| Deposit ID | 10056443 |
|---|---|
| MRDS ID | TC00259 |
| Record type | Site |
| Current site name | Unidentified Clay Occurrence. |
| Geographic coordinates: | -111.00211, 36.01335 (WGS84) |
|---|
Political divisions (FIPS codes)
Coconino(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Tuba City SE(quadrangle 1:24,000 scale)
Tuba City(quadrangle 1:100,000 scale)
Marble Canyon(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Moenkopi Wash(hydrologic unit)
Little Colorado(hydrologic accounting unit)
Little Colorado(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
BIA(Federal land areas administered by BIA)
| Country | State | County |
|---|---|---|
| United States | Arizona | Coconino |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 030N | 012E | 02 | Arizona |
| Commodity | Importance |
|---|---|
| Clay | Primary |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| Rock unit name | Cow Springs Formation;Dakota Sandstone |
| Rock description | Cow Springs Formation;Dakota Sandstone |
| (1) | -111.00211, 36.01335 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC00259 |
KIERSCH, G.A., 1955, MINERAL RESOURCES NAVAJO-HOPI INDIAN RESERVATIONS, ARIZONA-UTAH: U OF A.
ARIZONA GEOLOGICAL SURVEY FILES, 1990 (PEIRCE).
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-1992 | Wells, Tina M. (Orris, Greta J.) | U.S. Geological Survey | |
| Updater | 01-MAY-1995 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
These are landing pages for further research — the state agencies don't currently expose per-mine deep links.