| Deposit ID | 10042569 |
|---|---|
| MRDS ID | M060398 |
| Record type | Site |
| Current site name | Sec. 11 Clay Deposit |
| Related records | 10198549 |
| Geographic coordinates: | -118.34515, 40.22462 (WGS84) |
|---|---|
| Relative position | IN A NARROW CANYON 0.7 MI. S OF COAL CYN ROAD. |
Political divisions (FIPS codes)
Pershing(county)
Nevada(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Coal Canyon(quadrangle 1:24,000 scale)
Lovelock(quadrangle 1:100,000 scale)
Lovelock(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Lower Humboldt(hydrologic unit)
Humboldt(hydrologic accounting unit)
Black Rock Desert-Humboldt(hydrologic subregion)
Great Basin(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Nevada | Pershing |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Mount Diablo | 027N | 032E | 11 | Nevada |
| Commodity | Importance |
|---|---|
| Clay | Primary |
| Materials | Type of material |
|---|---|
| Montmorillonite | Ore |
| Calcite | Gangue |
| Quartz | Gangue |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale |
| (1) | -118.34515, 40.22462 |
|---|
| Strike | N |
|---|---|
| Dip | 30W |
| Development status | Past Producer |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| District name | Willard District |
|---|
| Ownership category | Private |
|---|
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M060398 |
JOHNSON, M.G., 1977, GEOLOGY AND MINERAL DEPOSITS OF PERSHING COUNTY, NEVADA; NBMG BULL. 89
PAPKE, 1970, MONTMORILLONITE, BENTONITE, & FULLER'S EARTH DEPOSITS IN NEVADA; NBMG BULL. 76
| Subject category | Comment text |
|---|---|
| Deposit | A CLAY BED COMFORMABLE TO THE SHALE SEQUENCE AT THIS PROSPECT IS EXPOSED IN AREA ABOUT 30 FT SQUARE, ABOUT 6 FEET THICK. CROSSCUTTING RELATIONSHIPS OF BODY AND A THIN ZONE OF HYDRATED IRON OXIDE AT THE CONTACT SUGGESTS A HYDROTHERMAL ORIGIN. THE MONTMORILLONITE IS FINE-GRAINED, SEMI-COMPACT AND HAS A BETTER THAN AVERAGE SWELLING ABILITY. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-AUG-1973 | Johnson, Maureen G. | U.S. Geological Survey | |
| Updater | 01-APR-1987 | La Pointe, D.D. | Nevada Bureau of Mines and Geology |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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