Uranium mining in Colorado, United States, goes back to 1872, when pitchblende ore was taken from gold mines near Central City, Colorado. The Colorado uranium industry has seen booms and busts, but continues to this day. Not counting byproduct uranium from phosphate, Colorado is considered to have the third largest uranium reserves of any US state, behind Wyoming and New Mexico. [1]
Uranium price increases from 2001 to 2007 prompted a number of companies to revive uranium mining in Colorado. However, price drops and financing problems in late 2008 have forced some companies to cancel or scale back uranium-mining projects. There are no currently producing uranium mines in Colorado. [2]
Hydrothermal uranium deposits are present through a widely spaced area in the Front Range of the Rocky Mountains, in Larimer, Boulder, Gilpin, Clear Creek, and Jefferson counties.
The first uranium identified in the USA was pitchblende from the Wood gold mine at Central City, Colorado in 1871. [3] Pitchblende orebodies were also discovered in the Calhoun mine, the Kirk mine, and some others. About 122,000 pounds (55 metric tons) of uranium oxide (U3O8) were shipped at irregular intervals from six gold mines in the Central City district from 1872 to about 1916. [4]
The uranium boom of the late 1940s revived the search for uranium orebodies in the gold and silver mines of the Front Range. Again, uranium was produced from a number of mines, but the orebodies were small and discontinuous. Pitchblende was discovered in 1948 in the Caribou silver mine at the town of Caribou, Boulder County. A small amount of uranium ore was produced. [5]
In 1949 janitor and weekend prospector Fred Schwartzwalder discovered uranium at an abandoned copper prospect in Jefferson County about ten miles (16 km) northeast of Central City and eight miles (13 km) north of Golden. [6] The deposit consists of Tertiary hydrothermal veins filling fracture zones oriented predominantly NNW-SSE in gneiss, schist, and quartzite of the Precambrian Idaho Springs Formation. The chief ore mineral is pitchblende, which occurs with adularia and ankerite. Schwartzwalder could interest no one in his discovery, so he drove the first adit of the Schwartzwalder mine by himself, made the first ore shipment in 1953, and sold the mine in 1955. [7] The Schwartzwalder mine was the source of more than 99% of the uranium produced from the Front Range. The mine operated until 1995, producing 17 million pounds (7700 metric tons) of uranium oxide. [8] The mine was owned by the General Atomics subsidiary Cotter Corporation, which estimated that there are an additional 16 million pounds (7300 metric tons) of uranium oxide resource remaining in the mine. In 2024, the Colorado Department of Natural Resources Division of Reclamation, Mining and Safety (DRMS) took the mine over from Colorado Legacy Land, LLC, which had acquired the mine from Cotter. [9] [10]
The Copper King mine, in Larimer County about 25 miles (40 km) northwest of Fort Collins and five miles (8.0 km) northeast of Red Feather Lakes contained a skarn deposit that was worked unsuccessfully for zinc in 1920 and 1936. Prospectors found uranium at the abandoned mine in 1949, and it was worked for uranium from 1951 until 1953. The uranium occurs as pitchblende in a hydrothermal vein deposit in Precambrian granite. Although the zinc skarn and the pitchblende vein are exposed in the same workings, the pitchblende appears to have been deposited much later. [11]
Other vein-type uranium mines in the Front Range were the Fairday A. M. mine near Jamestown in Boulder County, and the Wright Lease mine near Ideledale in Jefferson County. [12]
The 70-mile long (110 km) Uravan mineral belt is an arcuate zone of uranium-vanadium deposits in San Miguel, Montrose, and Mesa counties, Colorado, and Grand County, Utah. It was the area most productive of uranium in the United States in the early 20th century. The mineral belt includes the Slick Rock, Gypsum Valley, Uravan, and Gateway mining districts. [13] [14]
Uranium mining in southwest Colorado goes back to 1898, when a miner[ who? ] dug 10 tonnes (22,000 lb; 10,000 kg) of yellow ore that tested high in uranium and vanadium out of a deposit at Roc Creek in Montrose County, Colorado, and shipped it to France, where M. M. C. Friedel and E. Cumenge identified the new mineral that they named carnotite. The mineral was mined for its vanadium, with uranium as a byproduct.
