Skip to main content
Log in

Trona resources in southwest Wyoming

  • Articles
  • Published:
Nonrenewable Resources Aims and scope Submit manuscript

Abstract

Bedded trona (Na2CO3·NaHCO3·2H2O) in the lacustrine Green River Formation of Eocene age in the Green River Basin, southwest Wyoming, constitutes the largest known resource of natural sodium carbonate in the world. In this study, 116 gigatons (Gt) of trona ore are estimated to be present in 22 beds, ranging from 1.2 to 11 meters (m) in thickness. Of this total, 69 Gt of trona ore are estimated to be in beds containing less than 2 percent halite and 47 Gt in beds containing 2 or more percent halite. These 22 beds underlie areas of about 130 to more than 2,000 km2 at depths ranging from about 200 m to more than 900 m below the surface. The total resource of trona ore in the basin for which drilling information is available is estimated to be about 135 Gt.

Underveloped trona beds in the deeper southern part of the basin may be best developed by solution mining. Additional unevaluated sodium carbonate resources are present in disseminated shortite (Na2CO3·2CaCO3) in strata interbedded with the trona and in shallow sodium carbonate brines in the northeast part of the basin. Estimates of the shortite and brine resources were not made.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Similar content being viewed by others

References

  • Brown, N.A., 1995, Union Pacific instrumental in developing Wyoming trona: Mining Engineering, v. 47, p. 135–141.

    Google Scholar 

  • Burnside, M.J., and Culbertson, W.C., 1979, Trona deposits in the Green River Basin, Sweetwater, Uinta, and Lincoln Counties, Wyoming: U.S. Geological Survey Open-File Report 79-737, 28 plates, 10 p.

  • Culbertson, W.C., 1966, Trona in the Wilkins Peak Member of the Green River Formation, southwestern Wyoming,in Geological Survey research 1966: U.S. Geological Survey Professional Paper 550-B, p. B159–B164.

  • Culbertson, W.C., 1969, Oil shale in the Green River Formation, Green River Basin, Wyoming,in Wyoming Geological Association Guidebook, 21 st Annual Field Conference, p. 191–195.

  • Culbertson, W.C., Smith, J.W., and Trudell, L.G., 1980, Oil shale resources and geology of the Green River Formation in the Green River Basin, Wyoming: U.S. Department of Energy Laramie Energy Technology Center Report of Investigations 80/6, 102 p.

  • Dana, G.F., and Smith, J.W., 1973, Black trona water, northern Green River Basin,in Wyoming Geological Association Guidebook, 25th Field Conference: p. 153–156.

  • — 1976, Nature of black water occurrence, northern Green River Basin: Wyoming Geological Association Earth Sciences Bulletin, v. 9, no. 1, p. 9–16.

    Google Scholar 

  • Day, Roger, 1994, [preprint] White River nahcolite solution mine: Society for Mining, Metallurgy, and Exploration National Meeting, Feb. 14–17, 1994, Albuquerque, N. Mex., 4 p.

  • Dyni, J.R., Wiig, S.V., and Grundy, W.D., 1995, Trona resources in the Green River Basin, southwest Wyoming: Society for Mining, Metallurgy, and Exploration Annual Meeting, Denver, Colo., Preprint 95-138, 14 p.

  • Fahey, J.J., 1962, Saline minerals of the Green River Formation: U.S. Geological Survey Professional Paper 405, 50 p.

  • Kostick, D.S., 1992, Soda ash [annual report]: U.S. Department of the Interior, Bureau of Mines, 23 p.

  • Leigh, R.T., 1990, Wyoming trona—Anoverview of the geology and economic utilization,in 1990 Abstracts with Programs, Rocky Mountain Section: Geological Society of America, v. 22, no. 6, p. 19.

  • Lindeman, H.B., 1954, Sodium carbonate brine and trona deposits in Sweetwate County, Wyoming: U.S. Geological Survey Circular 35, 10 p.

    Google Scholar 

  • Mendenhall, W.C., 1940, Occurrence of a deposit of trona: Science, New Series, v. 91, no. 2349, p. 11–12.

    Google Scholar 

  • Phillips, T.E., 1978, Potential methods for resource recovery from black water on the northern Green River Basin of Wyoming: U.S. Department of Energy, Laramie Energy Technology Center Report of Investigation 78/21, 25 p.

  • Rosar, E.C., 1993, Method and apparatus for solution mining [of water-soluble evaporite minerals]: United State Patent 5,246,273, 17 p.

  • Schultz, A.R., 1910, Deposits of sodium salts in Wyoming,in Contributions to economic geology, 1909: U.S. Geological Survey Bulletin 430, p. 570–589.

  • Swanson, V.E., and Ging, T.G., 1972, Possible economic value of trona-leonardite mixtures: U.S. Geological Survey Professional Paper 800-D, p. D71-D74.

    Google Scholar 

  • Trudell, L.G., 1975, Lithologic description of samples submitted for assay [from Union Pacific Railroad Co., core hole El Paso 44-3 in sec. 3, T. 15 N., R. 109 W., Sweetwater County, Wyoming: U.S. Bureau of Mines Laramie Energy Research Center, 57 p.

    Google Scholar 

  • Webring, Michael, 1981, MINC-A gridding program based on minimum curvature: U.S. Geological Survey Open-File Report 81-1224, 41 p.

  • Wiig, S.V., Dyni, J.R., and Grundy, W.D., 1995, Trona resources of southwest Wyoming: U.S. Geological Survey Open-File Report, 88 p.

Download references

Author information

Authors and Affiliations

Authors

Rights and permissions

Reprints and permissions

About this article

Cite this article

Dyni, J.R., Wiig, S.V. & Grundy, W.D. Trona resources in southwest Wyoming. Nat Resour Res 4, 340–352 (1995). https://doi.org/10.1007/BF02263381

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Issue Date:

  • DOI: https://doi.org/10.1007/BF02263381

Key words

Navigation