| Deposit ID | 10098120 |
|---|---|
| MRDS ID | I001007 |
| Record type | Site |
| Current site name | Paddy Mccullochs Mountain |
| Geographic coordinates: | 149.14166, -31.17272 (WGS84) |
|---|---|
| Elevation | 610 |
| Location accuracy | 250(meters) |
| Relative position | 3 KM WEST OF YEARINAN AND 17 KM NORTHWEST OF COONABARABRAN., Estimated Location, But Believed To Be Within 10 Seconds Of True Location. |
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 |
| Quartz | 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 |
| Rock unit name | Warrumbungle Volcanic Complex |
| Rock description | Warrumbungle Volcanic Complex |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | 149.14166, -31.17272 |
|---|
| General form | STRATIFORM |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Year of last production | 1956 |
| District name | Coonabarabran Area |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I001007 |
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
| Subject category | Comment text |
|---|---|
| Deposit | DIATOMITE IS INTERBEDDED WITH TUFF AND WAS DEPOSITED DIRECTLY ON JURASSIC SANDSTONE. PREVIOUS PRODUCTION WAS FROM A 1 M THICK "PURE" DIATOMITE LAYER. THE DEPOSIT INCLUDES A 2.4 M THICK DIATOMITE BRECCIA (FRAGMENTS OF DIATOMITE, BASALT, AND LAVA BOMBS CEMENTED BY TUFFACEOUS CLAY). THIS HAS LED TO POSTULATION THAT DIATOMITE WAS DEPOSITED IN A DORMANT CRATER AND SUBSEQUENTLY FRAGMENTED BY RENEWED EXPLOSIVE VOLCANIC ACTIVITY. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-AUG-91 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.