Although radium had been discovered in 1898, it had been derived from pitchblende, and the radium content of carnotite was not known. Carnotite was suspected to contain radium as early as 1903, on the basis of the anomalously high radioactivity of carnotite ores. [15] But it was not until 1911 that the radium content of carnotite was confirmed by the Marie Curie laboratory in Paris. [16] Although no more than a trace of radium was present in the ore, newly discovered medical applications had made radium worth $100 per milligram (equivalent to $3,300 per milligram today), making the radium in the carnotite ore worth much more than the vanadium or uranium.
Once carnotite was known to contain radium, prospectors rushed to the Colorado Plateau of southwest Colorado and adjacent southeast Utah, and found carnotite-bearing sandstones of the Jurassic Morrison Formation in Mesa, Montrose, and San Miguel counties in Colorado. The carnotite was at first shipped to Europe for processing, but by 1913, the Standard Chemical Company had built a radium processing plant in Montrose County that had become the world's largest supplier of radium. [17]
The Uravan mineral belt of Colorado and Utah supplied about half the world's radium from 1910 to 1922, and vanadium and uranium were byproducts. The mines were forced out of business in 1923, when rich pitchblende deposits in the Belgian Congo forced down the price of radium. Mining revived in 1935 when the price of vanadium rose, and boomed after World War II when the government stockpiled uranium for nuclear weapons programs. [18]
The Uravan mineral belt contains what was the last producing uranium mine in the state, the Topaz Mine, part of the Sunday Complex near Uravan, Colorado, which was closed down on 18 March 2009 by then owner Denison Mines due to depressed uranium prices. [19]
Energy Fuels Inc. has applied for a permit to rehabilitate and begin pilot production at the Torbyn mine, a former uranium producer in Mesa County just east of Gateway. [20]
Prospectors examined copper-stained sandstone a mile south of Garo in Park County in 1903, but the copper content was too low to mine. In 1919, prospectors discovered that the sandstone contained uranium and vanadium, and about 40 tons of ore containing up to 1% uranium was mined from underground workings. The mine was reactivated as an open-pit uranium mine in 1951 and closed in 1952. The ore consisted of the uranium-vanadium minerals tyuyamunite, metatyuyamunite, and carnotite, along with the copper minerals covellite, chalcocite, azurite, and malachite, and the copper-vanadium mineral volborthite, in the Maroon Formation of Pennsylvanian-Permian age. The ore is associated with faulting-induced fractures in the sandstone. [21]
Horizon Nevada Uranium Inc. has announced plans for exploration drilling in 2008 for uranium in the South Park Ranch area of southeast Park County. [22]
The Cochetopa mining district is about 20 miles (32 km) southeast of Gunnison in northwest Saguache and southern Gunnison County. Uranium was discovered in outcrops of the Morrison Formation (Jurassic). Mineralization occurs in silicified (chalcedony and quartz) veins cutting the Morrison Formation and the subjacent Precambrian schist. The veins contain pitchblende, autunite and uranophane, with accessory marcasite and barite. Extraction started in 1954, by underground mining. [23]
Uranium was discovered near Marshall Pass in northern Saguache and southeastern Gunnison counties, in 1955. Although the initial discoveries were uneconomic, they attracted further prospecting, which located commercial orebodies along the Chester thrust fault of Laramide age. The deposits are about six-mile east of Sargents. The orebodies are primarily pyrite and pitchblende replacements of Paleozoic sedimentary rocks and Precambrian igneous and metamorphic rocks. Some uranophane and autunite are also present. Initial mining was by small open pits; underground mines were later developed. [24]
