Whitehouse Group

Past Producer in Mohave county in Arizona, United States with commodity Magnesite
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. Host and associated rocks
  9. Nearby scientific data
  10. Economic information about the deposit and operations
  11. Mining district
  12. Links to other databases
  13. Bibliographic references
  14. General comments
  15. Reporter information

Geologic information

Identification information

Deposit ID 10099389
MRDS ID TC10256
Record type Site
Current site name Whitehouse Group
Alternate or previous names Martin Claims, Whitehouse Claims

Geographic coordinates

Geographic coordinates: -114.43942, 35.0403 (WGS84)
Relative position WEST SIDE OF BLACK MOUNTAINS IN WESTERN ARIZONA NEAR OATMAN, AZ.

Site location context

Political divisions (FIPS codes)

Mohave(county)

Arizona(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Oatman(quadrangle 1:24,000 scale)

Davis Dam(quadrangle 1:100,000 scale)

Kingman(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Havasu-Mohave Lakes(hydrologic unit)

Lower Colorado(hydrologic accounting unit)

Lower Colorado(hydrologic subregion)

Lower Colorado(hydrologic region)

Federal lands

Bureau of Land Management(Bureau of Land Management AZ)

Bureau of Land Management AZ BLM(Type of land area)

BLM(Federal land areas administered by BLM)

Geographic areas

Country State County
United States Arizona Mohave

Public Land Survey System information

Meridian Township Range Section Fraction State
Gila and Salt River 019N 020W 07,08,17,18,20 Arizona

Commodities

Commodity Importance
Magnesite Primary

Materials information

Materials Type of material
Brucite Ore
Magnesite Ore
Serpentine Ore
Calcite Gangue
Dolomite Gangue

Host and associated rocks

  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Stratigraphic age (youngest) Pliocene
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Trachyte
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Latite
  • Host or associated Host
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite

Nearby scientific data

(1) -114.43942, 35.0403

Economic information

Comments on the geologic information

  • THE BLACK MOUNTAINS ARE IN A TILTED FAULT BLOCK IN WHICH THE VOLCANIC ROCKS STRIKE NORTHWARD AND DIP EASTWARD. AT OATMAN, THE VOLCANIC ROCKS DIP ABOUT 12 DEGREES EAST BUT TO THE WEST THEY DIP MORE STEEPLY.

Economic information about the deposit and operations

Development status Past Producer
Commodity type Metallic
Significant No
Discovery year 1943

Mining district

District name Oatman District

Comments on development

  • DIAMOND DRILLED IN THE 1940'S. ; ECON.COM: DEPOSITS ARE TOO SMALL AND TOO LOW GRADE TO BE MINED PROFITABLY.

Reference information

Bibliographic references

  • Deposit

    GALBRAITH, F.W., 1947, MINERALS OF ARIZONA: ABM BULLETIN NO. 153, P. 48.

  • Deposit

    ERICKSEN, G.E., 1969, "BRUCITE AND MAGNESITE", IN ABM BULLETIN 180, USGS BULLETIN 871, P. 320-324.

  • Deposit

    PEIRCE, H.W., 1990, ARIZONA GEOLOGICAL SURVEY INDUSTRIAL MINERALS CARD FILE.

  • Deposit

    PHILLIPS, K.A., 1987, ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES MINERAL REPORT 4, 185 P.

  • Other Database

    CIMRI

General comments

Subject category Comment text
Deposit THE BRUCITE DEPOSITS ARE LAYERS AS MUCH AS 30 FT THICK RESTING ON THE ALCYONE TRACHYTE, THE OLDEST UNIT OF THE MID-UPPER TERTIARY VOLCANIC ROCK SEQUENCE. THE DEPOSITS ARE GENERALLY OVERLAIN BY OATMAN ANDESITE BUT AT SEVERAL PLACES THE BRUCITE LAYERS APPEAR TO BE WITHIN THE ANDESITE. SOME LAYERS AS MUCH AS 4-5 FT THICK BUT MOSTLY THINLY LAMINATED MATERIAL OF ALTERNATING BANDS OF CONTRASTING SHADES OF GREEN, GRAY, YELLOW, AND WHITE. FRESH BRUCITE RANGES FROM SERPENTINE GREEN TO LIGHT GRAY TO ALMOST WHITE. THE BRUCITE IS CRYPTOCRYSTALLINE AND DENSE WITH SUBCONCHOIDAL FRACTURE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-SEP-1991 Carbonaro, Marguerite M. U.S. Geological Survey
Updater 01-DEC-1992 Orris, Greta J. U.S. Geological Survey

Beyond USGS

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

Authoritative Arizona resources

These are landing pages for further research — the state agencies don't currently expose per-mine deep links.