| Deposit ID | 10095636 |
|---|---|
| MRDS ID | M058735 |
| Record type | Site |
| Current site name | Hurricane Cliffs Clay Deposit |
| Related records | 10055116 |
| Geographic coordinates: | -113.22052, 37.4497 (WGS84) |
|---|---|
| Elevation | 1682 |
| Relative position | 13,100 FEET S 30 E FROM THE FORT HARMONY MONUMENT |
Political divisions (FIPS codes)
Washington(county)
Utah(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Kolob Arch(quadrangle 1:24,000 scale)
Saint George(quadrangle 1:100,000 scale)
Cedar City(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Upper Virgin(hydrologic unit)
Lower Colorado-Lake Mead(hydrologic accounting unit)
Lower Colorado-Lake Mead(hydrologic subregion)
Lower Colorado(hydrologic region)
| Country | State | County |
|---|---|---|
| United States | Utah | Washington |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| Salt Lake | 038S | 012W | 32 | SW OF NE OF NE | Utah |
| Commodity | Importance |
|---|---|
| Clay | Primary |
| Materials | Type of material |
|---|---|
| Alunite | Ore |
| Host or associated | Associated |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| Host or associated | Host |
|---|---|
| Rock type | Volcanic Rock (Aphanitic) > Pyroclastic Rock > Tuff |
| (1) | -113.22052, 37.4497 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Cordillern Hingeline, Sevier Overthrust Belt |
| Type of structure | Local |
| Structure description | Hurricane Fault |
| General form | IRREGULAR |
|---|---|
| Depth to top | 0M |
| Development status | Occurrence |
|---|---|
| Commodity type | Non-metallic |
| Deposit size | Small |
| Significant | No |
| District name | Hurricane Cliffs Area |
|---|
| Ownership category | State |
|---|
| Type of workings | Underground |
|---|---|
| Length | 30.48M |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | M058735 |
VAN SANT, J.N., 1964, REFRACTORY-CLAY DEPOSITS OF UTAH: U.S. BUREAU OF MINES INFORMATION CIRCULAR 8213, 176 P
| Subject category | Comment text |
|---|---|
| Deposit | VAN SANT STATES THAT THE HYDROTHERMAL DEPOSIT IS HETEROGENEOUS AND CHANGES IN QUALITY AND CHARACTER ABRUPTLY WITHIN A SHORT DISTANCE. CLAYS FORM A MATRIX FOR LARGE BOULDERS AND FORMS VEINLETS. BRECCIATED AND ALTERED ROCKS HOST THE VEINLETS. IGNEOUS ROCKS ARE HOSTS. TWO TYPES OF MATERIALS OCCUR, A HIGH-DUTY REFRACTORY CLAY AND ALUNITE-RICH MATERIAL. THE TWO MATERIALS ARE CLOSELY MIXED. NO LARGE BODIES OF UNIFORMLY ALTERED ROCK OCCUR, INDICATING THAT PROSPECT IS PROBABLY NOT COMMERCIAL. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JAN-1985 | Shubat, Michael A. | Utah Geological and Mineral Survey |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.