Using a portable flume to measure streamflow on a small stream
Using a portable flume to measure streamflow on a small streamUsing a portable flume to measure streamflow on a small stream
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Images described and linked on this webpage come from a wide variety of USGS science activities and presentations performed by USGS Science Center staff members in the Region 7: Upper Colorado Basin. A search tool is provided to narrow the number of image files shown.
Using a portable flume to measure streamflow on a small stream
Using a portable flume to measure streamflow on a small stream
Preparing to measure water level at Groundwater Streamgage
Preparing to measure water level at Groundwater Streamgage
For the first time since it was opened in 1984, water has stopped flowing through the Great Salt Lake causeway breach, an area that allows water to travel between the southern and northern parts of the lake.
For the first time since it was opened in 1984, water has stopped flowing through the Great Salt Lake causeway breach, an area that allows water to travel between the southern and northern parts of the lake.
A gage to measure lake water levels stands dry in the lake bed of the Great Salt Lake. For the first time since it was opened in 1984, water has stopped flowing through the Great Salt Lake causeway breach, an area that allows water to travel between the southern and northern parts of the lake.
A gage to measure lake water levels stands dry in the lake bed of the Great Salt Lake. For the first time since it was opened in 1984, water has stopped flowing through the Great Salt Lake causeway breach, an area that allows water to travel between the southern and northern parts of the lake.
Measuring streamflow of the Green River near LaBarge
Measuring streamflow of the Green River near LaBarge
Hydrologic technician wades stream to collect a water-quality sample on Muddy Creek near Tomsich Butte, eastern Utah.
Hydrologic technician wades stream to collect a water-quality sample on Muddy Creek near Tomsich Butte, eastern Utah.
Measuring streamflow of New Fork River
Aerial photograph of South Cascade Glacier, WA taken October 14th, 2015.
Aerial photograph of South Cascade Glacier, WA taken October 14th, 2015.
USGS scientist makes ADCP measurement from canoe where the Bear River enters Great Salt Lake
USGS scientist makes ADCP measurement from canoe where the Bear River enters Great Salt Lake
USGS hydrologic technician makes an ADCP measurement by walking across streambed on the Bear River below Alexander Reservoir, Idaho.
USGS hydrologic technician makes an ADCP measurement by walking across streambed on the Bear River below Alexander Reservoir, Idaho.
USGS hydrologist walks across Great Salt Lake beach to reach receding shoreline.
USGS hydrologist walks across Great Salt Lake beach to reach receding shoreline.
Great Salt Lake, declining water level
Great Salt Lake, declining water level
Stilling well on Lake Fork above Moon Lake that is used to measure stream stage, and ultimately amount of water entering Moon Lake, on the south slope of the Uintas.
Stilling well on Lake Fork above Moon Lake that is used to measure stream stage, and ultimately amount of water entering Moon Lake, on the south slope of the Uintas.
Measuring discharge at 06324970
Animas River downstream from Silverton, Colorado, showing right and left bank areas where streambed sediment sample was collected near USGS stream gage at site A72 (USGS site ID 09359020). Latitude 37.789964, Longitude -107.667394.
Animas River downstream from Silverton, Colorado, showing right and left bank areas where streambed sediment sample was collected near USGS stream gage at site A72 (USGS site ID 09359020). Latitude 37.789964, Longitude -107.667394.
Determining aboveground biomass of sagebrush, grasses, and forbs is important for estimating fuel loads, measuring carbon storage, and assessing habitat quality in shrublands. Remote sensing may offer a more efficient alternative to common, labor intensive methods of measuring aboveground biomass that are difficult to apply across large areas.
Determining aboveground biomass of sagebrush, grasses, and forbs is important for estimating fuel loads, measuring carbon storage, and assessing habitat quality in shrublands. Remote sensing may offer a more efficient alternative to common, labor intensive methods of measuring aboveground biomass that are difficult to apply across large areas.
Core from 2" well drilled into Wasatch Formation, Big Piney, WY
Core from 2" well drilled into Wasatch Formation, Big Piney, WY
Measuring pH at the outlet of the fourth settling pond downstream from the North Fork Cement Creek. Latitude 37.894451, Longitude -107.64763.
Measuring pH at the outlet of the fourth settling pond downstream from the North Fork Cement Creek. Latitude 37.894451, Longitude -107.64763.
USGS stream Gage (USGS site ID 09358000) on Animas River upstream from Silverton and Cement Creek. Latitude 37.811131, Longitude -107.659213.
USGS stream Gage (USGS site ID 09358000) on Animas River upstream from Silverton and Cement Creek. Latitude 37.811131, Longitude -107.659213.
Animas River downstream from Silverton, Colorado showing cableway for USGS stream gage at site A72 (USGS site ID 09359020). Latitude 37.789964, Longitude -107.667394.
Animas River downstream from Silverton, Colorado showing cableway for USGS stream gage at site A72 (USGS site ID 09359020). Latitude 37.789964, Longitude -107.667394.
North Fork Cement Creek showing visual results of sodium hydroxide (NaOH) addition which increases the pH causing precipitation of ferric (orange) and ferrous (green) iron hydroxides. Latitude 37.89517, Longitude -107.64656.
North Fork Cement Creek showing visual results of sodium hydroxide (NaOH) addition which increases the pH causing precipitation of ferric (orange) and ferrous (green) iron hydroxides. Latitude 37.89517, Longitude -107.64656.