Calichar

Occurrence in Jujuy, Argentina with commodities Boron-Borates, Travertine
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. Economic information about the deposit and operations
  10. Mining district
  11. Links to other databases
  12. Bibliographic references
  13. General comments
  14. Reporter information

Geologic information

Identification information

Deposit ID 10024194
MRDS ID I010145
Record type Site
Current site name Calichar
Alternate or previous names Violeta

Geographic coordinates

Geographic coordinates: -66.58278, -22.99751 (WGS84)

Site location context

Political divisions (FIPS codes)

Jujuy(province)

Argentina(country)

South America(continent)

Land(continent)

Geographic areas

Country State
Argentina Jujuy

Comments on the location information

  • IN A SHORT TRIBUTARY OF THE RIO BLANCO, IMMEDIATELY WEST OF VOLCANCITO.

Commodities

Commodity Importance
Boron-Borates Primary
Travertine Primary

Materials information

Materials Type of material
Travertine Ore
Ulexite Ore

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic)
    Stratigraphic age (youngest) Pliocene
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock

Nearby scientific data

(1) -66.58278, -22.99751

Economic information

Comments on the geologic information

  • IGNIMBRITES AND ALLUVIUM COVER THE HOST ROCK.

Economic information about the deposit and operations

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

Mining district

District name Rio Alumbrio Spring Area

Reference information

Bibliographic references

  • Deposit

    ALONSO, R.N., 1986, OCCURRENCE, STRATIGRAPHIC POSITION, AND GENESIS OF THE BORATE DEPOSITS OF THE PUNA REGION OF ARGENTINA: SALTA, UNIVERSIDAD NACIONAL DE SALTA, UNPUBLISHED PH.D DISSERTATION, 196 P

  • Other Database

    CIMRI

General comments

Subject category Comment text
Deposit A PAIR OF GEYSER STRUCTURES OCCUR ON THE WEST SLOPE OF A GULCH, ABOUT 30 M ABOVE THE STREAMBED. THE HIGHER GEYSER CONE IS NON-BORON-BEARING. THE LOWER HAS FORMED A DEPOSIT OF A FEW TENS OF TONS OF ULEXITE. BOTH ARE LARGELY COMPOSED OF LIMONITIC TRAVERTINE AND ARE EXTINCT.

Reporter information

Type Date Name Affiliation Comment
Reporter 04-NOV-1994 Orris, Greta J. U.S. Geological Survey

Beyond USGS

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