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Image shows two men hiking through a dense forest
Pennington Mountain Critical Minerals
Pennington Mountain Critical Minerals
Pennington Mountain Critical Minerals

Geologists in the field at Pennington Mountain. The orange instrument is a portable gamma spectrometer. University of Maine-Presque Isle professor Chunzeng Wang (the lead author) is in front, Preston Bass is carrying the meter.

Geologists in the field at Pennington Mountain. The orange instrument is a portable gamma spectrometer. University of Maine-Presque Isle professor Chunzeng Wang (the lead author) is in front, Preston Bass is carrying the meter.

Image shows a helicopter towing a hoop with mountains in the background
Airborne Geophysical Survey Helicopter in Nevada
Airborne Geophysical Survey Helicopter in Nevada
Airborne Geophysical Survey Helicopter in Nevada

A low-flying helicopter towing a geophysical device collects scientific data on groundwater and geology. Information collected during these surveys can help with studying critical mineral resources, natural hazards and groundwater potential.

Image shows a cow standing in the foreground with a helicopter towing geophysical data collecting equipment with mountains
Airborne Geophysical Survey Helicopter with Cow
Airborne Geophysical Survey Helicopter with Cow
Airborne Geophysical Survey Helicopter with Cow

A helicopter rigged with an airborne geophysical survey collecting equipment. Information collected during these surveys can help with studying critical mineral resources, natural hazards and groundwater potential. A cow is here too.

A helicopter rigged with an airborne geophysical survey collecting equipment. Information collected during these surveys can help with studying critical mineral resources, natural hazards and groundwater potential. A cow is here too.

Three geologists looking at igneous textures in granitic rocks hosting gold
Three geologists looking at igneous textures in granitic rocks
Three geologists looking at igneous textures in granitic rocks
Three geologists looking at igneous textures in granitic rocks

Alaska Science Center geologist Doug Kreiner and University of Alaska, Fairbanks professor Sean Regan look at igneous textures in granitic rocks hosting gold at the Pogo gold mine with Pogo exploration geologists.

Alaska Science Center geologist Doug Kreiner and University of Alaska, Fairbanks professor Sean Regan look at igneous textures in granitic rocks hosting gold at the Pogo gold mine with Pogo exploration geologists.

Geologists discuss the district-scale geology during a field visit at Pogo Mine, Alaska
Geologists discuss the district-scale geology at Pogo Mine, Alaska
Geologists discuss the district-scale geology at Pogo Mine, Alaska
Geologists discuss the district-scale geology at Pogo Mine, Alaska

Alaska Science Center geologist Doug Kreiner and University of Alaska, Fairbanks professor Sean Regan discuss the district-scale geology with the chief exploration geologist at Pogo Mine. This is a new collaborative study with USGS, UAF and Pogo Mine, to collaborate on unraveling the genesis of Pogo, an important producer of gold in Alaska with critical mi

Alaska Science Center geologist Doug Kreiner and University of Alaska, Fairbanks professor Sean Regan discuss the district-scale geology with the chief exploration geologist at Pogo Mine. This is a new collaborative study with USGS, UAF and Pogo Mine, to collaborate on unraveling the genesis of Pogo, an important producer of gold in Alaska with critical mi

person standing near rock with normal fault
Normal Fault Exposure in Outcrop
Normal Fault Exposure in Outcrop
Normal Fault Exposure in Outcrop

Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.

Exposure of breccia marking trace of normal fault. Clasts of country rock include Eocene granite dike materials and thus provide an age for the fault as Eocene or younger.

Figure 1. Photographs of commercial, expanded vermiculite ore from the four major historical sources.
Photographs of commercial, expanded vermiculite ore.
Photographs of commercial, expanded vermiculite ore.
Photographs of commercial, expanded vermiculite ore.

Figure 1. Photographs of commercial, expanded vermiculite ore from the four major historical sources: Libby, Montana; Palabora, South Africa; Louisa, Virginia; and Enoree, South Carolina. Scale of the rightmost image in each set is the same as the left image unless otherwise labeled.

Figure 1. Photographs of commercial, expanded vermiculite ore from the four major historical sources: Libby, Montana; Palabora, South Africa; Louisa, Virginia; and Enoree, South Carolina. Scale of the rightmost image in each set is the same as the left image unless otherwise labeled.

monazite grains SEM photo
SEM Photo of Monazite Grains with REE
SEM Photo of Monazite Grains with REE
SEM Photo of Monazite Grains with REE

Monazite grains with rare earth elements lanthenum, cerium and neodinium are associated with zirconium, pyrite and potassium feldspar. Mineral identification performed by a combination of scanning of electron microscopy (SEM) and electron microprobe.

