| Deposit ID | 10023615 |
|---|---|
| MRDS ID | I000803 |
| Record type | Site |
| Current site name | St. Johns |
| Geographic coordinates: | -109.30872, 34.50396 (WGS84) |
|---|---|
| Location accuracy | 10000(meters) |
| Relative position | Estimated Location, May Be Several Minutes Incorrect. |
Political divisions (FIPS codes)
Apache(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Saint Johns North(quadrangle 1:24,000 scale)
Saint Johns(quadrangle 1:100,000 scale)
Saint Johns(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Little Colorado(hydrologic unit)
Little Colorado(hydrologic accounting unit)
Little Colorado(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
ST(Federal land areas administered by ST)
| Country | State | County |
|---|---|---|
| United States | Arizona | Apache |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 013N | 029E | 30 | Arizona |
| Commodity | Importance |
|---|---|
| Silica | Primary |
| Semiprecious Gemstone | Primary |
| Materials | Type of material |
|---|---|
| Petrified Wood | Ore |
| Host or associated | Associated | ||||||
|---|---|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock | ||||||
| Rock unit name | Chinle Formation | ||||||
| Rock description | Chinle Formation | ||||||
| |||||||
| Host or associated | Host |
|---|---|
| Rock type | Unconsolidated Deposit > Gravel |
| (1) | Chinle Formation |
|---|
| Development status | Past Producer |
|---|---|
| Commodity type | Both |
| Significant | No |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | I000803 |
PEIRCE, H.W., 1969, GEM MATERIALS, IN USGS, ABM, AND USBR, MINERAL AND WATER RESOURCES OF ARIZONA: ABM BULLETIN 180, USGS BULLETIN 871, P. 359
| Subject category | Comment text |
|---|---|
| Deposit | PETRIFIED WOOD AND OTHER FINELY CRYSTALLINE VARIETIES OF QUARTZ OCCUR IN GRAVELS THAT CAP THE HIGHER SURFACES IN THIS AREA. THE SILICA MATERIALS WERE PROBABLY DERIVED FROM THE CHINLE FM. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-FEB-92 | Orris, Greta J. | U.S. Geological Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.
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