05/21/2026
🌊🌱Understanding how sediment moves through tidal marshes is essential for understanding how these landscapes change over time.
At Blackwater National Wildlife Refuge in Maryland, some marshes have been sinking relative to sea level for more than a century, while others have successfully maintained elevation. To better understand why, the USGS collected detailed measurements of suspended sediment in the tidal channels that feed these wetlands.
During two field campaigns in 2011, scientists deployed equipment at multiple sites to determine how much sediment was in the water, how it moved, and how these patterns differed between healthier and more vulnerable parts of the marsh. The resulting time‑series dataset includes water velocity, depth, turbidity, salinity, temperature, and pH.
This newly released dataset provides a valuable look at the processes that help—or hinder—marshes as they respond to sea‑level rise.
Researchers, coastal managers, and restoration planners can use these measurements to better understand sediment transport and support decisions that promote coastal resilience.
Learn more and download the data: https://ow.ly/G7Ek50YXT2S
📸: USGS scientists measuring sediment fluxes out of the Blackwater National Wildlife Refuge wetland complex.