Maltby Talc Mine

Past Producer in Cherokee 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. Controls for ore emplacement
  12. Economic information about the deposit and operations
  13. Mining district
  14. Ownership information
  15. Workings at the site
  16. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10026144
MRDS ID K002628
Record type Site
Current site name Maltby Talc Mine
Related records 10175023

Geographic coordinates

Geographic coordinates: -83.95601, 35.1565 (WGS84)
Relative position NORTHWEST SIDE OF RAILROAD AT MALTBY

Site location context

Political divisions (FIPS codes)

Cherokee(county)

North Carolina(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Marble(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)

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 Cherokee

Commodities

Commodity Importance
Talc-Soapstone Primary

Materials information

Materials Type of material
Talc Ore
Quartz Gangue
Tremolite Gangue

Host and associated rocks

  • Host or associated Associated
    Rock type Plutonic Rock > Mafic Intrusive Rock > Diorite
    Rock unit name Metadiorite, Dark-Green, Locally Porphyritic, Pyroxenite & Amphibolite. Van Horn ( 1948 , P. 15 ) Terms These Rocks Metadiorite Because He Considers Them To Be Metamorphosed Diorites That Have Lost Their Feldspar & Quartz Through Metamorphism
    Rock description Metadiorite, Dark-Green, Locally Porphyritic, Pyroxenite & Amphibolite. Van Horn ( 1948 , P. 15 ) Terms These Rocks Metadiorite Because He Considers Them To Be Metamorphosed Diorites That Have Lost Their Feldspar & Quartz Through Metamorphism
  • Host or associated Host
    Rock type Metamorphic Rock > Metasedimentary Rock > Marble
  • Host or associated Host
    Rock type Metamorphic Rock > Schist > Calc-Silicate Schist

Nearby scientific data

(1) -83.95601, 35.1565

Economic information

Geologic structures

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

Ore body information

  • General form LENS

Controls for ore emplacement

  • Fracture Zone; Bedding

Comments on the geologic information

  • THE TALC APPEARS TO BE IN THE TRANSITIONAL ZONE BETWEEN THE MURPHY MARBLE AND THE ANDREWS FORMATION (TVA OPEN-FILE REPORT).

Economic information about the deposit and operations

Development status Past Producer
Commodity type Non-metallic
Significant No
Discovery year 1900

Mining district

District name Murphy Marble Belt

Ownership information

  • Type Operator
    Owner J. W. Bailey

Comments on the production information

  • ANNUAL PRODUCTION IS PRE - 1900

Workings at the site

  • Type of workings Surface/Underground
    Overall length 30.48M
    Overall width 18.29M

Comments on the workings information

  • COUNTRY ROCK STRIKES N 35 E AND DIPS FROM 50 TO 70 SOUTH. THE PIT IS REPORTED TO HAVE BEEN 10 TO 20 FEET DEEP AROUND 1900, WITH SEVERAL SHAFTS IN THE BOTTOM OF THE CUT, WHICH WAS FILLED WITH WATER IN 1944. THE SHAFTS ARE REPORTED (VAN HORN, 1948) TO HAVE BEEN AS DEEP AS 30 FEET.

Comments on development

  • THE SOUTHERN MINERAL COMPANY MINED TALC AT THIS LOCALITY AROUND 1900. THE MOST-RECENT WORK ON THE PROPERTY WAS DONE BY J.W. BAILEY DURING 1939-1940. ; ECON.COM: TREMOLITE CONTENT IS TOO HIGH TO MEET MODERN SPECICATIONS

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.

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.