The Maybell district in Moffat County was discovered in 1954 by an airborne radiation survey. Uranium was present as meta-autunite, uranophane, uraninite, and coffinite in tufaceous fluvial sandstones of the Miocene Browns Park Formation. [25] Ore deposits are associated with faults, which are thought to have been pathways for reducing solutions from below. Ore was taken from numerous open-pit mines between two and three miles north of US Highway 40, between the towns of Maybell and Lay from 1953–1964 and 1976–1981. Ores were treated in a local ore mill, five miles (8.0 km) east-northeast of Maybell, during the 1953–1964 period; during 1976–1981, ore was heap-leached, and the eluate trucked to Wyoming for uranium recovery. Total production of the district was 5.3 million pounds (2.4 million kilograms) of uranium oxide. [26]
Surface radioactive anomalies led to uranium discoveries in 1954 at Tallahassee Creek in Fremont County. Mining in the 1950s was by both underground and open-pit methods. [27]
Exploration in the 1970s by Cyprus Mines and Wyoming Minerals defined two orebodies: the Hansen orebody, estimated to contain 12 million pounds of U3O8, and the Picnic Tree orebody, estimated to contain 1 million pounds U3O8. Uranium is present as uraninite, coffinite, and meta-autunite in Eocene and Oligocene arkosic sandstone, conglomerate, and in sediments interbedded with Miocene volcanic flows. Uranium is associated with carbonaceous material, and pyrite. The source of uranium is thought to be the Oligocene Wall Mountain Tuff. [28]
In December 2006, the Australian company Black Range Minerals bought rights to mine the Taylor Ranch property, which the company describes as a 30-million pound uranium orebody that had been discovered in the late 1970s, but abandoned because of low uranium prices. The company plans an extensive drilling program in 2008 to delineate the orebody. [29]
Relatively small amounts of uranium ore have been mined from the Dakota Sandstone along the western edge of the Denver Basin. The Mann mine, near Morrison, Colorado, produced 16,000 pounds (7.1 metric tons) of uranium oxide from 1955 to 1961. [30] The Mike Doyle mine in El Paso County produced 280 pounds (130 kg) of uranium oxide from Dakota sandstone in 1955. Also in 1955, a Dakota sandstone mine in Larimer County produced 8 pounds of uranium along with some vanadium. [31]
The Leyden coal mine, north of Golden, Colorado, produced 4500 pounds (2.1 metric tons) of uranium oxide from 1954 to 1956, as a byproduct of coal mining in the Laramie Formation.
Rancher Solomon Schlagel discovered uranium in Weld County, Colorado in 1969 when he noticed that cuttings from seismic shotholes were anomalously radioactive. [32] Exploration in the 1970s defined a number of roll-front uranium deposits in the Upper Cretaceous Laramie Formation and Fox Hills Formation in Weld County. They all occur along the southern margin of the Cheyenne sub-basin of the Denver Basin.
Wyoming Minerals Corporation operated a pilot in-situ leaching plant from June 1977 to May 1978, successfully extracting uranium from a deposit in the Laramie Formation near the town of Grover. The aquifer was then remediated. [33]
Power Resources Corporation began in-situ mining the uranium deposit in the Fox Hills Formation at Keota, Colorado in 1980. The Keota deposit was estimated to contain 5 to 10 million pounds (2300 to 4500 metric tons) of uranium oxide, but the project was halted because of low uranium prices. [34]
In 2006, Vancouver-based Powertech (USA) Inc. [35] bought mineral rights and leases over the Centennial Project in Weld County near Nunn, Colorado, which had been explored in the 1970s by Rocky Mountain Energy. Powertech is currently evaluating the property for in-situ leaching using a leach solution of dissolved carbon dioxide and oxygen.
The uranium occurs in a series of roll fronts in sandstones of the Fox Hills Formation aligned roughly north-south over 11 miles. A consultant for Powertech has estimated that the deposits contain identified reserves of 9.7 million pounds (4400 metric tons) of uranium oxide recoverable by in-situ and open-pit methods, with potential for another three to five million pounds. [36]
If all goes according to Powertech's proposed timeline, the process of obtaining government permits would extend through the end of 2009, after which the in-situ leaching would extract 800,000 pounds (360 metric tons) of uranium per year for ten years. The uranium would be stripped from the leachate using ion exchange resin. The loaded resin beads would be trucked to an off-site facility for reprocessing and precipitation of uranium concentrate. Solution mining would move progressively from north to south, with remediation following mining as each orebody is mined out.
