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Uranium mining in Utah
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.
Mining of uranium-vanadium ore in southeast Utah goes back to the late 19th century, at the northern end of the Uravan mineral belt (see Uranium mining in Colorado), where it crosses into Grand County, Utah. Uranium occurs in the Salt Wash member of the Morrison Formation of Jurassic age. Because much of the value depended on the vanadium content, the only economic ore minerals were carnotite and tyuyamunite. Following World War II buying for nuclear weapons programs made uranium valuable for its own sake, and attracted hundreds of prospectors to southeast Utah.
Uranium was discovered in sandstone of the Chinle Formation in Lisbon Valley, San Juan County in 1913, and some carnotite was mined on a small scale for vanadium in 1917, 1940, and 1941. In the uranium mining boom of 1948, mining began in sandstone of the Permian Cutler Formation. Then in 1952, Charles Steen drilled into a rich 70-foot-thick (21 m) uraninite orebody in the Triassic Chinle Formation; that type of deposit became the largest producer in the district. Ore is distributed along 15 mi (24 km) of outcrop on the southwest side of the Lisbon valley anticline. The district produced 49 million pounds (22 kt) of U3O8 (uranium oxide) through 1965.
The Rio Algom Uranium Mill operated from 1972 to 1988.
On November 4, 2016, a historical marker commemorating the Lisbon Valley's uranium heritage and noting Charlie Steen's discovery was dedicated on the Anticline Overlook road off U.S. 191. The marker was funded entirely by private donations. Artist Michael Ford Dunton created an arch to frame the historical marker and the view to the location of the Mi Vida mine, seven miles (11 km) to the east of the marker.
Uranium associated with copper mineralization at the White Canyon district was identified in 1920, but production did not begin until 1946. The geology is similar to that of the Monument Valley uranium district 40 mi (64 km) to the south which straddles the Utah/Arizona state line (see Uranium mining in Arizona). Uranium occurs in the Shinarump Member of the Triassic Chinle Formation. Primary ore minerals are uraninite and coffinite. Through 1965, the White Canyon district produced 10 million pounds (4.5 kt) of U3O8.
In 2009 White Canyon Uranium opened the Daneros underground mine, 40 miles west of Blanding in the White Canyon District, trucking ore to Denison Mines's White Mesa Mill. Daneros was the first new uranium mine permitted in Utah since the 1980s. In 2011 Denison took over White Canyon Uranium. In 2012 Energy Fuels acquired the Daneros mine from Denison. Energy Fuels produced from the Daneros mine until October 2012, at which time the mine was placed on standby, care, and maintenance.
At the Marysvale district, in Piute and Sevier counties, uranium occurs in hydrothermal veins in igneous rocks (quartz monzonite, latite porphyry, and aplite). Primary uranium minerals are uraninite and umohoite, with associated gangue minerals pyrite, fluorite, quartz, and adularia.
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Uranium mining in Utah
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.
Mining of uranium-vanadium ore in southeast Utah goes back to the late 19th century, at the northern end of the Uravan mineral belt (see Uranium mining in Colorado), where it crosses into Grand County, Utah. Uranium occurs in the Salt Wash member of the Morrison Formation of Jurassic age. Because much of the value depended on the vanadium content, the only economic ore minerals were carnotite and tyuyamunite. Following World War II buying for nuclear weapons programs made uranium valuable for its own sake, and attracted hundreds of prospectors to southeast Utah.
Uranium was discovered in sandstone of the Chinle Formation in Lisbon Valley, San Juan County in 1913, and some carnotite was mined on a small scale for vanadium in 1917, 1940, and 1941. In the uranium mining boom of 1948, mining began in sandstone of the Permian Cutler Formation. Then in 1952, Charles Steen drilled into a rich 70-foot-thick (21 m) uraninite orebody in the Triassic Chinle Formation; that type of deposit became the largest producer in the district. Ore is distributed along 15 mi (24 km) of outcrop on the southwest side of the Lisbon valley anticline. The district produced 49 million pounds (22 kt) of U3O8 (uranium oxide) through 1965.
The Rio Algom Uranium Mill operated from 1972 to 1988.
On November 4, 2016, a historical marker commemorating the Lisbon Valley's uranium heritage and noting Charlie Steen's discovery was dedicated on the Anticline Overlook road off U.S. 191. The marker was funded entirely by private donations. Artist Michael Ford Dunton created an arch to frame the historical marker and the view to the location of the Mi Vida mine, seven miles (11 km) to the east of the marker.
Uranium associated with copper mineralization at the White Canyon district was identified in 1920, but production did not begin until 1946. The geology is similar to that of the Monument Valley uranium district 40 mi (64 km) to the south which straddles the Utah/Arizona state line (see Uranium mining in Arizona). Uranium occurs in the Shinarump Member of the Triassic Chinle Formation. Primary ore minerals are uraninite and coffinite. Through 1965, the White Canyon district produced 10 million pounds (4.5 kt) of U3O8.
In 2009 White Canyon Uranium opened the Daneros underground mine, 40 miles west of Blanding in the White Canyon District, trucking ore to Denison Mines's White Mesa Mill. Daneros was the first new uranium mine permitted in Utah since the 1980s. In 2011 Denison took over White Canyon Uranium. In 2012 Energy Fuels acquired the Daneros mine from Denison. Energy Fuels produced from the Daneros mine until October 2012, at which time the mine was placed on standby, care, and maintenance.
At the Marysvale district, in Piute and Sevier counties, uranium occurs in hydrothermal veins in igneous rocks (quartz monzonite, latite porphyry, and aplite). Primary uranium minerals are uraninite and umohoite, with associated gangue minerals pyrite, fluorite, quartz, and adularia.