Bentonite includes any natural material dominantly composed of clay minerals in
the smectite group (Hosterman and Patterson, 1992). Wyoming bentonite consists
of hydrous silicate of alumina, commonly referred to as montmorillonite clay.
Also known as sodium bentonite, Wyoming bentonite is high-swelling sodium
montmorillonite clay used in kitty litter (25%), drilling mud (20%), binder in
foundry molds (19%), iron ore pelletizing (13%), and other applications (23%)
(Virta, 2005). Wyoming Bentonite can swell up to 16 times its original size and
absorb up to 10 times its own weight in water. Calcium bentonite, a low or
nonswelling variety, is relatively unimportant in Wyoming production.
Bentonite, originally known as ‘mineral soap’ or ‘soap clay’, was named
‘bentonite’ in 1898 by Wilbur C. Knight for deposits in the Benton Shale near
Rock River, Wyoming. The Benton Shale included Upper and Lower Cretaceous units
lying between the Niobrara and Cloverly Formations and their equivalents.
Currenty named equivalent stratigraphic units in Wyoming include the Frontier
Formation, Carlile Shale, Greenhorn Formation, Belle Fourche Shale, Mowry Shale,
Aspen Shale, Muddy Sandstone, Newcastle Sandstone, Thermopolis Shale, Skull
Creek Shale, and Bear River Formation. The best Wyoming bentonite is found
primarily in the Upper Cretaceous Mowry Shale (Hosterman and Patterson, 1992).
According to the Wyoming
Mining Association, bentonite deposits in Wyoming comprise as much as 70
percent of the world's known supply. In 2013, Wyoming bentonite producers mined
4.1 million tons of bentonite. Surface mining to
depths no greater than about 50 feet accounts for all bentonite production.
Bentonite is mined in Wyoming from numerous pits in various areas of the state.
Major producing districts are the Northern Black Hills (Colony) District, the
Southern Black Hills (Clay Spur) District, the Kaycee District west of Kaycee,
and the Eastern Big Horn Basin. Bentonite from pits in these areas is blended,
ground, dried, and processed into various products at fifteen active mills in
Download the 2014 Wyoming Bentonite Summary Report.
Hosterman, J.W., and Patterson, S.H., 1992, Bentonite and fuller’s earth
resources of the United States: U.S. Geological Survey Professional Paper 1522,
1 plate, 45 p.
Virta, R.L., 2005, Clays: U.S. Geological Survey Mineral Commodity Summaries
Performance Minerals, Inc
Wayne Sutherland (307) 766-2286 Ext. 247
Wyoming Construction Aggregate
Natural aggregate is one of our most abundant, accessible, and widely used natural resources.
Construction aggregate consists of sand, gravel, and crushed stone.
It is primarily used by highway and building construction industries.
Wyoming’s energy industry also requires large amounts of aggregate for the construction of well pads, wind generator bases, and access roads to industrial sites.
In Wyoming, aggregate ranks fourth in value among extracted geologic resources, after oil and gas, coal, and trona. According to USGS Mineral Industry Surveys in 2013, Wyoming ranked 35th in the nation in production of construction aggregate.
Wyoming's Construction Aggregate Resource
Download the 2015 Wyoming's Construction Aggregate Resource Summary Report.
Aggregate Industry Facts
- More than 6.5 tons of aggregate (construction-grade crushed stone and sand and gravel)
were produced for every person in the United States in 2013.
- It takes 400 tons of aggregate to build the average home in America, according to the National Stone, Sand and Gravel Association.
Construction of one mile of interstate highway is estimated to require 38,000 tons of aggregate, according to the National Stone, Sand and Gravel Association.
The Wyoming Department of Transportation indicated a mile of Wyoming highway may contain more than double that amount depending on the aggregate quality, native soils, and the use of the road.
Wyoming's Aggregate Industry
In 2013, Wyoming produced 21 million metric tons of construction aggregate, down from a peak of 34 million metric tons in 2009.
