| Deposit ID | 10014059 |
|---|---|
| MRDS ID | D010676 |
| Record type | Site |
| Current site name | Piceance Creek Basin Saline Deposits |
| Alternate or previous names | Piceance Creek Basin Nahcolite and Dawsonite Deposits, Piceance Basin Saline Beds |
| Geographic coordinates: | -108.3604, 39.95691 (WGS84) |
|---|---|
| Elevation | 1969 |
| Relative position | 5 TO 10 MILES N 47 W FROM RIFLE |
Political divisions (FIPS codes)
Rio Blanco(county)
Colorado(state)
United States(country)
North America(continent)
Land(continent)
USGS map quadrangles
Square S Ranch(quadrangle 1:24,000 scale)
Douglas Pass(quadrangle 1:100,000 scale)
Grand Junction(quadrangle 1:250,000 scale)
Hydrologic units (watersheds)
Piceance-Yellow(hydrologic unit)
White-Yampa(hydrologic accounting unit)
White-Yampa(hydrologic subregion)
Upper Colorado(hydrologic region)
Federal lands
Bureau of Land Management(Bureau of Land Management CO)
Bureau of Land Management CO BLM(Type of land area)
BLM(Federal land areas administered by BLM)
| Country | State | County |
|---|---|---|
| United States | Colorado | Rio Blanco |
| Meridian | Township | Range | Section | Fraction | State |
|---|---|---|---|---|---|
| 6th Principal | 001S;001S;001N;002S | 097W;098W;098W;098W | Colorado |
| Commodity | Importance |
|---|---|
| Sodium | Primary |
| Calcium | Primary |
| Aluminum Critical | Tertiary |
| Halite | Tertiary |
| Materials | Type of material |
|---|---|
| Dawsonite | Ore |
| Nahcolite | Ore |
| Halite | Gangue |
| Host or associated | Host | ||||
|---|---|---|---|---|---|
| Rock type | Sedimentary Rock > Clastic Sedimentary Rock > Shale > Oil Shale | ||||
| Rock unit name | Parachute Creek Member Of Green River Formation | ||||
| Rock description | Parachute Creek Member Of Green River Formation | ||||
| |||||
| (1) | -108.3604, 39.95691 |
|---|
| Type of structure | Regional |
|---|---|
| Structure description | Piceance Creek Basin, White River Uplift |
| Type of structure | Local |
| Structure description | Piceance Creek Dome, Red Wash Syncline, Hunter Creek Syncline |
| General form | IRREGULAR |
|---|---|
| Thickness | 335.28M |
| Length | 48279M |
| Width | 32186M |
| Depth to top | 411.48M |
| Depth to bottom | 746.76M |
| General form | IRREGULAR |
|---|
| General form | IRREGULAR |
|---|
| Development status | Producer |
|---|---|
| Commodity type | Both |
| Deposit size | Large |
| Significant | No |
| Discovery year | 1947 |
| District name | Piceance Creek Basin |
|---|
| Ownership category | Federal |
|---|
| Type | Owner |
|---|---|
| Owner | White River Nahcolite Minerals (Owned By Natec Resources Inc. (50%) North American Chemical Co. (50 |
| Type | Owner-Operator |
|---|---|
| Owner | Natural Soda Inc. |
| Year | 2011 |
| Agency | Database name | Acronym | Record ID | Notes |
|---|---|---|---|---|
| USGS | Mineral Resources Data System | MRDS | D010676 |
BEARD, T.N., AND OTHERS, 1974, NAHCOLITE AND DAWSONITE RESOURCES IN THE GREEN RIVER FORMATION, PICEANCE CREEK BASIN, COLORADO, IN MURRAY, D.K., ED., ENERGY RESOURCES OF THE PICEANCE CREEK BASIN, COLORADO: RMAG 25TH FIELD CONF. GUIDEBOOK, P. 101-109.
FARRIS, C.B., 1980, MARKET POTENTIAL OF THE GREEN RIVER NAHCOLITE/DAWSONITE IN COLORADO, IN SCHWOCHOW, S.D., ED., PROCEEDINGS OF THE FIFTEENTH FORUM ON GEOLOGY OF INDUSTRIAL MINERALS: CGS RESOURCE SER. 8, P. 96-104.
FARRIS, C.B., AND MAINS, C.J., 1978, DAWSONITE AND NAHCOLITE SURVEY, VOLUME 1--RESERVES, TECHNOLOGY, ECONOMICS, AND MARKET ASSESMENT: COLORADO SCHOOL OF MINES RESEARCH INST. (DOE DIV. INDUS. ENERGY CONSERV. CONTRACT NO. EC-77-S-07-1683).
HITE, R.J., AND DYNI, J.R., 1967, POTENTIAL RESOURCES OF DAWSONITE AND NAHCOLITE IN THE PICEANCE CREEK BASIN, NORTHWEST COLORADO: COLORADO SCHOOL OF MINES QUART., V. 62, NO. 3, P. 25-38.
