Sawyer Mine

Past Producer in Randolph county in North Carolina, United States with commodities Gold, Silver, Copper, Lead, Zinc
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. Mineral occurrence model information
  9. Host and associated rocks
  10. Nearby scientific data
  11. Geologic structures
  12. Ore body information
  13. Controls for ore emplacement
  14. Economic information about the deposit and operations
  15. Mining district
  16. Workings at the site
  17. Links to other databases
  18. Bibliographic references
  19. General comments
  20. Reporter information

Geologic information

Identification information

Deposit ID 10026505
MRDS ID K005182
Record type Site
Current site name Sawyer Mine
Related records 10273743

Geographic coordinates

Geographic coordinates: -79.91645, 35.78926 (WGS84)
Relative position 7.8 MILES NORTHWEST OF ASHEBORO AND 6.8 MILES SOUTHWEST OF RANDLEMAN.

Site location context

Political divisions (FIPS codes)

Randolph(county)

North Carolina(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Glenola(quadrangle 1:24,000 scale)

Chapel Hill(quadrangle 1:100,000 scale)

Raleigh(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Lower Yadkin(hydrologic unit)

Upper Pee Dee(hydrologic accounting unit)

Pee Dee(hydrologic subregion)

South Atlantic-Gulf(hydrologic region)

Geographic areas

Country State County
United States North Carolina Randolph

Comments on the location information

  • LOCATION APPROXIMATE

Commodities

Commodity Importance
Gold Primary
Silver Secondary
Copper Tertiary
Lead Tertiary
Zinc Critical Tertiary

Materials information

Materials Type of material
Galena Ore
Gold Ore
Pyrite Ore
Sphalerite Ore
Chlorite Gangue
Quartz Gangue
Sericite Gangue

Alteration

  • (Local) Muscovite, Chlorite, Silica

Analytical data

Result ASSAYS AND SELECTED BEDROCK SAMPLES ARE COMMONLY IN THE 0.05 TO 0.2 OPT FOR GOLD AT THE SURFACE. SEVERAL HIGH-GRADE ASSAYS OF OVER 1 OPT AU HAS BEEN REPORTED BY LUTTRELL, 1978. DRILL-HOLE ASSAYS FAILED TO INTERSECT HIGH-GRADE ASSAYS AND FOUND ONLY 0.02-0.2 OPT IN 0.75 M ASSAY INTERVALS. AG/AU COMMONLY IS FROM 1 TO 10, PB AND ZN ARE PRESENT IN QUANTITIES UP TO ABOUT 4000 PPM ZN AND 800 PPM PB.HUNDRED PPM

Mineral occurrence model information

Model code 104
USGS model code 25a
Deposit model name Hot-spring Au-Ag
Mark3 model number 45

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff
    Rock unit name Tillery Formation
    Rock description Tillery Formation
    Stratigraphic age (youngest) Early Cambrian
    Stratigraphic age (youngest) Early Cambrian
    Stratigraphic age (youngest) Early Cambrian
    Stratigraphic age (youngest) Early Cambrian
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Rock unit name Tillery Formation
    Rock description Tillery Formation

Nearby scientific data

(1) -79.91645, 35.78926

Economic information

Geologic structures

Type of structure Regional
Structure description Ne-Trending Open To Tight West-Verging Folds.
Type of structure Local
Structure description Ne Striking, N-Plunging Small-Scale Folds Indicate A Left Lateral Sense Of Shear Within The Highly Altered Rocks. Early Ne-Trending Faults May Have Been Associated With The Development Of The Nearby Rhyolitic Volcanic Center And Provided The Locus For Precious-Metal Deposits. Early Ne Tren

Ore body information

  • General form TABULAR
    Strike N 40 E
    Dip 50 NW
    Length 610M
    Width 15M
    Depth to bottom 46M

Controls for ore emplacement

  • Disrupted, Pre-Tectonic Quartz Veins And Disseminated Sulfide Accumulations. Some Redistribution Or Introduction Of Metals During Metamorphism May Have Occurred.

