Images

Wading measurements are taken for streamflow on the Gros Ventre River near Zenith, Wyoming while bridge construction is carried out upstream.

For the 10th anniversary of Kīlauea Volcano's summit eruption, USGS–Hawaiian Volcano Observatory research geologist Matt Patrick talks about his work monitoring the lava lake in the Halema'uma'u Crater. Dr.

Brett Tipple (University of California, Santa Cruz) collects a sample of charcoal and soil adjacent to a gully forming on a hillslope above Sonoma Creek, which was burned by the Nuns wildfire in October 2017.

John Pohlman (USGS), David Brankovits (USGS/WHOI) and Jake Emmert (MG) deploy acoustic devices in open water sinkhole (or cenote) prior to a 6-month long installation in the Yucatan Peninsula, Mexico cave

Measuring streamflow with ADCP on the South Fork of the Shoshone River near Valley, WYoming.

U.S. Geological Survey hydrologic technicians Kevin Kirlin (left) and Ryan Smith collect water-quality samples from the Coeur d'Alene River near Cataldo (USGS 12413500) as part of an ongoing monitoring program that the USGS conducts on behalf of the U.S. Environmental Protection Agency.

U.S. Geological Survey scientists, collecting oil from wells at the National Crude Oil Spill Fate and Natural Attenuation Research Site near Bemidji, Minnesota. 

Ice jam on the White River near White River, SD (USGS streamgage 06447450) on March 15, 2018. Ice jams occur when floating ice carried with a stream’s current accumulate at any obstruction to the stream flow. These ice jams can develop near river bends, mouths of tributaries, areas of decreased river slope, and upstream of obstructions like bridges.

Just before noon today, HVO's summit webcam (KIcam) captured this striking image of Kīlauea Volcano's ongoing summit eruption. A small rockfall on the north side of the Overlook crater triggered a small explosion in the lava lake, sending a dark-colored ash plume skyward.

USGS sign on flagstone at the Utah Water Science Center

Mother nature left us some cushions for a more comfortable cable car ride at Pine Creek above Fremont Lake.

Mokelumne River near confluence with the San Joaquin River in the Sacramento-San Joaquin Delta, CA, looking downstream, with Cordell Johnson (USGS PCMSC) and Rachel Allen (USGS PCMSC) collecting data from the R/V Fast Eddy.

Mokelumne River near confluence with the San Joaquin River in the Sacramento-San Joaquin Delta, CA, looking downstream, with Cordell Johnson (USGS PCMSC) and Rachel Allen (USGS PCMSC) collecting data from the R/V Fast Eddy.

Orthophoto of the mouth of the Elwha River in Washington. The orthophoto was compiled from images collected with a Ricoh GR camera operating at 2-second intervals and mounted on a Cessna 172 piloted by Rite Bros. Aviation.

Orthophoto (GigaPan) of the former Elwha Dam and former Lake Aldwell, on the Elwha River, Washington, compiled from ultra high-resolution images collected with a Ricoh GR camera operating at 2-second intervals, mounted on a Cessna 172 piloted by Rite Bros. Aviation and processed using Structure-from-Motion techniques.

Orthophoto (GigaPan) of the former Glines Canyon Dam and former Lake Mills, on the Elwha River, Washington, compiled from ultra high-resolution images collected with a Ricoh GR camera operating at 2-second intervals, mounted on a Cessna 172 piloted by Rite Bros. Aviation and processed using Structure-from-Motion techniques.

Greater White-fronted Goose marked with GSM/GPS collar is ready for release in the Sacramento Valley.

USGS Active Groundwater Level Network 3.12.18

Top left- Rob Thieler, Sandy Brosnahan and Alex Nichols deploying ground control targets for a UAS study on Coast Guard National Seashore in Eastham, MA.  

Hot springs can occur in many parts of the world. The water is hot not due to climate, but rather due to geothermal activity underground, such as volcanic activity or active hydrothermal heating from hot material in the ground. Hot springs result from water heated by underground geothermal activity finding its way to the land surface. 

On November 5, 1967, a line of vigorous lava fountains erupted on the floor of Halema‘uma‘u at the summit of Kīlauea. Lava soon covered the entire crater floor as volcanic gases billowed skyward (aerial view). Near the center, a pool of molten lava repeatedly overflowed a levee of crusted lava, spilling flows onto the lava-covered crater floor (inset).