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Images from the Geology, Energy and Minerals Mission Area

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Geologist stands in front of an entrance to an underground mine wearing an orange vest with pockets and rubber boots.
Evidence of previous exploration
Evidence of previous exploration
Evidence of previous exploration

A geologist, George Case, stands in front of an adit, an entrance to an underground mine, in the Graphite Creek Deposit on the Seward Peninsula, Alaska.

A geologist, George Case, stands in front of an adit, an entrance to an underground mine, in the Graphite Creek Deposit on the Seward Peninsula, Alaska.

Scenic view of the Seward Peninsula, Alaska. Photo taken from a ridge above Graphite Creek, looking out to body of water.
  A Seward Peninsula Vista
  A Seward Peninsula Vista
  A Seward Peninsula Vista

Scenic view of the Seward Peninsula, Alaska. Photo taken from a ridge above Graphite Creek, looking northwest towards the Imruk Basin. This area of the Seward Peninsula holds the largest graphite deposit in the US known as the Graphite Creek Deposit.

Scenic view of the Seward Peninsula, Alaska. Photo taken from a ridge above Graphite Creek, looking northwest towards the Imruk Basin. This area of the Seward Peninsula holds the largest graphite deposit in the US known as the Graphite Creek Deposit.

Arial view of   Graphite Creek Deposit. Looking down into valley with river below and mountains rising above.
Kigluaik Mountains Gneiss Dome
Kigluaik Mountains Gneiss Dome
Kigluaik Mountains Gneiss Dome

View of the Kigluaik Mountains gneiss dome which is the location of the Graphite Creek Deposit. The rocks of the gneiss dome were metamorphosed to as high as granulite facies during the middle Cretaceous (ca. 100 – 90 Ma), forming flake graphite ore in the process.

View of the Kigluaik Mountains gneiss dome which is the location of the Graphite Creek Deposit. The rocks of the gneiss dome were metamorphosed to as high as granulite facies during the middle Cretaceous (ca. 100 – 90 Ma), forming flake graphite ore in the process.

Click on image for full description.
Mineral Commodity Summary February 2021
Mineral Commodity Summary February 2021
Mineral Commodity Summary February 2021

The 26th annual Mineral Commodity Summaries report from the U.S. Geological Survey National Minerals Information Center is the earliest comprehensive source of 2020 mineral production data for the world.

The 26th annual Mineral Commodity Summaries report from the U.S. Geological Survey National Minerals Information Center is the earliest comprehensive source of 2020 mineral production data for the world.

A map of the world that shows which countries the United States relied on for mineral imports in 2020.
US Minerals Net Import Reliance in 2020
US Minerals Net Import Reliance in 2020
US Minerals Net Import Reliance in 2020

The United States continues to rely on foreign sources for some raw and processed mineral materials, including some critical minerals. This map shows the countries that supply mineral commodities for which the United States was more than 50% net import reliant in 2020. 

The United States continues to rely on foreign sources for some raw and processed mineral materials, including some critical minerals. This map shows the countries that supply mineral commodities for which the United States was more than 50% net import reliant in 2020. 

Image shows an aerial view of rolling hills and rock formations
Western North Slope Foothills
Western North Slope Foothills
Western North Slope Foothills

The Kukpowruk River cuts through folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

The Kukpowruk River cuts through folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

Image shows grass-covered rocks with rolling hills in the background
Tingmerkpuk Ridges
Tingmerkpuk Ridges
Tingmerkpuk Ridges

Jurassic rocks exposed in thurst-faulted structures near the southern limit of Western North Slope. In the subsurface farther north, these rocks may be reservoir rocks for natural gas.

Jurassic rocks exposed in thurst-faulted structures near the southern limit of Western North Slope. In the subsurface farther north, these rocks may be reservoir rocks for natural gas.

Image shows rocky ground with grasslands and a USGS scientist in the background
Western North Slope Foothills
Western North Slope Foothills
Western North Slope Foothills

Geologist hikes across folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

Geologist hikes across folded Cretaceous rocks in the central North Slope. These rocks were assessed by the USGS in 2017 and lie above the rocks assessed in the USGS 2021 Western North Slope assessment.

a tower in the middle of a bright orange sky with trees in the foreground
forest tower at the Alaska Peatland Experiment
forest tower at the Alaska Peatland Experiment
forest tower at the Alaska Peatland Experiment

A forest tower after a storm at the Alaska Peatland Experiment, a permafrost thaw research site. The tower helps researchers understand the ecosystem’s carbon balance.

A forest tower after a storm at the Alaska Peatland Experiment, a permafrost thaw research site. The tower helps researchers understand the ecosystem’s carbon balance.

Map
Flight area for Trans-Pecos aeromagnetic and radiometric survey
Flight area for Trans-Pecos aeromagnetic and radiometric survey
Flight area for Trans-Pecos aeromagnetic and radiometric survey

Map indicating flight area for Trans-Pecos aeromagnetic and radiometric survey. The survey area includes parts of El Paso and Hudspeth counties, Texas, and Otero County, New Mexico. Flights will begin in November 2020 and are expected to conclude in mid-January 2021. 

Map indicating flight area for Trans-Pecos aeromagnetic and radiometric survey. The survey area includes parts of El Paso and Hudspeth counties, Texas, and Otero County, New Mexico. Flights will begin in November 2020 and are expected to conclude in mid-January 2021. 