Powertech's mining plans are opposed by Coloradoans Against Resource Destruction (CARD), who point out that the Fox Hills Formation is an important water-supply aquifer. [37] [38]
Three former uranium mill sites in Colorado are current United States Environmental Protection Agency National Priorities List (Superfund) sites:
In addition, there are 15 Uranium Mill Tailings Remedial Action (UMTRA) sites in the state, under the purview of the United States Department of Energy. Eight of the sites are former uranium ore mills, and seven are engineered permanent disposal sites for the mill tailings. [43]
There are a variety of active uranium mines in Colorado in the Ivan belt. One currently active uranium mine in the state is the Sunday mine near Uravan, owned by Piñon Ridge Mining. [44] [45]
In 2007, Energy Fuels Inc. announced plans to build a uranium-vanadium processing mill in the Uravan district, west of Naturita. If permitted and built, the mill would be the first new uranium mill built in the United States in 25 years. [46] The US Bureau of Land Management has issued a "finding of no significant impact", which will allow Energy Fuels to start mining at its Whirlwind mine in Mesa County, Colorado. The mine is projected to produce 250,000 pounds (110,000 kg) of U3O8 and one million pounds of V2O5 per year. [47]
Canadian-based Powertech (USA) Inc. is currently evaluating roll-front uranium deposits in its Centennial Project in Weld County on Colorado's eastern plains. [48] In response to the proposed mining in Weld county, state lawmakers have put forward two proposals to more closely regulate uranium mining in Colorado; the first would require that mining companies prove that groundwater would not be adversely affected before mining could begin; the second would assure that local governments have the power to set health and environmental standards. [49]
Uraninite, also known as pitchblende, is a radioactive, uranium-rich mineral and ore with a chemical composition that is largely UO2 but because of oxidation typically contains variable proportions of U3O8. Radioactive decay of the uranium causes the mineral to contain oxides of lead and trace amounts of helium. It may also contain thorium and rare-earth elements.
Carnotite is a potassium uranium vanadate radioactive mineral with chemical formula K2(UO2)2(VO4)2·3H2O. The water content can vary and small amounts of calcium, barium, magnesium, iron, and sodium are often present.
The Denver Basin, variously referred to as the Julesburg Basin, Denver-Julesburg Basin, or the D-J Basin, is a geologic structural basin centered in eastern Colorado in the United States, but extending into southeast Wyoming, western Nebraska, and western Kansas. It underlies the Denver-Aurora Metropolitan Area on the eastern side of the Rocky Mountains.
The Eldorado Mine is a defunct mine located in Port Radium, Northwest Territories, Canada. The site, which covers 12 hectares, is located next to Echo Bay in the shore of Great Bear Lake.
Uranium mining is the process of extraction of uranium ore from the ground. Over 50 thousand tons of uranium were produced in 2019. Kazakhstan, Canada, and Australia were the top three uranium producers, respectively, and together account for 68% of world production. Other countries producing more than 1,000 tons per year included Namibia, Niger, Russia, Uzbekistan, the United States, and China. Nearly all of the world's mined uranium is used to power nuclear power plants. Historically uranium was also used in applications such as uranium glass or ferrouranium but those applications have declined due to the radioactivity of uranium and are nowadays mostly supplied with a plentiful cheap supply of depleted uranium which is also used in uranium ammunition. In addition to being cheaper, depleted uranium is also less radioactive due to a lower content of short-lived 234
U and 235
U than natural uranium.
Placerville is a census-designated place (CDP) and post office in and governed by San Miguel County, Colorado, United States. The Placerville post office has the ZIP Code 81430. At the United States Census 2020, the population of the Placerville CDP was 362.
Uranium mining in the United States produced 224,331 pounds (101.8 tonnes) of U3O8 in 2023, 15% of the 2018 production of 1,447,945 pounds (656.8 tonnes) of U3O8. The 2023 production represents 0.4% of the uranium fuel requirements of the US's nuclear power reactors for the year. Production came from five in-situ leaching plants, four in Wyoming (Nichols Ranch ISR Project, Lance Project, Lost Creek Project, and Smith Ranch-Highland Operation) and one in Nebraska (Crowe Butte Operation); and from the White Mesa conventional mill in Utah.
