Uranium deposits are generally classified based on host rocks, structural setting and deposit mineralogy. Learn more about them here.

Uranium is one of the more common elements in the Earth’s crust — it is often said to be some 40 times more common thansilver and 500 times more common thangold.

Uranium ore deposits are found globally, with the largest-known recoverable resources found in Kazakhstan, Canada, Australia and South Africa.

The metal is so abundant that it can be found almost everywhere, including soil, rivers, oceans and rocks. The challenge, however, is to find areas with concentrations adequate enough to form an economically viable deposit — or, better yet, a world-class deposit worthy of a mining and milling operation.

Uranium ore is mined in several ways, depending on the geological conditions; processes include open-pit mining, underground mining, in-situ leaching and borehole mining.

Once extracted, uranium ore is crushed and rendered into a powder, then leached with either an acid or alkali. The leachate is subjected to one of several sequences of precipitation, solvent extraction and ion exchange. The resulting enriched mixture, called yellowcake, contains at least 75 percent uranium oxide. It is then calcined to remove impurities from the mining and  milling process before refining and conversion.

Uranium deposits

Canada was once the world’s largest producer of uranium, but it has since been overtaken by Kazakhstan. That said, the highest-grade uranium deposits are in Canada’s Athabasca Basin in Northern Saskatchewan. The largest uranium-producing mine in the world is Cameco’s (TSX:CCO,NYSE:CCJ) McArthur River, an underground mine located in the Athabasca Basin; however, it is now on care and maintenance along with the company’s Key Lake mill.

Elliot Lake, Ontario, also played a vital role in establishing and building Canada’s uranium sector. In the 1950s and ’60s, Elliot Lake produced a vast majority of the global uranium supply. Other high-grade deposits in North America include the Colorado plateau, which had 800 uranium mines in operation in 1955. The Grand Canyon has also had a significant amount of uranium mining claims put forward, but former President Barack Obama issued a mining moratorium on the Grand Canyon and adjacent area in 2010, which still stands today.

Uraniumdeposits are generally classified based on host rock, structural setting and deposit mineralogy. The most widely used classification scheme was developed by the International Atomic Energy Agency with the objective of subdividing uranium deposits into 14 categories arranged according to their approximate economic significance. Geology and other resources in the deposit area also play a factor in developing a uranium mining project. Below, we outline the 14 types of uranium deposits. 

1. Unconformity-related uranium deposits

Unconformity-type deposits are one of the most discussed uranium deposit types, and for good reason — they can be some of the largest and richest deposits on Earth. Relative to other uranium deposits, unconformity-type deposits tend to be the highest grade. They occur in close proximity to major unconformities between relatively quartz-rich sandstones and deformed metamorphic basement rocks. The most significant area for this style of deposit is currently the Athabasca Basin.

Cameco owns and operates two of the highest-grade mines in the world, McArthur River and Cigar Lake. Also working on an unconformity project in the Athabasca Basin is exploration-stage Fission Uranium (TSX:FCU,OTCQX:FCUUF) with the Paterson Lake South uranium project, which hosts the Triple R deposit.

2. Sandstone deposits

Sandstone uranium deposits are contained within medium- to coarse-grained sandstones located in a continental fluvial or marginal marine sedimentary environment. Sandstone deposits constitute about 18 percent of the world’s uranium resources and are commonly classified as low to medium grade, in the range of 0.05 to 0.4 percent; individual orebodies are small to medium in size. Sandstone-hosted uranium deposits are widespread globally and span a broad range of host rock ages.

Some of the major provinces and production centers are Wyoming, New Mexico, Central Europe and Kazakhstan. Significant potential for sandstone deposits remains in those regions, as well as in Australia, Mongolia, South America and Africa.

3. Quartz-pebble conglomerate deposits

Quartz-pebble conglomerate uranium deposits were historically significant as the major source of primary production for several decades following World War II. This type of deposit has been identified in eight jurisdictions around the world; however, the most significant deposits are in the Huronian Supergroup in Southern Ontario, and in the Witwatersrand Supergroup of South Africa. These deposits make up approximately 13 percent of the world’s uranium resources.

4. Vein deposits

Vein deposits exist where uranium minerals have filled in cavities such as cracks, veins, fractures, breccias and stockworks associated with steeply dipping fault systems. These deposits are responsible for the term “pitchblende,” which originates from German vein deposits mined for silver in the 16th century. F.E. Brückmann made the first mineralogical description of the mineral in 1727.

