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5 labeled water-quality sample bottles lined up and bagged, ready for transport to the lab.
Water-quality Samples
Water-quality Samples
Water-quality Samples

Water quality samples collected at USGS monitoring station 01628500 - S F Shenandoah River Near Lynnwood, VA.

USGS scientists using a vehicle-mounted reel to retrieve a bedload sampler which has been deployed in a river.
Bedload Sampling
Bedload Sampling
Bedload Sampling

USGS staff retrieving a bedload sampler from a riverbed.

What is bedload?

USGS staff retrieving a bedload sampler from a riverbed.

What is bedload?

USGS scientists lowering a bedload sampler over the edge of a bridge.
Bedload Sampling
Bedload Sampling
Bedload Sampling

USGS staff preparing to deploy a bedload sampler into the river below.

What is bedload?

USGS staff preparing to deploy a bedload sampler into the river below.

What is bedload?

A bedload sampler suspended from a vehicle-mounted reel about to be lowered into a river.
Deploying a Bedload Sampler
Deploying a Bedload Sampler
Deploying a Bedload Sampler

USGS staff preparing to deploy a bedload sampler.

What is bedload?

A bedload sampler suspended by a reel over a bridge above a river. The sampler's reel is mounted on a utility vehicle.
Bedload Sampler
Bedload Sampler
Bedload Sampler

USGS staff preparing to deploy a bedload sampler.

What is bedload?

USGS staff preparing to deploy a bedload sampler.

What is bedload?

Scientist wading in water next to the bank covered in leaves and a large fallen branch
USGS geologists document potential paleoliquefaction features from past seismicity at the southernmost edge of the Central Virginia Seismic Zone
USGS geologists document potential paleoliquefaction features from past seismicity at the southernmost edge of the Central Virginia Seismic Zone
USGS geologists document potential paleoliquefaction features from past seismicity at the southernmost edge of the Central Virginia Seismic Zone

USGS geologists document potential paleoliquefaction features from past seismicity at the southernmost edge of the Central Virginia Seismic Zone. Radiocarbon data suggest these features along Fountain Creek near Skippers, VA may be related to an earthquake that occurred near Petersburg, VA in the late 1700s.

Fountain Creek, Skippers, Virginia

An urban creek in autumn
Accotink Creek
Accotink Creek
Accotink Creek

Upper Accotink Creek is the longer of the of two streams that feed Lake Accotink. The USGS has been monitoring water quality in Accokink Creek since 2011, and has been monitoring water depth in the creek as far back as 1947.

Upper Accotink Creek is the longer of the of two streams that feed Lake Accotink. The USGS has been monitoring water quality in Accokink Creek since 2011, and has been monitoring water depth in the creek as far back as 1947.

A creek with high, eroded banks. Its surface is covered in autumn leaves.
Accotink Creek
Accotink Creek
Accotink Creek

Upper Accotink Creek is the longer of the of two streams that feed Lake Accotink. The USGS has been monitoring water quality in Accokink Creek since 2011, and has been monitoring water depth in the creek as far back as 1947.

Upper Accotink Creek is the longer of the of two streams that feed Lake Accotink. The USGS has been monitoring water quality in Accokink Creek since 2011, and has been monitoring water depth in the creek as far back as 1947.

A screenshot of red and grey dots of a map depicting where landslides have occurred in the southern Appalachian Mountains.
USGS landslide event team activated in wake of Hurricane Helene
USGS landslide event team activated in wake of Hurricane Helene
USGS landslide event team activated in wake of Hurricane Helene

The Landslide Observation Dashboard, a multi-agency effort to map where landslides have occurred in the southern Appalachian Mountains, launched September 30, 2024, as a “timely best science” provisional interface that can be used by the general public and local authorities as they prioritize resources. 

The Landslide Observation Dashboard, a multi-agency effort to map where landslides have occurred in the southern Appalachian Mountains, launched September 30, 2024, as a “timely best science” provisional interface that can be used by the general public and local authorities as they prioritize resources. 

An aerial photo of green mountains with a landslide cutting through the trees. A red plane wing can also be seen.
USGS landslide event team activated in wake of Hurricane Helene
USGS landslide event team activated in wake of Hurricane Helene
USGS landslide event team activated in wake of Hurricane Helene

U.S. Geological Survey landslide experts conduct an aerial reconnaissance flight October 3, 2024, over the southern Appalachian Mountains to get a better understanding of the extent and severity of landslide impacts in the wake of Hurricane Helene, which brought widespread flooding and destruction. (USGS photo by Ben Mirus). 

