| Deposit ID | 10069039 |
|---|---|
| MRDS ID | W002321 |
| Record type | Site |
| Current site name | Morro Do Ferrothorium and Rare-Earth |
| Geographic coordinates: | -46.56566, -21.79745 (WGS84) |
|---|---|
| Elevation | 1500 |
| Relative position | 15 KM SOUTH OF TOWN OF POCOS DE CALDAS. |
Political divisions (FIPS codes)
Sao Paulo(province)
Brazil(country)
South America(continent)
Land(continent)
| Country | State |
|---|---|
| Brazil | Sao Paulo |
| Commodity | Importance |
|---|---|
| Thorium | Primary |
| REE Critical | Primary |
| Aluminum Critical | Primary |
| Iron | Primary |
| Materials | Type of material |
|---|---|
| Allanite | Ore |
| Bastnaesite | Ore |
| Bauxite | Ore |
| Cerianite | Ore |
| Gibbsite | Gangue |
| Kaolin | Gangue |
| Limonite | Gangue |
| Sandstone | Gangue |
| Tuff | Gangue |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Metamorphic Rock > Metasedimentary Rock | ||||
| |||||
| Host or associated | Associated |
|---|---|
| Rock type | Plutonic Rock > Granitoid > Granite |
| Host or associated | Host |
|---|---|
| Rock type | Plutonic Rock > Alkalic Intrusive Rock > Nepheline Syenite |
| (1) | -46.56566, -21.79745 |
|---|
| General form | LENTICULAR |
|---|---|
| Strike | N 55 W |
| Dip | NE |
| Thickness | 15M |
| Length | 500M |
| Width | 130M |
| Development status | Occurrence |
|---|---|
| Commodity type | Metallic |
| Significant | No |
| Discovery year | 1953 |
| Type | Owner-Operator |
|---|---|
| Owner | Companhia Geral De Minas |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | W002321 |
WEDOW, H., 1967, THE MORRO DO FERRO THORIUM AND RARE-EARTH ORE DEPOSIT, POCOS DE CALDAS DISTRICT, BRAZIL GEOLOGICAL SURVEY BULLETIN 1185-D34
WEDOW, HELMUTH, 1967, THE MORRO DO FERRO THORIUM AND RARE-EARTH ORE DEPOSIT, POCOS DE CALDAS DISTRICT, BRAZIL GEOLOGICAL SURVEY BULLETIN 1185-D34.
1953 DIREXPL WHITE, M.G., AND TOLBERT, G.E.
1956 DIREXPL HELMUTH WEDOW
| Subject category | Comment text |
|---|---|
| Deposit | THE AGE OF MINERALIZATION IS NOT KNOWN BUT THE MINERALS WERE DEPOSITED EITHER CONTEMPORANEOUSLY WITH THE MAGNETITE OR DEPOSITED LATER. THERE IS POSSIBILITY OF A CARBONATITE BEING PRESENT IN THE DEPOSIT. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-APR-1974 | Warfle, Thomas M. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.