Silver mining in Colorado has taken place since the 1860s. In the past, Colorado called itself the Silver State.
Uranium mining in Wyoming was formerly a much larger industry than it is today. Wyoming once had many operating uranium mines, and still has the largest known uranium ore reserves of any state in the U.S. At the end of 2008, the state had estimated reserves dependent on price: 539 million pounds of uranium oxide at $50 per pound, and 1,227 million pounds at $100 per pound.
Uranium mining in Utah, a state of the United States, has a history going back more than 100 years. Uranium mining started as a byproduct of vanadium mining about 1900, became a byproduct of radium mining about 1910, then back to a byproduct of vanadium when the radium price fell in the 1920s. Utah saw a uranium boom in the late 1940s and early 1950s, but uranium mining declined in the 1980s. Since 2001 there has been a revival of interest in uranium mining, as a result of higher uranium prices.
Uranium ore deposits are economically recoverable concentrations of uranium within Earth's crust. Uranium is one of the most common elements in Earth's crust, being 40 times more common than silver and 500 times more common than gold. It can be found almost everywhere in rock, soil, rivers, and oceans. The challenge for commercial uranium extraction is to find those areas where the concentrations are adequate to form an economically viable deposit. The primary use for uranium obtained from mining is in fuel for nuclear reactors.
Uranium mining in Arizona has taken place since 1918. Prior to the uranium boom of the late 1940s, uranium in Arizona was a byproduct of vanadium mining of the mineral carnotite.
Uranium mining in New Mexico was a significant industry from the early 1950s until the early 1980s. Although New Mexico has the second largest identified uranium ore reserves of any state in the United States, no uranium ore has been mined in New Mexico since 1998.
SAG/SDAG Wismut was a uranium mining company in East Germany during the time of the Cold War. It produced a total of 230,400 tonnes of uranium between 1947 and 1990 and made East Germany the fourth largest producer of uranium ore in the world at the time. It was the largest single producer of uranium ore in the entire sphere of control of the USSR. In 1991 after German reunification it was transformed into the Wismut GmbH company, owned by the Federal Republic of Germany, which is now responsible for the restoration and environmental cleanup of the former mining and milling areas. The head office of SDAG Wismut / Wismut GmbH is in Chemnitz-Siegmar.
Radium Hill is a former minesite in South Australia which operated from 1906 until 1961. It was Australia's first uranium mine, years before the country's next major mines at Rum Jungle in the Northern Territory (opened in 1950), and the Mary Kathleen mine in Queensland (1958). The associated settlement which once housed up to 1,100 people is now a ghost town, largely abandoned and demolished. The former townsite and cemetery were provisionally listed on the South Australian Heritage Register on 24 August 2016. During its main period of production between 1954 and 1961 the mine produced nearly 1 million tonnes of davidite-bearing ore to produce about 860 tons of U3O8.
The world's largest producer of uranium is Kazakhstan, which in 2019 produced 43% of the world's mining output. Canada was the next largest producer with a 13% share, followed by Australia with 12%. Uranium has been mined in every continent except Antarctica.
Colorado mining history is a chronology of precious metal mining, fuel extraction, building material quarrying, and rare earth mining.
Paramontroseite (V4+O2) is a relatively rare orthorhombic vanadium oxide mineral in the Ramsdellite Group. Synthetic paramontroseite may have applications in medicine, batteries and electronics.
Temple Mountain is a remote 6,820-foot (2,080 m) mountain and abandoned town, located on the southeast flank of the San Rafael Swell in Emery County, Utah, United States.
A yellowcake boomtown also known as a uranium boomtown, is a town or community that rapidly increases in population and economics due to the discovery of uranium ore-bearing minerals, and the development of uranium mining, milling or enrichment activities. After these activities cease, the town "goes bust" and the population decreases rapidly.