The State Inspector of Mines of Wyoming reported 65 aggregate operations in 21 of 23 Wyoming counties in 2013.
These quarries produced sand and gravel (40%), general aggregate (23%), granite (16%), limestone (12%), and scoria (9%), and employed approximately 1,010 people.
Wyoming has a variety of geologic landscapes providing plentiful aggregate resources including the following:
Sand is acquired from alluvial floodplains along stream and river valleys as well as from extensive dune sands.
Windblown sand deposits occur between the western Green River Basin through Wyoming and into western Nebraska.
Sand and gravel deposits occur on the tops of benches and terraces along mountain flanks.
The quality of these deposits varies greatly, as terraces may contain areas of caliche.
Caliche-coated gravels do not bind well with asphalt or cement.
Glacial gravels are not widely used due to location in national parks and national forests.
However, they are occasionally used for local road construction projects.
Older gravels from poorly consolidated conglomerates are a source of “natural gravel”,
that are useful if they can be extracted without blasting or cutting.
Limestone crops out along the flanks of the mountain ranges, and is a significant source of crushed stone.
Limestone is the preferred rock for highway construction.
Granite is another source of crushed stone. Specifically, quartzofeldspathic gneiss is mined in the largest aggregate quarry in Wyoming,
west of Cheyenne. Railroad ballast is one of the quarry’s main products, simply because the foliation in the gneiss allows the rock to have a
2:4:6 dimensional ratio, which is a requirement of certain types of railroad ballast.
Clinker, also called scoria or baked and fused rock, is formed by the burning, baking and melting of strata overlying burning coal beds.
Clinker is found and used extensively in the Powder River Basin (PRB), where no other aggregate sources exist.
It is used for the sub-base of roads and for well-pad construction. Although it is abundant in the PRB,
clinker is not as durable and breaks down more easily than sand and gravel.
Mine tailings are a unique source of gravel in the South Pass mining district, and are used locally for road building.
Aggregate Recycling and Renewal
Recycling of aggregate, primarily re-crushing concrete and asphalt, is economically viable in many situations. The Wyoming Department of Transportation recycles and turns into new pavement nearly all
the asphalt and concrete pavement they remove from Wyoming’s roadways. There are also various processes for creating lightweight synthetic aggregate from waste products such as coal ash and sewer sludge.
Recycled aggregate sources help relieve shortages and reduce landfill waste.
Suzanne Luhr (307) 766-2286 Ext. 250
Wyoming Decorative Stone
Wyoming contains a wide variety of granite, marble, sandstone, quartzite,
gneiss, limestone, and volcanic rocks suitable for use as decorative stone.
Because the United States imports more than 80% of the dimensional stone used in
interior and exterior construction, the decorative stone industry has great
potential for growth. With convenient transportation and a wide variety of rock
types and colors available, Wyoming is one of the most promising locations for
expansion of this industry. Limited exploration for stone has occurred in
southern Wyoming during the past 12 years. Requests for local stone products,
rather than imports, appears to be driving an increasing interest in Wyoming
Dimensional stone is quarried in large blocks by sawing or drilling the stone.
The material is then either processed on site or shipped by truck to a
Wyoming contains extensive outcrops of rocks of many different colors and
lithologies suitable for use as decorative and dimensional stone. Currently, the
only dimensional stone quarry is Strid Marble & Granite’s Rawlins sandstone
quarry in the Cretaceous Mesa Verde Formation, located southeast of Rawlins.
Strid operates a stone fabrication plant near Cheyenne.