U.S. Geological Survey landslide experts conduct an aerial reconnaissance flight October 3, 2024, over the southern Appalachian Mountains to get a better understanding of the extent and severity of landslide impacts in the wake of Hurricane Helene, which brought widespread flooding and destruction. (USGS photo by Ben Mirus). 

View across the Lake Accotink dam
Lake Accotink Dam
Lake Accotink Dam
Lake Accotink Dam

The Lake Accotink dam. 

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

The Lake Accotink dam. 

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

Lake Accotink
Lake Accotink
Lake Accotink
Lake Accotink

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

The Lake Accotink Dam
Lake Accotink Dam
Lake Accotink Dam
Lake Accotink Dam

The Lake Accotink dam. 

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

The Lake Accotink dam. 

Lake Accotink is a 55-acre lake that is greatly valued to the local community. High sediment loads puts this lake at risk of becoming a wetland if not regularly dredged.

A USGS scientist in a river during a harmful algal bloom event.
HAB event in the South Fork Shenandoah River
HAB event in the South Fork Shenandoah River
HAB event in the South Fork Shenandoah River

The South Fork of the Shenandoah River during a harmful algal bloom (HAB) event. A USGS scientist wades into the river to collect readings. Mats of algae float at the surface while filamentous algae coats the riverbed.

The South Fork of the Shenandoah River during a harmful algal bloom (HAB) event. A USGS scientist wades into the river to collect readings. Mats of algae float at the surface while filamentous algae coats the riverbed.

Two researchers in life vests stand at a table full of water quality sampling equipment. They demonstrate its use.
Water Quality Sampling Equipment Show-and-Tell
Water Quality Sampling Equipment Show-and-Tell
Water Quality Sampling Equipment Show-and-Tell

USGS scientists Jimmy Webber and Dan Burns explain how water quality equipment is used to take measurements at War Branch and other monitoring stations.

USGS scientists Jimmy Webber and Dan Burns explain how water quality equipment is used to take measurements at War Branch and other monitoring stations.

Community members gather at an outreach table, reading USGS fact sheets
Outreach Event at War Branch
Outreach Event at War Branch
Outreach Event at War Branch

The USGS and local partners hosted a meeting at the War Branch monitoring station to share water-quality and conservation work happening in the watershed with farmers, environmental and agricultural agencies, nonprofit groups, and local universities.

The USGS and local partners hosted a meeting at the War Branch monitoring station to share water-quality and conservation work happening in the watershed with farmers, environmental and agricultural agencies, nonprofit groups, and local universities.

Two USGS scientists collecting a groundwater sample by the Shenandoah River.
Collecting groundwater samples near the Shenandoah River
Collecting groundwater samples near the Shenandoah River
Collecting groundwater samples near the Shenandoah River

Two USGS scientists collecting groundwater samples from a piezometer along the bank of the North Fork Shenandoah River near Strausburg

This photo was taken as a part of the Shenandoah River HABs Project.

Flooding in the Shenandoah River South Fork. Water is rough and turbid as it flows past a cliffside outcrop.
South Fork Shenandoah River after Hurricane Debby
South Fork Shenandoah River after Hurricane Debby
South Fork Shenandoah River after Hurricane Debby

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. 

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. 

Aerial photo of the south fork of the Shenandoah River after a storm. The water flows fast and is very turbid.
South Fork Shenandoah River after Hurricane Debby
South Fork Shenandoah River after Hurricane Debby
South Fork Shenandoah River after Hurricane Debby

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. 

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. 

Aerial photo of debris carried downstream by a turbid, flooded river until it becomes caught in the trees along the bank.
Storm Debris in the Shenandoah River South Fork after Hurricane Debby
Storm Debris in the Shenandoah River South Fork after Hurricane Debby
Storm Debris in the Shenandoah River South Fork after Hurricane Debby

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. Floods can also carry large amounts of debris, which collect in backwaters or get caught in trees along the riverbank.

The South Fork of the Shenandoah River near Rileyville shortly after Hurricane Debby. Storms often lead to flooding, high water levels, and increased water velocities that lead to increased sediment transport downstream. Floods can also carry large amounts of debris, which collect in backwaters or get caught in trees along the riverbank.

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