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Information Sheet - DEPEstablishing the Starting Point for Measurement of the Shoreland Zone and Related Setback DeterminationsIssued: October 2003 Contact: (207) 287- 3901
Great Ponds, Rivers and Streams1. Great Ponds, Rivers, and Streams, Without Adjacent Wetlands at the Elevation of the High Water Line – The starting point for the shoreland zone is determined by locating that line which is apparent from visible markings, changes in the character of soils due to prolonged action of the water or changes in vegetation, and which distinguishes between predominantly aquatic and predominantly terrestrial land. 2. Great Ponds With Adjacent Wetlands – If a great pond has an adjacent non-forested wetland (attached or connected) the starting point for the shoreland zone is the shoreward point in the non-forested wetland that is at the same elevation as the high-water line of the great pond. 3. Rivers with Adjacent Floodplain Wetlands – The shoreland zone begins at the upland edge of non-forested, 100-year, floodplain wetlands (these are considered to be a part of the river). 4. Streams – The shoreland zone of a stream begins at the point described in #1 above in all cases, regardless of whether or not there is a floodplain wetland. Freshwater WetlandsIn order for a freshwater wetland to have a shoreland zone it must: Be at least 10 acres in size and;
Measurement - The starting point for measuring the shoreland zone of a 10 acre or larger non-forested freshwater wetland that is mapped and identified in a municipal shoreland zoning ordinance is: 1. The upland edge of the wetland; or 2. The edge (transition zone) of where the wetland becomes a forested wetland. Overlapping Shoreland Zones – If a 10 acre or larger non-forested freshwater wetland that is identified in a municipal ordinance as having a shoreland zone is located close enough to a great pond, river or stream, its shoreland zone may overlap that of the great pond, river or stream. In that case, the shoreland zone extends from the edge of the great pond, river or stream to the edge of the wetland. The area of overlap would be subject to the more restrictive standards applicable to the two resources. Where there is no overlap, the standards for the relevant resource would apply. Coastal Wetlands1. Visible Inspection Method – This is a common method used to make a determination of the starting point for measuring the shoreland zone of a coastal wetland, but may be less precise than the elevation method. The Visible Inspection Method consists of looking for evidence of shoreline scouring, a tidal debris line and/or the presence of salt tolerant vegetation. When visible evidence is not satisfactory to establish a definitive edge, the elevation method can be used to determine the upland edge of the wetland. 2. Elevation Method – Where visible evidence is lacking or is unclear, the method for determining the starting point of the shoreland zone for coastal wetlands is the use of Maximum Spring Tide Levels as identified in the tide tables published by the National Ocean Service. This determination requires surveying utilizing appropriate adjustments for site specific elevations. The DEP publishes conversion tables for ease in determining these elevations. There are times when there is little visual evidence of the upland edge of the coastal wetland at a particular location, but at a nearby location a clear upland edge can be found. In those situations it is reasonable to transfer the elevation from the known site to the site that lacks visual evidence. Note also that where visual evidence, such as the presence of salt tolerant vegetation, extends further inland than the measured tidal elevation, the line formed by the more restrictive criterion must be used. Additional information can be obtained by contacting the Department’s Shoreland Zoning Unit at 287-3901 or by mail at: Information can also be found on the Department’s shoreland zoning web site at: | |||||||||||||||||||||||||||||
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