| Deposit ID | 10400480 |
|---|---|
| Record type | District |
| Current site name | Crooks Gap - Green Mountain Uranium District |
| Alternate or previous names | Crooks Gap - Green Mountain uranium area |
| Point of reference | Approximate |
|---|---|
| Geographic coordinates: | -107.8292, 42.39 (WGS84) |
| Location accuracy | 10000(meters) |
| Relative position | District should be depicted as a polygon, not a point. These coordinates are near the western edge of the approx. 160 sq. mi. "district", at the major mines near Crooks Gap. |
Political divisions (FIPS codes)
Fremont(county)
Wyoming(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Jeffrey City(quadrangle 1:24,000 scale)
Bairoil(quadrangle 1:100,000 scale)
Casper(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Sweetwater(hydrologic unit)
North Platte(hydrologic accounting unit)
North Platte(hydrologic subregion)
Missouri(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management WY)
Bureau of Land Management WY BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Wyoming | Fremont |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 028N | 092W | 16, 20, 21, 22, 28, 29, 32 | Wyoming |
| Commodity | Importance |
|---|---|
| Uranium | Primary |
| Materials | Type of material |
|---|---|
| Uraninite | Ore |
| Coffinite | Ore |
| Uranophane | Ore |
| Autunite | Ore |
| Pyrite | Gangue |
| Calcite | Gangue |
| Selenium | Gangue |
| Result | Grade of ore mined is reported to be in the range: 0.18 to 0.23% U3O8. |
|---|
| Model code | 204 |
|---|---|
| USGS model code | 30c |
| Deposit model name | Sandstone U |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Sandstone | ||||
| Rock type qualifier | coarse-grained friable arkose sandstoens, conglomeratic sandstones, and interbedded layers of carbonaceous sandstones. | ||||
| Rock unit name | Battle Springs Formation | ||||
| |||||
| Approximate (1) | -107.8292, 42.39 |
|---|
| Type of structure | Local |
|---|---|
| Structure name | synclinal troughs |
| Operation type | Surface-Underground |
|---|---|
| Development status | Past Producer |
| Commodity type | E |
| Significant | Yes |
| District name | Crooks Gap - Green Mountain uranium area |
|---|
| Type | Unknown |
|---|---|
| Owner | Gaddis Mining Co. |
| Year | 1955 |
| Year | 2010 |
|---|---|
| Material | 4,838,938 short tons ore from 7 mines. |
| Ore mined | 4389811mt |
MINOBRAS, 1976, Uranium Guidebook for Wyoming, 63 p. and appendix.
Geological Survey of Wyoming, 1970, Mines and Minerals Map of Wyoming: Geological Survey of Wyoming, scale 1:500,000.
Stephens, J.G., 1964, Geology and uranium depoists at Crooks Gap, Fremont County, Wyoming: U.S. Geological Survey Bulletin 1147-F, 82 p, plate 1, scale 1:48,000.
Love, J.D., 1954, Wyoming, in Geological investigations of radioactive deposits, semiannual progress report, December 1, 1953 to may 31, 1954: U.S. Atomic Energy Commission TEI-440, 245 p.
MINING MAGAZINE, 1989, p. 45.
DMEA Docket No. 3462, 115 p., http://minerals.usgs.gov/dockets/scans/wy/dmea/3462_DMEA.pdf
Gregory, R.W., Jones, R.W., and Cottingham, K.D., 2010, Uranium Map of Wyoming: Wyoming State Geological Survey Map Series 94, scale 1:500,000.
Dahlkamp, F.J., Uranium deposits of the worldâUSA and Latin America, Wyoming Basins: SpringerLink, p. 149-207, available for download at http://www.springerlink.com/content/x74946/?MUD=MP. [Note that the bibliography, p. 381-414 is not available online, and since this is an online only publication, it is therefore not available at all].
DMEA Docket No. 3688, http://minerals.usgs.gov/dockets/scans/wy/dmea/3688_DMEA.pdf
| Subject category | Comment text |
|---|---|
| General | From TEI-440, p. 180: " Yellow uranium minerals occur in sec. 32, T28N, R92W, in arkosic conglomeratic sandstone in the lower Eocene rocks on the east side of Crooks Gap. The locality has been examined by geologists of the AEC. Minerals were observed in places thorugh a section of about 75 feet of rocks, but are concentrated adjacent to carbonaceous shale partings, carbonized wood fragments, and in highly ferruginous zones. The mineral was indentified as phosphuranylite [formula omitted here], and a selected sample contains 0.17 dU. The uranium-bearing zone is about 200 feet above the base of a sequence of brown and gray coarse clastic rocks, chiefly arkosic sandstones containing lenses of giant granite boulders, variegated claystones, and carbonacous shale, the total thickness of which is more than 1,000 feet. A sample of water from a spring, likewise in sec. 32, T25N, R92W, contained 250 ppb of U. The uranium appears to have been deposited in many places where there are concentrations of carbonized wood fragments, carbonaceous shale partings, or very ferruginous sandstones." |
| General | Mill or processing facility is north of Jeffrey City. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 2010-12-10 | Wilson, Anna B. | U.S. Geological Survey | Added mentions from DMEA Docket 3992 on 17-jan-2012. |
Supplemental information added by qvyshift.com. Not part of the original USGS MRDS record.