Image shows three men in safety equipment standing next to a drill rig
USGS Technicians Prepare to Take a Core of the Austin Chalk in Texas
USGS Technicians Prepare to Take a Core of the Austin Chalk in Texas
USGS Technicians Prepare to Take a Core of the Austin Chalk in Texas

USGS technicians at the USGS Gulf Coast #4 Bonham borehole in preparation for geophysical logging of the Austin Chalk Group and the Eagle Ford Group mudstones, Fannin County, Texas.

Image shows a rock core in a trough
Austin Chalk Core
Austin Chalk Core
Austin Chalk Core

Bedding features in the core from the USGS Gulf Coast #4 Bonham borehole, in the Eagle Ford Group mudstones from a depth of about 401 feet, Fannin County, Texas. The Eagle Ford Group lies underneath the Austin Chalk and serves as the source rock for much of the Austin Chalk's petroleum.

Bedding features in the core from the USGS Gulf Coast #4 Bonham borehole, in the Eagle Ford Group mudstones from a depth of about 401 feet, Fannin County, Texas. The Eagle Ford Group lies underneath the Austin Chalk and serves as the source rock for much of the Austin Chalk's petroleum.

Image shows a helicopter with four USGS scientists talking to each other next to it, with grasslands in the background
Tingmerkpuk Ridges
Tingmerkpuk Ridges
Tingmerkpuk Ridges

Geologists discuss the geology of Jurassic rocks in thurst-faulted structures near the southern limit of Western North Slope.

Geologists discuss the geology of Jurassic rocks in thurst-faulted structures near the southern limit of Western North Slope.

Image shows two pyramidal rock outcroppings with grass coverings
Kukpowruk Redwul
Kukpowruk Redwul
Kukpowruk Redwul

Geologist examines f Faulted and folded petroleum source rocks in Jurassic and Cretaceous rocks (Kingak Shale, pebble shale unit, and gamma-ray zone of Hue Shale) in southern part of Western North Slope. Thermal maturity of these rocks is at the upper limit of oil preservations.

Geologist examines f Faulted and folded petroleum source rocks in Jurassic and Cretaceous rocks (Kingak Shale, pebble shale unit, and gamma-ray zone of Hue Shale) in southern part of Western North Slope. Thermal maturity of these rocks is at the upper limit of oil preservations.

Image is an aerial shot showing grass-covered rolling hills with occasional exposed rock formations
Surprise Creek, Western North Slope of Alaska
Surprise Creek, Western North Slope of Alaska
Surprise Creek, Western North Slope of Alaska

Overview of folded Triassic, Jurassic, and Cretaceous rocks in southern part of Western North Slope.

Image shows a detail shot of a rock outcropping with grass covering in the background and two USGS scientists in hivis clothes
Kokolik River Oil Sand
Kokolik River Oil Sand
Kokolik River Oil Sand

Oil-saturated sandstone in the Nanushuk Formation in westernmost National Petroleum Reserve in Alaska (NPR-A). Oil in these rocks likely was generated beneath Western North Slope and migrated northeastward into NPR-A.

Oil-saturated sandstone in the Nanushuk Formation in westernmost National Petroleum Reserve in Alaska (NPR-A). Oil in these rocks likely was generated beneath Western North Slope and migrated northeastward into NPR-A.

Silica Crucible and Glass Desiccator
Silica Crucible and Glass Desiccator
Silica Crucible and Glass Desiccator
Silica Crucible and Glass Desiccator

Geochemists use platinum, silica, and ceramic crucibles, shown here in a glass container called a desiccator.  Silica is used because it is resistant to extremely high temperatures and because it is chemically inert. Silicon, linked up with a pair of oxygen molecules as silicon dioxide, is known as silica. 

Geochemists use platinum, silica, and ceramic crucibles, shown here in a glass container called a desiccator.  Silica is used because it is resistant to extremely high temperatures and because it is chemically inert. Silicon, linked up with a pair of oxygen molecules as silicon dioxide, is known as silica. 

Image shows a landscape of a large rock and sediment outcropping with grass coverings
Kukpowruk Redwul
Kukpowruk Redwul
Kukpowruk Redwul

Faulted and folded petroleum source rocks in Jurassic and Cretaceous rocks (Kingak Shale, pebble shale unit, and gamma-ray zone of Hue Shale) in southern part of Western North Slope. Thermal maturity of these rocks are at the upper limit of oil preservations.

Faulted and folded petroleum source rocks in Jurassic and Cretaceous rocks (Kingak Shale, pebble shale unit, and gamma-ray zone of Hue Shale) in southern part of Western North Slope. Thermal maturity of these rocks are at the upper limit of oil preservations.

Map of Earth MRI critical minerals projects in Texas
Earth MRI Funds Critical Minerals Projects in Texas
Earth MRI Funds Critical Minerals Projects in Texas
Click on image for full description.
GeoDAWN: Geoscience Data Acquisition for Western Nevada
GeoDAWN: Geoscience Data Acquisition for Western Nevada
GeoDAWN: Geoscience Data Acquisition for Western Nevada

The USGS Earth Mapping Resources Initiative and USGS 3D Elevation Program (3DEP), Department of Energy Geothermal Technologies Office, Natural Resources Conservation Services, and Bureau of Land Management have partnered to conduct airborne geophysical and 3DEP lidar surveys over parts of Nevada and California to collect information on undiscovered geothermal, criti

The USGS Earth Mapping Resources Initiative and USGS 3D Elevation Program (3DEP), Department of Energy Geothermal Technologies Office, Natural Resources Conservation Services, and Bureau of Land Management have partnered to conduct airborne geophysical and 3DEP lidar surveys over parts of Nevada and California to collect information on undiscovered geothermal, criti

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