Monazite grains with rare earth elements lanthenum, cerium and neodinium are associated with zirconium, pyrite and potassium feldspar. Mineral identification performed by a combination of scanning of electron microscopy (SEM) and electron microprobe.

scientist walking through graben
Eureka Graben, Silverton caldera complex, CO
Eureka Graben, Silverton caldera complex, CO
Eureka Graben, Silverton caldera complex, CO

USGS scientist David Fey walking through the Eureka Graben in the Silverton caldera complex.

Red Mountain, Colorado
Red Mountain near Silverton, Colorado
Red Mountain near Silverton, Colorado
Red Mountain near Silverton, Colorado

Intensely altered propylitic rocks (red and yellow) in the Red Mountain mining district, overprinting the regional, propylitically altered igneous rocks (grayish-green), peaks at top of image. View to west.

Intensely altered propylitic rocks (red and yellow) in the Red Mountain mining district, overprinting the regional, propylitically altered igneous rocks (grayish-green), peaks at top of image. View to west.

eudialyte and bastnäsite samples
Eudialyte and Bastnäsite Samples
Eudialyte and Bastnäsite Samples
Eudialyte and Bastnäsite Samples

Sample of eudialyte (pink) within layered vein consisting of quartz, albite, and sodic amphibole, Dora Bay, Alaska. Size of sample is 11 by 9 cm. Sample of coarse-grained, tabular bastnäsite within matrix of ferruginous dolomite, Birthday Claim, Mountain Pass, California. Photographs by Philip Verplanck, U.S. Geological Survey. SIR 2010-5070-J

Sample of eudialyte (pink) within layered vein consisting of quartz, albite, and sodic amphibole, Dora Bay, Alaska. Size of sample is 11 by 9 cm. Sample of coarse-grained, tabular bastnäsite within matrix of ferruginous dolomite, Birthday Claim, Mountain Pass, California. Photographs by Philip Verplanck, U.S. Geological Survey. SIR 2010-5070-J

Image shows a dry creek bed with two men standing on the banks
USGS Scientists Seeking Finchite by the Sulfur Springs Draw in Texas
USGS Scientists Seeking Finchite by the Sulfur Springs Draw in Texas
USGS Scientists Seeking Finchite by the Sulfur Springs Draw in Texas

Between Lamesa and Big Spring, Texas, runs the Sulfur Spring Draw, a dry creek. It's the site of an economic calcrete-type uranium deposit, the Sulfur Springs Draw Deposit, where a new mineral was discovered in 2015.

Image shows a scanning electron microscope image of finchite
Scanning Electron Microscope Image of Finchite
Scanning Electron Microscope Image of Finchite
Scanning Electron Microscope Image of Finchite

A scanning electron microscope image of the newly discovered mineral finchite. The Denver Microbeam Lab provided this scan of finchite in order to help describe and identify the mineral as a new one. Finchite is a uranium mineral first observed in Martin County, Texas.

A scanning electron microscope image of the newly discovered mineral finchite. The Denver Microbeam Lab provided this scan of finchite in order to help describe and identify the mineral as a new one. Finchite is a uranium mineral first observed in Martin County, Texas.

Image shows a sample of the mineral finchite with a chair wheel for scale
Finchite Mineral
Finchite Mineral
Finchite Mineral

A sample of finchite, a newly discovered uranium mineral. Finchite is the yellow material on the surface of the rock. Finchite is found in the late Pleistocene sediments deposited during the Illinoian glacial stage.

A sample of finchite, a newly discovered uranium mineral. Finchite is the yellow material on the surface of the rock. Finchite is found in the late Pleistocene sediments deposited during the Illinoian glacial stage.

Image shows a rock outcropping surrounded by desert vegation
Calcrete near Sulfur Springs Draw
Calcrete near Sulfur Springs Draw
Image shows a detail of a yellow mineral on white rock
Uranium-Vanadate Mineral in Calcrete
Uranium-Vanadate Mineral in Calcrete
Uranium-Vanadate Mineral in Calcrete

A uranium-vanadate mineral in calcrete. This sample came from near the Sulfur Springs Draw in Texas. USGS conducted an assessment of uranium resources in this region in 2015.

microscopic gold and lead particles
Microscopic Gold and Lead Particles
Microscopic Gold and Lead Particles
Microscopic Gold and Lead Particles

Microscopic gold and lead particles surrounded by organic and phosphorus-rich material in a municipal biosolids sample (combined surface topography and atomic weight images).

Microscopic gold and lead particles surrounded by organic and phosphorus-rich material in a municipal biosolids sample (combined surface topography and atomic weight images).

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