Tawas Quarry

Producer in Iosco county in Michigan, United States with commodity Gypsum-Anhydrite
Sections on this page
  1. Identification information
  2. Geographic coordinates
  3. Site location context
  4. Geographic areas
  5. Public Land Survey System information
  6. Commodities
  7. Materials information
  8. Mineral occurrence model information
  9. Nearby scientific data
  10. Geologic structures
  11. Ore body information
  12. Economic information about the deposit and operations
  13. Mining district
  14. Ownership information
  15. Production statistics
  16. Bibliographic references
  17. General comments
  18. Reporter information

Geologic information

Identification information

Deposit ID 10310003
MRDS ID LW00003
Record type Site
Current site name Tawas Quarry

Geographic coordinates

Geographic coordinates: -83.67988, 44.18 (WGS84)
Elevation 183
Location accuracy 1000(meters)
Relative position FROM TAWAS WEST ON M-55 7 MILES TO SAND LAKE RD, SOUTH ON SAND LAKE ROAD 2 MILES, QUARRY ON RIGHT (10 MILES FROM TAWAS), LAT/LONG POINT IS BASED ON CORNER COMMON TO SECTIONS 26,27,34,35

Site location context

Political divisions (FIPS codes)

Iosco(county)

Michigan(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

National City(quadrangle 1:24,000 scale)

Tawas City(quadrangle 1:100,000 scale)

Tawas City(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Au Gres-Rifle(hydrologic unit)

Southwestern Lake Huron(hydrologic accounting unit)

Southwestern Lake Huron(hydrologic subregion)

Great Lakes(hydrologic region)

Geographic areas

Country State County
United States Michigan Iosco

Public Land Survey System information

Meridian Township Range Section Fraction State
Michigan 022N 006E 26,27,34,35 Michigan

Comments on the location information

  • ALL SECTION 26, 27, 34, AND 35

Commodities

Commodity Importance
Gypsum-Anhydrite Primary

Materials information

Materials Type of material
Gypsum Ore

Mineral occurrence model information

Model code 253
USGS model code 35a.5 (35ae)
Deposit model name Bedded gypsum: marine evaporite gypsum

Nearby scientific data

(1) -83.67988, 44.18

Economic information

Geologic structures

Type of structure Regional
Structure description Michigan basin
Type of structure Local
Structure description Relatively flay lying beds

Ore body information

  • Name MICHIGAN FORMATION
    General form NATIONAL CITY GYPSUM MEMBER OF MICHIGAN FORMATION
    Strike FLAT
    Dip FLAT
    Thickness 5M
    Depth to top 20M
    Depth to bottom 30M
  • Thickness 2M
  • Thickness 2M

Comments on the ore body information

  • Orebody depth to top 60-80 ft., depth to bottom 90-120 ft., thickness 12-18 ft.

Comments on the geologic information

  • GYPSUM DEPOSIT CONSIST OF THREE BEDS OVERLAIN BY APPROXIMATELY 60-80 FEET OF GLACIAL BOULDER CLAY OVERBURDEN. THE BEDS ARE SEPARATED BY TWO THIN (3-5 FEET) SHALE LAYERS.

Economic information about the deposit and operations

Operation type Surface
Development status Producer
Significant Yes
Year of first production 1950

Mining district

District name Alabaster District

Ownership information

  • Type Owner
    Owner National Gypsum Company

Production statistics

  • Year 2003
    Material ore gypsum
    Ore mined 680400mt

Comments on the production information

  • AVERAGE ANNUAL PRODUCTION OVER PAST DECADE

Comments on the workings information

  • SINGLE BENCH STRIP MINE

Reference information

Bibliographic references

  • Deposit

    A.H. STEVENS, 1968, ECONOMIC POTENTIALS ON MICHIGAN'S GYPSUM DEPOSITS, CONSUMER POWER COMPANY, JACKSON, MICHIGAN.

  • Deposit

    L.I. BRIGGS, 1970, GEOLOGY OF GYPSUM IN THE LOWER PENINSULA, MICHIGAN, PROCEEDINGS SIXTH FORUM ON GEOLOGY OF INDUSTRIAL MINERALS, GEOLOGICAL SURVEY DIVISION, MICHIGAN DEPARTMENT OF NATURAL RESOURCES.

General comments

Subject category Comment text
Deposit THREE BEDS OVERLAIN BY GLACIAL BOULDER CLAY. FIRST BED IS WHITE GYPSUM BED (THICKEST), SECOND BED IS THE ORANGE GYPSUM BED (THINNEST), THE LOWEST BED IS HI-PURITY GYPSUM WITH SOME SALT (NACL). GYPSUM BEDS OCCUR AS IRREGULAR EROSIONAL SURFACE SUBCROPS AT BASE OF GLACIAL DRIFT.

Reporter information

Type Date Name Affiliation Comment
Reporter 16-AUG-01 Anderson, Arlene (M. Gere) Michigan Department of Natural Resources

Beyond USGS

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