| Deposit ID | 10023330 |
|---|---|
| MRDS ID | I000192 |
| Record type | Site |
| Current site name | Tajo Copal |
| Geographic coordinates: | -85.24995, 10.18441 (WGS84) |
|---|---|
| Location accuracy | 1000(meters) |
| Relative position | Estimated Location, It Is Believed To Be Within 1 Minute Of True Location. |
Political divisions (FIPS codes)
Costa Rica(country)
North America(continent)
Land(continent)
| Country |
|---|
| Costa Rica |
| Commodity | Importance |
|---|---|
| Limestone, General | Primary |
| Materials | Type of material |
|---|---|
| Limestone | Ore |
| Result | LIMESTONE IS OF "VERY HIGH PURITY". |
|---|
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone | ||||
| Rock unit name | Barra Honda Formation | ||||
| Rock description | Barra Honda Formation | ||||
| |||||
| (1) | -85.24995, 10.18441 |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Type | Owner |
|---|---|
| Owner | B. Jimenez |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000192 |
BERRANGE, J.P., MATHER, 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 (PACOMI), 181 P
CIMRI
BERRANGE AND OTHERS, 1990.
| Subject category | Comment text |
|---|---|
| Deposit | FRESH WATER EVAPORATION RATES ARE ABOUT 3000 MM/YR AND RAINFALL IS ABOUT 12.5-25 MM/YR. TEMPERATURES RANGE FROM FREEZING TO 24 DEG C IN JUNE (WINTER) AND 9 DEG C TO 35 DEG C IN JANUARY (SUMMER). SEE MRDS RECORD I000504: SALAR DE ATACAMA-SOCIEDAD CHILENA DE LITIO. ; INFO.SRC : 1 PUB LIT |
| Deposit | LIMESTONE IS MASSIVE AND WHITE. THE BARRA HONDA LIMESTONES CROP OUT IN A SERIES OF ISOLATED KNOLL-LIKE HILLS AROUND THE HEAD OF THE GOLFO DE NICOYA IN A TRIANGULAR AREA BETWEEN NICOYA IN THE WEST, COLORADO IN THE EAST, AND STRETCHING NORTHWARDS ALMOST TO LA GUINEA. |
| Deposit | THE SALAR COVERS AN AREA OF 3000 SQ KM AND HAS A SALT NUCLEUS COVERING 1400 SQ KM. THE TOTAL SALT THICKNESS EXCEEDS 400 M. THE TOP 30 M ARE POROUS AND IMPREGNATED WITH BRINES. SEDIMENTS OCCUPY THE NORTHERN HALF OF THE SALAR, BECOMING FINER TOWARDS THE SOUTH. K, LI, AND B ARE CONCENTRATED IN THE SALAR. THE SULFATE CONTENT IS HIGHER IN THE NORTH AND THERE IS AN AREA OF HIGHER CALCIUM CONTENTS TO THE SOUTH. THE BRINE CHEMISTRY IS SUCH THAT MURIATE AND POTASH SULFATE CAN BE PRECIPITATED SEQUENTIALLY. THE DRAINAGE BASIN OF THE SALAR EXTENDS OVER AN AREA OF 13,300 SQ KM. THE LITHIUM CONCENTRATION AT ATACAMA IS 7 TIMES THAT AT SILVER PEAK, NEVADA. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-OCT-90 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.