| Deposit ID | 10062184 |
|---|---|
| MRDS ID | TC35486 |
| Record type | Site |
| Current site name | Dripping Springs Valley Chabazite |
| Geographic coordinates: | -110.99153, 33.73285 (WGS84) |
|---|---|
| Location accuracy | 1000(meters) |
| Relative position | ABOUT 23 MILES SOUTH OF GLOBE, ARIZONA. |
Political divisions (FIPS codes)
Gila(county)
Arizona(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Meddler Wash(quadrangle 1:24,000 scale)
Seneca(quadrangle 1:100,000 scale)
Mesa(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Salt(hydrologic unit)
Salt(hydrologic accounting unit)
Salt(hydrologic subregion)
Lower Colorado(hydrologic region)
Federal lands
Tonto National Forest(National Forest)
National Forest FS(Type of land area)
FS(Federal land areas administered by FS)
| Country | State | County |
|---|---|---|
| United States | Arizona | Gila |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Gila and Salt River | 005N | 013E | 35 | Arizona |
| Commodity | Importance |
|---|---|
| Zeolites | Primary |
| Clay | Tertiary |
| Materials | Type of material |
|---|---|
| Chabazite | Ore |
| Erionite | Ore |
| Calcite | Gangue |
| Chlorite | Gangue |
| Dolomite | Gangue |
| Feldspar | Gangue |
| Illite | Gangue |
| Kaolinite | Gangue |
| Quartz | Gangue |
| Host or associated | Host | ||
|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Mudstone > Claystone | ||
| |||
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone |
| Host or associated | Host |
|---|---|
| Rock type | Sedimentary Rock > Carbonate > Limestone |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Felsic Volcanic Rock > Rhyolite |
| (1) | -110.99153, 33.73285 |
|---|
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Significant | No |
| Ownership category | |
|---|---|
| Area name | Tonto National Forest |
| Type | Owner |
|---|---|
| Owner | Anaconda Minerals Co. (Division Of Atlantic Richfield) |
| First year | 1983 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | TC35486 |
PHILLIPS, K.A., 1987, ARIZONA INDUSTRIAL MINERALS: ARIZONA DEPARTMENT OF MINES AND MINERAL RESOURCES REPORT 4, 185 P.
BOWIE, M.R., BARKER, J.M., AND PETERSON, S.L., 1987, COMPARISON OF SELECTED ZEOLITE DEPOSITS OF ARIZONA, NEW MEXICO, AND TEXAS, IN PEIRCE, H.W., ED., PROCEEDINGS OF THE 21ST FORUM ON THE GEOLOGY OF INDUSTRIAL MINERALS: ARIZONA BUREAU OF GEOLOGY AND MINERAL TECHNOLOGY GEOLOGICAL SURVEY BRANCH SPECIAL PAPER 4, P. 37-43.
EYDE, TED, WILKINSON, P.A.K., AND WEILAND, E.F., 1986, FIELD TRIP TO SELECTED INDUSTRIAL MINERAL DEPOSITS OF ARIZONA, IN BEATTY, BARBARA, AND WILKINSON, P.A.K., EDS., FRONTIERS IN GEOLOGY AND ORE DEPOSITS OF ARIZONA AND THE SOUTHWEST: ARIZONA GEOLOGICAL SOCIETY DIGEST, V. XVI, P. 312-318.
CIMRI
| Subject category | Comment text |
|---|---|
| Deposit | FORMED IN A CLOSED-HYDROLOGIC, SHALLOW-LAKE BASIN. CHABAZITE IN ALTERED VITRIC TUFF OF GRAYISH-WHITE COLOR. THERE ARE 2 POTENTIALLY COMMERCIAL, CHABAZIE-RICH TUFFS IN THE VALLEY. THE MAIN ZEOLITE TUFF UNDERLIES ABOUT 1 SQ MILE OF BASIN FILL, IS 0.25 TO 1.74 FT THICK, AND CONTAINS UP TO 90% CHABAZITE. THE UPPER ZEOLITE TUFF UNDERLIES OVER 3 SQ MILES OF BASIN FILL, AVERAGES 1.5 FT THICK, AND CONTAINS APPROXIMATELY 67% CHABAZITE. CHABAZITE CONTENT INCREASES BASINWARD. THE MAIN TUFF IS STRATIGRAPHICALLY THE LOWEST TUFF EXPOSED. THE UPPER ZEOLITE TUFF IS 5 FT STRATIGRAPHICALLY ABOVE THE MAIN ZEOLITE TUFF. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-DEC-1992 | Orris, Greta J. | U.S. Geological Survey | |
| Updater | 01-AUG-1993 | Orris, Greta J. | U.S. Geological Survey | |
| Updater | 19-SEP-1994 | 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.