Loma Camastro

Producer in Guanacaste, Costa Rica with commodity Diatomite
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. Ore body information
  10. Economic information about the deposit and operations
  11. Links to other databases
  12. Bibliographic references
  13. General comments
  14. Reporter information

Geologic information

Identification information

Deposit ID 10106731
MRDS ID I000188
Record type Site
Current site name Loma Camastro

Geographic coordinates

Geographic coordinates: -85.49996, 10.81021 (WGS84)
Relative position ON NATIONAL COORDINATES: 3722, 3100

Site location context

Political divisions (FIPS codes)

Guanacaste(province)

Costa Rica(country)

North America(continent)

Land(continent)

Geographic areas

Country State
Costa Rica Guanacaste

Commodities

Commodity Importance
Diatomite Primary

Comments on the commodity information

  • CURRENT PRODUCTION (1990) IS USED AS ANTI-CAKING AGENT FOR FERTILIZER. BULK DENSITY 242-299 KG/CUBIC M.

Materials information

Materials Type of material
Diatomite Ore
Cristobalite Gangue
Quartz Gangue

Host and associated rocks

  • Host or associated Associated
    Rock type Volcanic Rock (Aphanitic) > Intermediate Volcanic Rock > Andesite
    Stratigraphic age (youngest) Pleistocene
    Stratigraphic age (youngest) Pleistocene
  • Host or associated Host
    Rock type Sedimentary Rock > Clastic Sedimentary Rock > Lake Sediments

Nearby scientific data

(1) -85.49996, 10.81021

Economic information

Ore body information

  • Thickness 100M

Economic information about the deposit and operations

Development status Producer
Commodity type Non-metallic
Significant No

Comments on the production information

  • APPROXIMATE ANNUAL PRODUCTION.

Reference information

Bibliographic references

  • Deposit

    BERRANGE, J.P., MATHERS, S.J., MORALES C., NURY, AND ALVARADO V., FERNANDO, 1990, THE NON-METALLIC INDUSTRIAL MINERALS AND ROCKS OF COSTA RICA: SAN JOSE, COSTA RICA, PROYECTO ANGLO-COSTARRICENSE DE MINERALES INDUSTRIALES, 181 P

  • Other Database

    CIMRI

  • Production

    BERRANGE ET AL (1990).

General comments

Subject category Comment text
Deposit THE DIATOMITE FORMS PART OF A >100 M THICK LACUSTRINE SEQUENCE WHICH INFILLS A BASIN AT LEAST 5 SQ KM IN SIZE. IN THE NORTH PART OF THE BASIN, THE DIATOMITE FORMS THE UPPER PART OF THE SEQUENCE. INFERENCE FROM SURFACE EVIDENCE SUGGESTS THAT THE DIATOMITE MAY BE 80-100 M THICK LOCALLY. LOCALLY, THE DIATOMITE IS OVERLAIN BY AN ANDESITIC FLOW, BUT IN OTHER AREAS FORMS THE SURFACE ROCK. THIS IS THOUGHT TO BE THE LARGEST DIATOMITE DEPOSIT IN COSTA RICA.

Reporter information

Type Date Name Affiliation Comment
Reporter 01-MAY-1990 Orris, Greta J. U.S. Geological Survey
Updater 01-OCT-1994 Page, Norman J. U.S. Geological Survey

Beyond USGS

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