Unnamed Talc Prospect

Occurrence in Swain county in North Carolina, United States with commodity Talc-Soapstone
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 10026152
MRDS ID K002640
Record type Site
Current site name Unnamed Talc Prospect
Related records 10199870

Geographic coordinates

Geographic coordinates: -83.66878, 35.28955 (WGS84)
Relative position 0.4 MILE NORTH OF MOUTH OF QUEEN'S CREEK

Site location context

Political divisions (FIPS codes)

Swain(county)

North Carolina(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Hewitt(quadrangle 1:24,000 scale)

Fontana Lake(quadrangle 1:100,000 scale)

Knoxville(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Upper Little Tennessee(hydrologic unit)

Upper Tennessee(hydrologic accounting unit)

Upper Tennessee(hydrologic subregion)

Tennessee(hydrologic region)

Federal lands

Nantahala National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Croatan National Forest(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

National Forests in North Carolina(National Forest)

National Forest FS(Type of land area)

FS(Federal land areas administered by FS)

Geographic areas

Country State County
United States North Carolina Swain

Commodities

Commodity Importance
Talc-Soapstone Tertiary

Materials information

Materials Type of material
Talc Ore

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) Neoproterozoic
  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Quartzite
    Rock unit name Murphy Marble, White To Bluish-Gray Or-Black, Fine-To Coarse-Grained Marble;Brasstown Schist-Thin Bedded Schist And Micaceous Quartzite
    Rock description Murphy Marble, White To Bluish-Gray Or-Black, Fine-To Coarse-Grained Marble;Brasstown Schist-Thin Bedded Schist And Micaceous Quartzite

Nearby scientific data

(1) -83.66878, 35.28955

Economic information

Geologic structures

Type of structure Regional
Structure description Northeast-Trending Strike Belts Defining A Major Syncline

Ore body information

  • General form IRREGULAR

Comments on the geologic information

  • THE OCCURRENCE IS DESCRIBED BY VAN HORN (1948) AS "...TALCOSE, SERPENTINIZED SCHIST..."

Economic information about the deposit and operations

Development status Occurrence
Commodity type Non-metallic
Significant No

Mining district

District name Murphy Marble Belt

Comments on the workings information

  • NEARLY ALL OF THE PITS AND TUNNELS, OF WHICH LITTLE IS KNOWN, ARE CAVED AND COVERED WITH DEBRIS.

Comments on development

  • ECON.COM: ECONOMIC DEPOSITS OF TALC ARE NOT LIKELY TO OCCUR IN SCHIST OF THE MURPHY MARBLE BELT.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit THE WHITE, FINE-GRAINED, DOLOMITIC MARBLE ZONE WHICH LOCALLY CONTAINS TALC DEPOSITS IS AT THE APPROXIMATE STRATIGRAPHIC CENTER OF THE FORMATION (VAN HORN, 1948). THE MURPHY MARBLE LIES STRATIGRAPHICALLY ABOVE AND TO THE SOUTHEAST OF THE BRASSTOWN SCHIST IN THIS VICINITY.

Reporter information

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

Beyond USGS

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