Overlying Spor Mountain rhyolite caprock and underlying Beryllium Tuff member.
Images
Mineral Resources Program images.
Overlying Spor Mountain rhyolite caprock and underlying Beryllium Tuff member.
Map showing sediment-hosted copper and porphyry copper deposits across the world.
Map showing sediment-hosted copper and porphyry copper deposits across the world.
USGS scientist David Fey walking through the Eureka Graben in the Silverton caldera complex.
USGS scientist David Fey walking through the Eureka Graben in the Silverton caldera complex.
Layered deposit of unconsolidated heavy mineral sands along the shores of Folly Beach, South Carolina.
Layered deposit of unconsolidated heavy mineral sands along the shores of Folly Beach, South Carolina.
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.
Geologist doing field work in Alaska
Geologist doing field work in Alaska
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
Aerial view looking into the center of the dome-shaped pluton.
Aerial view looking into the center of the dome-shaped pluton.
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 CableA 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.
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 CableA 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.
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.
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.
Aerial view over Weka Dur, Afghanistan’s largest known gold deposit, Badakhshan Province.
Aerial view over Weka Dur, Afghanistan’s largest known gold deposit, Badakhshan Province.
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 CableHelicopter towing a large, wire-loop contraption hanging from a cable is turning in air on a relatively clear day in Nebraska.
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 CableHelicopter towing a large, wire-loop contraption hanging from a cable is turning in air on a relatively clear day in Nebraska.
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.
Searching for Sulfides at the Blackbird Cobalt-Copper Mine
Searching for Sulfides at the Blackbird Cobalt-Copper MineUSGS 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.
Searching for Sulfides at the Blackbird Cobalt-Copper Mine
Searching for Sulfides at the Blackbird Cobalt-Copper MineUSGS 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 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.
Banded Siltite at the Blackbird Cobalt-Copper Mine
Banded Siltite at the Blackbird Cobalt-Copper MineUSGS scientist Steve Box takes an oriented sample of folded, crenulated, and metamorphosed banded siltite, exposed in the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.
Banded Siltite at the Blackbird Cobalt-Copper Mine
Banded Siltite at the Blackbird Cobalt-Copper MineUSGS scientist Steve Box takes an oriented sample of folded, crenulated, and metamorphosed banded siltite, exposed in the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.
Transition Measurement at the Blackbird Cobalt-Copper Mine
Transition Measurement at the Blackbird Cobalt-Copper MineUSGS scientist Tom Frost measures the distance across the transition from garnet-bearing rocks, upslope from the end of the tape, to garnet-free rocks below it, as exposed on the northeast wall of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.
Transition Measurement at the Blackbird Cobalt-Copper Mine
Transition Measurement at the Blackbird Cobalt-Copper MineUSGS scientist Tom Frost measures the distance across the transition from garnet-bearing rocks, upslope from the end of the tape, to garnet-free rocks below it, as exposed on the northeast wall of the Blacktail pit of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.
USGS scientist Art Bookstrom looks at greenish copper stain and pale pink cobalt bloom on limonite-stained meta-siltite and meta-argillite at the No Name prospect, near Iron Creek, in the southeastern part of the Idaho cobalt belt, in east-central Idaho.
USGS scientist Art Bookstrom looks at greenish copper stain and pale pink cobalt bloom on limonite-stained meta-siltite and meta-argillite at the No Name prospect, near Iron Creek, in the southeastern part of the Idaho cobalt belt, in east-central Idaho.
Metasedimentary Rocks at the Apple Creek Formation
Metasedimentary Rocks at the Apple Creek FormationUSGS scientist Art Bookstrom looks at puzzling sedimentary structures in metasedimentary rocks of the Apple Creek Formation, near the Jackass prospect, near Iron Creek, in the southeastern part of the Idaho cobalt belt, in east-central Idaho.
Metasedimentary Rocks at the Apple Creek Formation
Metasedimentary Rocks at the Apple Creek FormationUSGS scientist Art Bookstrom looks at puzzling sedimentary structures in metasedimentary rocks of the Apple Creek Formation, near the Jackass prospect, near Iron Creek, in the southeastern part of the Idaho cobalt belt, in east-central Idaho.
USGS scientist Art Bookstrom hammers on limonite-stained breccia, cutting banded siltite of the Apple Creek Formation, exposed near the Uncle Sam portal of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.
USGS scientist Art Bookstrom hammers on limonite-stained breccia, cutting banded siltite of the Apple Creek Formation, exposed near the Uncle Sam portal of the Blackbird cobalt-copper mine, in the Salmon River Mountains of east-central Idaho.