| Deposit ID | 10023632 |
|---|---|
| MRDS ID | I001009 |
| Record type | Site |
| Current site name | Tintenbar Diatomite Deposit |
| Alternate or previous names | Snow Queen Mine |
| Geographic coordinates: | 153.46524, -28.82979 (WGS84) |
|---|---|
| Relative position | 9 KM NORTHWEST OF BALLINA IN PARISH TEVEN. |
Political divisions (FIPS codes)
New South Wales(province)
Australia(country)
Australia(continent)
Land(continent)
| Country | State |
|---|---|
| Australia | New South Wales |
| Commodity | Importance |
|---|---|
| Diatomite | Primary |
| Gemstone | Tertiary |
| Materials | Type of material |
|---|---|
| Diatomite | Ore |
| Limonite | Gangue |
| Quartz | Gangue |
| Opal | Unknown |
| Result | 85.2-85.7% SIO2 |
|---|---|
| Result | 2.2-2.6% AL2O3. 6.5-10.2% FREE QUARTZ |
| Model code | 222 |
|---|---|
| USGS model code | 31s |
| Deposit model name | Lacustrine diatomite |
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Mafic Volcanic Rock > Basalt | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Diatomite |
| (1) | 153.46524, -28.82979 |
|---|
| General form | STRATIFORM |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Year of first production | 1916 |
| Year of last production | 1975 |
| Production years | INTERMITTANT |
| District name | Lismore-Ballina Area |
|---|
| Type | Owner |
|---|---|
| Owner | J. H. And C.A . Johnson 2000) |
| First year | 1979 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I001009 |
HOLMES, G.G., STANLEY, C., SWEENEY, V., 1989, DIATOMITE IN NEW SOUTH WALES: GEOLOGICAL SURVEY OF NEW SOUTH WALES MINERAL RESOURCES 46, 161 P
HOLMES AND OTHERS, 1989.
| Subject category | Comment text |
|---|---|
| Deposit | PRECIOUS OPAL IS FOUND IN SOME OF THE VESICALES OF THE BASALT, BUT ARE SMALL AND HARD TO EXTRACT. GRAY COMMON OPAL IS FOUND BETWEEN LAYERS OF PARTLY RESILICIFIED DIATOMITE. THE DIATOMITE IS GOOD-QUALTITY, MASSIVE, FLAT-LYING, AND AT LEAST 4.5 M THICK. THE DIATOMITE LIES BETWEEN 2 LAYERS OF PORCELLANITE WHICH IN TURN ARE OVERLAIN AND UNDERALIN BY VESICULAR BASALT. THE PORCELLANITE IS PROBABLY DIATOMITE ALTERED BY GROUNDWATER AND (OR) HEAT AND PRESSURE. EXPOSED TO AIR, THE DIATOMITE SHOWS A SURFACE BLACKENING EFFECT. SLIGHT LIMONITE STAINING IS PRESENT THROUGHOUT THE DEPOSIT. THE DEPOSIT HAS EXTENSIVE BASALTIC OVERBURDEN. THE DIATOMITE WAS DEPOSITED IN A LAKE WHICH FORMED ON THE UNEVEN SURFACES OF THE EARLIER LAVA FLOWS. SIMILAR SMALL DEPOSITS ARE POSSIBLE ELSEWHERE. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-AUG-1991 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.