In the past, stone quarried in Wyoming was mostly used locally. Quarries near
developing towns provided stone blocks for public and private buildings, curbs,
walkways, and other purposes. During the late 1800s, three quarries in Wyoming
shipped stone to out-of-state markets. The Waterfall Quarry near Kemmerer in
western Wyoming was the source of the stone used to construct and face the city
hall in Portland, Oregon. A gray sandstone quarry near Rawlins supplied dimensional
blocks for construction of the Wyoming State Capitol, the Union Pacific Railroad
depot in Ogden, Utah, and several buildings in northern Colorado. The University Quarry in the Casper Formation near
Laramie furnished stone for about half of the buildings on the University of
Wyoming Campus. Some stone from this quarry was also used on private buildings
in Laramie and Cheyenne, Wyoming, and in Fort Collins, Colorado.
From the early 1900s through the 1950s, the Jay Em Stone Company in Jay Em,
Wyoming quarried granite, marble, onyx, quartzite, and other rock types in
eastern Wyoming and in the Black Hills of South Dakota for use as monuments and
other products. In the 1950s and 1960s, Basins, Inc. of Wheatland, Wyoming
quarried and sold several types of decorative aggregate including green
serpentine and various colors of marble. In the late 1970s, Georgia Marble
acquired Basins, and continued quarrying white marble west of Wheatland and
processing it into decorative aggregate. Georgia Marble was purchased by Imerys
Marble in March of 2000, and the pit operation closed in March of 2004.
Raven Quarries operated a site in northern Albany County where they produced two
types of granitic rocks until 2003. A black amphibolite, Wyoming Raven, quarried
here was used to construct Bill Gates' house in Seattle, Washington.
Other contracts included decorative accents in federal buildings, church
cornerstones, and monuments. The variegated pink granite, first called
Fantastico, then Mirage, was quarried until February 2003.
Wyoming continues to produce decorative aggregate and fieldstone, most of which
is sold to the Colorado Front Range and Utah Wasatch Front markets. However,
distributors in California, Illinois, and elsewhere have expressed interest in
some of these products, and have purchased small amounts of material for market
testing. Wyoming hosts nearly as many different colors and varieties of stone as
the rest of the world combined.
However, no dimension stone quarries are currently active in Wyoming.
Recommended Decorative Stone References
Further information on Wyoming’s decorative stone resources can be found in the
following WSGS publications, both of which present colorful summaries of the
wide variety of decorative stones found in Wyoming.
WSGS Public Information Circular 31, Decorative stones of Wyoming, by R.E.
Harris, 1991, 27 p.
WSGS Map Series 42, Decorative stones of southern Wyoming, by R.E. Harris, 2003,
Wayne Sutherland (307) 766-2286 Ext. 247
Gypsum is mined at three locations in Wyoming. Mountain Cement mines small
amounts of gypsum near Laramie for use as a retardant in cement. Two plants in
the Bighorn Basin of northwest Wyoming mine gypsum and process it into wallboard
at nearby plants. The gypsum wallboard plants in Wyoming, the Georgia-Pacific
Himes gypsum mill and the BPB Cody gypsum mill, have operated at capacity since
1995. Construction booms in the Wyoming market areas of the Colorado Front
Range, Utah Wasatch Front, and Pacific Northwest have increased the demand for
construction materials, including wallboard. Gypsum production declined in 2000
due to reduced demand, corporate restructuring, and plant maintenance. Celotex
sold its gypsum mining and wallboard production to British Paper Board Ltd.
(BPB), which now operates the Cody facilities under the BPB name. Wyoming has
large gypsum resources capable of supporting additional production.
Recommended Gypsum Reference
WSGS Preliminary Report 9, Gypsum deposits in the Cody area, by J.M.
Bullock and W.H. Wilson, 1969, 1 plate, 12 p.
Wayne Sutherland (307) 766-2286 Ext. 247
Trona, or natural soda ash, is a sodium sesquicarbonate compound
(Na2CO3.NaHCO3.2H2O) that occurs as an evaporite mineral in the Wilkins Peak
member of the Eocene Green River Formation in southwest Wyoming. Trona, which is
70% sodium carbonate, is refined to produce sodium compounds, particularly soda
ash (Na2CO3). Baking soda is pure soda ash. Soda ash is the second ingredient by
weight in glass after silica, where it lowers the melting temperature of silica
sand. It is also used in soaps, detergents, inorganic chemicals, water
purification, flue gas desulfurization, and a number of other products and
processes. The manufacture of compounds such as sodium phosphate, caustic soda
(NaOH), and sodium cyanide (used in gold refining) also depends on trona.