Comments on the geologic information

  • QUARTZ-SERICITE MYLONITE IS DEVELOPED IN THE MOST INTENSELY ALTERED PART OF THE FELSIC VOLCANIC SECTION. THE MINERALIZED ZONE CONTAINS FOLDED QUARTZ STRINGERS AND VEINLETS. FRACTURES IN THE QUARTZ ARE HEALED WITH SILICA. THE GOLD IS REPORTED TO HAVE BEEN FOUND IN FIVE OR SIX PARALLEL "BEDS". THE LODE WAS A MINERALIZED ZONE IN WHICH THE SULFIDES WERE REPORTED TO BEGIN AT A DEPTH OF 80 FT., THE BASE OF WEATHERING. THE MINERALIZED ZONE RANGES FROM 6 TO 50 FT. IN THICKNESS AND AVERAGES 15 FT. IN THE WALL ROCK, PYRITE CUBES AS LARGE AS ONE INCH ON A SIDE WERE FOUND, ALTHOUGH MOST ARE FINE-GRAINED.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Deposit size Small
Significant No
Discovery year 1850
Year of first production 1850
Year of last production 1906

Mining district

District name Carolina Slate Belt

Workings at the site

  • Type of workings Surface/Underground
    Overall depth 46M
    Overall length 548.64M
    Overall width 100M

Comments on the workings information

  • A TOTAL OF SEVEN SHAFTS, WERE OPENED ON THE VEIN WITH THE DEEPEST BEING 150 FT. IN 1968, THERE WERE EXTENSIVE WORKINGS ON THE WEST SIDE OF SR 1004. LARGE OPEN PITS WITH ACCESSIBLE PORTALS AND DRIFTS EXTENDED WEST FROM THE ROAD FOR ABOUT 500 FT. NORTHEAST OF THE ROAD MANY SHAFTS, PITS AND TRENCHES WERE OPENED ALONG A LENGTH OF ABOUT 500 FT.

Comments on development

  • THE MINE WAS FIRST WORKED PRIOR TO 1856 AND HAS SINCE BEEN SPORADICALLY WORKED. SOME PROSPECTING WAS CARRIED OUT IN THE 1930'S. TWO DIAMOND DRILLING PROGRAMS WITH 6 CORE HOLES AND APPROXIMATELY 20 REVERSE CIRCULATION HOLES WAS COMPLETED IN THE MID-1980'S BY GOLDFIELDS AND NICOR CORPORATIONS.

Reference information

Bibliographic references

  • Analytical Data

    KLEIN, UNPUBLISHED DATA; LUTTRELL, 1978, USGS OPEN-FILE REPORT 78-152.

  • Deposit

    CARPENTER, P. A., III, 1976, METALLIC MINERAL DEPOSITS OF THE CAROLINA SLATE BELT, NORTH CAROLINA: NORTH CAROLINA MINERAL RESOURCES SEC. BULL. 84, 166 P.

  • Deposit

    PARDEE, J. T., AND PARK, C. F., JR., 1948, GOLD DEPOSITS OF THE SOUTERN PIEDMONT: U.S. GEOLOGICAL SURVEY PROF. PAPER 213, 156 P.

General comments

Subject category Comment text
Deposit THREE DISTINCT VEINS OR MINERALIZED ZONES WERE MINED. THEuSULPHUR VEIN, BEING THE EASTERN MOST, AND THE MILLER VEIN, AND THEuDAVIS VEIN WHICH IS POSSIBLY AN OFFSETT SEGMENT OF THE MILLERuVEIN. ALL TREND N 40 TO N 52 DEG E AND MAY DIP AT ABOUT 45 DEGuWEST. ALTERATION AND SOME SURFACE GEOCHEMICAL ANOMALIES EXTENDuTO THE NORTH-EAST FOR A DISTANCE OF 500M BEYOND THE NORTHERN ENDuOF THE WORKINGS. TWO OTHER POSSIBLY RELATED GOLD-BEARING ZONESu, THE BRUMMEL HILL AND OLD PACE WORKINGS LIE 60 METERS TO THEuENE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-OCT-1976 Mcdaniel, Ronald D. North Carolina Division of Land Resources
Updater 01-JUN-1991 Klein, T.L. U.S. Geological Survey

Beyond USGS

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