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Image: Great Lakes Beach Monitoring
Great Lakes Beach Monitoring
Great Lakes Beach Monitoring
Great Lakes Beach Monitoring

To ensure that Great Lakes beaches are safe for public recreational use, USGS GLSC researchers have ongoing beach monitoring programs in place.

To ensure that Great Lakes beaches are safe for public recreational use, USGS GLSC researchers have ongoing beach monitoring programs in place.

Image: The James River
The James River
The James River
The James River

James River by Arrowwood National Wildlife Refuge. The picture was taken from the scenic view site to the North and above headquarters.

James River by Arrowwood National Wildlife Refuge. The picture was taken from the scenic view site to the North and above headquarters.

Image: Mud Lake Channel Arrowwood National Wildlife Refuge
Mud Lake Channel Arrowwood National Wildlife Refuge
Mud Lake Channel Arrowwood National Wildlife Refuge
Mud Lake Channel Arrowwood National Wildlife Refuge

Mud Lake Channel from Arrowwood Lake to Jim Lake, looking toward Arrowwood Lake. Photograph taken from 11th Street SE between Edmunds, North Dakota, and State Highway 9. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Mud Lake Channel from Arrowwood Lake to Jim Lake, looking toward Arrowwood Lake. Photograph taken from 11th Street SE between Edmunds, North Dakota, and State Highway 9. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Image: Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge

Jim Lake drawdown channel, looking south. Photograph from Humpback Road. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Jim Lake drawdown channel, looking south. Photograph from Humpback Road. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Image: Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge
Jim Lake Drawdown Channel Arrowwood National Wildlife Refuge

Jim Lake drawdown channel looking north. Photograph taken from 17th Street SE between Pingree, North Dakota, and State Highway 20. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Jim Lake drawdown channel looking north. Photograph taken from 17th Street SE between Pingree, North Dakota, and State Highway 20. The downstream Jamestown Reservoir was filled in 1965 and backed water onto the Arrowwood National Wildlife Refuge, preventing ideal management in most years.

Image: Columbia Glacier Terminus
Columbia Glacier Terminus
Columbia Glacier Terminus
Columbia Glacier Terminus

View of Columbia Glacier's terminus as it enters the waters of Prince William Sound. Columbia Glacier is one of Alaska's many tidewater glaciers, and it has been the focus of numerous studies due to its unusually high rate of retreat. The glacier has retreated nearly 20 km (12.43 mi) since 1980.

View of Columbia Glacier's terminus as it enters the waters of Prince William Sound. Columbia Glacier is one of Alaska's many tidewater glaciers, and it has been the focus of numerous studies due to its unusually high rate of retreat. The glacier has retreated nearly 20 km (12.43 mi) since 1980.

Image: Invertebrate Sampler on the Mississippi River
Invertebrate Sampler on the Mississippi River
Invertebrate Sampler on the Mississippi River
Invertebrate Sampler on the Mississippi River

Biological sampling devices are deployed on the upper Mississippi River to collect invertebrates for science. Each sampler is attached to a floating buoy and multiple samplers are placed together near a wing dam structure on the river to study the river's food web and productivity.

Biological sampling devices are deployed on the upper Mississippi River to collect invertebrates for science. Each sampler is attached to a floating buoy and multiple samplers are placed together near a wing dam structure on the river to study the river's food web and productivity.

Image: Creek Bank and Flood Plain
Creek Bank and Flood Plain
Creek Bank and Flood Plain
Creek Bank and Flood Plain

High bank and flood plain of Short Creek (a tributary of the Souris River in North Dakota) below International Boundary near Roche Percee, Saskatchewan, Canada.

High bank and flood plain of Short Creek (a tributary of the Souris River in North Dakota) below International Boundary near Roche Percee, Saskatchewan, Canada.

Image: Short Creek
Short Creek
Short Creek
Short Creek

Short Creek (a tributary of the Souris River in North Dakota) below International Boundary near Roche Percee, Saskatchewan, Canada.

Short Creek (a tributary of the Souris River in North Dakota) below International Boundary near Roche Percee, Saskatchewan, Canada.

Image: Sage-Grouse Population Model
Sage-Grouse Population Model
Sage-Grouse Population Model
Sage-Grouse Population Model

Changes to greater sage-grouse distribution in the American West predicted by a new scientific model based on extensive study of sage-grouse range contraction. "Likely secure populations" indicates areas where sage-grouse are present and currently stable. "Currently extirpated" indicates areas where sage-grouse are now locally extinct, as the model predicted.

Changes to greater sage-grouse distribution in the American West predicted by a new scientific model based on extensive study of sage-grouse range contraction. "Likely secure populations" indicates areas where sage-grouse are present and currently stable. "Currently extirpated" indicates areas where sage-grouse are now locally extinct, as the model predicted.

Image: Cratered Cones in the Isidis Region
Cratered Cones in the Isidis Region
Cratered Cones in the Isidis Region
Cratered Cones in the Isidis Region

Cratered Cones in the Isidis Region, Mars. These are almost certainly not cinder cones despite their appearance. Their alignment in rows is not typical of cinder cones on Earth; more likely these are mud volcanoes formed from the shaking of an impact event.

Cratered Cones in the Isidis Region, Mars. These are almost certainly not cinder cones despite their appearance. Their alignment in rows is not typical of cinder cones on Earth; more likely these are mud volcanoes formed from the shaking of an impact event.

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