| Deposit ID | 10005839 |
|---|---|
| MRDS ID | BL00062 |
| Record type | Site |
| Current site name | Laguna Busch O Kalina |
| Geographic coordinates: | -67.21197, -22.60725 (WGS84) |
|---|---|
| Elevation | 4530 |
Political divisions (FIPS codes)
Potosi(province)
Bolivia(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Bolivia | Potosi |
| Commodity | Importance |
|---|---|
| Bromine | Primary |
| Potassium | Tertiary |
| Lithium Critical | Tertiary |
| Boron-Borates | Tertiary |
| Strontium | Tertiary |
| Sodium | Tertiary |
| Materials | Type of material |
|---|---|
| Brine | Ore |
| Result | A SINGLE SAMPLE OF TURBID LAKE WATER COLLECTED IN AUGUST, 1990 RAN 500 PPM B, 200 PPM LI, 20 PPM SR, 1110 PPM K, 2780 PPM NA, 526 PPM CA, 120 PPB TI, AND 130 PPB MO. BRINE CHEMISTRY INDICATES THAT THIS LAKE HAS A NA-CL-(SO4) BRINE (NA AND CL ARE GREATER THAN 25 MOLE PERCENT AND SO4 IS 5 TO 25 MOLE PERCENT). SEE RISACHER AND FRITZ (1991) FOR INFLOW WATER ANALYSES |
|---|---|
| Result | THEY ALSO REPORT LAKE SURFACE WATER CHEMISTRY WHERE TEMP = 8.8 DEG C, PH = 8.3, AND DENSITY = 1.052 G/CUBIC CM. |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Lake Sediments | ||
| |||
| (1) | -67.21197, -22.60725 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Both |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | BL00062 |
AUGUST, 1990: BRIEF VISIT BY S. ASHER-BOLINDER (USGS) AND J.E. SORIA (GEOBOL) TO COLLECT WATER SAMPLE
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | LAGUNA BUSCH O KALINA HAS NO EVAPORITE PRECIPITATE AROUND OR ON THE EASTERN EXTREMES OF THE LAKE. RISACHER AND FRITZ CLASSIFY THIS SITE AS A LAKE WITH A MEAN DEPTH OF 0.6 M. THE WATER SAMPLE COLLECTED BY THE USGS WAS COLLECTED FROM THE EAST SIDE OF THE LAKE ON A WINDY DAY AND THE WATER WAS TURBID, YELLOW, OPAQUE, AND WHITE-CAPPED. THE SAMPLE MAY HAVE BEEN CONTAMINATED BY SIGNIFICANT QUANTITIES OF LAKE-BOTTOM SEDIMENTS. A SAMPLE OF INFLOW WATER FROM CERRO COJINO AT THE EAST END OF THE LAKE WAS ACID (PH = 4.5) AND HAD A VERY LOW TOTAL DISSOLVED SOLIDS CONTENT. THERE ARE SEVERAL OTHER INLETS INTO THIS BASIN AND FOUR OLDER LAKE TERRACES CAN BE IDENTIFIED ON BASINAL SLOPES ABOVE THE LAGUNA. EXTENSIVE SALAR AREAS SHOW ON THE MAPS JUST TO THE SOUTHWEST OF LAGUNA BUSCH O KALINA; SMALLER SALAR AREAS RIM THE NORTHERNMOST SHORE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-NOV-1990 | Orris, Greta J. (Asher-Bolinder, Sigrid) | U.S. Geological Survey | |
| Updater | 03-MAY-1994 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.