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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 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 sample of finchite with a quarter 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 man examine rock layers
USGS Scientist Examining Texas Rock Layers for Finchite Minerals
USGS Scientist Examining Texas Rock Layers for Finchite Minerals
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.

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 rock outcropping surrounded by desert vegation
Calcrete near Sulfur Springs Draw
Calcrete near Sulfur Springs Draw
Calcrete near Sulfur Springs Draw

A calcrete outcropping near Sulfur Springs Draw in Texas. This deposit dates to the Pliocene and Pleistocene, and hosts uranium-vanadate minerals.

A calcrete outcropping near Sulfur Springs Draw in Texas. This deposit dates to the Pliocene and Pleistocene, and hosts uranium-vanadate minerals.

Image shows a landscape of the Southern High Plains
The Southern High Plains
The Southern High Plains
The Southern High Plains

The Southern High Plains of New Mexico, Oklahoma, and Texas. USGS conducted a uranium assessment in this region in 2015.

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.

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).

Image shows a landscape view of the Southern High Plains
The Southern High Plains
The Southern High Plains
The Southern High Plains

The Southern High Plains of New Mexico, Oklahoma, and Texas. USGS conducted a uranium assessment in this region in 2015.

Bluish-gray elongate amphibole bundles found in samples of commercial expanded vermiculite ore from Libby.
Bluish-gray elongate amphibole bundles found in samples.
Bluish-gray elongate amphibole bundles found in samples.
Bluish-gray elongate amphibole bundles found in samples.

Figure 2. Bluish-gray elongate amphibole bundles found in samples of commercial expanded vermiculite ore from Libby.

Figure 2. Bluish-gray elongate amphibole bundles found in samples of commercial expanded vermiculite ore from Libby.

 Figure 3.   Secondary electron images of elongate amphibole bundles from the sink fractions of commercial expanded vermiculite
Secondary electron images of elongate amphibole bundles.
Secondary electron images of elongate amphibole bundles.
Secondary electron images of elongate amphibole bundles.

Figure 3. Secondary electron images of elongate amphibole bundles from the sink fractions of commercial expanded vermiculite ore.

Figure 3. Secondary electron images of elongate amphibole bundles from the sink fractions of commercial expanded vermiculite ore.

Red Mountain CO
Red Mountain, CO Hydrothermal Alteration
Red Mountain, CO Hydrothermal Alteration
Red Mountain, CO Hydrothermal Alteration

Photo showing intense acid-sulfate hydrothermal alteration on Red Mountain No. 2, Silverton CO. View is looking to the west across Corkscrew Gulch. 

Photo showing intense acid-sulfate hydrothermal alteration on Red Mountain No. 2, Silverton CO. View is looking to the west across Corkscrew Gulch. 

Image: Supergene Leached Zone at Silver Bell Mine
Supergene Leached Zone at Silver Bell Mine
Supergene Leached Zone at Silver Bell Mine
Supergene Leached Zone at Silver Bell Mine

Supergene Leached zone at Silver Bell Mine, AZ.

asbestos standard
UICC Asbestos Amosite Standard
UICC Asbestos Amosite Standard
UICC Asbestos Amosite Standard

Union for International Cancer Control (UICC) asbestos amosite standard.

Union for International Cancer Control (UICC) asbestos amosite standard.

asbestos
Winchite-richterite asbestos
Winchite-richterite asbestos
diatom
Diatom in Yellowstone Lake Spire
Diatom in Yellowstone Lake Spire
Diatom in Yellowstone Lake Spire

Diatom in spire from floor of Yellowstone Lake, Yellowstone National Park.

lake spire material
Yellowstone Lake Spire
Yellowstone Lake Spire
Yellowstone Lake Spire

Spires from the floor of Yellowstone Lake appear to be composed of diatoms and silicified bacteria.

Spires from the floor of Yellowstone Lake appear to be composed of diatoms and silicified bacteria.

lake spire material
Yellowstone Lake Spire
Yellowstone Lake Spire
Yellowstone Lake Spire

Spires from the floor of Yellowstone Lake appear to be composed of diatoms and silicified bacteria.

Spires from the floor of Yellowstone Lake appear to be composed of diatoms and silicified bacteria.