NIELSEN, IRVIN, 1980, DEVELOPMENT OF NAHCOLITE-RICH OIL SHALES, IN SCHWOCHOW, S.D., ED., PROCEEDINGS OF THE FIFTEENTH FORUM ON GEOLOGY OF INDUSTRIAL MINERALS: CGS RESOURCE SER. 8, P. 89-95.
YOUNG, N.B., AND SMITH, J.W., 1970, DAWSONITE AND NAHCOLITE ANALYSES OF GREEN RIVER FORMATION OIL-SHALE SECTION, PICEANCE CREEK BASIN, COLORADO: USBM RI-7445.
CASHION, W.B., 1973, GEOLOGIC AND STRUCTURE MAP OF THE GRAND JUNCTION QUADRANGLE, COLORADO AND UTAH: USGS MAP I-736.
ROWLEY, P.D., AND OTHERS, 1979, GEOLOGIC MAP OF THE VERNAL 1X2 QUADRANGLE, COLORADO, UTAH, AND WYOMING, USGS MAP MF-1163.
INDUSTRIAL MINERALS, 1993, WORLD OF MINERALS- USA: NO. 304, P. 17.
FARRIS, 1980; BEARD AND OTHERS, 1974; INDUSTRIAL MINERALS, 1993.
The Denver Post, 2011, Colo. baking soda maker doubling its capacity: Denver Post, Sept. 6, 2011.
| Subject category | Comment text |
|---|---|
| Deposit | NAHCOLITE, DAWSONITE, AND HALITE OCCUR IN THICK INTERVAL IN LOWER PARACHUTE CREEK MEMBER OF GREEN RIVER FM. DAWSONITE INTERVAL THICKER AND MORE LATERALLY EXTENSIVE THAN NAHCOLITE AND CONSISTS OF MINUTE CRYSTALS DISSEMINATED IN OIL SHALE MATRIX, COMPRISING UP TO 25% OF DEPOSIT. CENTRAL THICKEST PART OF INTERVAL ESTIMATED TO CONTAIN AT LEAST 5 WT%. DAWSONITE HAS APPARENTLY NOT BEEN EXTENSIVELY DISSOLVED BY GROUND WATER, AND PRESENT EXTENT REPRESENTS ORIGINAL DEPOSITIONAL PATTERN. TOP OF ABUNDANT DAWSONITE ZONE MARKED BY UPPER HALITE. NAHCOLITE INTERVAL THINS AWAY FROM BASIN DEPOSITIONAL CENTER DUE TO DEPOSITIONAL THINNING AND TO POST-DEPOSITIONAL LEACHING. OVERLYING NAHCOLITE SECTION IS LEACHED ZONE CHARACTERIZED BY SOLUTION CAVITIES, OPEN FRACTURES, BRECCIA ZONES, POROUS AND EARTHY MARLSTONE. LEACHED ZONE IS STRATIGRAPHICALLY HIGHEST AT BASIN DEPOSITONAL CENTER. IN LOWER PARACHUTE CREEK MBR NAHCOLITE OCCURS AS NODULES AND RADIATING MASSES SURROUNDED BY OIL SHALE. BEDDED FORMS INCLUDE |
| Deposit | 1) WHITE COARSE CRYSTALLINE VARIETY; 2) BROWN MICROCRYSTALLINE TYPE; 3) CRYSTAL MUSH, UP TO 0.5-INCH CRYSTALS IN OIL SHALE MATRIX. INTERVAL CONTAINS SEVERAL THICK UNITS OF INTERBEDDED NAHCOLITE AND HALITE. THICKNESS AND DEPTHS REPORTED ABOVE APPROXIMATED FROM BEARD AND OTHER' (1974) CROSS-SECTION. MAXIMUM LENGTH AND WIDTH APPROXIMATED FROM BEARD AND OTHERS' (1974) ISOPACH MAP OF DAWSONITE-BEARING INTERVAL (300-FT)CONTOUR ON SOUTH TO 500-FT CONTOUR ON NORTH; 300-FT CONTOUR ON WEST TO 60-FT CONTOUR ON WEST TO 600-FT CONTOUR LIMIT OF RESOURCE EVALUATION ON EAST. |
| Type | Date | Name | Affiliation | Comment |
|---|---|---|---|---|
| Reporter | 01-JUN-83 | Schwochow, Stephen D. | Colorado Geological Survey | |
| Updater | 01-AUG-93 | Orris, Greta J. | U.S. Geological Survey | |
| Editor | 07-SEP-11 | Wilson, Anna B | U.S. Geological Survey | Merged duplicate record 10119432 (from MAS 0081030001) and corrected erroneous info and location. |
| Reporter | 14-OCT-94 | Fitzpatrick | U.S. Bureau of Mines | = 10119432 (from MAS 0081030001) |
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.