horn (1948, P. 15) Terms These Rocks Metadiorite Because He Considers Them To Be Metamorphosed Diorites That Have Lost Their Feldspar And Quartz Through Metamorphi
    Stratigraphic age (youngest) Holocene
  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Marble
    Rock unit name Residuum; Recent.;Andrews Formation-Thin Alt. Layers Of Marble And Biotite Schist;Murphy Marble, White-Bluish Gray-Black Fine-Coarse
    Rock description Residuum; Recent.;Andrews Formation-Thin Alt. Layers Of Marble And Biotite Schist;Murphy Marble, White-Bluish Gray-Black Fine-Coarse

Nearby scientific data

(1) -83.9324, 35.07511

Economic information

Ore body information

  • General form LINEAR, IRREGULAR

Controls for ore emplacement

  • Bedding, Fractures, And Residuum

Comments on the geologic information

  • FLOAT ORE OCCURS AS "BOMBSHELL", PEBBLE, AND SHOT-SIZED MATERIAL, VARYING FROM LIGHT YELLOW TO DARK BROWN OR RED. LIMONITE ALSO OCCURS AS BANDED LAYERS IN THE SCHIST.

Economic information about the deposit and operations

Development status Occurrence
Commodity type Metallic
Significant No

Mining district

District name Brasstown Belt Of Murphy Marble

Ownership information

  • Type Owner
    Owner J. S. Cooper Heirs; George S. Evans (Heirs)

Comments on the workings information

  • SURFACE CONCENTRATIONS OF LIMONITE OCCUR AS SCATTERED BOULDERS AND MASSES ALONG A 1,000 FOOT INTERVAL, ALONG ANOTHER 300 FOOT INTERVAL, AND A THIRD AREA WHICH IS OVAL AND ABOUT 150 FEET LONG. THE SCHIST STRIKES FROM DUE NORTH TO N 20 E, AND DIPS FROM 16 TO 20 W.

Comments on development

  • EXCEPT FOR A FEW OLD, SHALLOW, PARTLY-FILLED PITS, NO WORK HAS BEEN DONE ON THE PROPERTY OTHER THAN THAT OF THE U.S. BUREAU OF MINES DURING 1944-1945. 322 FEET OF TRENCHES AND TWO DRILL HOLES TOTALING 201 FEET CONSITITUTED THEIR EXPLORATION. ; ECON.COM: GRADE OF MATERIAL DOES NOT MEET CURRENT SPECIFICATIONS FOR LOW-PHOSPHOROUS IRON ORE.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DEPOSITS OF LIMONITE OCCUR ALONG AN ISOLATED BELT OF THE MURPHY MARBLE ALMOST ALONG ITS ENTIRE LENGTH, IN THE BRASSTOWN-PEACHTREE AREA. BAYLEY (1925) MENTIONS THE POSSIBILITY THAT THE LIMONITE DEPOSITS ARE MORE CLOSELY RELATED TO THE CONTACT OF THE MURPHY MARBLE WITH ADJACENT FORMATIONS.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-OCT-1974 Hale, Robin C. U.S. Geological Survey

Beyond USGS

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