Trona is white, gray, amber, or yellow with vitreous, or glass-like, luster.
Trona is soluble in a dilute (10%) hydrochloric acid and water solution. It has
a monoclinic crystal structure and is soft, about 2.5 to 3 on the 10 point Mohs
hardness scale. For a better understanding of crystal structure, hardness, and
other characteristics of trona and other minerals, WSGS Bulletin No.72, Minerals
and Rocks of Wyoming, or a mineralogy text is recommended.
Trona deposits were first discovered in Wyoming during October of 1937 when Mountain Fuel Supply Company took core samples from the John Hay #1 well while drilling for oil and gas. Core from this well contained thick zones of trona and other evaporite minerals, some of which (such as shortite) were identified for the first time. In 1939, the United States Geological Survey (USGS) began a strategic minerals study and later published a reference to the minerals found in this core in 1940. Westvaco Chemical Corporation produced the first trona from trona Bed 17 at a depth of 1,500 feet in 1947 (Kostick, 1998).
Trona currently forms as an evaporite mineral in places such as Africa and
California. Wyoming’s trona is believed to have formed in the same manner.
During the Eocene (40 to 50 million years ago), an immense lake known as Lake
Gosiute occupied the Green River Basin. Over millions of years, Lake Gosiute
expanded and contracted due to regional climatic cycles. During intervals of
dryness and evaporation, Wyoming’s rich trona deposits were deposited in parts
of the Wilkins Peak member of the Green River Formation. The Wilkins Peak member
consists of trona beds up to 40 feet thick separated by lake-bottom shaley
sediments, sandstone, and carbonate rocks. Trona beds in the Wilkins Peak member
lie at depths of 600 to 2,000 feet beneath the Green River Basin. Other members
of the Green River Formation are sediments deposited in a freshwater lake
environment. For detailed geologic information on the various theories of trona
formation see Garrett (1998), and Leigh (1998).
Wyoming hosts the world’s largest trona deposits, an estimated resource of 127
billion tons. Of this, 40 billion tons are mineable using conventional ’hard
rock ‘ methods (Leigh, 1997). The soda ash industry in Wyoming’s Green River
Basin produces approximately 16 million tons annually. This accounted for more
than 95% of U.S. production, and about 38% of the world’s production in 2006
Download the 2014 Wyoming Trona Summary Report.
Dyni, J.R., 1997, Sodium carbonate resources of the Green River Formation,
in Jones, R.W., and Harris, R.E., (eds.), Proceedings of the 32nd
Annual Forum of Industrial Minerals – Laramie, Wyoming, May 19-21, 1996:
Wyoming State Geological Survey Public Information Circular 38, p.123-143.
Garrett, D.E., 1998, Origin of the Green River trona deposit (from a chemical
and other saline mineral perspective, in Dyni, J. R., and Jones,
R. W., (eds.), Proceedings of the first international soda ash
conference volume II: Wyoming State Geological Survey Public Information
Circular 40, p.15-20.
Hausel, W.D., 2005, Minerals & Rocks of Wyoming: Wyoming State Geological Survey
Bulletin 72, 159 p.
Kostick, D.S., 1994, Soda ash in Carr, D. D., (ed.),
Industrial minerals and rocks, 6th edition: Society for Mining, Metallurgy
and Exploration, Inc., p.929-958.
Kostick, D.S., 1998, The origin of the U.S. natural and synthetic soda ash
industries, in Dyni, J.R., and Jones, R.W., (eds.), Proceedings
of the first international soda ash conference volume I: Wyoming State
Geological Survey Public Information Circular 39, p.11-33.
