Document Type



The ability of coastal wetlands to migrate inland is a primary determinant of global salt marsh area in the face of sea level rise. Large scale levee systems designed to protect urban coasts from flooding are known to impede salt marsh migration in many regions of the world, but little is known about the extent and effectiveness of small, privately owned levee systems along rural coasts. Here, we explore small-scale earthen levees in the Chesapeake region of Virginia, which have been constructed for centuries by individual landowners and can reach up to a meter in height. LIDAR elevation datasets and aerial imagery were used to identify these levees, and 40 km of levees with at least 5 km2 of potentially protected land were mapped in Gloucester County. Impacts on marsh migration were evaluated on five levees at four distinct sites, in which I measured elevation, soil salinity, vegetation type and organic matter accumulation on transects spanning the landward and seaward sides of each levee. On the landward sides of the levees, vegetation was generally less flood tolerant and depths of organic matter depths were generally shallower. Three of the five levees have lower elevations on the landward sides, which was unexpected. Results suggest that, in some cases, levees may actually enhance marsh migration by increasing subsidence and inhibiting tidal sediment deposition on the landward side of the levee. These effects lead to relatively low elevations which may encourage inland ponding and marsh development. Results are variable and site dependent; while levees seem to have historically inhibitory effects on marsh migration, as has been observed in larger levee systems on developed coasts, some privately owned levees on rural coasts may encourage inland marsh migration today.

Date Awarded

Spring 2021



Advisor 1

Matthew Kirwan