Coastal Ocean Analytics

Living Shorelines in Connecticut

Why Living Shorelines
The Connecticut Coast
Marshes
Beaches and Dunes
Bluffs
Hardened Shorelines
Types of Living Shorelines
Design Considerations
Permitting
Resources
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The Connecticut Coast

The Connecticut shoreline of Long Island Sound is highly variable, consisting of three major geomorphological types: beaches and dune, bluffs and wetlands. The different shoreline types provide nesting and foraging habitat for a wide range of aquatic plants and animals. Maintaining the shoreline’s ability to absorb wave energy and reduce coastal flooding while preserving the ecosystem services provided by the natural shoreline is the goal of Living Shorelines. The most appropriate type of Living Shoreline for stabilization will depend on the natural geomorphological conditions.
eroding bluff
beach
marsh
To understand what option will best suit your site, select your shoreline type below:

Marshes

Greenwich marsh
Coastal marshes are low-lying areas of salt tolerant plants that are subjected to regular or occasional flooding by tides and storm surges. Marsh plants are highly dependent on salinity resulting in distinct zones of plant species based on elevation and the occurrence of salt water flooding surges.

Marshes  in Connecticut can be extensive meadows of salt tolerant plants, such as at Barn Island Wildlife Management Area or Hammonasset Beach State Park, usually dominated by high marsh, or fringe marshes, located along protected coastlines or at the toe of eroding bluffs. Fringe marshes may be bordered by mud flats.
Tidal salt marshes, whether natural or restored, can provide critical protection to coastal communities by reducing wave heights and therefore wave energy, storm surge levels and durations, and mitigating coastal erosion. In addition, marshes improve water quality by filtering groundwater, reduce surface water runoff, and decrease sediment transport. Waterford marsh
Want to learn more about marshes and stabilization options?

Beaches and Dunes

Connecticut beaches occupy about 14% of the Connecticut shoreline of Long Island Sound, consisting of:

sandy barrier beaches  backed by low dunes such as at Bluff Point State Park and Long Beach in Stratford, Hammonasset Beach
Rocky Neck Beach pocket beaches bounded by headlands,
and  cobbled beaches.

Branford Beach

Beaches and dunes are natural barriers to the destructive forces of waves and storm surge. By absorbing the impact of storm surge and waves, they prevent or delay erosion, flooding of inland areas and damage to coastal infrastructure. During storms, beaches and dunes provide sacrificial sediment which is transported offshore into a sand bar system to causing waves to break and reducing wave energy reaching the beach.

In addition to storm protection, beaches and dunes provide critical nesting and foraging habitat for shore birds and other aquatic species, and recreation opportunities for property owners and the public.

Want to learn more about beaches and dunes, and how to protect them from coastal erosion?

Rocky and Soft Bluffs

The Connecticut shoreline also consists of rocky and erodible bluffs. Rocky headlans are formed over time by wave action removing the more easily erodible mater. Soft bluffs, fored of loose stone, gravel, clay or sand, erode easily. Erosion of soft bluffs provides sediment to nearby beaches and dune systems.

Bluff at Bluff Point
Want to learn more about bluffs and how to protect them from coastal erosion?

 

 

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Jennifer O'Donnell, Ph.D.
Coastal Ocean Analystics, LLC
jodonnell@coastaloa.com
860.961.2467
www.CoastalOA.com