| Deposit ID | 10024195 |
|---|---|
| MRDS ID | I010146 |
| Record type | Site |
| Current site name | San Marcos |
| Alternate or previous names | Neptune, Huayra Yurac |
| Geographic coordinates: | -66.49945, -22.99751 (WGS84) |
|---|---|
| Elevation | 4150 |
Political divisions (FIPS codes)
Jujuy(province)
Argentina(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Argentina | Jujuy |
| Commodity | Importance |
|---|---|
| Boron-Borates | Primary |
| Travertine | Primary |
| Materials | Type of material |
|---|---|
| Travertine | Ore |
| Ulexite | Ore |
| Onyx | Gangue |
| Host or associated | Associated | ||||||||
|---|---|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Dacite | ||||||||
| Rock unit name | Zapaleri Formation | ||||||||
| Rock description | Zapaleri Formation | ||||||||
| |||||||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Mudstone |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| Rock unit name | Acoite Formation |
| Rock description | Acoite Formation |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| (1) | -66.49945, -22.99751 |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| District name | Rio Alumbrio Spring Area |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I010146 |
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POSITION, AND GENESIS OF THE BORATE DEPOSITS OF THE PUNA REGION OF ARGENTINA: SALTA, UNIVERSIDAD NACIONAL DE SALTA, UNPUBLISHED PH.D DISSERTATION, 196 P.
ALONSO, R.N., AND VIRAMONTE, J.G., 1985, PROVINCIA BORATIFERA CENTROANDINA: ANTOFAGASTA, IV CONGRESSO GEOLOGICAO CHILENO, V. 2(3), P. 45-61.
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | THE MAIN CONE IS PERFECTLY PRESERVED AND HAS A DRY VENT. SECONDARY VENTS ARE LOCATED A FEW METERS BELOW THE MAIN VENT. AT THE FOOT OF THIS GEYSER, THERE IS A SLOW LEAKING OF FERRUGINOUS SALINE WATER WITH A MINOR VENTING OF CO2. THE TRAVERTINE FORMING THE CONE IS YELLOW-GRAY, POROUS, AND LIMONITIC WITH A FEW LENSES OF ONYX. THE ULEXITE IS VERY PURE, WHITE, SILKY, AND HARD AND HAS A MAXIMUM THICKNESS OF 50 CM. SIMILAR, BUT SMALLER, DEPOSITS OCCUR IN THE VICINITY OF THE MAIN GEYSER, THE LARGEST AT THE EXTREME S END OF THE GULCH. FOUR OTHER B-BEARING AND ONE NON-B-BEARING GEYSERS ARE ALIGNED ALONG THE SAME SIDE OF THE RIVER. ANOTHER 8 SPRING DEPOSITS ARE NEAR THE MAIN GEYSER; 1 TO THE WEST OF THE MAIN GEYSER AND 7 IN TWO SMALL GULLIES TO THE EAST. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 04-NOV-1994 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.