USGS Denver Federal Center Building 25 Entrance
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USGS Denver Federal Center Building 25 Entrance
USGS researchers drill a research well located on the south side of U.S. 90, 7.1 miles east of Brackettville, Texas. This core was drilled by USGS during field work for an oil and gas assessment for the Eagle Ford of the Gulf Coast Basins. Cores like these provide information on the various rock layers, such as their make-up, their age, etc.
USGS researchers drill a research well located on the south side of U.S. 90, 7.1 miles east of Brackettville, Texas. This core was drilled by USGS during field work for an oil and gas assessment for the Eagle Ford of the Gulf Coast Basins. Cores like these provide information on the various rock layers, such as their make-up, their age, etc.
Gas hydrate from offshore Korea courtesy of the Korean Institute of Geoscience and Mineral Resources. Learn more about gas hydrates at https://woodshole.er.usgs.gov/project-pages/hydrates/
Gas hydrate from offshore Korea courtesy of the Korean Institute of Geoscience and Mineral Resources. Learn more about gas hydrates at https://woodshole.er.usgs.gov/project-pages/hydrates/
Seth Haines, USGS research geophysicist, on a Korean Institute of Geoscience and Mineral Resources laboratory tour, which included stops at their gas hydrate and sediment pressure chamber - it's a whopping 320 gallons, dwarfing even Seth, a 6-footer. The chamber is the silvery ring and the black cylinder beneath it. It's so big and heavy
Seth Haines, USGS research geophysicist, on a Korean Institute of Geoscience and Mineral Resources laboratory tour, which included stops at their gas hydrate and sediment pressure chamber - it's a whopping 320 gallons, dwarfing even Seth, a 6-footer. The chamber is the silvery ring and the black cylinder beneath it. It's so big and heavy
Core storage facility at the the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Core storage facility at the the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
USGS scientists, Bill Waite, Tim Collett, and Seth Haines in front of a archway in Daejeon, South Korea
USGS scientists, Bill Waite, Tim Collett, and Seth Haines in front of a archway in Daejeon, South Korea
Tim Collett, research geologist in gas hydrates, is chief for the U.S. Geological Survey (USGS) Energy Resources Program gas hydrate research efforts offering a presentation on unconventional oil and gas resources at KIGAM, the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Tim Collett, research geologist in gas hydrates, is chief for the U.S. Geological Survey (USGS) Energy Resources Program gas hydrate research efforts offering a presentation on unconventional oil and gas resources at KIGAM, the Korean Institute of Geoscience and Mineral Resources in Daejeon, South Korea
Tim Collett, USGS research geologist, presenting at the Korean Institute of Geoscience and Mineral Resources' (KIGAM) international program for geoscience resources.
Tim Collett, USGS research geologist, presenting at the Korean Institute of Geoscience and Mineral Resources' (KIGAM) international program for geoscience resources.
![Image shows squares of permafrost](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/NPRA_Permafrost_polygons.jpg?itok=2nRB7jkm)
Permafrost forms a grid-like pattern in the National Petroleum Reserve-Alaska, a 22.8 million acre region managed by the Bureau of Land Management on Alaska's North Slope. USGS has periodically assessed oil and gas resource potential there. These assessments can be found here.
Permafrost forms a grid-like pattern in the National Petroleum Reserve-Alaska, a 22.8 million acre region managed by the Bureau of Land Management on Alaska's North Slope. USGS has periodically assessed oil and gas resource potential there. These assessments can be found here.
Coal is loaded into trucks at the Trapper Mine in northwest Colorado.
Coal is loaded into trucks at the Trapper Mine in northwest Colorado.
Cannel coal is a type of bituminous coal, which is the second-highest rank of coal (just behind anthracite). This particular sample has a high carbon content with high pollen and spore content as well. Unlike most bituminous coal, Cannel coal can be carved into ornaments. This sample came from the Eastern Interior Coalfield in Kentucky.
Cannel coal is a type of bituminous coal, which is the second-highest rank of coal (just behind anthracite). This particular sample has a high carbon content with high pollen and spore content as well. Unlike most bituminous coal, Cannel coal can be carved into ornaments. This sample came from the Eastern Interior Coalfield in Kentucky.
USGS scientist Sarah Hawkins, lead scientist for the Mancos Shale assessment, examining a core drilled by the USGS Core Research Center. This core provided valuable data for the assessment. Image credit: Joshua Hicks, USGS.
USGS scientist Sarah Hawkins, lead scientist for the Mancos Shale assessment, examining a core drilled by the USGS Core Research Center. This core provided valuable data for the assessment. Image credit: Joshua Hicks, USGS.
The USGS Core Research Center collaborated with the USGS Energy Resources Program to drill a core from the Mancos Shale to aid in the oil and gas assessment. Image Credit: Joshua Hicks, USGS.
The USGS Core Research Center collaborated with the USGS Energy Resources Program to drill a core from the Mancos Shale to aid in the oil and gas assessment. Image Credit: Joshua Hicks, USGS.
Coal project personnel visiting Trapper Mine in northwest Colorado in June, 2016.
Coal project personnel visiting Trapper Mine in northwest Colorado in June, 2016.
from usgs files
from usgs files
![Image shows two scientists in hard hats collecting a research core aboard a drill rig](https://d9-wret.s3.us-west-2.amazonaws.com/assets/palladium/production/s3fs-public/styles/masonry/public/thumbnails/image/PCTB%20Recovery.jpg?itok=FJlF_iLH)
Scientists aboard the D/S Chikyu prepare to collect a research core drilled from marine sediments in the Indian Ocean. This research is part of the 2015 Indian National Gas Hydrate Program Expedition 02 (NGHP-02), which is a follow-up to the 2006 NGHP-01.
Scientists aboard the D/S Chikyu prepare to collect a research core drilled from marine sediments in the Indian Ocean. This research is part of the 2015 Indian National Gas Hydrate Program Expedition 02 (NGHP-02), which is a follow-up to the 2006 NGHP-01.
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.
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.
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.
USGS scientist Bradley Van Gosen examines rock layers for the newly discovered mineral finchite near Lamesa, Texas.
USGS scientist Bradley Van Gosen examines rock layers for the newly discovered mineral finchite near Lamesa, 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.