| Deposit ID | 10023341 |
|---|---|
| MRDS ID | I000213 |
| Record type | Site |
| Current site name | Balangero |
| Geographic coordinates: | 7.51871, 45.49889 (WGS84) |
|---|---|
| Location accuracy | 10000(meters) |
| Relative position | 30 KM NORTH OF TURIN ON THE WESTERN SIDE OF MONTE SAN VITTORE., Estimated, Believed To Be Within 5 Km. |
Political divisions (FIPS codes)
Italy(country)
Europe(continent)
Land(continent)
| Country |
|---|
| Italy |
| Commodity | Importance |
|---|---|
| Asbestos | Primary |
| Materials | Type of material |
|---|---|
| Asbestos | Ore |
| Chrysotile | Ore |
| Aragonite | Gangue |
| Calcite | Gangue |
| Magnetite | Gangue |
| Model code | 18 |
|---|---|
| USGS model code | 8d |
| Deposit model name | Serpentine-hosted asbestos |
| Host or associated | Host |
|---|---|
| Rock type | Metamorphic Rock > Serpentinite |
| Rock unit name | Lanzo Serpentinite |
| Rock description | Lanzo Serpentinite |
| (1) | 7.51871, 45.49889 |
|---|
| Length | 1000M |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Year of first production | 1920 |
| District name | Piemonte District |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000213 |
MINING MAGAZINE, 1987, BALANGERO: V. 157, NO. 1, P. 20-25
MINING MAGAZINE, 1987.
| Subject category | Comment text |
|---|---|
| Deposit | DEPOSIT IS AT THE EASTERN END OF THE LANZO SERPENTINITE. THE MINERALIZED SERPENTINITE EXTENDS FOR OVER 1 KM FROM BRIC FORCOLA (ELEVATION 859 M) IN THE WEST TO MONTE ROLEI (ELEVATION 898 M) IN THE EAST. A SMALLER LENSE CROPS OUT ALONG THE SLOPES OF MONTE GIOVETTO (ELEVATION 755 M) AND LOCAL OUTCROPS OCCUR IN A LINEAR TREND FROM MT. GIOVETTO TO BRIC COCHETTO. DEPOSIT IS LENTICULAR AND ELONGATE IN AN EAST-WEST DIRECTION AND IS ZONED. THE ZONES STRIKE NORTHWEST AND DIP 30-60 DEGREES TO THE NORTHEAST. THE MINERALIZED SERPENTINITE IS FRACTURED AND SCHISTOSE WITH A GREEN TO WHITISH-GREY COLOR. LOCALLY GEODES OF CALCITE AND ARAGONITE OCCUR. THERE IS A CORRELATION BETWEEN THE AMOUNT OF FAULTING AND THE CHRYSOTILE CONTENT. THE ASBESTOS FIBERS LIE PARALLEL TO VEIN DIRECTIONS, I.E. ARE SLIP FIBER. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-MAR-91 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.