Kostick, D.S., 2007, Soda Ash, in U.S. Geological Survey Mineral Commodity
Summaries, 2006, p.150-151,
website accessed 3/30/2007.
Leigh, R.T., 1997, Wyoming Trona – an overview of the geology, in
Jones, R.W., and Harris, R.E., (eds.), Proceedings of the 32nd Annual
Forum of Industrial Minerals – Laramie, Wyoming, May 19-21, 1996: Wyoming
State Geological Survey Public Information Circular 38, p.319.
Leigh, R.T., 1998, Wyoming trona : An overview of the geology, in Dyni,
J.R., and Jones, R.W., (eds.), Proceedings of the first
international soda ash conference volume II: Wyoming State Geological Survey
Public Information Circular 40, p.1-14.
Mendenhall, W.C., 1940, Occurrence of a deposit of trona: Science, v.91,
no. 239, p.11-12.
- ►Recommended Trona References
Further information on Wyoming trona can be found in the following WSGS
WSGS Public Information Circular 39, Proceedings of the first international
soda ash conference, vol. I, edited by J.R. Dyni, and R.W. Jones, 1998, 95
WSGS Public Information Circular 40, Proceedings of the first international
soda ash conference, vol. II, edited by J.R. Dyni, and R.W. Jones, 1998,
WSGS Bulletin 72, Minerals and Rocks of Wyoming, by W.D. Hausel, 2005,
OCI Chemical Corporation
Bob Gregory (307) 766-2286 Ext. 237
Phosphate rock is the primary source of phosphorus for industrial applications. Phosphorus in phosphate rock most commonly occurs within apatite (Ca5(PO4)3(F,Cl,OH). Apatite is found in sedimentary, igneous, and metamorphic rocks. There are six economic deposit types for phosphate rock: 1) marine phosphorites; 2) igneous apatite; 3) residual phosphorites; 4) river pebble phosphate deposits; 5) phosphatized rock; and 6) guano (McKelvey and others, 1953).
Phosphate Rock in Wyoming
Download the Phosphate Rock in Wyoming report.
The primary industrial application of phosphate rock is the production of fertilizer used to add phosphorus to soil. Phosphorus (P) is a nutrient vital for all life as a component in DNA and RNA, and also adenosine triphosphate, which facilitates energy transfer within cells (Environmental Literacy Council, 2013). Terrestrial plants incorporate phosphorus from soil, while animals receive phosphorus through their diet. In nature, phosphorus is often a limiting factor with respect to the quantity of life an ecosystem can support (Ozanne, 1980). In soil, natural soluble phosphorus that can be taken up by plants typically makes up less than 10 percent of total phosphorus in the soil (Ozanne, 1980). In agricultural settings, natural availability of soluble phosphorus is prohibitively low, thus phosphorus must be added to the soil by means of a topical fertilizer (Ozanne, 1980). Similarly, phosphorus feed-additives may be required for ruminant livestock (Allaway, 1962; Reid, 1980; Underwood, 1999).
The United States is the third largest producer of phosphate rock globally. Currently, the bulk of domestic production occurs in Florida and North Carolina, with remaining production in Idaho and Utah (Jasinski, 2015). Phosphate production in Idaho and Utah is from the so-called Western Phosphate Field, an area covered by the Permian aged Phosphoria Formation. The eastern portion of the Western Phosphate Field covers the western half of Wyoming. Though the Phosphoria Formation thins eastward from Idaho into Wyoming, notable phosphate rock deposits within the Phosphoria Formation are present within Wyoming.
