CNN interviews USGS National Flood Coordinator Bob Holmes live from the Mississippi River in St. Louis.
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CNN interviews USGS National Flood Coordinator Bob Holmes live from the Mississippi River in St. Louis.
NBC Nightly News not only came out to interview USGS field crews on the Mississippi, they brought a team to fly overhead and capture video with a drone.
NBC Nightly News not only came out to interview USGS field crews on the Mississippi, they brought a team to fly overhead and capture video with a drone.
NBC Nightly News not only came out to interview USGS field crews on the Mississippi, they brought a team to fly overhead and capture video with a drone.
NBC Nightly News not only came out to interview USGS field crews on the Mississippi, they brought a team to fly overhead and capture video with a drone.
USGS scientists Paul Rydlund, Eric Looper and Jason Carron dock the boat and coordinate with emergency managers.
USGS scientists Paul Rydlund, Eric Looper and Jason Carron dock the boat and coordinate with emergency managers.
Here’s our river ray, peeking over the bridge at the water it’s going to measure soon. This is the Meramec River near Eureka, Missouri on December 30, 2015.
Here’s our river ray, peeking over the bridge at the water it’s going to measure soon. This is the Meramec River near Eureka, Missouri on December 30, 2015.
Here, you can see the effects of the Gasconade River’s flooding on a campground at Rich Fountain, Missouri. The floodwaters ate out the banks and scoured the surface, damaging concrete, steel, and asphalt. The water has since receded, but it will take some time to repair the damage and for the ecosystem to rebound.
Here, you can see the effects of the Gasconade River’s flooding on a campground at Rich Fountain, Missouri. The floodwaters ate out the banks and scoured the surface, damaging concrete, steel, and asphalt. The water has since receded, but it will take some time to repair the damage and for the ecosystem to rebound.
Here we are, taking the river ray out for a walk. Actually, our technician, Scott Southern, is taking the river ray over to where the Meramec River is overflowing the bridge to take a discharge measurement on December 30, 2015.
Here we are, taking the river ray out for a walk. Actually, our technician, Scott Southern, is taking the river ray over to where the Meramec River is overflowing the bridge to take a discharge measurement on December 30, 2015.
USGS Hydrologic Technician Christopher Rowden is seen here documenting a high water mark on Maries River at Westphalia, MO.
USGS Hydrologic Technician Christopher Rowden is seen here documenting a high water mark on Maries River at Westphalia, MO.
Non-native Cuban treefrogs have established a breeding population in New Orleans, Louisiana, the first such population on the U.S. mainland outside Florida. The treefrogs were discovered at the Audubon Zoo shortly after a shipment of palm trees from Florida were planted in the zoo's elephant enclosure in 2016.
Non-native Cuban treefrogs have established a breeding population in New Orleans, Louisiana, the first such population on the U.S. mainland outside Florida. The treefrogs were discovered at the Audubon Zoo shortly after a shipment of palm trees from Florida were planted in the zoo's elephant enclosure in 2016.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon's Wall of Windows.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon's Wall of Windows.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is also home to large numbers of cedar trees that spread throughout the canyon.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
Bryce Canyon is a unique sandstone formation in southern Utah. It is home to a large number of hoodoos, which are oddly shaped pillars of rock that formed due to different erosion rates for the dolomite that caps them and the sandstone that forms their base.
A U.S. Geological Survey hydrologist collects a water sample from the Williamson River below Chiloquin, Oregon. The sample was analyzed as part of a water-quality study the USGS conducted in cooperation with the U.S. Bureau of Reclamation and the Klamath Tribes.
A U.S. Geological Survey hydrologist collects a water sample from the Williamson River below Chiloquin, Oregon. The sample was analyzed as part of a water-quality study the USGS conducted in cooperation with the U.S. Bureau of Reclamation and the Klamath Tribes.
Scanning Electron Microscope image of volcanic ash
Scanning Electron Microscope image of volcanic ashScanning Electron Microscope image of resuspended volcanic ash from the 1912 Novarupta-Katmai deposits in the Katmai region, picked up during high winds on November 1, 2015 and carried to Larsen Bay on Kodiak Island, AK. Sample collected by Sherry Harmes of Larsen Bay.
Scanning Electron Microscope image of volcanic ash
Scanning Electron Microscope image of volcanic ashScanning Electron Microscope image of resuspended volcanic ash from the 1912 Novarupta-Katmai deposits in the Katmai region, picked up during high winds on November 1, 2015 and carried to Larsen Bay on Kodiak Island, AK. Sample collected by Sherry Harmes of Larsen Bay.