| Deposit ID | 10023626 |
|---|---|
| MRDS ID | I001002 |
| Record type | Site |
| Current site name | Kyooma East |
| Alternate or previous names | One of the Bells Mountain Deposits |
| Geographic coordinates: | 150.63026, -30.27831 (WGS84) |
|---|---|
| Relative position | ON THE SOUTH SIDE OF BUNDARLEER ROAD, ABOUT 2.5 KM WEST OF BUNDARLEER AND 3 KM EAST OF KYOOMA WEST. |
Political divisions (FIPS codes)
New South Wales(province)
Australia(country)
Australia(continent)
Land(continent)
| Country | State |
|---|---|
| Australia | New South Wales |
| Commodity | Importance |
|---|---|
| Diatomite | Primary |
| Materials | Type of material |
|---|---|
| Diatomite | Ore |
| Clay | Gangue |
| Feldspar | Gangue |
| Model code | 222 |
|---|---|
| USGS model code | 31s |
| Deposit model name | Lacustrine diatomite |
| Host or associated | Associated | ||||
|---|---|---|---|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff | ||||
| |||||
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Clay, Mud |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Diatomite |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | 150.63026, -30.27831 |
|---|
| General form | STRATIFORM |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Year of first production | 1982 |
| District name | Barraba Area |
|---|
| Type | Owner-Operator |
|---|---|
| Owner | Australian Diatomite Mining Party Ltd. |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I001002 |
HOLMES, G.G., STANLEY, C., AND SWEENEY, V., 1989, DIATOMITE IN NEW SOUTH WALES: GEOLOGICAL SURVEY OF NEW SOUTH WALES MINERAL RESOURCES 46, 161 P
HOMES & OHTERS, 1989.
| Subject category | Comment text |
|---|---|
| Deposit | THIS DEPOSIT FORMS PART OF A LATERALLY AND VERICALLY CONSISTENT SEQUENCE OF LACUSTRINE AND PYROCLASTIC SEDIMENTS. ALTHOUGH THE LITHOLOGIES ARE SIMILAR, NO CORRELATION IS RECOGNIZED BETWEEN THE KYOOMA EAST AND KYOOMA WEST STRATIGRAPHIC SEQUENCES. THE KYOOMA EAST DEPOSIT EXHIBITS LESS FAULTING AND CONTORTION THAN THE KYOOMA WEST DEPOSIT. THE KYOOMA EAST DEPOSIT IS CAPPED BY A RELATIVELY THICK BASALT. THE INFERIOR GRADE AND QUALITY OF THIS DEPOSIT AND THE THICKNESS OF THE BASALT CAP MAKE THIS DEPOSIT CURRENTLY UNECONOMIC. |
| 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.