Connecticut Department of Energy & Environmental Protection

Emergency Burn Ban In Effect 10/26/24 - An emergency burn ban is now in effect for all Connecticut State Parks, Forests, and Wildlife Management areas, prohibiting the use of all outdoor grills, firepits, and campfires, and the kindling and use of flame outdoors. DEEP and local agencies are working to contain several active fires across the state. Please avoid all affected State Parks and Forests, as well as the blue-blazed Mattabesett Trail. The Enduro Trail in Voluntown and portions of North Stonington within the Pachaug State Forest are closed at this time. Please note that today's forest fire danger report remains at an 'extreme' level. More information about the current fire danger, burn ban and recommended safety measures can be found here

How are Inland Wetlands and Watercourses
Defined in Connecticut?

We usually identify wetlands and watercourses using the familiar terms marsh, swamp, river, brook, pond or lake. However, the CT Inland Wetlands and Watercourse Act (Act) defines inland wetlands by soil type. The soil types are poorly drained, very poorly drained, alluvial, and floodplain.

Identifying inland wetlands by soils allows us to recognize those areas during times of drought when there is no surface water present, or during winter when characteristic wetland indicator plants may not be obvious.

Inland wetlands may not always appear wet. For example, all floodplain soils are considered inland wetlands regardless of drainage class and some floodplain soils can be quite dry.

Areas disturbed by human activities and no longer in their natural state, may or may not be classified as wetlands due to their soil characteristics. The National Resources Conservation Service (NRCS) provides Clarification of Wetland Criteria as guidance for interpreting Connecticut's soil types. Consult with a natural resource professional with the proper expertise, such as a soil scientist, if this is an issue at your location of interest.

Wetland Soils

Wetland soils are defined in the Act by soil drainage class and landscape position:

Poorly drained

These soils occur where the water table is at or just below the ground surface, usually from late fall to early spring. The land where poorly drained soils occur is nearly level or gently sloping. Many of our red maple swamps are on these soils.

Very poorly drained

These soils generally occur on level land or in depressions. In these areas, the water table lies at or above the surface during most of the growing season. Most of our marshes and bogs are on these soils.

Alluvial and Floodplain

These soils occur along watercourses occupying nearly all level areas subject to periodic flooding. These soils are formed when material is deposited by flowing water. Such material can be composed of clay, silt, sand or gravel. Alluvial and floodplain soils range from excessively drained to very poorly drained.

Types of Watercourses

The Act also defines the term watercourses very broadly to mean rivers, streams, brooks, waterways, lakes, ponds, marshes, swamps, bogs and all other bodies of water, natural or artificial, vernal or intermittent, public or private. Although the Act defines inland wetlands and watercourses separately, they occasionally may represent the same area as in the case of a marsh or swamp. Types of watercourses include:

Marshes

Located in low lying areas having a high water table and characterized by the absence of trees and shrubs. The dominant vegetation in marshes is soft-stemmed plants such as cattail, bull rush and pickerelweed. However, some marshes can support woody vegetation.

Swamps

Located in low lying or gently sloping areas, but unlike marshes, are characterized by the presence of trees and shrubs. Soft-stemmed plants, such as tussock sedge, form the ground level vegetation.

Bogs

Unlike marshes and swamps, bogs are most often located in glacial kettle holes. Water pools in these depressions forming an acidic environment where many unique forms of vegetation grow. The most characteristic plant in a bog is Sphagnum moss. Sphagnum forms mats along the bog surface. New layers grow on top of the old, which subsequently become compacted with other plant debris to form peat. The depth of peat accumulation can exceed 40 feet.

Intermittent Watercourses

Recognized by a defined permanent channel and bank and the occurrence of two or more of the following characteristics:

  1. Evidence of scour or deposits of recent alluvium or detritus;
  2. The presence of standing or flowing water for a duration longer than a particular storm incident; and,
  3. The presence of hydrophytic vegetation.

Intermittent watercourses provide valuable fishery habitat during the spring months and during times of high flow and are an integral part of the natural storm water drainage system.

Other Waterbodies

Includes ephemeral waterbodies, such as vernal pools.

Inland vs. Tidal Wetlands

Unlike inland wetlands which are defined by soil type and typically regulated by the municipalities of CT, tidal wetlands are defined in the Tidal Wetlands Act by their current or former tidal connection, and their capacity to support certain wetland vegetation. Tidal wetlands are regulated exclusively by the CT DEEP and not by municipal inland wetlands agencies.

Federal vs. Connecticut's Wetlands Definitions

These separate and independent regulatory processes define wetlands differently:

For more information regarding tidal or inland wetlands contact the DEEP's Land and Water Resources Division at (860) 424-3019.

For information on federal wetlands contact the U.S. Army Corps of Engineers at (800) 343-4789.


Content last updated March 10, 2020.