At present there are no active phosphate rock mines in Wyoming, though mining did occur intermittently through the 20th century. Phosphate rock in Wyoming was first mined in 1907, and production in the western portion of the state continued sporadically until the opening of the Leefe mine in 1947 (Jasinski and others, 2004). Production of phosphate rock in Wyoming last occurred in 1977. The Leefe Mine, located approximately 30 miles west of Kemmerer, produced phosphate rock from 1947 to 1977 from the Phosphoria Formation (Wyoming Board of Equalization, 1948-1972; Wyoming Department of Revenue, 1973-1978; Jasinski and others, 2004). Though production in Wyoming has been dormant for more than three and half decades, the phosphate mining industry has a robust presence in southeastern Idaho and northeastern Utah, and a phosphate processing facility is located near Rock Springs, WY. Thus, phosphate rock deposits in western Wyoming are relatively close to existing phosphate processing infrastructure.
Of the six deposit types listed above, only marine phosphorites and igneous apatite are known to occur in Wyoming. Marine phosphorites are well documented within the Permian Phosphoria Formation of western to central Wyoming; these are the only phosphate rock occurrences in Wyoming likely to be of a grade and extent to attract economic interest. No extensive high-grade igneous phosphate deposits are known in Wyoming, but the typical host rock-types are not uncommon to the state, and anomalously high concentrations of igneous apatite have been recognized in the state. In the central Laramie Range, apatite is associated with magnetite-ilmenite deposits within the Laramie Anorthosite Complex (Diemer, 1941; Osterwald and others, 1966). Magnetite-ilmenite bodies at the Taylor Deposit host up to 60 percent apatite (Diemer, 1941). Diemer (1941) also identified apatite at two other magnetite-ilmenite deposits, which he labeled deposits #1 and #6. At deposit #1, varying amounts of apatite occur within iron-rich lenses. At deposit #6, apatite is abundant within an irregular dike, though a sample of this dike yielded only slightly greater than 2 percent P2O5.
Thick, medium- to high-grade occurrences of phosphate rock of the Phosphoria Formation are most common in western Wyoming, but may extend into central Wyoming. The Meade Peak Member of the Phosphoria Formation in the Overthrust Belt exhibits the highest potential for economically viable phosphate rock deposits with respect to grade and thickness; however, the steep inclination and discontinuity of beds may preclude mineability at many locations. All historic phosphate mining in Wyoming targeted the Meade Peak Member in the Overthrust Belt.
Southeast of Lander, the Meade Peak Member and, to a lesser degree, the Retort Member of the Phosphoria Formation host important phosphate deposits along the northeastern flank of the Wind River Mountains. The Lander deposits are low- to medium-grade, but the structural geology of the area is relatively simple compared to the Overthrust Belt.
Wyoming Phosphate Occurrences
Allaway, W.H., 1962, Relation of soil to plant and animal nutrition, in Proceedings, Cornell Nutrition Conference: Cornell University, Ithaca, New York, p. 13–23.
Diemer, R. A., 1941, Titaniferous magnetite deposits of the Laramie Range, Wyoming: Geological Survey of Wyoming [Wyoming State Geological Survey], Bulletin 31, 23 p.
Environmental Literacy Council, 2013, Phosphorus Cycle, at http://www.enviroliteracy.org/article.php/480.html, accessed April 23, 2015.
Jasinski, S.M., 2015, Phosphate rock, in Mineral commodity summaries 2015: U.S. Geological Survey, p. 118–119.
Jasinski, S.M., Lee, W.H., and Causey, J.D., 2004, The history of the Western Phosphate Field, in Hein, J.R., ed., Life cycle of the Phosphoria Formation: Handbook of Exploration and Environmental Geochemistry, v. 8: Amsterdam, Elsevier, p. 45–61.
McKelvey, V.E., Cathcart, J.B., Altschuler, Z.S., Swanson, R.W., Lutz, K., 1953, Domestic phosphate deposits: U.S. Geological Survey Open-File Report 53-165, 49 p.
Osterwald, F.W., Osterwald, D.B., Long, L.S., Jr., and Wilson, W.H., (revised by Wilson), 1966, Mineral resources of Wyoming: Geological Survey of Wyoming [Wyoming State Geological Survey] Bulletin 50, 287 p.
