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Mineral Resources Program images.

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Image shows a rotating sample of bastnaesite on a white background
Bastnaesite Sample
Bastnaesite Sample
Bastnaesite Sample

A sample of bastnaesite, one of the principal mineral sources of rare-earth elements. Rare-earth elements are essential components in most modern electronics.

A sample of bastnaesite, one of the principal mineral sources of rare-earth elements. Rare-earth elements are essential components in most modern electronics.

beryllium tuff
Beryllium Tuff, Spor Mountain
Beryllium Tuff, Spor Mountain
Beryllium Tuff, Spor Mountain

Closeup of the Beryllium Tuff member, Spor Mountain, Utah.

scientists collecting samples
Sampling at Spor Mountain
Sampling at Spor Mountain
Sampling at Spor Mountain

USGS scientists Brian Jaskula and Robert Ayuso collecting samples at Spor Mountain, Utah.

USGS scientists Brian Jaskula and Robert Ayuso collecting samples at Spor Mountain, Utah.

mine pit
Spor Mountain Open Pit
Spor Mountain Open Pit
Spor Mountain Open Pit

Spor Mountain open pit; mineralized tuff in foreground; mine staff and USGS scientists collecting samples.

Spor Mountain open pit; mineralized tuff in foreground; mine staff and USGS scientists collecting samples.

core mineral photomicrograph
Local Boy Drill Core - 10089 (microscope image)
Local Boy Drill Core - 10089 (microscope image)
Local Boy Drill Core - 10089 (microscope image)

Cross-polarized light photomicrograph of minerals in drill core samples from the Local Boy deposit, Duluth Complex, Minnesota. The number in the upper right hand corner is the drill core number.

Cross-polarized light photomicrograph of minerals in drill core samples from the Local Boy deposit, Duluth Complex, Minnesota. The number in the upper right hand corner is the drill core number.

core mineral photomicrograph
Mesaba Deposit Drill Core (microscope image)
Mesaba Deposit Drill Core (microscope image)
Mesaba Deposit Drill Core (microscope image)

Cross-polarized light photomicrograph of minerals in drill core samples from the Mesaba copper-nickel deposit, Duluth Complex, Minnesota. The number in the upper right hand corner is the drill core number.

Cross-polarized light photomicrograph of minerals in drill core samples from the Mesaba copper-nickel deposit, Duluth Complex, Minnesota. The number in the upper right hand corner is the drill core number.

Map showing locations of Copper ores in the World
Global Copper Map_0_0.jpg
Global Copper Map_0_0.jpg
Global Copper Map_0_0.jpg

Map showing sediment-hosted copper and porphyry copper deposits across the world.

Map showing sediment-hosted copper and porphyry copper deposits across the world.

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: Ahankashan Copper Gold
Ahankashan Copper Gold
Ahankashan Copper Gold
Ahankashan Copper Gold

Aerial view looking into the center of the dome-shaped pluton.

Image: Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging from a Cable
Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging from a Cable
Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging from a Cable
Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging from a Cable

A low-level helicopter towing a large wire-loop contraption hanging from a cable is flying straight across an open field in Nebraska on a clear day.

Image: Aerial Over Weka Dur Gold Deposit, Badakhshan
Aerial Over Weka Dur Gold Deposit, Badakhshan
Aerial Over Weka Dur Gold Deposit, Badakhshan
Aerial Over Weka Dur Gold Deposit, Badakhshan

Aerial view over Weka Dur, Afghanistan’s largest known gold deposit, Badakhshan Province.

Image: Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging From a Cable
Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging From a Cable
Low-level Helicopter Towing a Large Wire-Loop Contraption Hanging From a Cable
Image: Ahankashan Copper Gold
Ahankashan Copper Gold
Ahankashan Copper Gold
Ahankashan Copper Gold

Light-colored rocks in the foreground overlay a pluton, formed as a plume of magma rose, cooled and deposited minerals in the earth’s crust. Sedimentary rocks dip away from the intrusion.

 

Light-colored rocks in the foreground overlay a pluton, formed as a plume of magma rose, cooled and deposited minerals in the earth’s crust. Sedimentary rocks dip away from the intrusion.

 

Image: Redbeds Near Herat
Redbeds Near Herat
Redbeds Near Herat
Redbeds Near Herat

Aerial view near Herat. Dark red iron stains hint that other minerals might be found.

Aerial view near Herat. Dark red iron stains hint that other minerals might be found.

Image: Northeast Rim of the Blackbird Cobalt-Copper Mine
Northeast Rim of the Blackbird Cobalt-Copper Mine
Northeast Rim of the Blackbird Cobalt-Copper Mine
Northeast Rim of the Blackbird Cobalt-Copper Mine

USGS scientist Tom Frost stands on the northeast rim of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.

USGS scientist Tom Frost stands on the northeast rim of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.

Image: Searching for Sulfides at the Blackbird Cobalt-Copper Mine
Searching for Sulfides at the Blackbird Cobalt-Copper Mine
Searching for Sulfides at the Blackbird Cobalt-Copper Mine
Searching for Sulfides at the Blackbird Cobalt-Copper Mine

USGS scientist Art Bookstrom uses a hand-lens to search for sulfide minerals in oxidized copper-cobalt-bearing siltite of the banded siltite unit of the Apple Creek Formation, exposed in the Blacktail pit of the Blackbird cobalt-copper mine, Salmon River Mountains, east-central Idaho.

USGS scientist Art Bookstrom uses a hand-lens to search for sulfide minerals in oxidized copper-cobalt-bearing siltite of the banded siltite unit of the Apple Creek Formation, exposed in the Blacktail pit of the Blackbird cobalt-copper mine, Salmon River Mountains, east-central Idaho.

Image: A Gossan at the Blackbird Cobalt-Copper Mine
A Gossan at the Blackbird Cobalt-Copper Mine
A Gossan at the Blackbird Cobalt-Copper Mine
A Gossan at the Blackbird Cobalt-Copper Mine

USGS scientist Art Bookstrom maps and samples a gossan, developed on tightly folded, mineralized, metamorphosed, and weathered banded siltite, exposed on the southwest rim of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho. The gossan is overlain by unconsolidated colluvial debris.

USGS scientist Art Bookstrom maps and samples a gossan, developed on tightly folded, mineralized, metamorphosed, and weathered banded siltite, exposed on the southwest rim of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho. The gossan is overlain by unconsolidated colluvial debris.

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