The first industrial production of uranium was made from a vein deposit in the Czech Republic, and Marie and Pierre Curie used tailings from the mine for their discovery of polonium and radium.

5. Breccia complex deposits

Olympic Dam is one of the world’s largest orebodies. Located in Australia’s Gawler Craton, it is also one of the world’s biggest deposits of copper, gold and uranium, and it has a significant deposit of silver.

BHP (ASX:BHP,LSE:BLT,NYSE:BHP) owns Olympic Dam, and along with the Carrapateena mine it occurs in a hematite-rich granite breccia complex that is overlain by approximately 300 meters of flat-lying sedimentary rocks of the Stuart Shelf geological province. Olympic Dam is reportedly the only iron oxide-copper-gold (IOCG) deposit known to contain economically significant quantities of uranium.

6. Intrusive deposits

Intrusive uranium deposits make up a large proportion of the world’s uranium resources and are associated with a number of rock types, including alaskite, granite, pegmatite and monzonites. Major world deposits are found in Namibia, Greenland and South Africa.

7. Phosphorite deposits

Low-grade concentrations of notably large uranium deposits can be found in marine sedimentary phosphorite structures, ranging from 0.01 to 0.015 percent U3O8. Very large phosphorite deposits occur in Florida and Idaho in the US, as well as in Morocco and in some Middle Eastern countries.

8. Collapse breccia pipe deposits

Collapse breccia pipe deposits occur within vertical, circular solution collapse structures formed by the dissolution of limestone by groundwater. Resources within individual pipes can reach up to 2,500 tonnes of U3O8 at an average grade of 0.3 to 1 percent. The best-known examples of this deposit type are in Arizona, where several of these deposits have been mined.

9. Volcanic deposits

The principal uranium mineral in volcanic deposits is pitchblende, which is usually associated withmolybdenum sulfide and minor amounts oflead,tin andtungsten mineralization. The average deposit size is rather small, with grades of 0.02 to 0.2 percent U3O8. These deposits make up only a small proportion of the world’s uranium resources. Currently, the only volcanic-hosted deposits being exploited are those in the Streltsovkoye district of Eastern Siberia.

10. Surficial deposits (calcretes)

Surficial deposits account for approximately 4 percent of world uranium resources, and are interbedded with sand and clay, usually cemented by calcium and magnesium carbonates. These deposits may also occur in peat bogs, karst caverns and soils. The Yeelirrie deposit in Western Australia is by far the world’s largest surficial deposit, averaging 0.15 percent U3O8.

11. Metasomatite deposits

Metasomatite deposits consist of disseminated uranium minerals within structurally deformed rocks formed from geochemical processes. Uranium levels are very low, on average less than 0.005 percent U3O8. These deposits are typically small in size, containing less than 1,000 tonnes, and currently do not warrant commercial extraction.

12. Metamorphic deposits

Metamorphic deposits can be found in metasediments and/or metavolcanics unrelated to granite. Examples of this deposit type can be found around the world, but in Australia the biggest one is the Mary Kathleen uranium-rare earths deposit near Mount Isa in Queensland. It was mined from 1958 to 1963 and from 1976 to 1982. This orebody occurs in a zone of calcium-rich alteration within Proterozoic metamorphic rocks

13. Lignite

When uranium occurs in lignite, a type of coal, it is with mineral detritus such as silt or clay, and is found immediately adjacent to carbonaceous mud and silt/sandstone beds. Pyrite content is high in these deposits, with examples being present across the globe. Most uranium in this type of deposit is currently not economic.

14. Black shale deposits

Black shale uranium deposits include large, low-grade uranium resources. They form in submarine environments under oxygen-free conditions. Because of their low grade, almost no black shale deposit has ever produced significant amounts of uranium.

There is one exception: Germany’s Ronneburg deposit. Production between 1950 and 1990 was about 100,000 tonnes of uranium at an average grade of 0.07 to 0.1 percent. Measured and inferred resources containing 87,000 tonnes of uranium grading between 0.02 and 0.09 percent remain.

Which uranium deposits are you most interested in? Tell us in the comments.

This is an updated version of an article originally published by the Investing News Network in 2010.

Don’t forget to follow us @INN_Resource for real-time updates!

Securities Disclosure: I, Georgia Williams, hold no investment interest in any of the companies mentioned in this article.



S&P 5004283.74+9.70


Heating Oil3.610.00
Natural Gas9.22+0.04