Ozanne, P.G., 1980, Phosphate nutrition of plants – a general treatise, in Khasawneh, F.E., Sample, E.C., and Kamprath, E. J. eds., The Role of Phosphorus in Agriculture: Madison, Wis., American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, p. 559–590.
Reid, R.L., 1980, Relationship between phosphorus nutrition of plants and the phosphorus nutrition of animals and man, in Khasawneh, F.E., Sample, E.C., and Kamprath, E. J. eds., The Role of Phosphorus in Agriculture: Madison, Wis., American Society of Agronomy, Crop Science Society of America, Soil Science Society of America, p. 847–886.
Underwood, E.J., and Suttle, E.J., 1999, The mineral nutrition of livestock, 3d edition: Wallingford, UK, CAB International, 614 p.
Wyoming Department of Revenue, 1973–1978, Annual report: Cheyenne, Wyoming.
Wyoming State Board of Equalization, 1926–1972, Biennial report: Cheyenne, Wyoming.
Jacob Carnes (307) 766-2286 Ext. 259
Lithium is the earth’s 25th most abundant element. It is present in many geologic materials but almost always in low concentrations. Metallic lithium is so reactive with water and air that it does not occur naturally in its pure state, but only in the form of various salts.
Lithium was first identified as a new element in the early 1800s. The first major commercial use for lithium was for lithium based aviation lubricants (lithium greases) during WWII. In the following decades, commercial applications for lithium were developed by the glass making, ceramic, cement and aluminum smelting industries. Since 2007, the demand for lithium compounds has risen dramatically for use in the rechargeable batteries that power many small, portable electrical devices such as cellphones, digital cameras, cordless power tools, laptop computers and the growing number of electric and hybrid powered vehicles.
Currently, most of the world’s lithium is produced from shallow brine deposits that underlie saline lakes in the Atacama Desert of South America, and from a spodumene mine in Australia. Chile, Australia, China, and Argentina produce most of the world’s lithium compounds (fig. 1) while minor amounts are produced by Portugal, Brazil and Zimbabwe (Jaskula, 2015). Production in the U.S. is limited to a single brine operation in Silver Peak, Nevada. Lithium concentrations in producing brine deposits typically exceed 200 parts per million (ppm); concentrations in lithium mineral ores are higher than 5,000 ppm. Furthermore, the facilities that produce lithium at these minimal concentrations operate under financially advantageous conditions such as low production costs, or reduced capital expenditures.
Mineral companies are looking for other sources of lithium throughout the world and in North America as industrial demands grow. Recycling, too, will provide additional sources although the technology is in the early stage of development.
WSGS reviewed geochemical data for nearly 68,000 Wyoming sediment, soil, rock, and water samples obtained from seven state and federal databases. Additionally, WSGS geologists collected nearly 100 rock and soil samples for this study which were evaluated along with over 600 other WSGS samples collected in conjunction with other projects. Together, the database records and WSGS collected samples produced lithium concentration data for 26,386 samples of Wyoming geo-materials. The results of this study show lithium occurs in low levels in soils, groundwater and rocks across Wyoming. With the exception a small deposit of spodumene, a lithium-enriched mineral, in the Rattlesnake Hills of southwestern Natrona County, lithium concentrations in Wyoming deposits are substantially lower than those found at the world’s currently producing sites. Small amounts of spodumene were mined at the Natrona County site during World War II, but the deposit is likely too small to be of interest today.
Jaskula, B.W., 2009 - 2015, Lithium: U.S. Geological Survey, mineral commodity summaries, January 2009–2015, 2 p.
Kamienski, C.W., McDonald, D.P., Stark, M.W., and Papcun, J.R., 2004, “Lithium and lithium compounds” in Kirk-Othmer Encyclopedia of Chemical Technology. John Wiley & Sons, Inc., var. pagination.
Ober, J.A., 1998–2008, Lithium: U.S. Geological Survey, mineral commodity summaries, January 1998–2008, 2 p.
Karl Taboga (307) 766-2286 Ext. 226