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Technical Aspects of Wetland Identification and Delineation

A creek flowing through an emergent wetland area
Environment, Great Lakes, and Energy

Technical Aspects of Wetland Identification and Delineation

The majority of the remaining wetlands in Michigan formed when the last glaciers retreated thousands of years ago. For a wetland to develop over time, the presence of water (the hydrology) is necessary as a saturated zone near the soil surface during a significant portion of the growing season. The timing, frequency, and amount of soil saturation each year influences the specific type of vegetation that can grow in an area and the type of chemical, biological, and physical processes that occur in the soil.

Michigan's Wetland Protection Statute and Rules (i.e., Part 303) require the use of the technical wetland delineation standards set forth in the United States Army Corps (USACE) of Engineers 1987 Wetland Delineation Manual (i.e., ’87 Manual), and especially the two modern, regional supplements, when identifying wetland boundaries. 

USACE wetland delineation manuals
Three examples of wetland plants
Profile of wetland soils

For highly disturbed sites, as described in the USACE Regional Supplements and other technical publications, the use of mapped hydric soil data from the NRCS and mapping data derived from modern remote sensing (e.g., aerial photography, LIDAR topographic data) can be extremely important when trying to ascertain where wetland boundaries were located on site prior to any major disturbance.

Resources

Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Northcentral and Northeast Region

Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Midwest Region

The National Wetland Plant List

Field Indicators of Hydric Soils in the United States

Are there wetlands on my site? [link to Wetland Identification and Mapping]

Finding a Wetland Consultant

State and Federal Wetland Regulations