Cuatro Palmas Fluorspar Deposit

Producer in Coahuila De Zaragoza, Mexico with commodity Fluorine-Fluorite
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 10107279
MRDS ID W006955
Record type Site
Current site name Cuatro Palmas Fluorspar Deposit
Related records 10182540

Geographic coordinates

Geographic coordinates: -102.33932, 29.29746 (WGS84)
Elevation 1280
Relative position 130 AIR KM SE OF MARATHON, TEXAS. ABOUT 30 KM EAST OF BIG BEND NATIONAL PARK, TEXAS, AND SEVERAL KILOMETERS NW OF AGUACHILE.

Site location context

Political divisions (FIPS codes)

Pima(county)

Arizona(state)

United States(country)

North America(continent)

Land(continent)

USGS map quadrangles

Boquillas(quadrangle 1:100,000 scale)

Emory Peak(quadrangle 1:250,000 scale)

Geographic areas

Country State
Mexico Coahuila De Zaragoza

Comments on the location information

  • LATITUDE AND LONGITUDE ARE FOR THE APPROXIMATE CENTER OF THE PICO ETERO DISTRICT.

Commodities

Commodity Importance
Fluorine-Fluorite Critical Primary

Comments on the commodity information

  • FLUORITE IS BRECCIATED AND MICROCRYSTALLINE. IT IS COLORED PURPLE, WHITE, PINK, YELLOW, OR RED AND HAS COON-TAIL BANDING.

Materials information

Materials Type of material
Fluorite Ore
Calcite Gangue
Quartz Gangue

Analytical data

Result CAF2 - 70%
Result CACO3 - 18%
Result SIO2 - 5%
Result OTHER - 7% (MCANULTY, 1963, P. 741)

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite
    Stratigraphic age (youngest) Pliocene
    Stratigraphic age (youngest) Early Cretaceous
    Stratigraphic age (youngest) Early Cretaceous
  • Host or associated Host
    Rock type Sedimentary Rock > Carbonate > Limestone
    Rock unit name Georgetown Limestone
    Rock description Georgetown Limestone

Nearby scientific data

(1) -102.33932, 29.29746

Economic information

Geologic structures

Type of structure Regional
Structure description Nw-Trending Synclinorium Bounded On The Ne By The Serranias Del Burro And On The Sw By The Sierra Del Carmen
Type of structure Local
Structure description Cuatro Palmas Dome And Rhyolite Dike

Ore body information

  • General form IRREGULAR (INVERTED CONE)
    Length 90M
    Width 90M
    Depth to top 0M

Controls for ore emplacement

  • Faulted Contact Between The Rhyolite Dike And Strongly Brecciated Limestone

Economic information about the deposit and operations

Development status Producer
Commodity type Non-metallic
Deposit size Medium
Significant No
Year of first production 1953

Mining district

District name Pico Etero District

Ownership information

  • Type Operator
    Owner La Domincia, Sa
  • Type Owner
    Owner La Domincia, Sa (49% Owned By E. I. Dupont De Nemours And Co. Inc.)

Comments on the production information

  • A 400 MTPD MILL PROCESSES ORE FROM CUATRO PALMAS AND AGUACHILE MINES.

Workings at the site

  • Type of workings Surface
    Area 0.64HA
    Overall length 82.3M
    Overall width 90M

Comments on the workings information

  • ORE IS MINED IN 4 M HIGH BENCHES FROM THE QUARRY FACES.

Comments on development

  • ECON.COM: IT IS 42 KM BY ROAD TO THE FLOTATION MILL AT HEATH CROSSING. THE RAILROAD AT MARATHON IS ANOTHER 120 KM DISTANT.

Reference information

Bibliographic references

General comments

Subject category Comment text
Deposit DEPOSIT IS LOCALIZED ALONG THE FAULTED CONTACT OF A 1.8 KM RHYOLITE DIKE AND STRONGLY BRECCIATED GEORGETOWN LIMESTONE. THE DEPOSIT IS IN THE SHAPE OF AN INVERTED CONE THAT HAS A 90-M DIAMETER ON THE OUTCROP. MINERALIZATION PROBABLY OCCURRED IN SEVERAL STAGES, WITH A RHYTHMIC REPLACEMENT OF THE LIMESTONE AND BY DIRECT PRECIPITATION IN VOIDS.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-JUL-1975 Schruben, Paul G. U.S. Geological Survey
Updater 01-AUG-1991 Orris, Greta J. U.S. Geological Survey
Updater 04-JAN-1995 Orris, Greta J. U.S. Geological Survey

Beyond USGS

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