White Bluff Prospect

Occurrence in Luna county in New Mexico, United States with commodity Fluorine-Fluorite
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. Alteration
  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. Ownership information
  16. Links to other databases
  17. Bibliographic references
  18. General comments
  19. Reporter information

Geologic information

Identification information

Deposit ID 10013679
MRDS ID D010101
Record type Site
Current site name White Bluff Prospect
Related records 10295964

Geographic coordinates

Geographic coordinates: -107.75754, 31.99042 (WGS84)
Location accuracy 500(meters)
Relative position 19 MI S 05 E OF DEMING, NM

Site location context

Political divisions (FIPS codes)

Luna(county)

New Mexico(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

West Lime Hills(quadrangle 1:24,000 scale)

Columbus(quadrangle 1:100,000 scale)

El Paso(quadrangle 1:250,000 scale)

Hydrologic units (watersheds)

Mimbres(hydrologic unit)

Mimbres(hydrologic accounting unit)

Rio Grande-Mimbres(hydrologic subregion)

Rio Grande(hydrologic region)

Geographic areas

Country State County
United States New Mexico Luna

Public Land Survey System information

Meridian Township Range Section Fraction State
New Mexico 027S;027S 008W;009W 06,07;01,12 SW (06); NW (07); SE (01); NE (12) New Mexico

Commodities

Commodity Importance
Fluorine-Fluorite Critical Primary

Materials information

Materials Type of material
Fluorite Ore
Calcite Gangue
Quartz Gangue

Alteration

  • (Local) Silicification

Analytical data

Result TWO SAMPLES FROM THE JASPERIZED AREA AVERAGED 48.6% CAF2, 45.9% SIO2, AND 3.1% CACO3. TWO SAMPLES FROM BRECCIA IN LAKE VALLEY LIMESTONE AVERAGED 50.6% CAF2, 40.5% SIO2, AND 7.4% CACO3.

Host and associated rocks

  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Shale
    Rock unit name Lake Valley Limestone
    Rock description Lake Valley Limestone
    Stratigraphic age (youngest) Mississippian
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone

Nearby scientific data

(1) -107.75754, 31.99042

Economic information

Geologic structures

Type of structure Regional
Structure description Nw Trending Basin And Range Fault
Type of structure Local
Structure description Nw Trending Fault

Ore body information

  • General form PODS, LENSES

Controls for ore emplacement

  • Brecciated Faults In Favorable Horizons, Particularly Where Rocks Are Jasperized

Economic information about the deposit and operations

Development status Occurrence
Commodity type Non-metallic
Deposit size Small
Significant No

Ownership information

  • Type Operator
    Owner James E. Wilson
    Home office Brady, Tx.
    First year 1978
  • Type Owner
    Owner Barbara L. And Frances Leach
    Home office Deming, N.M.
    First year 1978

Comments on the workings information

  • A FEW TEST PITS, ALL LESS THAN 15 FT DEEP HAVE BEEN DUG.

Comments on development

  • PROPERTY CONSISTS OF WHITE BLUFF UNPATENTED MINING CLAIMS NOS. 1 TO 7.

Reference information

Bibliographic references

  • Deposit

    MCANULTY, WN, 1978, NMBMMR MEM 34, P. 41

General comments

Subject category Comment text
Deposit PENNSYVANIAN-PERMIAN ROCKS ARE STRONGLY JASPERIZED IN A SWATH 50 TO 200 FT WIDE FOR A DISTANCE OF SEVERAL HUNDRED FEET ADJACENT TO A NW TRENDING BASIN AND RANGE FAULT WHICH BRINGS THE PENN-PERM ROCKS IN CONTACT WITH TERTIARY GILA CONGLOMERATE. THIS JASPERIZED AREA CONSTITUTES THE PRINCIPAL SOURCE OF FLUORSPAR ON THE CLAIMS. MOST, IF NOT ALL OF SEVERAL ARROYOS IN THE AREA ARE DEVELOPED ON FAULTS. A LINEAR, BRECCIATED ZONE IN THE LAKE VALLEY LIMESTONE ALONGSIDE ONE FAULT-CONTROLLED ARROYO IN THE SW CORNER OF THE PROPERTY IS STRONGLY MINERALIZED WITH FLUORITE.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-FEB-1983 Haug, Jerry L. (Worl, Ronald G.) U.S. Geological Survey

Beyond USGS

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