Images

USGS Monitoring Station 016701405, alongside tributary and road side, Near Lake Anna, Virginia

Data for this monitoring station can be found at USGS Water Data for the Nation

A USGS hydrologist conducts horizontally-integrated synoptic water sampling of the James River at Cartersville as part of the USGS's nontidal network monitoring efforts.

A U.S. Geological Survey (USGS) hydrologic technician prepares a sonde for deployment for collecting continuous water-quality data.

Turbidity is a measure of water clarity. High amounts of suspended solids increase turbidity. The more turbid the water, the less light can penetrate. In turbid waters, aquatic plants may die due to decreased light availability.

Nutrient pollution is caused when excess nutrients in the form of nitrogen and phosphorus are introduced into aquatic ecosystems, often due to leaching or surface water runoff. These excess nutrients can contribute to the degradation of downstream ecosystems.

Brendan Foster, a USGS scientist, collects a water quality sample from a Lake Anna dock. 

USGS scientists are exploring factors driving Harmful Algal Blooms. Learn more here.

Lake Anna is a lake in Virginia impacted by Harmful Algal Blooms, or HABs. Note the greenish color of the water. This is caused by an excess of algae, some species of which could be toxic.

USGS Scientist Brendan Foster taking and sealing an algal sample on a dock at Lake Anna, Virginia.

Deer Rapids, North Fork Shenandoah River, Virginia.

Data for this monitoring site can be found at USGS Water Data for the Nation.

A cableway training session conducted during the Virginia and West Virginia Water Science Center's annual data summit in Lexington, Virginia. Photo is taken at a streamgage at Maury River near Buena Vista, Virginia.

Spring 2023 Photo Contest Winner: Carson Wright, People category

A stream's flashiness is determined by how quickly water levels peak after a rain event, and how quickly water levels fall after the peak. The figure above shows and urban canal (left) that is very flashy, compared to a less flashy natural stream (right).

Turbidity is a measure of water clarity. High amounts of suspended solids increase turbidity. The more turbid the water, the less light can penetrate. In turbid waters, aquatic plants may die due to decreased light availability.

When precipitation falls over urban watersheds, its fate may differ from precipitation that falls over undeveloped, rural or natural watersheds. Different urban land use types can affect strormwater runoff patterns in different ways. There are many potential non-point sources of nutrients, sediment, and other contaminants within urban watersheds.

Drilling a new borehole extensometer is a delicate task.

While drilling the 1420-foot-deep borehole for the West Point Extensometer, USGS geologists take the opportunity to learn all they can about the underlying geology. As they drill deeper, sediments are pumped out of the borehole. Geologists take samples of the sediments every 20 feet and note their composition.

In order to construct the borehole extensometer at West Point, 1420 feet of 7 inch steel casing was fed into the ground using the drilling rig, as pictured here. This steel casing allows the borehole to hold its shape and not collapse in on itself, and isolates the 2 inch thick extensometer rod from the surrounding sediments.

Nutrient pollution is caused when excess nutrients in the form of nitrogen and phosphorus are introduced into aquatic ecosystems, often due to leaching or surface water runoff. These excess nutrients can contribute to the degradation of downstream ecosystems.

When rainwater falls over a watershed, its fate is determined by multiple factors, such as the relief of the watershed, the permeability of the surface it falls on, the presence and density of plant life, and the drainage density of the watershed.

Photograph of the USGS precipitation gage located at Fairfax Middle School in Fairfax County. Data for this station can be found on USGS Water Data For the Nation.

Photograph of the USGS precipitation gage located at Churchill Road Park in Fairfax County. Data for this station can be found on USGS Water Data For the Nation.

A USGS crest stage gage used for measuring peak flow. Part of the Fairfax County Water Resources Monitoring Network.